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Journal of Medicine and Pharmacy","Tạp chí Y Dược học Cần Thơ",{"EN":487,"VI":488},"\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">04\u002F10\u002F2015 Ministry of Information and Communications allowed Can Tho journal of medicine and pharmacy to operate (102 \u002FGP-BTTTT)\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">07\u002F16\u002F2015 Can Tho journal of medicine and pharmacy is internationally recognized: ISSN 2354-1210\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">In 2016, The journal has been included in the list of medical science journals by The State Council for professorship which is awarded a work score of 0-0.5 points for a published article.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Can Tho Journal of Medicine and Pharmacy welcome original works that haven’t been submitted or published in other medical journals. Posts must contain content related to one of the journal’s categories.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">The content published\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">The journal is divided into 3 categories:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Scientific research article: are valuable scientific works, which have been researched and accepted.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Overview of medicine, biology and pharmacy: serving the objective of continuing training in the fields of medicine, biology and pharmacy; to systematize classical and modern knowledge.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Update information on new knowledge about medicine, biology, pharmacy in the country and in the world.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Scope\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Publication and introduction of scientific research in the fields:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">+ Medicine (internal medicine, surgery, pediatrics, obstetrics and gynecology, odonto-stomatology, laboratory, oncology, traditional medicine, nursing).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">+ Biology (genetics, biotechnology).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">+ Pharmacology (pharmaceutics, drug quality analysis-control, synthetic pharmaceutical chemistry, biochemistry, pharmacognosy, botany, clinical pharmacy).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- To enhance the quality of undergraduate, postgraduate education, scientifically researching and meet the necessary treatment in hospital.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Introducing the updated domestic and oversea information about science technology to promote scientific research and exchanging technology in local, other universities.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">- Exchanging pharmaceutical and medical information for social health developing in the Mekong Delta and Vietnam.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">The object\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Postgraduate students, student of Can Tho University of Medicine and Pharmacy, scientists from schools, research institutes, hospitals, health centers, pharmaceutical companies of the Mekong Delta; other provinces and regions in Vietnam and other country.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Address\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Headquarters of Can Tho Journal of Medicine and Pharmacy, located Scientific Research and International Cooperation Office: 179 Nguyen Van Cu Street, An Khanh Ward, Ninh Kieu District, Can Tho City, Vietnam.\u003C\u002Fspan>\u003C\u002Fp>","\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Ngày 16\u002F7\u002F2015, Tạp chí Y Dược học Cần Thơ được cấp chỉ số quốc tế: ISSN 2354-1210.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Từ tháng 4\u002F2016, Tạp chí đã được Hội đồng Giáo sư ngành Y đưa vào danh sách các tạp chí khoa học Y học được tính điểm công trình 0-0,5 điểm cho một bài báo đăng.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Năm 2020 Tạp chí Y Dược học Cần Thơ đã được phê duyệt vào danh mục của các Hội đồng Giáo sư ngành Dược học được tính điểm công trình 0-0,5 điểm cho một bài báo đăng.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ ra 12 số\u002Fnăm, 180-200 trang\u002Fsố.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Từ tháng 12\u002F2022 Tạp chí Y Dược học Cần Thơ là thành viên của hệ thống Crossref và từ tháng 01\u002F2023 tạp chí thực hiện bình duyệt online kín 2 chiều nhằm tăng tính minh bạch, tin cậy của các công trình nghiên cứu khoa học và đảm bảo tốt nhất chất lượng khoa học của bài viết.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tôn chỉ, mục đích và phạm vi của tạp chí\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tôn chỉ và mục đích hoạt động của tạp chí: xuất bản nhằm mục đích phổ biến kết quả từ các đề tài nghiên cứu khoa học; giao lưu trao đổi khoa học, chia sẻ kinh nghiệm, học tập, đồng thời cập nhật thông tin khoa học mới trong các lĩnh vực y, sinh, dược học trong và ngoài nước.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Phạm vi của tạp chí: Tạp chí xuất bản được chia thành 3 chuyên mục: (i) Bài báo nghiên cứu khoa học là kết quả công trình nghiên cứu khoa học có giá trị đã được triển khai nghiên cứu, (ii) Bài tổng quan y, sinh, dược học: phục vụ mục tiêu đào tạo liên tục trong lĩnh vực y, sinh, dược học; nhằm hệ thống hóa những kiến thức kinh điển và hiện đại; (iii) Thông tin cập nhật kiến thức mới về y, sinh, dược học trong nước và trên thế giới.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Chính sách truy cập mở\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ áp dụng chính sách truy cập mở đối với các bài báo đã xuất bản đến với độc giả, nhằm mở rộng cơ hội tiếp cận các kết quả nghiên cứu chất lượng cao và tăng cường trao đổi kiến thức. Tạp chí đăng tải trực tuyến (miễn phí) toàn văn các bài báo được công bố trên website của Tạp chí (https:\u002F\u002Ftapchi.ctump.edu.vn).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Đạo đức xuất bản\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ cam kết tuân thủ đạo đức xuất bản phù hợp với các hướng dẫn và tiêu chuẩn của the Committee on Publication Ethics (COPE), tuân thủ các nguyên tắc của COPE’s Core Practices, Best Practices Guidelines for Journal Editors và Guidelines on Good Publication Practices.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Bản thảo bài báo chỉ được chấp nhận khi được tác giả chịu trách nhiệm chính cam kết các nội dung sau: Các nội dung của bản thảo chưa được đăng tải toàn bộ hoặc một phần ở các tạp chí khác; Tất cả các tác giả đều có đóng góp một cách đáng kể vào quá trình nghiên cứu hoặc chuẩn bị bản thảo và cùng chịu trách nhiệm về các nội dung của bản thảo; Tuân thủ các biện pháp đảm bảo đạo đức nghiên cứu (ví dụ thỏa thuận đồng ý tham gia nghiên cứu).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Cam kết bảo mật\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí cam kết thực hiện và tuân thủ các quy định của luật và các văn bản hướng dẫn liên quan đến bảo mật thông tin cá nhân trên không gian mạng. Các thông tin mà người dùng (tác giả, độc giả, biên tập viên, người phản biện) nhập vào các biểu mẫu trên Hệ thống Quản lý xuất bản trực tuyến của tạp chí chỉ được sử dụng vào các mục đích đã được tuyên bố rõ ràng và sẽ không được cung cấp cho bất kỳ bên thứ ba nào khác, hay dùng vào bất kỳ mục đích nào khác.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Phí gửi bài\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Lệ phí gửi đăng bài: 1.000.000đ\u002Fbài báo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Lệ phí gửi đăng nhanh: 1.500.000đ\u002Fbài báo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Đối với tác giả là cán bộ viên chức thuộc Trường Đại học Y Dược Cần Thơ thì được hỗ trợ 50% lệ phí gửi đăng bài.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Đối với sinh viên thực hiện đề tài nghiên cứu khoa học cấp trường được hỗ trợ 100% lệ phí đăng bài ( Tác giả gửi đính kèm “ Quyết định về việc giao tổ chức thực hiện đề tài nghiên cứu khoa học cấp Trường của sinh viên”).\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Hình thức nộp lệ phí:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Tiền mặt:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Nộp trực tiếp tại Phòng Tài chính - Kế toán, Trường Đại học Y Dược Cần Thơ, số 179 Nguyễn Văn Cừ, P. An Khánh, Q. Ninh Kiều, thành phố Cần Thơ.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Chuyển khoản:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tên Tài khoản: Trường ĐHYD Cần Thơ, Số TK: 0111000115668, tại ngân hàng Vietcombank chi nhánh Cần Thơ.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Thời gian: Áp dụng từ ngày 01\u002F02\u002F2023.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">* Phí gửi bài không được hoàn trả khi bài viết bị từ chối hoặc tác giả xin rút bài viết.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Quy trình phản biện bài báo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tạp chí Y Dược học Cần Thơ thực hiện quy trình phản biện kín hai chiều nghiêm ngặt. Danh tính của những người phản biện không được tiết lộ cho các tác giả và ngược lại. Quy trình thẩm định bài báo đăng gồm các bước sau:\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tiếp nhận bản thảo\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Tác giả liên hệ gửi bản thảo đến Tạp chí qua hệ thống trực tuyến tại website: https:\u002F\u002Ftapchi.ctump.edu.vn. Hướng dẫn về cách đăng ký, gửi bài và chuẩn bị bản thảo được cung cấp trên website của Tạp chí.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Sàng lọc sơ bộ\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Sau khi Tòa soạn nhận được bài báo của tác giả, Ban Thư ký sẽ tiến hành kiểm tra sơ bộ bài báo (các yêu cầu về nội dung và hình thức). Những bài báo không đúng quy cách hoặc có nội dung không phù hợp hoặc vi phạm bản quyền sẽ bị từ chối (Ban Thư ký thông báo phản hồi đến tác giả trong vòng 1 tuần). Những bài báo đủ điều kiện, được Ban Thư ký tòa soạn chuyển đến Ban Biên tập có cùng chuyên môn với nội dung bài báo để đề xuất người phản biện. Thời gian kể từ khi Ban Biên tập nhận bài báo đến khi đề xuất người phản biện bài báo chậm nhất là 5 ngày.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Vòng phản biện\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Ban Thư ký gửi bài và yêu cầu phản biện đến 02 phản biện độc lập.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Các phản biện gởi nhận xét cho Ban Thư ký. Thời gian từ khi gửi bài cho phản biện đến khi nhận ý kiến của phản biện tối đa là 20 ngày.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Xử ký kết quả phản biện\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Nếu ý kiến đồng ý cho đăng và không cần chỉnh sửa, Ban Thư ký tiếp tục đăng bài theo qui trình.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Nếu ý kiến đồng ý đăng và cần chỉnh sửa, Ban Thư ký sẽ thông tin đến tác giả chỉnh sửa theo yêu cầu của người phản biện. Thời gian chỉnh sửa và gửi lại kéo dài không quá 2 tuần, từ khi tác giả bài báo nhận được thông tin (Quá trình này có thể lặp lại tối đa 2 lần\u002F1 bài báo). Khi có sự thống nhất, đồng ý của người phản biện; bài báo được tiếp tục đăng theo qui trình.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">3. Những bài báo có chất lượng không đạt yêu cầu, cả 2 phản biện không đồng ý cho đăng sẽ bị Tòa soạn từ chối đăng.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">Xuất bản\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">1. Ban Thư ký tổng hợp các bản thảo đã được tác giả hoàn thiện sau thẩm định trình Ban Biên tập xem xét, Tổng Biên tập phê duyệt, quyết định bài đăng theo các tiêu chí: sự phù hợp nội dung với tôn chỉ và mục đích, thể loại bài viết (ưu tiên các bài có bài có nghiên cứu chuyên sâu, hàm lượng khoa học cao), đóng góp mới bài báo, bài báo được ưu tiên đăng trong số gần nhất của Tạp chí theo thứ tự: tính thời sự, chất lượng bài báo và thời gian gửi bài.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">2. Ban Biên tập và Ban Thư ký biên tập bản thảo, chế bản, đọc rà soát lỗi. Thời gian hoàn thành từ 10-15 ngày.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">3. Ban Thư ký có trách nhiệm thông báo cho tác giả bài báo (bằng e-mail) về tình hình phê duyệt bài báo, thời gian, số kỳ, tập xuất bản bài báo theo qui định.