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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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We use satellite imagery (Advanced Very High Resolution Radiometer and International Satellite Cloud Climatology Project solar radiation), along with historical climate (monthly temperature and precipitation) and soil attributes (texture, C and N contents) from global (1°) data sets as model inputs. The Carnegie‐Ames‐Stanford approach (CASA) Biosphere model runs on a monthly time interval to simulate seasonal patterns in net plant carbon fixation, biomass and nutrient allocation, litterfall, soil nitrogen mineralization, and microbial CO\u003Cjats:sub>2\u003C\u002Fjats:sub> production. The model estimate of global terrestrial net primary production is 48 Pg C yr\u003Cjats:sup>−1\u003C\u002Fjats:sup> with a maximum light use efficiency of 0.39 g C MJ\u003Cjats:sup>−1\u003C\u002Fjats:sup>PAR. Over 70% of terrestrial net production takes place between 30°N and 30°S latitude. Steady state pools of standing litter represent global storage of around 174 Pg C (94 and 80 Pg C in nonwoody and woody pools, respectively), whereas the pool of soil C in the top 0.3 m that is turning over on decadal time scales comprises 300 Pg C. Seasonal variations in atmospheric CO\u003Cjats:sub>2\u003C\u002Fjats:sub> concentrations from three stations in the Geophysical Monitoring for Climate Change Flask Sampling Network correlate significantly with estimated net ecosystem production values averaged over 50°–80° N, 10°–30° N, and 0°–10° N.\u003C\u002Fjats:p>",{"EN":1670},"Terrestrial ecosystem production: A process model based on global satellite and surface data",{"VOID":1672},"10.1029\u002F93gb02725","Author affiliation is blank",[31],"https:\u002F\u002Fagupubs.onlinelibrary.wiley.com\u002Fdoi\u002F10.1029\u002F93GB02725",[1677,1688,1699,1710,1721,1732,1743],{"id":1678,"sortIndex":32,"researcher":28,"roles":1679,"affiliations":1680,"properties":1681,"displayName":1685,"givenName":28,"familyName":28},"81d9ba25-e813-4885-bd0c-d024e0950153",[],[],{"orcid":1682,"title":1684,"openalex":1686},{"VOID":1683},"https:\u002F\u002Forcid.org\u002F0000-0002-8949-6182",{"EN":1685},"Christopher Potter",{"VOID":1687},"A5041666616",{"id":1689,"sortIndex":40,"researcher":28,"roles":1690,"affiliations":1691,"properties":1692,"displayName":1696,"givenName":28,"familyName":28},"706b67ec-117c-4ace-a9ea-b25dca1a5f8e",[],[],{"orcid":1693,"title":1695,"openalex":1697},{"VOID":1694},"https:\u002F\u002Forcid.org\u002F0000-0001-6559-7387",{"EN":1696},"James T. 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K.Sebastian andS. J.Scherr(2000) Pilot analysis of global ecosystems: Agroecosystems 110 pp Int. Food Policy Res. Inst. and World Resour. Inst. Washington D. C.",{},{"id":28,"text":2532,"url":28,"identifiers":2533},"10.1002\u002Fhyp.1441",{"doi":2532},{"id":2535,"createTime":2536,"updateTime":2536,"relativeEntities":2537,"slug":2538,"properties":2539,"entityType":1049,"verifyStatus":26,"verifyTime":2536,"verifyNote":1050,"languages":2550,"translateLanguages":28,"viewCount":32,"primaryUrl":2551,"fullTextUrl":28,"authors":2552,"publicationType":1089,"publisherRelationship":2943,"citationCount":976,"citationInfo":3005,"publishDate":3008,"publishYear":3006,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":3009,"openAccess":28,"references":3010,"isForceReanalyzing":1656},"69d48fe5-76d8-40a6-9a45-aaf5225b1938","2024-10-03T08:44:15.688+00:00",[],"The-atmospheric-input-of-trace-species-to-the-world-ocean",{"openalex":2540,"mag":2542,"abstract":2544,"title":2546,"doi":2548},{"VOID":2541},"W2142180479",{"VOID":2543},"2142180479",{"EN":2545},"\u003Cjats:p>Over the past