\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>\u003Cp>\u003Cspan style=\"color: rgb(0, 0, 0);\">4. Danh sách bài báo theo số Tạp chí được in ấn và phát hành trong năm định kỳ được công bố chính thức trên website: https:\u002F\u002Ftapchi.ctump.edu.vn\u003C\u002Fspan>\u003C\u002Fp>\u003Cp>\u003Cbr>\u003C\u002Fp>",{"VOID":490},"wcQ1uqwAAAAJ","2023-05-30T08:17:21.868+00:00",[],[494],{"id":495,"createTime":28,"updateTime":28,"relativeEntities":496,"slug":28,"properties":497,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":507,"parentIds":508,"statistic":28},"6413896b-eca9-442b-a73f-182a58a0ce40",[],{"title":498,"address":501,"country":504,"abbreviation":505},{"EN":499,"VI":500},"Can Tho University of Medicine and Pharmacy","Trường Đại học Y Dược Cần Thơ",{"EN":502,"VI":503},"No 179, Nguyen Van Cu street, An Khanh ward, Ninh Kieu district, Can Tho city, Vietnam","Số 179, đường Nguyễn Văn Cừ, phường An Khánh, quận Ninh Kiều, thành phố Cần Thơ, Việt Nam",{"VOID":15},{"VOID":506},"ctump","http:\u002F\u002Fwww.ctump.edu.vn\u002F",[],[],"https:\u002F\u002Ftapchi.ctump.edu.vn\u002Findex.php\u002Fctump",{"impactFactor":32,"impactFactorByYear":512,"i10Index":32,"i10IndexLast5Year":32,"totalPublication":514,"totalPublicationByYear":515,"totalCitation":520,"totalCitationByYear":521,"totalCitationPerPublication":108,"totalCitationPerPublicationByYear":523,"hindexLast5Year":45,"hindex":45},{"2022":513,"2023":111,"2024":106},0.01,1556,{"2020":47,"2021":516,"2022":517,"2023":518,"2024":519,"2025":122},57,306,801,358,161,{"2021":146,"2022":280,"2023":522},99,{"2021":524,"2022":318,"2023":104},0.23,{"impactFactor":28,"impactFactorByYear":28,"i10Index":123,"i10IndexLast5Year":123,"totalPublication":526,"totalPublicationByYear":527,"totalCitation":526,"totalCitationByYear":528,"totalCitationPerPublication":40,"totalCitationPerPublicationByYear":531,"hindexLast5Year":49,"hindex":49},476,{"0":205,"2019":123,"2021":139,"2022":459,"2023":451,"2024":357,"2025":49,"2026":48},{"2021":42,"2022":123,"2023":161,"2024":529,"2025":360,"2026":530},136,83,{"2021":105,"2022":513,"2023":532,"2024":127,"2025":533,"2026":534},0.62,25.43,13.83,{"id":536,"createTime":537,"updateTime":382,"relativeEntities":538,"slug":539,"properties":540,"entityType":25,"verifyStatus":26,"verifyTime":28,"verifyNote":28,"languages":552,"translateLanguages":28,"viewCount":133,"subjectFields":553,"manageAffiliations":554,"indexDatabases":555,"url":556,"thumbnailPath":557,"statistic":558,"gsStatistic":594,"type":55,"analyzePriority":28},"6984a56a-db70-403b-9cc4-4013e1ceaffa","2023-05-09T06:47:40.346+00:00",[],"T%E1%BA%A1p%20ch%C3%AD%20Nghi%C3%AAn%20c%E1%BB%A9u%20n%C6%B0%E1%BB%9Bc%20ngo%C3%A0i",{"country":541,"issn":542,"title":544,"introduce":547,"gsId":550},{"VOID":15},{"VOID":543},"25252445",{"EN":545,"VI":546},"VNU Journal of Foreign Studies","Tạp chí Nghiên cứu nước ngoài",{"EN":548,"VI":549},"{\"ops\":[{\"insert\":\"\\n\\nThe \\n\"},{\"attributes\":{\"italic\":true},\"insert\":\"VNU Journal of Science\"},{\"insert\":\"\\n was established in 1985 for the publication of national and international research papers in all fields of natural sciences and technology, social sciences and humanities. 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Invitational papers may be published in the journal if accepted by the editorial board.","PENDING",[886],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":888,"label":889,"description":891,"parentId":28,"standard":28,"scholarHubFieldId":28},"57a0fcf0-87d5-4174-a54a-b9f64e3f7ea2",[],{"EN":890},"Soil Science",{},[893,900],{"id":894,"createTime":28,"updateTime":28,"relativeEntities":895,"slug":28,"properties":896,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":899,"statistic":28},"43d4a537-d044-4372-8544-ca45c3bea38f",[],{"title":897},{"EN":898},"WILEY",[],{"id":901,"createTime":28,"updateTime":28,"relativeEntities":902,"slug":28,"properties":903,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":906,"statistic":28},"2ea55c76-ecc2-4e81-94b5-baabc3f11863",[],{"title":904},{"EN":905},"John Wiley & Sons Inc.",[],[908,924],{"id":909,"indexDatabase":910,"url":921,"indexYears":28,"academicFieldIds":922,"indexDatabaseRanking":28},"a41d5c95-93c0-4545-a574-fa72c4f11a3f",{"id":911,"createTime":28,"updateTime":28,"relativeEntities":912,"label":913,"description":915,"key":918,"publicationTags":919,"standard":28},"a4921856-b128-4d9f-8f1f-e80813d3bbd4",[],{"EN":914,"VI":914},"ISI\u002FSCIE - Science Citation Index Expanded",{"EN":916,"VI":917},"SCIE database","Cơ sở dữ liệu SCIE","scie",[920,813],"SCIE","https:\u002F\u002Fmjl.clarivate.com\u002Fsearch-results?issn=0361-5995",[923],"7d3206dd-533f-41ef-a012-54551fd2be47",{"id":925,"indexDatabase":926,"url":931,"indexYears":932,"academicFieldIds":933,"indexDatabaseRanking":935},"c83a9f27-312d-48fb-b99b-f9c6b50b75bd",{"id":775,"createTime":28,"updateTime":28,"relativeEntities":927,"label":928,"description":929,"key":781,"publicationTags":930,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],"https:\u002F\u002Fwww.scopus.com\u002Fsourceid\u002F37206","1976-2025",[934],"11eafb22-4c9c-40a4-bb0c-649d942b9b3d","SCOPUS__Q1","https:\u002F\u002Facsess.onlinelibrary.wiley.com\u002Fjournal\u002F14350661",{"meta":938,"data":940},{"total":939},"403",[941,1055,1172,1302,1505,1624,1737,1845,2083,2178],{"id":942,"createTime":943,"updateTime":944,"relativeEntities":945,"slug":946,"properties":947,"entityType":962,"verifyStatus":26,"verifyTime":943,"verifyNote":963,"languages":964,"translateLanguages":965,"viewCount":32,"primaryUrl":966,"fullTextUrl":28,"authors":967,"publicationType":987,"publisherRelationship":988,"citationCount":1034,"citationInfo":1035,"publishDate":1051,"publishYear":1036,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":1052,"openAccess":28,"references":1053,"isForceReanalyzing":1054},"6a5dc996-cd56-4c84-a618-26a591f1ae45","2024-09-04T13:39:56.892+00:00","2024-12-24T23:08:54.918+00:00",[],"A-Closed-form-Equation-for-Predicting-the-Hydraulic-Conductivity-of-Unsaturated-Soils",{"openalex":948,"mag":950,"abstract":952,"title":955,"keywords":958,"doi":960},{"VOID":949},"W2162604832",{"VOID":951},"2162604832",{"EN":953,"VI":954},"\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>A new and relatively simple equation for the soil‐water content‐pressure head curve, θ(\u003Cjats:italic>h\u003C\u002Fjats:italic>), is described in this paper. The particular form of the equation enables one to derive closed‐form analytical expressions for the relative hydraulic conductivity, \u003Cjats:italic>K\u003Cjats:sub>r\u003C\u002Fjats:sub>\u003C\u002Fjats:italic>, when substituted in the predictive conductivity models of N.T. Burdine or Y. Mualem. The resulting expressions for \u003Cjats:italic>K\u003Cjats:sub>r\u003C\u002Fjats:sub>\u003C\u002Fjats:italic>(\u003Cjats:italic>h\u003C\u002Fjats:italic>) contain three independent parameters which may be obtained by fitting the proposed soil‐water retention model to experimental data. Results obtained with the closed‐form analytical expressions based on the Mualem theory are compared with observed hydraulic conductivity data for five soils with a wide range of hydraulic properties. The unsaturated hydraulic conductivity is predicted well in four out of five cases. It is found that a reasonable description of the soil‐water retention curve at low water contents is important for an accurated prediction of the unsaturated hydraulic conductivity.\u003C\u002Fjats:p>","\u003Cjats:title>Tóm tắt\u003C\u002Fjats:title>\u003Cjats:p>Một phương trình mới và tương đối đơn giản cho đường cong áp suất chứa nước trong đất, θ(\u003Cjats:italic>h\u003C\u002Fjats:italic>), được giới thiệu trong bài báo này. Dạng cụ thể của phương trình này cho phép đưa ra các biểu thức phân tích dạng khép kín cho độ dẫn thủy lực tương đối, \u003Cjats:italic>K\u003Cjats:sub>r\u003C\u002Fjats:sub>\u003C\u002Fjats:italic>, khi thay thế vào các mô hình độ dẫn dự đoán của N.T. Burdine hoặc Y. Mualem. Các biểu thức thu được cho \u003Cjats:italic>K\u003Cjats:sub>r\u003C\u002Fjats:sub>\u003C\u002Fjats:italic>(\u003Cjats:italic>h\u003C\u002Fjats:italic>) chứa ba tham số độc lập có thể được xác định bằng cách điều chỉnh mô hình giữ nước trong đất đã đề xuất với dữ liệu thực nghiệm. Kết quả thu được từ các biểu thức khép kín dựa trên lý thuyết Mualem được so sánh với dữ liệu độ dẫn thủy lực quan sát cho năm loại đất có đặc tính thủy lực khác nhau. Độ dẫn thủy lực không bão hòa được dự đoán tốt trong bốn trên năm trường hợp. Kết quả cho thấy rằng việc mô tả hợp lý đường cong giữ nước trong đất ở mức chứa nước thấp là quan trọng để dự đoán chính xác độ dẫn thủy lực không bão hòa.\u003C\u002Fjats:p>",{"EN":956,"VI":957},"A Closed‐form Equation for Predicting the Hydraulic Conductivity of Unsaturated Soils","Phương Trình Dạng Khép Kín Dự Báo Độ Dẫn Thủy Lực của Đất Không Bão Hòa",{"VI":959},"Herardic, độ dẫn thủy lực, đường cong giữ nước đất, lý thuyết Mualem, mô hình dự đoán, độ dẫn thủy lực không bão hòa, dữ liệu thực nghiệm, điều chỉnh mô hình, đặc tính thủy lực giấy phép. ",{"VOID":961},"10.2136\u002Fsssaj1980.03615995004400050002x","PUBLICATION","Auto Verify",[31],[30],"https:\u002F\u002Facsess.onlinelibrary.wiley.com\u002Fdoi\u002F10.2136\u002Fsssaj1980.03615995004400050002x",[968],{"id":969,"sortIndex":32,"researcher":28,"roles":970,"affiliations":971,"properties":980,"displayName":984,"givenName":28,"familyName":28},"eafe9497-f216-4552-bb8c-94195a32a302",[],[972],{"id":973,"sortIndex":32,"affiliation":974,"properties":28},"14526df4-8846-4131-aa7c-13f79f67db12",{"id":973,"createTime":28,"updateTime":28,"relativeEntities":975,"slug":28,"properties":976,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":979,"statistic":28},[],{"title":977},{"EN":978},"Soil Scientist, Dep. of Soil and Environmental Sciences, University of California, Riverside, CA 92521. The author is located at the U. S. Salinity Lab., 4500 Glenwood Dr., Riverside, CA 92502.",[],{"orcid":981,"title":983,"openalex":985},{"VOID":982},"https:\u002F\u002Forcid.org\u002F0000-0003-1654-8858",{"EN":984},"Martinus Th. van Genuchten",{"VOID":986},"A5067513167","ARTICLE",{"url":28,"publisher":989,"properties":1027},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":990,"slug":872,"properties":991,"entityType":25,"verifyStatus":884,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":996,"manageAffiliations":1001,"indexDatabases":1012,"url":936,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":28,"analyzePriority":28},[],{"country":992,"eissn":993,"issn":994,"title":995},{"VOID":875},{"VOID":877},{"VOID":879},{"EN":881},[997],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":998,"label":999,"description":1000,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":890},{},[1002,1007],{"id":894,"createTime":28,"updateTime":28,"relativeEntities":1003,"slug":28,"properties":1004,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1006,"statistic":28},[],{"title":1005},{"EN":898},[],{"id":901,"createTime":28,"updateTime":28,"relativeEntities":1008,"slug":28,"properties":1009,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1011,"statistic":28},[],{"title":1010},{"EN":905},[],[1013,1020],{"id":909,"indexDatabase":1014,"url":921,"indexYears":28,"academicFieldIds":1019,"indexDatabaseRanking":28},{"id":911,"createTime":28,"updateTime":28,"relativeEntities":1015,"label":1016,"description":1017,"key":918,"publicationTags":1018,"standard":28},[],{"EN":914,"VI":914},{"EN":916,"VI":917},[920,813],[923],{"id":925,"indexDatabase":1021,"url":931,"indexYears":932,"academicFieldIds":1026,"indexDatabaseRanking":935},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1022,"label":1023,"description":1024,"key":781,"publicationTags":1025,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[934],{"issue":1028,"pages":1030,"volume":1032},{"VOID":1029},"5",{"VOID":1031},"892-898",{"VOID":1033},"44",24167,{"total":1034,"publishYear":1036,"statisticByYear":1037},1980,{"2012":1038,"2013":1039,"2014":1040,"2015":1041,"2016":1042,"2017":1043,"2018":1044,"2019":1045,"2020":1046,"2021":1047,"2022":1048,"2023":1049,"2024":1050},930,1015,1131,1112,1089,1047,1193,1363,1392,1610,1583,1616,1110,"1980-09-01",[920,935],[],false,{"id":1056,"createTime":1057,"updateTime":1058,"relativeEntities":1059,"slug":1060,"properties":1061,"entityType":962,"verifyStatus":884,"verifyTime":1057,"verifyNote":1076,"languages":1077,"translateLanguages":1078,"viewCount":32,"primaryUrl":1079,"fullTextUrl":28,"authors":1080,"publicationType":987,"publisherRelationship":1107,"citationCount":1153,"citationInfo":1154,"publishDate":1169,"publishYear":1155,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":1170,"openAccess":28,"references":1171,"isForceReanalyzing":1054},"34d2b119-dfb3-46f4-ae37-f0f4134f4e2b","2024-12-06T11:24:38.553+00:00","2024-12-24T07:21:22.548+00:00",[],"Development-of-a-DTPA-Soil-Test-for-Zinc-Iron-Manganese-and-Copper",{"openalex":1062,"mag":1064,"abstract":1066,"title":1069,"keywords":1072,"doi":1074},{"VOID":1063},"W2162774880",{"VOID":1065},"2162774880",{"EN":1067,"VI":1068},"\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>A DTPA soil test was developed to identify near‐neutral and calcareous soils with insufficient available Zn, Fe, Mn, or Cu for maximum yields of crops. The extractant consists of 0.005\u003Cjats:italic>M\u003C\u002Fjats:italic> DTPA (diethylenetriaminepentaacetic acid), 0.1\u003Cjats:italic>M\u003C\u002Fjats:italic> triethanolamine, and 0.01\u003Cjats:italic>M\u003C\u002Fjats:italic> CaCl\u003Cjats:sub>2\u003C\u002Fjats:sub>, with a pH of 7.3. The soil test consists of shaking 10 g of air‐dry soil with 20 ml of extractant for 2 hours. The leachate is filtered, and Zn, Fe, Mn, and Cu are measured in the filtrate by atomic absorption spectrophotometry.