decade it has become apparent that the atmosphere is a significant pathway for the transport of many natural and pollutant materials from the continents to the ocean. The atmospheric input of many of these species can have an impact (either positive or negative) on biological processes in the sea and on marine chemical cycling. For example, there is now evidence that the atmosphere may be an important transport path for such essential nutrients as iron and nitrogen in some regions. In this report we assess current data in this area, develop global scale estimates of the atmospheric fluxes of trace elements, mineral aerosol, nitrogen species, and synthetic organic compounds to the ocean; and compare the atmospheric input rates of these substances to their input via rivers. Trace elements considered were Pb, Cd, Zn, Cu, Ni, As, Hg, Sn, Al, Fe, Si, and P. Oxidized and reduced forms of nitrogen were considered, including nitrate and ammonium ions and the gaseous species NO, NO\u003Cjats:sub>2\u003C\u002Fjats:sub>, HNO\u003Cjats:sub>3\u003C\u002Fjats:sub>, and NH\u003Cjats:sub>3\u003C\u002Fjats:sub>. Synthetic organic compounds considered included polychlorinated biphenyls (PCBs), hexachlorocyclohexanes (HCHs), DDTs, chlordane, dieldrin, and hexachlorobenzenes (HCBs). Making this assessment was difficult because there are very few actual measurements of deposition rates of these substances to the ocean. However, there are considerably more data on the atmospheric concentrations of these species in aerosol and gaseous form. Mean concentration data for 10° × 10° ocean areas were determined from the available concentration data or from extrapolation of these data into other regions. These concentration distributions were then combined with appropriate exchange coefficients and precipitation fields to obtain the global wet and dry deposition fluxes. Careful consideration was given to atmospheric transport processes as well as to removal mechanisms and the physical and physicochemical properties of aerosols and gases. Only annual values were calculated. On a global scale atmospheric inputs are generally equal to or greater than riverine inputs, and for most species atmospheric input to the ocean is significantly greater in the northern hemisphere than in the southern hemisphere. For dissolved trace metals in seawater, global atmospheric input dominates riverine input for Pb, Cd, and Zn, and the two transport paths are roughly equal for Cu, Ni, As, and Fe. Fluxes and basin‐wide deposition of trace metals are generally a factor of 5‐10 higher in the North Atlantic and North Pacific regions than in the South Atlantic and South Pacific. Global input of oxidized and reduced nitrogen species are roughly equal to each other, although the major fraction of oxidized nitrogen enters the ocean in the northern hemisphere, primarily as a result of pollution sources. Reduced nitrogen species are much more uniformly distributed, suggesting that the ocean itself may be a significant source. The global atmospheric input of such synthetic organic species as HCH,PCBs, DDT, and HCB completely dominates their input via rivers.\u003C\u002Fjats:p>",{"EN":2547},"The atmospheric input of trace species to the world ocean",{"VOID":2549},"10.1029\u002F91gb01778",[31],"https:\u002F\u002Fagupubs.onlinelibrary.wiley.com\u002Fdoi\u002F10.1029\u002F91GB01778",[2553,2572,2591,2608,2627,2644,2663,2680,2699,2714,2733,2748,2767,2784,2801,2820,2839,2858,2875,2890,2907,2924],{"id":2554,"sortIndex":32,"researcher":28,"roles":2555,"affiliations":2556,"properties":2565,"displayName":2569,"givenName":28,"familyName":28},"6f5a8ab5-58d0-4568-8013-d6217d26b8a8",[],[2557],{"id":2558,"sortIndex":32,"affiliation":2559,"properties":28},"4cde6a96-81fc-4063-9737-7dda589b5224",{"id":2558,"createTime":28,"updateTime":28,"relativeEntities":2560,"slug":28,"properties":2561,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":2564,"statistic":28},[],{"title":2562},{"EN":2563},"URI - University of Rhode Island (45 Upper College Rd, Kingston, RI 02881, USA - United States)",[],{"orcid":2566,"title":2568,"openalex":2570},{"VOID":2567},"https:\u002F\u002Forcid.org\u002F0000-0001-5939-8277",{"EN":2569},"Robert A. 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M., 1981, The Oceanic Lithosphere, 801",{},{"id":28,"text":3593,"url":28,"identifiers":3594},"10.1007\u002F978-94-009-0503-0_4",{"doi":3593},{"id":28,"text":3596,"url":28,"identifiers":3597},"10.1038\u002F339687a0",{"doi":3596},{"id":28,"text":3599,"url":28,"identifiers":3600},"10.1029\u002FJD090iD06p10586",{"doi":3599},{"id":28,"text":3602,"url":28,"identifiers":3603},"10.1029\u002FJD092iD12p14723",{"doi":3602},{"id":28,"text":3605,"url":28,"identifiers":3606},"Prospero J. M., 1989, Chemical Oceanography, 188",{},{"id":28,"text":3608,"url":28,"identifiers":3609},"Pszenny A. A. P. Atmospheric deposition of nitrate to the ocean surface Ph.D. thesis Univ. of R. I. Kingston 1987.",{},{"id":28,"text":3611,"url":28,"identifiers":3612},"10.3402\u002Ftellusb.v39i5.15359",{"doi":3611},{"id":28,"text":3614,"url":28,"identifiers":3615},"10.1038\u002F335336a0",{"doi":3614},{"id":28,"text":3617,"url":28,"identifiers":3618},"10.1029\u002FJD095iD10p16405",{"doi":3617},{"id":28,"text":3620,"url":28,"identifiers":3621},"Rahn K. The chemical composition of the atmospheric aerosol technical report 265Grad. Sch. of Oceanogr. Univ. R. I. Kingston 1976.",{},{"id":28,"text":3623,"url":28,"identifiers":3624},"10.1021\u002Fes00173a011",{"doi":3623},{"id":28,"text":3626,"url":28,"identifiers":3627},"10.1016\u002F0045-6535(85)90138-9",{"doi":3626},{"id":28,"text":3629,"url":28,"identifiers":3630},"Ray P. K., 1985, Pesticides‐Major environmental problem, Sci. Cult., 51, 363",{},{"id":28,"text":3632,"url":28,"identifiers":3633},"Reinhardt K. H. 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C.Parker 63–78Allen Press Lawrence Kansas 1972.",{},{"id":28,"text":3653,"url":28,"identifiers":3654},"10.1007\u002F978-94-009-5476-2_7",{"doi":3653},{"id":28,"text":3656,"url":28,"identifiers":3657},"10.1007\u002F978-1-4684-5215-0_10",{"doi":3656},{"id":28,"text":3659,"url":28,"identifiers":3660},"10.1029\u002FJD092iD06p06653",{"doi":3659},{"id":28,"text":3662,"url":28,"identifiers":3663},"Ryaboshapko A. G. V. I.Lepeskin E. D.Podgurskaya V. I.Medinets Air pollution monitoring over the North Atlantic Proceedings of the International Symposium on Integrated Global Monitoring of the State of the Biosphere 2WMO\u002FTD 151 261–282World Meteorol. Organ. Geneva 1986.",{},{"id":28,"text":3665,"url":28,"identifiers":3666},"Savoie D. Nitrate and non‐sea‐salt sulfate aerosols over major regions of the world ocean: Concentration sources and fluxes Ph.D. thesis Univ. of Miami Coral Gables Fla. 1984.",{},{"id":28,"text":3668,"url":28,"identifiers":3669},"10.1029\u002FGL009i010p01207",{"doi":3668},{"id":28,"text":3671,"url":28,"identifiers":3672},"Savoie D. L. J. M.Prospero Nitrate and non‐seasalt sulfate concentrations at BermudaWATOX workshopBermuda Biological Station for ResearchFerry Reach Bermuda 1983.",{},{"id":28,"text":3674,"url":28,"identifiers":3675},"10.1029\u002FJD092iD01p00933",{"doi":3674},{"id":28,"text":3677,"url":28,"identifiers":3678},"10.1007\u002FBF00052712",{"doi":3677},{"id":28,"text":3680,"url":28,"identifiers":3681},"Savoie D. L., 1989, Chemical Oceanography, 220",{},{"id":28,"text":3683,"url":28,"identifiers":3684},"Schaug J. J. E.Hansen K.Nodop B.Ottar J. 