\u003C\u002Fjats:p>\u003Cjats:p>The soil test successfully separated 77 Colorado soils on the basis of crop response to Zn, Fe, and Mn fertilizers. Critical nutrient levels must be determined separately for each crop using standardized procedures for soil preparation, grinding, and extraction. The critical levels for corn using the procedures reported herein were: 0.8 ppm for Zn, 4.5 ppm for Fe, and tentatively 1.0 ppm for Mn, and 0.2 ppm for Cu.\u003C\u002Fjats:p>\u003Cjats:p>Development of the soil test was based, in part, on theoretical considerations. The extractant is buffered at pH 7.30 and contains CaCl\u003Cjats:sub>2\u003C\u002Fjats:sub> so that equilibrium with CaCO\u003Cjats:sub>3\u003C\u002Fjats:sub> is established at a CO\u003Cjats:sub>2\u003C\u002Fjats:sub> level about 10 times that of the atmosphere. Thus, the extractant precludes dissolution of CaCO\u003Cjats:sub>3\u003C\u002Fjats:sub> and the release of occluded nutrients which are normally not available to plants. DTPA was selected as the chelating agent because it can effectively extract all four micronutrient metals. Factors such as pH, concentration of chelating agent, time of shaking, and temperature of extraction affect the amount of micronutrients extracted and were adjusted for maximum overall effectiveness.\u003C\u002Fjats:p>","\u003Cjats:title>Tóm tắt\u003C\u002Fjats:title>\u003Cjats:p>Một phương pháp kiểm tra đất DTPA đã được phát triển để nhận diện các loại đất gần trung tính và đất vôi có hàm lượng Zn, Fe, Mn, hoặc Cu không đủ cho năng suất cây trồng tối đa. Chất triết suất gồm 0.005\u003Cjats:italic>M\u003C\u002Fjats:italic> DTPA (axit diethylenetriaminepentaacetic), 0.1\u003Cjats:italic>M\u003C\u002Fjats:italic> triethanolamine, và 0.01\u003Cjats:italic>M\u003C\u002Fjats:italic> CaCl\u003Cjats:sub>2\u003C\u002Fjats:sub>, với pH là 7.3. Phương pháp kiểm tra đất bao gồm việc lắc 10 g đất khô không khí với 20 ml chất triết suất trong 2 giờ. Dung dịch được lọc, và hàm lượng Zn, Fe, Mn, và Cu được đo lường trong dung dịch lọc bằng phương pháp quang phổ hấp thu nguyên tử.\u003C\u002Fjats:p>\u003Cjats:p>Phương pháp kiểm tra đất đã phân biệt thành công 77 loại đất ở Colorado dựa trên sự phản ứng của cây trồng với phân bón kẽm, sắt và mangan. Mức độ dinh dưỡng quan trọng phải được xác định riêng biệt cho từng loại cây trồng sử dụng quy trình tiêu chuẩn hóa cho việc chuẩn bị đất, nghiền và triết suất. Các mức độ quan trọng cho ngô sử dụng quy trình báo cáo trong nghiên cứu này là: 0.8 ppm cho Zn, 4.5 ppm cho Fe, tạm thời 1.0 ppm cho Mn, và 0.2 ppm cho Cu.\u003C\u002Fjats:p>\u003Cjats:p>Việc phát triển phương pháp kiểm tra đất một phần dựa trên các cân nhắc lý thuyết. Chất triết suất được đệm tại pH 7.30 và chứa CaCl\u003Cjats:sub>2\u003C\u002Fjats:sub> để cân bằng với CaCO\u003Cjats:sub>3\u003C\u002Fjats:sub> tại mức CO\u003Cjats:sub>2\u003C\u002Fjats:sub> cao hơn khoảng 10 lần so với mức trong không khí. Nhờ đó, chất triết suất tránh việc hòa tan CaCO\u003Cjats:sub>3\u003C\u002Fjats:sub> và phát thải các dưỡng chất bị mắc kẹt thường không có sẵn cho cây trồng. DTPA được chọn làm chất tạo phức vì có khả năng hiệu quả chiết xuất cả bốn kim loại vi lượng. Các yếu tố như pH, nồng độ chất tạo phức, thời gian lắc, và nhiệt độ triết suất ảnh hưởng đến lượng vi lượng được chiết xuất và được điều chỉnh để đạt hiệu quả tối đa.",{"EN":1070,"VI":1071},"Development of a DTPA Soil Test for Zinc, Iron, Manganese, and Copper","Phát triển phương pháp kiểm tra đất bằng DTPA cho kẽm, sắt, mangan và đồng",{"VI":1073},"DTPA; kiểm tra đất; Zn; Fe; Mn; Cu; triết suất đệm; quang phổ hấp thu nguyên tử; dinh dưỡng cây trồng; phương pháp chuẩn hóa; đất gần trung tính; đất vôi; diethylenetriaminepentaacetic",{"VOID":1075},"10.2136\u002Fsssaj1978.03615995004200030009x","Author affiliation is blank",[31],[30],"https:\u002F\u002Facsess.onlinelibrary.wiley.com\u002Fdoi\u002F10.2136\u002Fsssaj1978.03615995004200030009x",[1081,1090],{"id":1082,"sortIndex":32,"researcher":28,"roles":1083,"affiliations":1084,"properties":1085,"displayName":1087,"givenName":28,"familyName":28},"47329dc9-9fcf-4bfa-9bf8-8210923ccf06",[],[],{"title":1086,"openalex":1088},{"EN":1087},"W. L. Lindsay",{"VOID":1089},"A5110170344",{"id":1091,"sortIndex":40,"researcher":28,"roles":1092,"affiliations":1093,"properties":1102,"displayName":1104,"givenName":28,"familyName":28},"dc06a8ed-b3a1-4f29-bce5-aa0f29f399d5",[],[1094],{"id":1095,"sortIndex":32,"affiliation":1096,"properties":28},"0ed76524-edaf-47ac-9be8-b6832dbd8eb0",{"id":1095,"createTime":28,"updateTime":28,"relativeEntities":1097,"slug":28,"properties":1098,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1101,"statistic":28},[],{"title":1099},{"EN":1100},"Professor of Agronomy, Colorado State Univ., Fort Collins, CO 80523, and Associate Scientist, Connecticut Agric. Exp. Stn., New Haven, Conn., respectively.",[],{"title":1103,"openalex":1105},{"EN":1104},"W. A. Norvell",{"VOID":1106},"A5113503365",{"url":28,"publisher":1108,"properties":1146},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1109,"slug":872,"properties":1110,"entityType":25,"verifyStatus":884,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1115,"manageAffiliations":1120,"indexDatabases":1131,"url":936,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":28,"analyzePriority":28},[],{"country":1111,"eissn":1112,"issn":1113,"title":1114},{"VOID":875},{"VOID":877},{"VOID":879},{"EN":881},[1116],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":1117,"label":1118,"description":1119,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":890},{},[1121,1126],{"id":894,"createTime":28,"updateTime":28,"relativeEntities":1122,"slug":28,"properties":1123,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1125,"statistic":28},[],{"title":1124},{"EN":898},[],{"id":901,"createTime":28,"updateTime":28,"relativeEntities":1127,"slug":28,"properties":1128,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1130,"statistic":28},[],{"title":1129},{"EN":905},[],[1132,1139],{"id":909,"indexDatabase":1133,"url":921,"indexYears":28,"academicFieldIds":1138,"indexDatabaseRanking":28},{"id":911,"createTime":28,"updateTime":28,"relativeEntities":1134,"label":1135,"description":1136,"key":918,"publicationTags":1137,"standard":28},[],{"EN":914,"VI":914},{"EN":916,"VI":917},[920,813],[923],{"id":925,"indexDatabase":1140,"url":931,"indexYears":932,"academicFieldIds":1145,"indexDatabaseRanking":935},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1141,"label":1142,"description":1143,"key":781,"publicationTags":1144,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[934],{"issue":1147,"pages":1149,"volume":1151},{"VOID":1148},"3",{"VOID":1150},"421-428",{"VOID":1152},"42",8961,{"total":1153,"publishYear":1155,"statisticByYear":1156},1978,{"2012":1157,"2013":1158,"2014":1159,"2015":1160,"2016":616,"2017":1161,"2018":1162,"2019":1163,"2020":1164,"2021":1165,"2022":1166,"2023":1167,"2024":1168},315,343,381,349,449,393,482,543,563,618,627,585,"1978-05-01",[920,935],[],{"id":1173,"createTime":1174,"updateTime":1175,"relativeEntities":1176,"slug":1177,"properties":1178,"entityType":962,"verifyStatus":884,"verifyTime":1174,"verifyNote":1076,"languages":1193,"translateLanguages":1194,"viewCount":32,"primaryUrl":1195,"fullTextUrl":28,"authors":1196,"publicationType":987,"publisherRelationship":1241,"citationCount":1286,"citationInfo":1287,"publishDate":1299,"publishYear":1288,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":1300,"openAccess":28,"references":1301,"isForceReanalyzing":1054},"7c9d25ca-f1a7-4d85-a711-6bd9f0062971","2024-12-29T08:50:07.242+00:00","2025-01-08T03:11:03.822+00:00",[],"Analysis-of-Factors-Controlling-Soil-Organic-Matter-Levels-in-Great-Plains-Grasslands",{"openalex":1179,"mag":1181,"abstract":1183,"title":1186,"keywords":1189,"doi":1191},{"VOID":1180},"W2162066644",{"VOID":1182},"2162066644",{"VI":1184,"EN":1185},"\u003Cjats:title>Tóm tắt\u003C\u002Fjats:title>\u003Cjats:p>Chúng tôi đã phân tích các yếu tố khí hậu và kết cấu ảnh hưởng đến carbon hữu cơ (C) và nitơ (N) trong đất tại vùng Đại Bình nguyên của Hoa Kỳ. Chúng tôi đã sử dụng một mô hình về số lượng và thành phần chất hữu cơ trong đất (SOM) để mô phỏng mức độ chất hữu cơ ổn định tại 24 địa điểm đồng cỏ trong khu vực này. Mô hình có khả năng mô phỏng tác động của các gradient khí hậu đến SOM và năng suất. Kết cấu đất cũng là một yếu tố kiểm soát quan trọng đối với động lực học của chất hữu cơ. Mô hình đã dự đoán một cách chính xác sản lượng thực vật trên mặt đất cũng như mức độ C và N trong đất qua các loại kết cấu đất (cát, trung bình và mịn); tuy nhiên, mô hình có xu hướng đánh giá quá mức mức độ C và N trong đất thuộc loại kết cấu mịn từ 10 đến 15%. Tác động của việc chăn thả đối với hệ thống đã được mô phỏng và cho thấy rằng các mức C và N trong đất ổn định nhạy cảm với cường độ chăn thả, với mức C và N trong đất giảm khi tần suất chăn thả tăng lên. Các xu hướng vùng trong SOM có thể được dự đoán bằng bốn biến cụ thể cho địa điểm, bao gồm nhiệt độ, độ ẩm, kết cấu đất và hàm lượng lignin trong thực vật. Các đầu vào nitơ cũng cần phải được xác định. Cường độ chăn thả trong quá trình phát triển đất cũng là một yếu tố kiểm soát quan trọng đối với các mức SOM ổn định, và do ít dữ liệu có sẵn về việc chăn thả trước khi định cư, một số sự không chắc chắn là bất khả kháng trong các dự đoán của mô hình.\u003C\u002Fjats:p>","\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>We analyzed climatic and textural controls of soil organic C and N for soils of the U.S. Great Plains. We used a model of soil organic matter (SOM) quantity and composition to simulate steady‐state organic matter levels for 24 grassland locations in the Great Plains. The model was able to simulate the effects of climatic gradients on SOM and productivity. Soil texture was also a major control over organic matter dynamics. The model adequately predicted aboveground plant production and soil C and N levels across soil textures (sandy, medium, and fine); however, the model tended to overestimate soil C and N levels for fine textured soil by 10 to 15%. The impact of grazing on the system was simulated and showed that steady‐state soil C and N levels were sensitive to the grazing intensity, with soil C and N levels decreasing with increased grazing rates. Regional trends in SOM can be predicted using four site‐specific variables, temperature, moisture, soil texture, and plant lignin content. Nitrogen inputs must also be known. Grazing intensity during soil development is also a significant control over steady‐state levels of SOM, and since few data are available on presettlement grazing, some uncertainty is inherent in the model predictions.