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Polar Res., 44, 167",{},{"id":28,"text":3745,"url":28,"identifiers":3746},"10.1016\u002F0269-7491(87)90166-7",{"doi":3745},{"id":28,"text":3748,"url":28,"identifiers":3749},"10.1007\u002F978-1-4612-3850-8_1",{"doi":3748},{"id":28,"text":3751,"url":28,"identifiers":3752},"10.1021\u002Fes00151a005",{"doi":3751},{"id":28,"text":3754,"url":28,"identifiers":3755},"10.1029\u002FJD091iD04p05173",{"doi":3754},{"id":28,"text":3757,"url":28,"identifiers":3758},"10.1029\u002FJD095iD06p07553",{"doi":3757},{"id":28,"text":3760,"url":28,"identifiers":3761},"10.1016\u002F0269-7491(88)90183-2",{"doi":3760},{"id":28,"text":3763,"url":28,"identifiers":3764},"10.1007\u002FBF02070335",{"doi":3763},{"id":28,"text":3766,"url":28,"identifiers":3767},"Tanabe S., 1983, Proceedings of BIOMASS Colloquium in 1982, 64",{},{"id":28,"text":3769,"url":28,"identifiers":3770},"Tanabe S., 1986, PCB's and the Environment",{},{"id":28,"text":3772,"url":28,"identifiers":3773},"Tanabe S., 1982, Chlorinated hydrocarbons in the Antarctic, western Pacific and eastern Indian oceans, Trans. Tokyo Univ. Fish., 5, 97",{},{"id":28,"text":3775,"url":28,"identifiers":3776},"10.1007\u002FBF02110285",{"doi":3775},{"id":28,"text":3778,"url":28,"identifiers":3779},"10.1016\u002F0045-6535(83)90171-6",{"doi":3778},{"id":28,"text":3781,"url":28,"identifiers":3782},"10.1016\u002F0045-6535(83)90132-7",{"doi":3781},{"id":28,"text":3784,"url":28,"identifiers":3785},"Tateya S., 1988, Toxic Contaminants in Large Lakes, 237",{},{"id":28,"text":3787,"url":28,"identifiers":3788},"Tatsukawa R., 1990, Oceanic Processes in Marine Pollution, 39",{},{"id":28,"text":3790,"url":28,"identifiers":3791},"Taylor G. S., 1983, The Major Biogeochemical Cycles and Their Interactions, SCOPE, 115",{},{"id":28,"text":3793,"url":28,"identifiers":3794},"Taylor S. R., 1985, The Continental Crust: Its Composition and Evolution",{},{"id":28,"text":3796,"url":28,"identifiers":3797},"10.1029\u002FJC087iC11p08870",{"doi":3796},{"id":28,"text":3799,"url":28,"identifiers":3800},"10.1007\u002FBF02109036",{"doi":3799},{"id":28,"text":3802,"url":28,"identifiers":3803},"10.1007\u002FBF00058712",{"doi":3802},{"id":28,"text":3805,"url":28,"identifiers":3806},"10.1146\u002Fannurev.ea.05.050177.001303",{"doi":3805},{"id":28,"text":3808,"url":28,"identifiers":3809},"10.1029\u002FJC088iC09p05411",{"doi":3808},{"id":28,"text":3811,"url":28,"identifiers":3812},"Turekian K. K., 1989, Chemical Oceanography, 51",{},{"id":28,"text":3814,"url":28,"identifiers":3815},"Unified Deposition Data Base Committee (UDDBC), 1986, A unified wet deposition data base for eastern North America: Addendum with results for sulfates and nitrates (1980–1983)",{},{"id":28,"text":3817,"url":28,"identifiers":3818},"10.1029\u002FJC088iC09p05343",{"doi":3817},{"id":28,"text":3820,"url":28,"identifiers":3821},"10.1007\u002FBF00049372",{"doi":3820},{"id":28,"text":3823,"url":28,"identifiers":3824},"Van Bennekom A. J., 1979, River Input to the Ocean System, 33",{},{"id":28,"text":3826,"url":28,"identifiers":3827},"10.1029\u002FGL014i007p00711",{"doi":3826},{"id":28,"text":3829,"url":28,"identifiers":3830},"Veron A. Dynamique du transfert du plomb dans rocean Atlantique nord‐est depuis l'atmosphere jusqu'au sediment These Docteur en Sciences Univ. Paris‐Sud France 1988.",{},{"id":28,"text":3832,"url":28,"identifiers":3833},"Vet R. J. W. B.Sukloff M. E.Still R.Gilbert Canadian Air and Precipitation Network (CAPMoN) precipitation chemistry data summary 1983–1984Report AQRB‐86‐001‐M 544Atmo. Environ. Serv. Downsview Ont. Canada 1986.",{},{"id":28,"text":3835,"url":28,"identifiers":3836},"10.1016\u002F0045-6535(86)90562-X",{"doi":3835},{"id":28,"text":3838,"url":28,"identifiers":3839},"10.1029\u002FJD095iD12p20623",{"doi":3838},{"id":28,"text":3841,"url":28,"identifiers":3842},"10.1016\u002F0004-6981(88)90347-2",{"doi":3841},{"id":28,"text":3844,"url":28,"identifiers":3845},"10.2307\u002F1351969",{"doi":3844},{"id":28,"text":3847,"url":28,"identifiers":3848},"10.1111\u002Fj.1600-0889.1988.tb00114.x",{"doi":3847},{"id":28,"text":3850,"url":28,"identifiers":3851},"10.1029\u002FGL003i007p00375",{"doi":3850},{"id":28,"text":3853,"url":28,"identifiers":3854},"10.1029\u002FJD093iD07p08339",{"doi":3853},{"id":28,"text":3856,"url":28,"identifiers":3857},"10.1126\u002Fscience.227.4691.1224",{"doi":3856},{"id":28,"text":3859,"url":28,"identifiers":3860},"Warneck P., 1988, Chemistry of the Natural Atmosphere",{},{"id":28,"text":3862,"url":28,"identifiers":3863},"10.1038\u002F349145a0",{"doi":3862},{"id":28,"text":3865,"url":28,"identifiers":3866},"10.1029\u002FJD089iD07p11607",{"doi":3865},{"id":28,"text":3868,"url":28,"identifiers":3869},"Wells D. E., 1978, The occurrence of organochlorine residues in rainwaters, Water Air Soil Pollut., 9, 271, 10.1007\u002FBF00280675",{"doi":3870},"10.1007\u002FBF00280675",{"id":28,"text":3872,"url":28,"identifiers":3873},"10.1007\u002F978-94-009-0503-0_2",{"doi":3872},{"id":28,"text":3875,"url":28,"identifiers":3876},"10.1029\u002FGB001i004p00357",{"doi":3875},{"id":28,"text":3878,"url":28,"identifiers":3879},"10.1016\u002F0272-7714(85)90084-8",{"doi":3878},{"id":28,"text":3881,"url":28,"identifiers":3882},"10.1016\u002F0004-6981(86)90158-7",{"doi":3881},{"id":28,"text":3884,"url":28,"identifiers":3885},"10.1080\u002F00022470.1986.10466094",{"doi":3884},{"id":28,"text":3887,"url":28,"identifiers":3888},"Wollast R., 1981, Some Perspectives of the Major Biogeochemical Cycles, 125",{},{"id":28,"text":3890,"url":28,"identifiers":3891},"Wollast R., 1983, The Major Biogeochemical Cycles and Their Interactions, SCOPE, 385",{},{"id":28,"text":3893,"url":28,"identifiers":3894},"10.1007\u002F978-94-009-5333-8_5",{"doi":3893},{"id":28,"text":3896,"url":28,"identifiers":3897},"10.1021\u002Fes00098a003",{"doi":3896},{"id":28,"text":3899,"url":28,"identifiers":3900},"10.1029\u002FJC086iC04p03173",{"doi":3899},{"id":28,"text":3902,"url":28,"identifiers":3903},"10.1029\u002FJD090iD01p02409",{"doi":3902},{"id":28,"text":3905,"url":28,"identifiers":3906},"10.1029\u002FJC095iC09p16207",{"doi":3905},{"id":3908,"createTime":3909,"updateTime":3909,"relativeEntities":3910,"slug":3911,"properties":3912,"entityType":1049,"verifyStatus":26,"verifyTime":3909,"verifyNote":1050,"languages":3923,"translateLanguages":28,"viewCount":32,"primaryUrl":3924,"fullTextUrl":28,"authors":3925,"publicationType":1089,"publisherRelationship":4102,"citationCount":4161,"citationInfo":4162,"publishDate":4168,"publishYear":4163,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":4169,"openAccess":28,"references":4170,"isForceReanalyzing":1656},"e03f6066-dea5-4aea-baa9-7cca8f049646","2024-11-25T22:15:07.885+00:00",[],"A-global-ocean-carbon-climatology-Results-from-Global-Data-Analysis-Project-GLODAP-",{"openalex":3913,"mag":3915,"abstract":3917,"title":3919,"doi":3921},{"VOID":3914},"W1609491364",{"VOID":3916},"1609491364",{"EN":3918},"\u003Cjats:p>During the 1990s, ocean sampling expeditions were carried out as part of the World Ocean Circulation Experiment (WOCE), the Joint Global Ocean Flux Study (JGOFS), and the Ocean Atmosphere Carbon Exchange Study (OACES). Subsequently, a group of U.S. scientists synthesized the data into easily usable and readily available products. This collaboration is known as the Global Ocean Data Analysis Project (GLODAP). Results were merged into a common format data set, segregated by ocean. For comparison purposes, each ocean data set includes a