\u003C\u002Fjats:p>",{"EN":1187,"VI":1188},"Analysis of Factors Controlling Soil Organic Matter Levels in Great Plains Grasslands","Phân tích các yếu tố kiểm soát mức độ chất hữu cơ trong đất ở các đồng cỏ vùng Đại Bình nguyên",{"VI":1190},"",{"VOID":1192},"10.2136\u002Fsssaj1987.03615995005100050015x",[31],[30],"https:\u002F\u002Facsess.onlinelibrary.wiley.com\u002Fdoi\u002F10.2136\u002Fsssaj1987.03615995005100050015x",[1197,1206,1215,1224],{"id":1198,"sortIndex":32,"researcher":28,"roles":1199,"affiliations":1200,"properties":1201,"displayName":1203,"givenName":28,"familyName":28},"74b3ac94-8a10-459c-9f94-6359b57757a7",[],[],{"title":1202,"openalex":1204},{"EN":1203},"W. J. Parton",{"VOID":1205},"A5023794679",{"id":1207,"sortIndex":40,"researcher":28,"roles":1208,"affiliations":1209,"properties":1210,"displayName":1212,"givenName":28,"familyName":28},"520cd81b-48be-4201-9e43-a1dcfc1a9fb9",[],[],{"title":1211,"openalex":1213},{"EN":1212},"D. Schimel",{"VOID":1214},"A5070730987",{"id":1216,"sortIndex":123,"researcher":28,"roles":1217,"affiliations":1218,"properties":1219,"displayName":1221,"givenName":28,"familyName":28},"473c8c9b-7605-40a3-993a-7dfa0a972fb8",[],[],{"title":1220,"openalex":1222},{"EN":1221},"C. V. Cole",{"VOID":1223},"A5113595640",{"id":1225,"sortIndex":42,"researcher":28,"roles":1226,"affiliations":1227,"properties":1236,"displayName":1238,"givenName":28,"familyName":28},"e0dc1166-eb22-411c-8192-44961a858bfa",[],[1228],{"id":1229,"sortIndex":32,"affiliation":1230,"properties":28},"69384c0f-799c-4754-a6b2-f82cc3e9464b",{"id":1229,"createTime":28,"updateTime":28,"relativeEntities":1231,"slug":28,"properties":1232,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1235,"statistic":28},[],{"title":1233},{"EN":1234},"Senior Research Scientist, Research Scientist, Soil Scientist, USDA-ARS (Fort Collins, CO) and Graduate Research Assistant, Natural Resource Ecology Lab., Colorado State Univ., Fort Collins, CO 80523.",[],{"title":1237,"openalex":1239},{"EN":1238},"Dennis S. Ojima",{"VOID":1240},"A5113494448",{"url":28,"publisher":1242,"properties":1280},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1243,"slug":872,"properties":1244,"entityType":25,"verifyStatus":884,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1249,"manageAffiliations":1254,"indexDatabases":1265,"url":936,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":28,"analyzePriority":28},[],{"country":1245,"eissn":1246,"issn":1247,"title":1248},{"VOID":875},{"VOID":877},{"VOID":879},{"EN":881},[1250],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":1251,"label":1252,"description":1253,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":890},{},[1255,1260],{"id":894,"createTime":28,"updateTime":28,"relativeEntities":1256,"slug":28,"properties":1257,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1259,"statistic":28},[],{"title":1258},{"EN":898},[],{"id":901,"createTime":28,"updateTime":28,"relativeEntities":1261,"slug":28,"properties":1262,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1264,"statistic":28},[],{"title":1263},{"EN":905},[],[1266,1273],{"id":909,"indexDatabase":1267,"url":921,"indexYears":28,"academicFieldIds":1272,"indexDatabaseRanking":28},{"id":911,"createTime":28,"updateTime":28,"relativeEntities":1268,"label":1269,"description":1270,"key":918,"publicationTags":1271,"standard":28},[],{"EN":914,"VI":914},{"EN":916,"VI":917},[920,813],[923],{"id":925,"indexDatabase":1274,"url":931,"indexYears":932,"academicFieldIds":1279,"indexDatabaseRanking":935},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1275,"label":1276,"description":1277,"key":781,"publicationTags":1278,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[934],{"issue":1281,"pages":1282,"volume":1284},{"VOID":1029},{"VOID":1283},"1173-1179",{"VOID":1285},"51",3728,{"total":1286,"publishYear":1288,"statisticByYear":1289},1987,{"2012":1290,"2013":1291,"2014":1292,"2015":1293,"2016":1294,"2017":608,"2018":212,"2019":1295,"2020":154,"2021":1296,"2022":1297,"2023":358,"2024":1298},158,191,127,142,115,133,103,96,81,"1987-09-01",[920,935],[],{"id":1303,"createTime":1304,"updateTime":1305,"relativeEntities":1306,"slug":1307,"properties":1308,"entityType":962,"verifyStatus":26,"verifyTime":1304,"verifyNote":963,"languages":1322,"translateLanguages":1323,"viewCount":32,"primaryUrl":1324,"fullTextUrl":28,"authors":1325,"publicationType":987,"publisherRelationship":1447,"citationCount":1492,"citationInfo":1493,"publishDate":1502,"publishYear":1494,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":1503,"openAccess":28,"references":1504,"isForceReanalyzing":1054},"54b61e96-b215-49d7-94a5-7a30f30e569a","2024-09-04T00:07:53.146+00:00","2025-01-08T03:12:00.834+00:00",[],"Field-Scale-Variability-of-Soil-Properties-in-Central-Iowa-Soils",{"openalex":1309,"mag":1311,"abstract":1313,"title":1316,"keywords":1319,"doi":1320},{"VOID":1310},"W2056193610",{"VOID":1312},"2056193610",{"VI":1314,"EN":1315},"\u003Cjats:title>Tóm tắt\u003C\u002Fjats:title>\u003Cjats:p>Phân bố không gian của các đặc tính đất ở quy mô đồng ruộng và lưu vực có thể ảnh hưởng đến tiềm năng năng suất, phản ứng thủy văn, và khả năng vận chuyển thuốc diệt cỏ và NO\u003Cjats:sup>−\u003C\u002Fjats:sup>\u003Cjats:sub>3\u003C\u002Fjats:sub> tới bề mặt hoặc nước ngầm. Nghiên cứu của chúng tôi mô tả các phân bố theo quy mô đồng ruộng và xu hướng không gian cho 28 đặc tính đất khác nhau tại hai địa điểm trong một lưu vực ở trung Iowa. Hai trong số 27 thông số đo được tại một địa điểm và 10 trong số 14 thông số đo được tại địa điểm thứ hai có phân bố chuẩn. Biến đổi không gian được nghiên cứu thông qua các bán phương sai và tỷ lệ giữa phần ngẫu nhiên và tổng bán phương sai, được biểu thị dưới dạng phần trăm, được sử dụng để phân loại sự phụ thuộc không gian. Tỷ lệ \u003C25% cho thấy sự phụ thuộc không gian mạnh, từ 25 đến 75% cho thấy sự phụ thuộc không gian trung bình, và >75% cho thấy sự phụ thuộc không gian yếu. Mười hai tham số tại Địa điểm một, bao gồm carbon hữu cơ, tổng nitơ, pH, và phân đoạn lớn, và bốn tham số tại Địa điểm hai, bao gồm carbon hữu cơ và tổng nitơ, có sự phụ thuộc không gian mạnh. Sáu tham số tại Địa điểm một, bao gồm carbon và nitơ sinh khối, mật độ khối và quá trình khử nitrat, và 9 tham số tại Địa điểm hai, bao gồm carbon và nitơ sinh khối và mật độ khối, có sự phụ thuộc không gian trung bình. Ba tham số tại Địa điểm một, bao gồm nitrat N và ergosterol, và một tham số tại Địa điểm hai, nitơ liên kết khoáng, có sự phụ thuộc không gian yếu. Phân bố của canxi hoán đổi và magiê tại Địa điểm một không có sự phụ thuộc không gian. Phân bố theo không gian cho một số đặc tính đất là tương tự ở cả hai địa điểm đồng ruộng. Chúng tôi sẽ có thể khai thác những sự tương đồng này để cải thiện khả năng suy diễn thông tin lấy từ một đồng ruộng tới các đồng ruộng khác trong những cảnh quan tương tự.\u003C\u002Fjats:p>","\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>Spatial distributions of soil properties at the field and watershed scale may affect yield potential, hydrologic responses, and transport of herbicides and NO\u003Cjats:sup>−\u003C\u002Fjats:sup>\u003Cjats:sub>3\u003C\u002Fjats:sub> to surface or groundwater. Our research describes field‐scale distributions and spatial trends for 28 different soil parameters at two sites within a watershed in central Iowa. Two of 27 parameters measured at one site and 10 of 14 parameters measured at the second site were normally distributed. Spatial variability was investigated using semivariograms and the ratio of nugget to total semivariance, expressed as a percentage, was used to classify spatial dependence. A ratio of <25% indicated strong spatial dependence, between 25 and 75% indicated moderate spatial dependence, and >75% indicated weak spatial dependence. Twelve parameters at Site one, including organic C, total N, pH, and macroaggregation, and four parameters at Site two, including organic C and total N, were strongly spatially dependent. Six parameters at Site one, including biomass C and N, bulk density, and denitrification, and 9 parameters at Site two, including biomass C and N and bulk density, were moderately spatially dependent. Three parameters at Site one, including NO\u003Cjats:sup>−\u003C\u002Fjats:sup>\u003Cjats:sub>3\u003C\u002Fjats:sub> N and ergosterol, and one parameter at Site two, mineral‐associated N, were weakly spatially dependent. Distributions of exchangeable Ca and Mg at Site one were not spatially dependent. Spatial distributions for some soil properties were similar for both field sites. We will be able to exploit these similarities to improve our ability to extrapolate information taken from one field to other fields within similar landscapes.\u003C\u002Fjats:p>",{"EN":1317,"VI":1318},"Field‐Scale Variability of Soil Properties in Central Iowa Soils","Biến Đổi Đặc Tính Đất Tại Quy Mô Đồng Ruộng Ở Các Đất Trung Iowa",{"VI":1190},{"VOID":1321},"10.2136\u002Fsssaj1994.03615995005800050033x",[31],[30],"https:\u002F\u002Facsess.onlinelibrary.wiley.com\u002Fdoi\u002F10.2136\u002Fsssaj1994.03615995005800050033x",[1326,1343,1358,1377,1392,1409,1428],{"id":1327,"sortIndex":32,"researcher":28,"roles":1328,"affiliations":1329,"properties":1338,"displayName":1340,"givenName":28,"familyName":28},"e7c3246a-a375-4191-aad5-b3347db5334c",[],[1330],{"id":1331,"sortIndex":32,"affiliation":1332,"properties":28},"129e9d90-dae4-4883-84b8-cf4660256d03",{"id":1331,"createTime":28,"updateTime":28,"relativeEntities":1333,"slug":28,"properties":1334,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1337,"statistic":28},[],{"title":1335},{"EN":1336},"USDA‐ARS National Soil Tilth Lab. 2150 Pammel Drive Ames IA 50011",[],{"title":1339,"openalex":1341},{"EN":1340},"Cynthia A. Cambardella",{"VOID":1342},"A5045694869",{"id":1344,"sortIndex":40,"researcher":28,"roles":1345,"affiliations":1346,"properties":1353,"displayName":1355,"givenName":28,"familyName":28},"9a500502-ecdd-4998-bb6c-da42e3ba5eee",[],[1347],{"id":1331,"sortIndex":32,"affiliation":1348,"properties":28},{"id":1331,"createTime":28,"updateTime":28,"relativeEntities":1349,"slug":28,"properties":1350,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1352,"statistic":28},[],{"title":1351},{"EN":1336},[],{"title":1354,"openalex":1356},{"EN":1355},"T. B. Moorman",{"VOID":1357},"A5005465835",{"id":1359,"sortIndex":123,"researcher":28,"roles":1360,"affiliations":1361,"properties":1370,"displayName":1374,"givenName":28,"familyName":28},"c9eae01b-b2ab-4901-b4c8-fb6d8a7ba48c",[],[1362],{"id":1363,"sortIndex":32,"affiliation":1364,"properties":28},"9758aa27-4982-4164-a616-6407b02fe64c",{"id":1363,"createTime":28,"updateTime":28,"relativeEntities":1365,"slug":28,"properties":1366,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1369,"statistic":28},[],{"title":1367},{"EN":1368},"USDA‐ARS, Coastal Plains Soil and Water Research Center P.O. Box 3039 Florence SC 29502",[],{"orcid":1371,"title":1373,"openalex":1375},{"VOID":1372},"https:\u002F\u002Forcid.org\u002F0000-0003-1580-7141",{"EN":1374},"J. M. 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Xantheas",{"VOID":1446},"A5068503645",{"url":28,"publisher":1448,"properties":1486},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1449,"slug":872,"properties":1450,"entityType":25,"verifyStatus":884,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1455,"manageAffiliations":1460,"indexDatabases":1471,"url":936,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":28,"analyzePriority":28},[],{"country":1451,"eissn":1452,"issn":1453,"title":1454},{"VOID":875},{"VOID":877},{"VOID":879},{"EN":881},[1456],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":1457,"label":1458,"description":1459,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":890},{},[1461,1466],{"id":894,"createTime":28,"updateTime":28,"relativeEntities":1462,"slug":28,"properties":1463,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1465,"statistic":28},[],{"title":1464},{"EN":898},[],{"id":901,"createTime":28,"updateTime":28,"relativeEntities":1467,"slug":28,"properties":1468,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1470,"statistic":28},[],{"title":1469},{"EN":905},[],[1472,1479],{"id":909,"indexDatabase":1473,"url":921,"indexYears":28,"academicFieldIds":1478,"indexDatabaseRanking":28},{"id":911,"createTime":28,"updateTime":28,"relativeEntities":1474,"label":1475,"description":1476,"key":918,"publicationTags":1477,"standard":28},[],{"EN":914,"VI":914},{"EN":916,"VI":917},[920,813],[923],{"id":925,"indexDatabase":1480,"url":931,"indexYears":932,"academicFieldIds":1485,"indexDatabaseRanking":935},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1481,"label":1482,"description":1483,"key":781,"publicationTags":1484,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[934],{"issue":1487,"pages":1488,"volume":1490},{"VOID":1029},{"VOID":1489},"1501-1511",{"VOID":1491},"58",3307,{"total":1492,"publishYear":1494,"statisticByYear":1495},1994,{"2012":1290,"2013":213,"2014":605,"2015":1496,"2016":605,"2017":603,"2018":1497,"2019":1498,"2020":360,"2021":1499,"2022":614,"2023":1500,"2024":1501},221,196,234,213,204,69,"1994-09-01",[920,935],[],{"id":1506,"createTime":1507,"updateTime":1508,"relativeEntities":1509,"slug":1510,"properties":1511,"entityType":962,"verifyStatus":884,"verifyTime":1507,"verifyNote":1076,"languages":1525,"translateLanguages":1526,"viewCount":32,"primaryUrl":1527,"fullTextUrl":28,"authors":1528,"publicationType":987,"publisherRelationship":1570,"citationCount":1615,"citationInfo":1616,"publishDate":1621,"publishYear":1617,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":1622,"openAccess":28,"references":1623,"isForceReanalyzing":1054},"accf1d30-6d59-4442-b056-a4f5721b32f5","2024-10-06T17:18:55.506+00:00","2025-01-08T03:12:56.842+00:00",[],"Changes-in-Inorganic-and-Organic-Soil-Phosphorus-Fractions-Induced-by-Cultivation-Practices-and-by-Laboratory-Incubations",{"openalex":1512,"mag":1514,"abstract":1516,"title":1519,"keywords":1522,"doi":1523},{"VOID":1513},"W2071909768",{"VOID":1515},"2071909768",{"VI":1517,"EN":1518},"\u003Cjats:title>Tóm tắt\u003C\u002Fjats:title>\u003Cjats:p>Những thay đổi trong các phân số photpho (P) vô cơ và hữu cơ do 65 năm canh tác trong quy trình gieo trồng lúa mì – lúa mì – nghỉ đông đã được nghiên cứu bằng kỹ thuật chiết xuất tuần tự. Hàm lượng P tổng trong đất canh tác thấp hơn 29% so với đất cỏ thường xuyên liền kề; mất mát chính về P (74% tổng lượng P mất) là từ P hữu cơ và P còn lại. Trong tổng lượng P mất, 22% đến từ các dạng P hữu cơ có thể chiết xuất, trong khi 52% đến từ P ổn định.\u003C\u002Fjats:p>\u003Cjats:p>Các nghiên cứu ủ đã được sử dụng để nghiên cứu sự biến đổi P theo mùa trong quá trình nghỉ đông mô phỏng với và không có việc bổ sung dư lượng và phân bón P. Chín lần bổ sung hàng tháng cellulose (765 µg C · g\u003Cjats:sup>−1\u003C\u002Fjats:sup> đất) có hoặc không có P (9 µg · g\u003Cjats:sup>−1\u003C\u002Fjats:sup> đất) đã làm thay đổi đáng kể mức độ P hữu cơ có thể chiết xuất và P vô cơ trong đất được ủ. Bằng chứng cho thấy hoạt động của vi sinh vật đóng vai trò quan trọng trong việc phân phối lại P thành các dạng khác nhau trong đất.\u003C\u002Fjats:p>","\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>Changes in inorganic and organic phosphorus (P) fractions resulting from 65 years of cropping in a wheat‐wheat‐fallow rotation were studied using a sequential extraction technique. Total P content of the cultivated soil was 29% lower than that of the adjacent permanent pasture; the major loss of P (74% of total P lost) was organic P and residual P. Of the total P lost, 22% was from the extractable organic P forms, whereas 52% originated from stable P.\u003C\u002Fjats:p>\u003Cjats:p>Incubation studies were used to study seasonal P transformations during simulated fallow with and without residue incorporation and P fertilization. Nine monthly additions of cellulose (765 µg C · g\u003Cjats:sup>−1\u003C\u002Fjats:sup> soil) with and without P (9 µg · g\u003Cjats:sup>−1\u003C\u002Fjats:sup> soil) significantly altered levels of total extractable organic P and inorganic P in incubated soils. Evidence is provided for microbial activity playing a major role in redistributing P into different forms in the soil.\u003C\u002Fjats:p>",{"EN":1520,"VI":1521},"Changes in Inorganic and Organic Soil Phosphorus Fractions Induced by Cultivation Practices and by Laboratory Incubations","Thay đổi trong các phân số photpho vô cơ và hữu cơ trong đất do các phương pháp canh tác và thí nghiệm ủ trong phòng thí nghiệm gây ra",{"VI":1190},{"VOID":1524},"10.2136\u002Fsssaj1982.03615995004600050017x",[31],[30],"https:\u002F\u002Facsess.onlinelibrary.wiley.com\u002Fdoi\u002F10.2136\u002Fsssaj1982.03615995004600050017x",[1529,1540,1551],{"id":1530,"sortIndex":32,"researcher":28,"roles":1531,"affiliations":1532,"properties":1533,"displayName":1537,"givenName":28,"familyName":28},"d8217def-38a0-4a5d-bcb0-8a507267e7cd",[],[],{"orcid":1534,"title":1536,"openalex":1538},{"VOID":1535},"https:\u002F\u002Forcid.org\u002F0000-0002-3739-2533",{"EN":1537},"M. J. Hedley",{"VOID":1539},"A5015127146",{"id":1541,"sortIndex":40,"researcher":28,"roles":1542,"affiliations":1543,"properties":1544,"displayName":1548,"givenName":28,"familyName":28},"922ae334-be70-48c2-9c7a-7f62cdaecb42",[],[],{"orcid":1545,"title":1547,"openalex":1549},{"VOID":1546},"https:\u002F\u002Forcid.org\u002F0000-0001-5766-6733",{"EN":1548},"John Stewart",{"VOID":1550},"A5059368390",{"id":1552,"sortIndex":123,"researcher":28,"roles":1553,"affiliations":1554,"properties":1563,"displayName":1567,"givenName":28,"familyName":28},"b9226467-011f-41d4-8da0-be2c2c139384",[],[1555],{"id":1556,"sortIndex":32,"affiliation":1557,"properties":28},"52936098-52b3-49ff-bde0-be9276f67c7f",{"id":1556,"createTime":28,"updateTime":28,"relativeEntities":1558,"slug":28,"properties":1559,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1562,"statistic":28},[],{"title":1560},{"EN":1561},"Post Doctorate Fellow, Professor of Soil Science and Post Doctorate Fellow, respectively, Saskatchewan Institute of Pedology.",[],{"orcid":1564,"title":1566,"openalex":1568},{"VOID":1565},"https:\u002F\u002Forcid.org\u002F0000-0003-1540-4668",{"EN":1567},"Bhagirath Singh Chauhan",{"VOID":1569},"A5077353489",{"url":28,"publisher":1571,"properties":1609},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1572,"slug":872,"properties":1573,"entityType":25,"verifyStatus":884,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1578,"manageAffiliations":1583,"indexDatabases":1594,"url":936,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":28,"analyzePriority":28},[],{"country":1574,"eissn":1575,"issn":1576,"title":1577},{"VOID":875},{"VOID":877},{"VOID":879},{"EN":881},[1579],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":1580,"label":1581,"description":1582,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":890},{},[1584,1589],{"id":894,"createTime":28,"updateTime":28,"relativeEntities":1585,"slug":28,"properties":1586,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1588,"statistic":28},[],{"title":1587},{"EN":898},[],{"id":901,"createTime":28,"updateTime":28,"relativeEntities":1590,"slug":28,"properties":1591,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1593,"statistic":28},[],{"title":1592},{"EN":905},[],[1595,1602],{"id":909,"indexDatabase":1596,"url":921,"indexYears":28,"academicFieldIds":1601,"indexDatabaseRanking":28},{"id":911,"createTime":28,"updateTime":28,"relativeEntities":1597,"label":1598,"description":1599,"key":918,"publicationTags":1600,"standard":28},[],{"EN":914,"VI":914},{"EN":916,"VI":917},[920,813],[923],{"id":925,"indexDatabase":1603,"url":931,"indexYears":932,"academicFieldIds":1608,"indexDatabaseRanking":935},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1604,"label":1605,"description":1606,"key":781,"publicationTags":1607,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[934],{"issue":1610,"pages":1611,"volume":1613},{"VOID":1029},{"VOID":1612},"970-976",{"VOID":1614},"46",2581,{"total":1615,"publishYear":1617,"statisticByYear":1618},1982,{"2012":1501,"2013":209,"2014":209,"2015":1296,"2016":154,"2017":212,"2018":1295,"2019":1619,"2020":602,"2021":1620,"2022":1500,"2023":1291,"2024":613},144,164,"1982-09-01",[920,935],[],{"id":1625,"createTime":1626,"updateTime":1627,"relativeEntities":1628,"slug":1629,"properties":1630,"entityType":962,"verifyStatus":26,"verifyTime":1626,"verifyNote":963,"languages":1644,"translateLanguages":1645,"viewCount":32,"primaryUrl":1646,"fullTextUrl":28,"authors":1647,"publicationType":987,"publisherRelationship":1680,"citationCount":1725,"citationInfo":1726,"publishDate":1734,"publishYear":1727,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":1735,"openAccess":28,"references":1736,"isForceReanalyzing":1054},"c9e00e64-01ff-49e0-9ebd-2932897d6a83","2024-10-10T00:19:19.785+00:00","2025-01-08T03:13:53.745+00:00",[],"Particulate-Soil-Organic-Matter-Changes-across-a-Grassland-Cultivation-Sequence",{"openalex":1631,"mag":1633,"abstract":1635,"title":1638,"keywords":1641,"doi":1642},{"VOID":1632},"W2067019078",{"VOID":1634},"2067019078",{"VI":1636,"EN":1637},"\u003Cjats:title>Tóm tắt\u003C\u002Fjats:title>\u003Cjats:p>Nhiều mô hình đã được xây dựng nhằm cố gắng mô tả động lực của sự tuần hoàn hợp chất hữu cơ trong đất (SOM), phần lớn trong số đó bao gồm 2 đến 3 bể chứa hợp chất hữu cơ được định nghĩa về động học. Việc xác định vật lý và hóa học của các bể chứa SOM được khái niệm này đã gặp nhiều khó khăn. Chúng tôi mô tả một phương pháp đơn giản để phân tán đất nhằm tách biệt một phần hợp chất hữu cơ dạng hạt (POM) có thể đại diện cho một bể chứa SOM quan trọng trong đất đồng cỏ. Phần POM được tách ra bằng cách phân tán đất trong dung dịch hexametaphosphate 5 g L\u003Cjats:sup>−1\u003C\u002Fjats:sup> và lọc các mẫu đất đã phân tán qua một lưới 53 µm. Chúng tôi so sánh C POM và C liên kết khoáng trong ba biện pháp canh tác (20 năm canh tác) và một đồng cỏ chưa bị xáo trộn tại Sidney, NE. C POM trong cỏ native đại diện cho 39% tổng hợp chất hữu cơ trong đất. Hai mươi năm quản lý bỏ hoang, trồng trọt nông sản và không cày đã giảm hàm lượng C trong phần này xuống còn 18, 19 và 25%, tương ứng, so với tổng hợp chất hữu cơ. Phần hợp chất hữu cơ liên kết khoáng không cho thấy sự giảm hàm lượng C trong biện pháp bỏ hoang so với đất đồng cỏ nhưng tăng lên trong biện pháp không cày và trồng mật. Động lực nitơ nói chung phản ánh những gì quan sát được ở C. Phân tích phần POM về hàm lượng lignin và cellulose chỉ ra rằng phần này có 47% lignin và có chỉ số lignocellulose là 0,7. Thành phần đồng vị C ổn định của phần POM gợi ý rằng POM có nguồn gốc từ lúa mì phân hủy nhanh hơn so với POM có nguồn gốc từ cỏ. Chúng tôi cho rằng phần POM rất gần với các đặc tính của một bể chứa SOM được mô tả khác nhau là hợp chất hữu cơ phân hủy chậm, có khả năng phân hủy, hoặc đã ổn định.\u003C\u002Fjats:p>","\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>Many models have been constructed in an attempt to describe the dynamics of soil organic‐matter (SOM) turnover, most of which include 2 to 3 kinetically defined organic‐matter pools. Physical and chemical definition of these conceptualized SOM pools has been difficult. We describe a simple method for dispersion of soil to isolate a particulate organic‐matter (POM) fraction that may represent an important SOM pool in grassland soils. The POM fraction was isolated by dispersing the soil in 5 g L\u003Cjats:sup>−1\u003C\u002Fjats:sup> hexametaphosphate and passing the dispersed soil samples through a 53‐µm sieve. We compared POM and mineral‐associated C among three tillage treatments (20 yr under cultivation) and an undisturbed grassland at Sidney, NE. The POM C in the native sod represented 39% of the total soil organic C. Twenty years of bare‐fallow, stubble‐mulch, and no‐till management reduced the C content in this fraction to 18, 19, and 25%, respectively, of the total organic C. The mineral‐associated organic‐matter fraction showed no reduction in C content in the bare‐fallow treatment compared with the grassland soil but increased in the no‐till and stubble‐mulch treatments. Nitrogen dynamics generally mirrored those observed for C. Analysis of the POM fraction for lignin and cellulose content indicated that this fraction was 47% lignin and had a lignocellulose index of 0.7. The stable C‐isotope composition of the POM fraction suggests that wheat‐derived POM turns over faster than grass‐derived POM. We suggest the POM fraction closely matches the characteristics of a SOM pool variously described as slow, decomposable, or stabilized organic matter.