small number of high‐quality historical cruises. The data were subjected to rigorous quality control procedures to eliminate systematic data measurement biases. The calibrated 1990s data were used to estimate anthropogenic CO\u003Cjats:sub>2\u003C\u002Fjats:sub>, potential alkalinity, CFC watermass ages, CFC partial pressure, bomb‐produced radiocarbon, and natural radiocarbon. These quantities were merged into the measured data files. The data were used to produce objectively gridded property maps at a 1° resolution on 33 depth surfaces chosen to match existing climatologies for temperature, salinity, oxygen, and nutrients. The mapped fields are interpreted as an annual mean distribution in spite of the inaccuracy in that assumption. Both the calibrated data and the gridded products are available from the Carbon Dioxide Information Analysis Center. 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The estimated global emission for 1990 is about 54 Tg N yr\u003Cjats:sup>−1\u003C\u002Fjats:sup>. The major sources identified include excreta from domestic animals (21.6 Tg N yr\u003Cjats:sup>−1\u003C\u002Fjats:sup>) and wild animals (0.1 Tg N yr\u003Cjats:sup>−1\u003C\u002Fjats:sup>), use of synthetic N fertilizers (9.0 Tg N yr\u003Cjats:sup>−1\u003C\u002Fjats:sup>), oceans (8.2 Tg N yr\u003Cjats:sup>−1\u003C\u002Fjats:sup>), biomass burning (5.9 Tg N yr\u003Cjats:sup>−1\u003C\u002Fjats:sup>), crops (3.6 Tg N yr\u003Cjats:sup>−1\u003C\u002Fjats:sup>), human population and pets (2.6 Tg N yr\u003Cjats:sup>−1\u003C\u002Fjats:sup>), soils under natural vegetation (2.4 Tg N yr\u003Cjats:sup>−1\u003C\u002Fjats:sup>), industrial processes (0.2 Tg N yr\u003Cjats:sup>−1\u003C\u002Fjats:sup>), and fossil fuels (0.1 Tg N yr\u003Cjats:sup>−1\u003C\u002Fjats:sup>). About half of the global emission comes from Asia, and about 70% is related to food production. The regions with highest emission rates are located in Europe, the Indian subcontinent, and China, reflecting the patterns of animal densities and type and intensity of synthetic fertilizer use. The overall uncertainty in the global emission estimate is 25%, while the uncertainty in regional emissions is much greater. 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C.Meiqiu W.Xiaoke Y.Heng Spatial distribution of trace gas emissions from crop residue burning in ChinaInternational Geosphere‐Biosphere Programme Scientific Advisory Committee meeting IVBeijing ChinaOctober 22–27 1995.",{},{"id":6192,"createTime":6193,"updateTime":6193,"relativeEntities":6194,"slug":6195,"properties":6196,"entityType":1049,"verifyStatus":26,"verifyTime":6193,"verifyNote":1050,"languages":6207,"translateLanguages":28,"viewCount":32,"primaryUrl":6208,"fullTextUrl":28,"authors":6209,"publicationType":1089,"publisherRelationship":6248,"citationCount":5656,"citationInfo":6309,"publishDate":6311,"publishYear":5658,"citationAnalyzeStatus":884,"lastCitationAnalyze":28,"indexDatabases":6312,"openAccess":28,"references":6313,"isForceReanalyzing":1656},"421993ce-4fda-4bde-9d9e-e301d8dd8edc","2024-08-31T04:13:13.217+00:00",[],"Global-patterns-of-marine-nitrogen-fixation-and-denitrification",{"openalex":6197,"mag":6199,"abstract":6201,"title":6203,"doi":6205},{"VOID":6198},"W2090851717",{"VOID":6200},"2090851717",{"EN":6202},"\u003Cjats:p>A new quasi‐conservative tracer \u003Cjats:italic>N*\u003C\u002Fjats:italic>, defined as a linear combination of nitrate and phosphate, is proposed to investigate the distribution of nitrogen fixation and denitrification in the world oceans. Spatial patterns of \u003Cjats:italic>N*\u003C\u002Fjats:italic> are determined in the different ocean basins using data from the Geochemical Ocean Sections Study (GEOSECS) cruises (1972–1978) and