\u003C\u002Fjats:p>",{"EN":1639,"VI":1640},"Particulate Soil Organic‐Matter Changes across a Grassland Cultivation Sequence","Sự thay đổi của hợp chất hữu cơ dạng hạt trong đất qua chuỗi canh tác đồng cỏ",{"VI":1190},{"VOID":1643},"10.2136\u002Fsssaj1992.03615995005600030017x",[31],[30],"https:\u002F\u002Facsess.onlinelibrary.wiley.com\u002Fdoi\u002F10.2136\u002Fsssaj1992.03615995005600030017x",[1648,1663],{"id":1649,"sortIndex":32,"researcher":28,"roles":1650,"affiliations":1651,"properties":1660,"displayName":1340,"givenName":28,"familyName":28},"eabc0b21-3f5f-4ae2-a3d9-aba7ae074749",[],[1652],{"id":1653,"sortIndex":32,"affiliation":1654,"properties":28},"e82017e4-ffee-4366-a61a-738bf507974a",{"id":1653,"createTime":28,"updateTime":28,"relativeEntities":1655,"slug":28,"properties":1656,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1659,"statistic":28},[],{"title":1657},{"EN":1658},"National Soil Tilth Lab. 2150 Pammel Drive Ames IA 50011",[],{"title":1661,"openalex":1662},{"EN":1340},{"VOID":1342},{"id":1664,"sortIndex":40,"researcher":28,"roles":1665,"affiliations":1666,"properties":1675,"displayName":1677,"givenName":28,"familyName":28},"2a0042c1-bb16-46e8-9e17-337dedc6a4da",[],[1667],{"id":1668,"sortIndex":32,"affiliation":1669,"properties":28},"ca091140-7b4a-47c1-804b-b61f38605d8a",{"id":1668,"createTime":28,"updateTime":28,"relativeEntities":1670,"slug":28,"properties":1671,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1674,"statistic":28},[],{"title":1672},{"EN":1673},"Natural Resource Ecology Lab., Colorado State Univ., Fort Collins, CO, 80523",[],{"title":1676,"openalex":1678},{"EN":1677},"Edward T. Elliott",{"VOID":1679},"A5066297690",{"url":28,"publisher":1681,"properties":1719},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1682,"slug":872,"properties":1683,"entityType":25,"verifyStatus":884,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1688,"manageAffiliations":1693,"indexDatabases":1704,"url":936,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":28,"analyzePriority":28},[],{"country":1684,"eissn":1685,"issn":1686,"title":1687},{"VOID":875},{"VOID":877},{"VOID":879},{"EN":881},[1689],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":1690,"label":1691,"description":1692,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":890},{},[1694,1699],{"id":894,"createTime":28,"updateTime":28,"relativeEntities":1695,"slug":28,"properties":1696,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1698,"statistic":28},[],{"title":1697},{"EN":898},[],{"id":901,"createTime":28,"updateTime":28,"relativeEntities":1700,"slug":28,"properties":1701,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1703,"statistic":28},[],{"title":1702},{"EN":905},[],[1705,1712],{"id":909,"indexDatabase":1706,"url":921,"indexYears":28,"academicFieldIds":1711,"indexDatabaseRanking":28},{"id":911,"createTime":28,"updateTime":28,"relativeEntities":1707,"label":1708,"description":1709,"key":918,"publicationTags":1710,"standard":28},[],{"EN":914,"VI":914},{"EN":916,"VI":917},[920,813],[923],{"id":925,"indexDatabase":1713,"url":931,"indexYears":932,"academicFieldIds":1718,"indexDatabaseRanking":935},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1714,"label":1715,"description":1716,"key":781,"publicationTags":1717,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[934],{"issue":1720,"pages":1721,"volume":1723},{"VOID":1148},{"VOID":1722},"777-783",{"VOID":1724},"56",2483,{"total":1725,"publishYear":1727,"statisticByYear":1728},1992,{"2012":611,"2013":435,"2014":435,"2015":354,"2016":154,"2017":153,"2018":1729,"2019":1730,"2020":1731,"2021":213,"2022":1732,"2023":830,"2024":1733},120,116,152,180,155,"1992-05-01",[920,935],[],{"id":1738,"createTime":1739,"updateTime":1740,"relativeEntities":1741,"slug":1742,"properties":1743,"entityType":962,"verifyStatus":884,"verifyTime":1757,"verifyNote":1076,"languages":1758,"translateLanguages":1759,"viewCount":32,"primaryUrl":1760,"fullTextUrl":28,"authors":1761,"publicationType":987,"publisherRelationship":1790,"citationCount":1836,"citationInfo":1837,"publishDate":1842,"publishYear":1838,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":1843,"openAccess":28,"references":1844,"isForceReanalyzing":1054},"b85ec220-1f18-4374-a4be-f30520a6c6b9","2024-09-22T03:57:16.313+00:00","2025-01-08T03:14:51.775+00:00",[],"Effect-of-Water-Filled-Pore-Space-on-Carbon-Dioxide-and-Nitrous-Oxide-Production-in-Tilled-and-Nontilled-Soils",{"openalex":1744,"mag":1746,"abstract":1748,"title":1751,"keywords":1754,"doi":1755},{"VOID":1745},"W2037893757",{"VOID":1747},"2037893757",{"VI":1749,"EN":1750},"\u003Cjats:title>Tóm tắt\u003C\u002Fjats:title>\u003Cjats:p>Phần trăm không gian lỗ đất được lấp đầy bằng nước (phần trăm lỗ chứa nước, % WFP), được xác định bởi độ ẩm và tổng độ rỗng, dường như có liên quan chặt chẽ đến hoạt động vi sinh vật trong đất dưới các chế độ cày xới khác nhau. Đất được ủ trong phòng thí nghiệm với 60% WFP hỗ trợ hoạt động vi sinh vật hiếu khí tối đa được xác định qua sản xuất CO\u003Cjats:sub>2\u003C\u002Fjats:sub> và hấp thụ O\u003Cjats:sub>2\u003C\u002Fjats:sub>. Tại hiện trường, % WFP của đất bề mặt không cày xới (0–75 mm) ở bốn địa điểm tại Hoa Kỳ trung bình là 62% tại thời điểm lấy mẫu, trong khi đó đối với đất đã cày xới là 44%. Sự khác biệt này trong % WFP được phản ánh qua sản xuất CO\u003Cjats:sub>2\u003C\u002Fjats:sub> và N\u003Cjats:sub>2\u003C\u002Fjats:sub>O lần lượt cao hơn 3.4 và 9.4 lần từ các đất không cày xới bề mặt trong 24 giờ so với đất đã cày xới. Ở độ sâu từ 75 đến 150 mm, các giá trị % WFP tăng lên ở cả đất không cày xới và đất đã cày xới, trung bình khoảng 70% đối với đất không cày xới so với 50 đến 60% đối với đất đã cày xới. Sản xuất CO\u003Cjats:sub>2\u003C\u002Fjats:sub> trong các đất đã cày xới được cải thiện bởi % WFP tăng lên, dẫn đến ít hoặc không có sự khác biệt trong sản xuất CO\u003Cjats:sub>2\u003C\u002Fjats:sub> giữa các phương pháp xử lý đất. Tuy nhiên, sản xuất nitrous oxide vẫn cao hơn trong điều kiện không cày xới. Lượng lớn nitrous oxide được sản xuất từ các đất bón phân N, bất kể phương pháp cày xới. Sản xuất CO\u003Cjats:sub>2\u003C\u002Fjats:sub> và N\u003Cjats:sub>2\u003C\u002Fjats:sub>O chủ yếu liên quan đến % WFP của các phương pháp cày xới, mặc dù trong một số trường hợp, C hòa tan trong nước và mức NO\u003Cjats:sup>−\u003C\u002Fjats:sup>\u003Cjats:sub>3\u003C\u002Fjats:sub> cũng quan trọng. Các phép tính về hoạt động vi sinh vật hiếu khí tương đối giữa đất không cày xới và đất đã cày xới, dựa trên sự khác biệt về % WFP liên quan đến hoạt động tối đa ở 60%, chỉ ra mối quan hệ tuyến tính cho sản xuất CO\u003Cjats:sub>2\u003C\u002Fjats:sub> và N\u003Cjats:sub>2\u003C\u002Fjats:sub>O giữa các giá trị WFP từ 30 đến 70%. Dưới 60% WFP, nước giới hạn hoạt động vi sinh vật, nhưng trên 60%, hoạt động vi sinh vật hiếu khí giảm — dường như là kết quả của việc giảm không khí thông qua đất.\u003C\u002Fjats:p>","\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>The percentage of soil pore space filled with water (percent water‐filled pores, % WFP), as determined by water content and total porosity, appears to be closely related to soil microbial activity under different tillage regimes. Soil incubated in the laboratory at 60% WFP supported maximum aerobic microbial activity as determined by CO\u003Cjats:sub>2\u003C\u002Fjats:sub> production and O\u003Cjats:sub>2\u003C\u002Fjats:sub> uptake. In the field, % WFP of surface no‐tillage soils (0–75 mm) at four U.S. locations averaged 62% at time of sampling, whereas that for plowed soils was 44%. This difference in % WFP was reflected in 3.4 and 9.4 times greater CO\u003Cjats:sub>2\u003C\u002Fjats:sub> and N\u003Cjats:sub>2\u003C\u002Fjats:sub>O production, respectively, from surface no‐tillage soils over a 24‐h period as compared to plowed soils. At a depth of 75 to 150 mm, % WFP values increased in both no‐tillage and plowed soils, averaging approximately 70% for no tillage compared with 50 to 60% for plowed soils. Production of CO\u003Cjats:sub>2\u003C\u002Fjats:sub> in the plowed soils was enhanced by the increased % WFP, resulting in little or no difference in CO\u003Cjats:sub>2\u003C\u002Fjats:sub> production between tillage treatments. Nitrous oxide production, however, remained greater under no‐tillage conditions. Substantially greater amounts of N\u003Cjats:sub>2\u003C\u002Fjats:sub>O were produced from the N‐fertilized soils, regardless of tillage practice. Production of CO\u003Cjats:sub>2\u003C\u002Fjats:sub> and N\u003Cjats:sub>2\u003C\u002Fjats:sub>O was primarily related to the % WFP of tillage treatments although, in several instances, soil‐water‐soluble C and NO\u003Cjats:sup>‐\u003C\u002Fjats:sup>\u003Cjats:sub>3\u003C\u002Fjats:sub> levels were important as well. Calculations of relative aerobic microbial activity between no‐tillage and plowed soils, based on differences in % WFP relative to maximum activity at 60%, indicated linear relationships for CO\u003Cjats:sub>2\u003C\u002Fjats:sub> and N\u003Cjats:sub>2\u003C\u002Fjats:sub>O production between WFP values of 30 to 70%. Below 60% WFP, water limits microbial activity, but above 60%, aerobic microbial activity decreases—apparently the result of reduced aeration.\u003C\u002Fjats:p>",{"EN":1752,"VI":1753},"Effect of Water‐Filled Pore Space on Carbon Dioxide and Nitrous Oxide Production in Tilled and Nontilled Soils","Ảnh hưởng của không gian dạng lỗ chứa nước đến sản xuất carbon dioxide và nitrous oxide trong đất cày xới và không cày xới",{"VI":1190},{"VOID":1756},"10.2136\u002Fsssaj1984.03615995004800060013x","2024-09-22T03:57:16.312+00:00",[31],[30],"https:\u002F\u002Facsess.onlinelibrary.wiley.com\u002Fdoi\u002F10.2136\u002Fsssaj1984.03615995004800060013x",[1762,1771],{"id":1763,"sortIndex":32,"researcher":28,"roles":1764,"affiliations":1765,"properties":1766,"displayName":1768,"givenName":28,"familyName":28},"4c58cc60-37f1-40e0-8898-39401d9ba87c",[],[],{"title":1767,"openalex":1769},{"EN":1768},"D. M. Linn",{"VOID":1770},"A5065148431",{"id":1772,"sortIndex":40,"researcher":28,"roles":1773,"affiliations":1774,"properties":1783,"displayName":1787,"givenName":28,"familyName":28},"b066ec39-d3ac-4f2d-9438-72887a858b58",[],[1775],{"id":1776,"sortIndex":32,"affiliation":1777,"properties":28},"f6b48f5c-81fc-48f1-9c87-d62e790ce383",{"id":1776,"createTime":28,"updateTime":28,"relativeEntities":1778,"slug":28,"properties":1779,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1782,"statistic":28},[],{"title":1780},{"EN":1781},"Research Associate, University of Minnesota, St. Paul (formerly Research Technologist, Univ. Nebraska-Lincoln), and Soil Scientist, ARS, USDA, Lincoln, NE.",[],{"orcid":1784,"title":1786,"openalex":1788},{"VOID":1785},"https:\u002F\u002Forcid.org\u002F0000-0001-9077-1623",{"EN":1787},"John W. Doran",{"VOID":1789},"A5028818674",{"url":28,"publisher":1791,"properties":1829},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1792,"slug":872,"properties":1793,"entityType":25,"verifyStatus":884,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1798,"manageAffiliations":1803,"indexDatabases":1814,"url":936,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":28,"analyzePriority":28},[],{"country":1794,"eissn":1795,"issn":1796,"title":1797},{"VOID":875},{"VOID":877},{"VOID":879},{"EN":881},[1799],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":1800,"label":1801,"description":1802,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":890},{},[1804,1809],{"id":894,"createTime":28,"updateTime":28,"relativeEntities":1805,"slug":28,"properties":1806,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1808,"statistic":28},[],{"title":1807},{"EN":898},[],{"id":901,"createTime":28,"updateTime":28,"relativeEntities":1810,"slug":28,"properties":1811,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1813,"statistic":28},[],{"title":1812},{"EN":905},[],[1815,1822],{"id":909,"indexDatabase":1816,"url":921,"indexYears":28,"academicFieldIds":1821,"indexDatabaseRanking":28},{"id":911,"createTime":28,"updateTime":28,"relativeEntities":1817,"label":1818,"description":1819,"key":918,"publicationTags":1820,"standard":28},[],{"EN":914,"VI":914},{"EN":916,"VI":917},[920,813],[923],{"id":925,"indexDatabase":1823,"url":931,"indexYears":932,"academicFieldIds":1828,"indexDatabaseRanking":935},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1824,"label":1825,"description":1826,"key":781,"publicationTags":1827,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[934],{"issue":1830,"pages":1832,"volume":1834},{"VOID":1831},"6",{"VOID":1833},"1267-1272",{"VOID":1835},"48",2199,{"total":1836,"publishYear":1838,"statisticByYear":1839},1984,{"2012":1297,"2013":334,"2014":451,"2015":43,"2016":1840,"2017":1297,"2018":210,"2019":154,"2020":354,"2021":690,"2022":1841,"2023":1297,"2024":201},108,111,"1984-11-01",[920,935],[],{"id":1846,"createTime":1847,"updateTime":1848,"relativeEntities":1849,"slug":1850,"properties":1851,"entityType":962,"verifyStatus":26,"verifyTime":1847,"verifyNote":963,"languages":1865,"translateLanguages":1866,"viewCount":32,"primaryUrl":1867,"fullTextUrl":28,"authors":1868,"publicationType":987,"publisherRelationship":1903,"citationCount":1948,"citationInfo":1949,"publishDate":1956,"publishYear":1950,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":1957,"openAccess":28,"references":1958,"isForceReanalyzing":1054},"7e759818-c42a-4d21-8c37-f774c79e260b","2024-10-06T13:53:08.168+00:00","2025-01-08T03:15:48.700+00:00",[],"Soil-Water-Characteristic-Estimates-by-Texture-and-Organic-Matter-for-Hydrologic-Solutions",{"openalex":1852,"mag":1854,"abstract":1856,"title":1859,"keywords":1862,"doi":1863},{"VOID":1853},"W2083735459",{"VOID":1855},"2083735459",{"VI":1857,"EN":1858},"\u003Cjats:p>Phân tích thủy văn thường liên quan đến việc đánh giá sự thấm nước trong đất, độ dẫn nước, khả năng lưu trữ và mối quan hệ giữa thực vật và nước. Để xác định các ảnh hưởng của nước trong đất đến thủy văn, cần ước lượng các đặc tính nước trong đất cho tiềm năng nước và độ dẫn thuỷ lực bằng cách sử dụng các biến đất như kết cấu, vật chất hữu cơ (OM) và cấu trúc. Việc đo đạc tại hiện trường hoặc trong phòng thí nghiệm thường khó khăn, tốn kém và thường không thực tế cho nhiều phân tích thủy văn. Các mối tương quan thống kê giữa kết cấu đất, tiềm năng nước trong đất và độ dẫn thuỷ lực có thể cung cấp những ước lượng đủ chính xác cho nhiều phân tích và quyết định. Nghiên cứu này đã phát triển các phương trình đặc tính nước trong đất mới từ cơ sở dữ liệu đất hiện có của USDA chỉ bằng cách sử dụng các biến dễ dàng thu thập như kết cấu đất và OM. Các phương trình này tương tự như những phương trình đã được Saxton và cộng sự báo cáo trước đó nhưng bao gồm nhiều biến và phạm vi ứng dụng hơn. Chúng được kết hợp với các mối quan hệ đã được báo cáo trước đó cho độ căng và độ dẫn cũng như tác động của mật độ, sỏi và độ mặn để hình thành một hệ thống dự đoán đặc tính nước trong đất toàn diện cho quản lý nước nông nghiệp và phân tích thủy văn. Việc xác minh được thực hiện bằng cách sử dụng các tập dữ liệu độc lập cho một phạm vi rộng các kết cấu đất. Hệ thống dự đoán được lập trình cho một mô hình máy tính đồ họa để cung cấp ứng dụng dễ dàng và giải pháp nhanh chóng và có sẵn tại \u003Cjats:ext-link xmlns:xlink=\"http:\u002F\u002Fwww.w3.org\u002F1999\u002Fxlink\" xlink:href=\"http:\u002F\u002Fhydrolab.arsusda.gov\u002Fsoilwater\u002FIndex.htm\">http:\u002F\u002Fhydrolab.arsusda.gov\u002Fsoilwater\u002FIndex.htm\u003C\u002Fjats:ext-link>\u003C\u002Fjats:p>","\u003Cjats:p>Hydrologic analyses often involve the evaluation of soil water infiltration, conductivity, storage, and plant‐water relationships. To define the hydrologic soil water effects requires estimating soil water characteristics for water potential and hydraulic conductivity using soil variables such as texture, organic matter (OM), and structure. Field or laboratory measurements are difficult, costly, and often impractical for many hydrologic analyses. Statistical correlations between soil texture, soil water potential, and hydraulic conductivity can provide estimates sufficiently accurate for many analyses and decisions. This study developed new soil water characteristic equations from the currently available USDA soil database using only the readily available variables of soil texture and OM. These equations are similar to those previously reported by Saxton et al. but include more variables and application range. They were combined with previously reported relationships for tensions and conductivities and the effects of density, gravel, and salinity to form a comprehensive predictive system of soil water characteristics for agricultural water management and hydrologic analyses. Verification was performed using independent data sets for a wide range of soil textures. The predictive system was programmed for a graphical computerized model to provide easy application and rapid solutions and is available at \u003Cjats:ext-link xmlns:xlink=\"http:\u002F\u002Fwww.w3.org\u002F1999\u002Fxlink\" xlink:href=\"http:\u002F\u002Fhydrolab.arsusda.gov\u002Fsoilwater\u002FIndex.htm\">http:\u002F\u002Fhydrolab.arsusda.gov\u002Fsoilwater\u002FIndex.htm\u003C\u002Fjats:ext-link>\u003C\u002Fjats:p>",{"EN":1860,"VI":1861},"Soil Water Characteristic Estimates by Texture and Organic Matter for Hydrologic Solutions","Ước lượng đặc tính nước trong đất theo kết cấu và chất hữu cơ cho các giải pháp thủy văn",{"VI":1190},{"VOID":1864},"10.2136\u002Fsssaj2005.0117",[31],[30],"https:\u002F\u002Facsess.onlinelibrary.wiley.com\u002Fdoi\u002F10.2136\u002Fsssaj2005.0117",[1869,1886],{"id":1870,"sortIndex":32,"researcher":28,"roles":1871,"affiliations":1872,"properties":1881,"displayName":1883,"givenName":28,"familyName":28},"b6448a93-4529-4bf8-a63a-da07e6c7ff26",[],[1873],{"id":1874,"sortIndex":32,"affiliation":1875,"properties":28},"cd650543-3c2e-482d-b778-4642dcd9332f",{"id":1874,"createTime":28,"updateTime":28,"relativeEntities":1876,"slug":28,"properties":1877,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1880,"statistic":28},[],{"title":1878},{"EN":1879},"Saxton Engineering and Associates, 1250 SW Campus View, Pullman WA 99163",[],{"title":1882,"openalex":1884},{"EN":1883},"K. E. Saxton",{"VOID":1885},"A5064872565",{"id":1887,"sortIndex":40,"researcher":28,"roles":1888,"affiliations":1889,"properties":1898,"displayName":1900,"givenName":28,"familyName":28},"488d9ee7-9c6d-4665-befd-3d6f45b2057c",[],[1890],{"id":1891,"sortIndex":32,"affiliation":1892,"properties":28},"295d4217-b571-4b2e-a8e1-26ed061ccf37",{"id":1891,"createTime":28,"updateTime":28,"relativeEntities":1893,"slug":28,"properties":1894,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1897,"statistic":28},[],{"title":1895},{"EN":1896},"USDA-ARS; Hydrology and Remote Sensing Lab; Bldg. 007, Rm. 104, BARC-W Beltsville MD 20705",[],{"title":1899,"openalex":1901},{"EN":1900},"W. J. Rawls",{"VOID":1902},"A5049795906",{"url":28,"publisher":1904,"properties":1942},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":1905,"slug":872,"properties":1906,"entityType":25,"verifyStatus":884,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":1911,"manageAffiliations":1916,"indexDatabases":1927,"url":936,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":28,"analyzePriority":28},[],{"country":1907,"eissn":1908,"issn":1909,"title":1910},{"VOID":875},{"VOID":877},{"VOID":879},{"EN":881},[1912],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":1913,"label":1914,"description":1915,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":890},{},[1917,1922],{"id":894,"createTime":28,"updateTime":28,"relativeEntities":1918,"slug":28,"properties":1919,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1921,"statistic":28},[],{"title":1920},{"EN":898},[],{"id":901,"createTime":28,"updateTime":28,"relativeEntities":1923,"slug":28,"properties":1924,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":1926,"statistic":28},[],{"title":1925},{"EN":905},[],[1928,1935],{"id":909,"indexDatabase":1929,"url":921,"indexYears":28,"academicFieldIds":1934,"indexDatabaseRanking":28},{"id":911,"createTime":28,"updateTime":28,"relativeEntities":1930,"label":1931,"description":1932,"key":918,"publicationTags":1933,"standard":28},[],{"EN":914,"VI":914},{"EN":916,"VI":917},[920,813],[923],{"id":925,"indexDatabase":1936,"url":931,"indexYears":932,"academicFieldIds":1941,"indexDatabaseRanking":935},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":1937,"label":1938,"description":1939,"key":781,"publicationTags":1940,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[934],{"issue":1943,"pages":1944,"volume":1946},{"VOID":1029},{"VOID":1945},"1569-1578",{"VOID":1947},"70",2172,{"total":1948,"publishYear":1950,"statisticByYear":1951},2006,{"2012":1298,"2013":435,"2014":324,"2015":1952,"2016":1953,"2017":212,"2018":1954,"2019":215,"2020":1291,"2021":864,"2022":1955,"2023":575,"2024":210},135,157,181,210,"2006-09-01",[920,935],[1959,1962,1965,1968,1971,1975,1979,1982,1985,1988,1991,1994,1997,2000,2003,2006,2009,2012,2015,2018,2021,2024,2027,2030,2033,2036,2039,2042,2045,2048,2051,2054,2057,2060,2063,2066,2069,2071,2074,2077,2080],{"id":28,"text":1960,"url":28,"identifiers":1961},"10.2136\u002Fsssaj1984.03615995004800040001x",{"doi":1960},{"id":28,"text":1963,"url":28,"identifiers":1964},"10.2136\u002Fsssaj1985.03615995004900050005x",{"doi":1963},{"id":28,"text":1966,"url":28,"identifiers":1967},"Ahuja L.R., 1999, Agricultural drainage, 1207",{},{"id":28,"text":1969,"url":28,"identifiers":1970},"10.2136\u002Fsssaj1981.03615995004500060004x",{"doi":1969},{"id":28,"text":1972,"url":28,"identifiers":1973},"Brakensiek D.L., 1984, Determining the saturated hydraulic conductivity of a soil containing rock fragments, Soil Sci. Soc. Am. J, 50, 834, 10.2136\u002Fsssaj1986.03615995005000030053x",{"doi":1974},"10.2136\u002Fsssaj1986.03615995005000030053x",{"id":28,"text":1976,"url":28,"identifiers":1977},"Brakensiek D.L., 1986, A note on determining soil properties for soils containing rock fragments, J. Range Manage, 39, 408, 10.2307\u002F3899439",{"doi":1978},"10.2307\u002F3899439",{"id":28,"text":1980,"url":28,"identifiers":1981},"Brooks R.H., 1964, Hydraulic properties of porous media",{},{"id":28,"text":1983,"url":28,"identifiers":1984},"10.1097\u002F00010694-197406000-00001",{"doi":1983},{"id":28,"text":1986,"url":28,"identifiers":1987},"Carman P.C., 1956, Flow of gases through porous media",{},{"id":28,"text":1989,"url":28,"identifiers":1990},"Flint A.L., 1984, Erosion and productivity of soils containing rock fragments. SSSA Spec. Pub. 13, 91",{},{"id":28,"text":1992,"url":28,"identifiers":1993},"10.1016\u002FS1161-0301(02)00098-9",{"doi":1992},{"id":28,"text":1995,"url":28,"identifiers":1996},"Grossman R.B., 2001, Coupling use‐dependent and use‐invariant data for soil quality evaluation in the United States, J. Soil Water Conserv, 56, 63",{},{"id":28,"text":1998,"url":28,"identifiers":1999},"10.1029\u002FWR015i006p01633",{"doi":1998},{"id":28,"text":2001,"url":28,"identifiers":2002},"Hahn C.T., 1982, Statistical methods in hydrology",{},{"id":28,"text":2004,"url":28,"identifiers":2005},"Hillel D., 1998, Environmental soil physics",{},{"id":28,"text":2007,"url":28,"identifiers":2008},"Hudson B., 1994, Soil organic matter and available water capacity, J. Soil Water Conserv, 49, 189",{},{"id":28,"text":2010,"url":28,"identifiers":2011},"10.2136\u002Fsssaj1995.03615995005900040027x",{"doi":2010},{"id":28,"text":2013,"url":28,"identifiers":2014},"10.2136\u002Fsssabookser5.1.2ed",{"doi":2013},{"id":28,"text":2016,"url":28,"identifiers":2017},"Pachepsky Y.A., 2005, Development of pedotransfer functions in soil hydrology",{},{"id":28,"text":2019,"url":28,"identifiers":2020},"Peck A.J. andD.Watson.1979.Hydraulic conductivity and flow in non‐uniform soil.Conf. Proc. Workshop on Soil Physics and Field Heterogeneity CSIROCanberra Australia.",{},{"id":28,"text":2022,"url":28,"identifiers":2023},"10.1097\u002F00010694-198302000-00007",{"doi":2022},{"id":28,"text":2025,"url":28,"identifiers":2026},"Rawls W.J., 1992, Indirect methods for estimating the hydraulic properties of unsaturated soils, 329",{},{"id":28,"text":2028,"url":28,"identifiers":2029},"Rawls W.J., 1992, Handbook of hydrology, 5.1",{},{"id":28,"text":2031,"url":28,"identifiers":2032},"10.13031\u002F2013.33720",{"doi":2031},{"id":28,"text":2034,"url":28,"identifiers":2035},"10.13031\u002F2013.17270",{"doi":2034},{"id":28,"text":2037,"url":28,"identifiers":2038},"10.1097\u002F00010694-200207000-00001",{"doi":2037},{"id":28,"text":2040,"url":28,"identifiers":2041},"10.1016\u002FS0016-7061(03)00094-6",{"doi":2040},{"id":28,"text":2043,"url":28,"identifiers":2044},"Saxton K.E., 1986, Estimating generalized soil water characteristics from texture, Trans. ASAE, 50, 1031",{},{"id":28,"text":2046,"url":28,"identifiers":2047},"Saxton K.E. andP.H.Willey.1999.Agricultural wetland and pond hydrologic calculations using the SPAW‐II Model.Conf. Proc. ASAE. Toronto ON 18–21 July 1999.ASAE St. Joseph MI.",{},{"id":28,"text":2049,"url":28,"identifiers":2050},"Saxton K.E. andP.H.Willey.2004.Agricultural wetland and pond hydrologic analyses using the SPAW model.Conf. Proc. Self‐sustaining solutions for streams watersheds and wetlands 12–15 Sept. 2004 ASAE.St. Joseph MI.",{},{"id":28,"text":2052,"url":28,"identifiers":2053},"Saxton K.E., 2006, Watershed models, 401",{},{"id":28,"text":2055,"url":28,"identifiers":2056},"10.2136\u002Fsssaj1998.03615995006200040001x",{"doi":2055},{"id":28,"text":2058,"url":28,"identifiers":2059},"Soil