from eight additional cruises in the Atlantic Ocean. \u003Cjats:italic>N*\u003C\u002Fjats:italic> is low (< −3 µmol kg\u003Cjats:sup>−1\u003C\u002Fjats:sup>) in the Arabian Sea and in the eastern tropical North and South Pacific. This distribution is consistent with direct observations of water column denitrification in these oxygen minimum zones. Low \u003Cjats:italic>N*\u003C\u002Fjats:italic> concentrations in the Bering Sea and near the continental shelves of the east and west coasts of North America also indicate a sink of \u003Cjats:italic>N*\u003C\u002Fjats:italic> due to benthic denitrification. High concentrations of \u003Cjats:italic>N*\u003C\u002Fjats:italic> (>2.0 µmol kg\u003Cjats:sup>−1\u003C\u002Fjats:sup>) indicative of prevailing nitrogen fixation are found in the thermocline of the tropical and subtropical North Atlantic and in the Mediterranean. This suggests that on a global scale these basins are acting as sources of fixed nitrogen, while the Indian Ocean and parts of the Pacific Ocean are acting as sinks. Nitrogen fixation is estimated in the North Atlantic Ocean (10°N–50°N) using the \u003Cjats:italic>N*\u003C\u002Fjats:italic> distribution along isopycnal surfaces and information about the water age. We calculate a fixation rate of 28 Tg N yr\u003Cjats:sup>−1\u003C\u002Fjats:sup> which is about 3 times larger than the most recent global estimate. Our result is in line, however, with some recent suggestions that pelagic nitrogen fixation may be seriously underestimated. The implied flux of 0.072 mol N m\u003Cjats:sup>−2\u003C\u002Fjats:sup> yr\u003Cjats:sup>−1\u003C\u002Fjats:sup> is sufficient to meet all the nitrogen requirement of the estimated net community production in the mixed layer during summer at the Bermuda Atlantic Time‐series Study (BATS) site in the northwestern Sargasso Sea. Extrapolation of our North Atlantic estimate to the global ocean suggests that the present‐day budget of nitrogen in the ocean may be in approximate balance.\u003C\u002Fjats:p>",{"EN":6204},"Global patterns of marine nitrogen fixation and denitrification",{"VOID":6206},"10.1029\u002F97gb00077",[31],"https:\u002F\u002Fagupubs.onlinelibrary.wiley.com\u002Fdoi\u002F10.1029\u002F97GB00077",[6210,6229],{"id":6211,"sortIndex":32,"researcher":28,"roles":6212,"affiliations":6213,"properties":6222,"displayName":6226,"givenName":28,"familyName":28},"c7880eec-61df-474e-8278-37f7f7d8d005",[],[6214],{"id":6215,"sortIndex":32,"affiliation":6216,"properties":28},"525439f9-7c49-402a-91d8-987791d3034d",{"id":6215,"createTime":28,"updateTime":28,"relativeEntities":6217,"slug":28,"properties":6218,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":6221,"statistic":28},[],{"title":6219},{"EN":6220},"University of Bern",[],{"orcid":6223,"title":6225,"openalex":6227},{"VOID":6224},"https:\u002F\u002Forcid.org\u002F0000-0002-2085-2310",{"EN":6226},"Nicolas Gruber",{"VOID":6228},"A5033288125",{"id":6230,"sortIndex":40,"researcher":28,"roles":6231,"affiliations":6232,"properties":6241,"displayName":6245,"givenName":28,"familyName":28},"fe746d16-48cc-4770-9814-9aaf3b99a74a",[],[6233],{"id":6234,"sortIndex":32,"affiliation":6235,"properties":28},"c769c7a7-0dcf-46ad-a9bc-cb0af5f4d901",{"id":6234,"createTime":28,"updateTime":28,"relativeEntities":6236,"slug":28,"properties":6237,"entityType":28,"verifyStatus":28,"verifyTime":28,"verifyNote":28,"languages":28,"translateLanguages":28,"viewCount":28,"url":28,"parentIds":6240,"statistic":28},[],{"title":6238},{"EN":6239},"Princeton Environmental Institute",[],{"orcid":6242,"title":6244,"openalex":6246},{"VOID":6243},"https:\u002F\u002Forcid.org\u002F0000-0001-5219-2604",{"EN":6245},"Jorge L. 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