Survey Staff, 2004, National soil characterization data",{},{"id":28,"text":2061,"url":28,"identifiers":2062},"10.2136\u002Fsssaj1994.03615995005800060002x",{"doi":2061},{"id":28,"text":2064,"url":28,"identifiers":2065},"Tanji K.K., 1990, Agricultural salinity assessment and management",{},{"id":28,"text":2067,"url":28,"identifiers":2068},"USDA‐SCS.1982.Procedures for collecting soil samples and methods of analysis for soil survey.Soil Survey Investigations Report I Washington DC.",{},{"id":28,"text":961,"url":28,"identifiers":2070},{"doi":961},{"id":28,"text":2072,"url":28,"identifiers":2073},"Van Genuchten M.Th., 1992, Indirect methods for estimating the hydraulic properties of unsaturated soils, 1",{},{"id":28,"text":2075,"url":28,"identifiers":2076},"10.1097\u002F00010694-198912000-00001",{"doi":2075},{"id":28,"text":2078,"url":28,"identifiers":2079},"10.1097\u002F00010694-199203000-00002",{"doi":2078},{"id":28,"text":2081,"url":28,"identifiers":2082},"10.1071\u002FSR9830015",{"doi":2081},{"id":2084,"createTime":2085,"updateTime":2086,"relativeEntities":2087,"slug":2088,"properties":2089,"entityType":962,"verifyStatus":26,"verifyTime":2103,"verifyNote":963,"languages":2104,"translateLanguages":2105,"viewCount":32,"primaryUrl":2106,"fullTextUrl":28,"authors":2107,"publicationType":987,"publisherRelationship":2123,"citationCount":2168,"citationInfo":2169,"publishDate":2175,"publishYear":2170,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":2176,"openAccess":28,"references":2177,"isForceReanalyzing":1054},"02c0c87f-3629-46da-9755-26e650e7eea7","2024-09-21T10:24:51.129+00:00","2025-01-08T03:16:47.508+00:00",[],"Aggregate-Structure-and-Carbon-Nitrogen-and-Phosphorus-in-Native-and-Cultivated-Soils",{"openalex":2090,"mag":2092,"abstract":2094,"title":2097,"keywords":2100,"doi":2101},{"VOID":2091},"W2072627116",{"VOID":2093},"2072627116",{"VI":2095,"EN":2096},"\u003Cjats:title>Tóm tắt\u003C\u002Fjats:title>\u003Cjats:p>Công trình này bổ trợ mô hình khái niệm phân lớp về cấu trúc tập hợp đất đã được Tisdall và Oades (1982) trình bày, mở rộng nó ra thực tiễn đất cỏ ở Bắc Mỹ, và làm rõ những khía cạnh liên quan đến ảnh hưởng của canh tác lên việc mất mát chất hữu cơ trong đất. Phân bố kích thước tập hợp quan sát được cho các loại đất của chúng tôi rất giống với những loại đất ở Úc, chỉ ra rằng mô hình vi tập hợp - đại tập hợp có thể áp dụng cho nhiều loại đất cỏ trên toàn thế giới. Việc sử dụng hai phương pháp tưới nước trước khi rây cho thấy đất sod tự nhiên có các đặc tính cấu trúc chung tương tự như đất canh tác nhưng các đại tập hợp thì ổn định hơn. Khi bị nở ra, đất tự nhiên và đất canh tác thuộc các kích thước vi tập hợp có ít C hữu cơ, N và P hơn so với đất còn lại ở dạng đại tập hợp, ngay cả khi được biểu diễn trên cơ sở không có cát. Hơn nữa, tỷ lệ C\u002FN, C\u002FP và N\u002FP của vi tập hợp hẹp hơn so với các kích thước đại tập hợp. Có sự mất mát C và N nhiều hơn P trong điều kiện của nghiên cứu này. Sự khác biệt theo yếu tố trong các quá trình chuyển hóa vi sinh vật so với hoạt động enzym ngoại bào và sự kiểm soát phản hồi đi kèm được suy diễn để giải thích cho sự khác biệt này. Khi các đại tập hợp bị nghiền nát đến kích thước của các vi tập hợp, C có thể khoáng hóa tính theo phần trăm tổng C hữu cơ thường lớn hơn cho các đại tập hợp so với vi tập hợp vào giai đoạn đầu của quá trình ủ trong đất canh tác, và trong suốt thời gian ủ cho đất sod tự nhiên. N có thể khoáng hóa tính theo phần trăm tổng N hữu cơ lớn nhất trong các đại tập hợp ngay cả khi các đại tập hợp không bị nghiền nát. Mô hình khái niệm đại tập hợp - vi tập hợp được áp dụng để giúp giải thích sự tích lũy chất hữu cơ trong đất trong điều kiện tự nhiên và sự mất mát của nó khi canh tác.\u003C\u002Fjats:p>","\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:p>This work corroborates the hierarchical conceptual model for soil aggregate structure presented by Tisdall and Oades (1982), extends it to North American grassland soils, and elaborates on the aspects relating to the influence of cultivation upon losses of soil organic matter. Aggregate size distributions observed for our soils are very similar to those of Australian soils, indicating that the microaggregate‐macroaggregate model may hold for a wide array of grassland soils from around the world. The use of two wetting treatments prior to sieving demonstrated that the native sod soil had the same general structural characteristics as cultivated soil but the macroaggregates were more stable. When slaked, native and cultivated soil present in the microaggregate size classes had less organic C, N, and P than the soil remaining as macroaggregates, even when expressed on a sand‐free basis. Moreover, the C\u002FN, C\u002FP, and N\u002FP ratios of microaggregates were narrower than those of macroaggregate size classes. Much more C and N was lost than P under the conditions of this study. Element‐specific differences in microbial catabolic processes vs. extracellular enzyme activity and its attendant feedback controls are postulated to account for this difference. When the macroaggregates were crushed to the size of microaggregates, mineralizable C as a percent of the total organic C was generally greater for macro‐ than microaggregates early in the incubation for the cultivated soil and throughout most of the incubation for the native sod soil. Mineralizable N as a percent of the total organic N was greatest in macroaggregates even when the macroaggregates were not crushed. The macroaggregate‐micraggregate conceptual model is applied to help explain accumulation of soil organic matter under native conditions and its loss upon cultivation.\u003C\u002Fjats:p>",{"EN":2098,"VI":2099},"Aggregate Structure and Carbon, Nitrogen, and Phosphorus in Native and Cultivated Soils","Cấu trúc Tập hợp và Carbon, Nitơ, và Phốt pho trong Đất Bản địa và Đất Canh tác",{"VI":1190},{"VOID":2102},"10.2136\u002Fsssaj1986.03615995005000030017x","2024-09-21T10:24:51.128+00:00",[31],[30],"https:\u002F\u002Facsess.onlinelibrary.wiley.com\u002Fdoi\u002F10.2136\u002Fsssaj1986.03615995005000030017x",[2108],{"id":2109,"sortIndex":32,"researcher":28,"roles":2110,"affiliations":2111,"properties":2120,"displayName":1677,"givenName":28,"familyName":28},"898c085d-75e2-4936-9a3a-c161d025bf43",[],[2112],{"id":2113,"sortIndex":32,"affiliation":2114,"properties":28},"9c5633cd-0971-487f-8c84-048a3ec8d1d1",{"id":2113,"createTime":28,"updateTime":28,"relativeEntities":2115,"slug":28,"properties":2116,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2119,"statistic":28},[],{"title":2117},{"EN":2118},"Research Ecologist, Natural Resource Ecology Lab., Colorado State Univ., Fort Collins, CO 80523.",[],{"title":2121,"openalex":2122},{"EN":1677},{"VOID":1679},{"url":28,"publisher":2124,"properties":2162},{"id":868,"createTime":869,"updateTime":870,"relativeEntities":2125,"slug":872,"properties":2126,"entityType":25,"verifyStatus":884,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":32,"subjectFields":2131,"manageAffiliations":2136,"indexDatabases":2147,"url":936,"thumbnailPath":28,"statistic":28,"gsStatistic":28,"type":28,"analyzePriority":28},[],{"country":2127,"eissn":2128,"issn":2129,"title":2130},{"VOID":875},{"VOID":877},{"VOID":879},{"EN":881},[2132],{"id":887,"createTime":28,"updateTime":28,"relativeEntities":2133,"label":2134,"description":2135,"parentId":28,"standard":28,"scholarHubFieldId":28},[],{"EN":890},{},[2137,2142],{"id":894,"createTime":28,"updateTime":28,"relativeEntities":2138,"slug":28,"properties":2139,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2141,"statistic":28},[],{"title":2140},{"EN":898},[],{"id":901,"createTime":28,"updateTime":28,"relativeEntities":2143,"slug":28,"properties":2144,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2146,"statistic":28},[],{"title":2145},{"EN":905},[],[2148,2155],{"id":909,"indexDatabase":2149,"url":921,"indexYears":28,"academicFieldIds":2154,"indexDatabaseRanking":28},{"id":911,"createTime":28,"updateTime":28,"relativeEntities":2150,"label":2151,"description":2152,"key":918,"publicationTags":2153,"standard":28},[],{"EN":914,"VI":914},{"EN":916,"VI":917},[920,813],[923],{"id":925,"indexDatabase":2156,"url":931,"indexYears":932,"academicFieldIds":2161,"indexDatabaseRanking":935},{"id":775,"createTime":28,"updateTime":28,"relativeEntities":2157,"label":2158,"description":2159,"key":781,"publicationTags":2160,"standard":28},[],{"EN":778,"VI":778},{"EN":778,"VI":780},[783],[934],{"issue":2163,"pages":2164,"volume":2166},{"VOID":1148},{"VOID":2165},"627-633",{"VOID":2167},"50",2169,{"total":2168,"publishYear":2170,"statisticByYear":2171},1986,{"2012":564,"2013":566,"2014":2172,"2015":522,"2016":428,"2017":2172,"2018":209,"2019":2173,"2020":153,"2021":1290,"2022":1290,"2023":2174,"2024":43},87,121,139,"1986-05-01",[920,935],[],{"id":2179,"createTime":2180,"updateTime":2180,"relativeEntities":2181,"slug":2182,"properties":2183,"entityType":962,"verifyStatus":26,"verifyTime":2194,"verifyNote":963,"languages":2195,"translateLanguages":28,"viewCount":32,"primaryUrl":2196,"fullTextUrl":28,"authors":2197,"publicationType":987,"publisherRelationship":2234,"citationCount":2279,"citationInfo":2280,"publishDate":2285,"publishYear":2281,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":2286,"openAccess":28,"references":2287,"isForceReanalyzing":1054},"69ca93d7-6d74-4d09-8adc-3d464c27bc6c","2024-09-04T21:27:59.721+00:00",[],"Soil-Organic-Carbon-Sequestration-Rates-by-Tillage-and-Crop-Rotation",{"openalex":2184,"mag":2186,"abstract":2188,"title":2190,"doi":2192},{"VOID":2185},"W136628441",{"VOID":2187},"136628441",{"EN":2189},"\u003Cjats:p>Changes in agricultural management can potentially increase the accumulation rate of soil organic C (SOC), thereby sequestering CO\u003Cjats:sub>2\u003C\u002Fjats:sub> from the atmosphere. This study was conducted to quantify potential soil C sequestration rates for different crops in response to decreasing tillage intensity or enhancing rotation complexity, and to estimate the duration of time over which sequestration may occur. Analyses of C sequestration rates were completed using a global database of 67 long‐term agricultural experiments, consisting of 276 paired treatments. Results indicate, on average, that a change from conventional tillage (CT) to no‐till (NT) can sequester 57 ± 14 g C m\u003Cjats:sup>−2\u003C\u002Fjats:sup> yr\u003Cjats:sup>−1\u003C\u002Fjats:sup>, excluding wheat (\u003Cjats:italic>Triticum aestivum\u003C\u002Fjats:italic> L.)‐fallow systems which may not result in SOC accumulation with a change from CT to NT. Enhancing rotation complexity can sequester an average 20 ± 12 g C m\u003Cjats:sup>−2\u003C\u002Fjats:sup> yr\u003Cjats:sup>−1\u003C\u002Fjats:sup>, excluding a change from continuous corn (\u003Cjats:italic>Zea mays\u003C\u002Fjats:italic> L.) to corn‐soybean (\u003Cjats:italic>Glycine max\u003C\u002Fjats:italic> L.) which may not result in a significant accumulation of SOC. Carbon sequestration rates, with a change from CT to NT, can be expected to peak in 5 to 10 yr with SOC reaching a new equilibrium in 15 to 20 yr. Following initiation of an enhancement in rotation complexity, SOC may reach a new equilibrium in approximately 40 to 60 yr. Carbon sequestration rates, estimated for a number of individual crops and crop rotations in this study, can be used in spatial modeling analyses to more accurately predict regional, national, and global C sequestration potentials.\u003C\u002Fjats:p>",{"EN":2191},"Soil Organic Carbon Sequestration Rates by Tillage and Crop Rotation",{"VOID":2193},"10.2136\u002Fsssaj2002.1930","2024-09-04T21:27:59.720+00:00",[31],"https:\u002F\u002Facsess.onlinelibrary.wiley.com\u002Fdoi\u002F10.2136\u002Fsssaj2002.1930",[2198,2217],{"id":2199,"sortIndex":32,"researcher":28,"roles":2200,"affiliations":2201,"properties":2210,"displayName":2214,"givenName":28,"familyName":28},"fc468370-daa2-4f02-88f9-5ac8f27e9840",[],[2202],{"id":2203,"sortIndex":32,"affiliation":2204,"properties":28},"3ea036c8-bb97-4d63-b42f-513536757316",{"id":2203,"createTime":28,"updateTime":28,"relativeEntities":2205,"slug":28,"properties":2206,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2209,"statistic":28},[],{"title":2207},{"EN":2208},"Environmental Sciences Division Oak Ridge National Lab. 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