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Here we conducted a warming experiment in an alpine meadow dominated by \u003Cjats:italic>Koresbia\u003C\u002Fjats:italic> in the permafrost region of the Qinghai‐Tibet Plateau (\u003Cjats:styled-content style=\"fixed-case\">QTP\u003C\u002Fjats:styled-content>) to examine effects of warming on \u003Cjats:italic>R\u003Cjats:sub>s\u003C\u002Fjats:sub>\u003C\u002Fjats:italic> and its components. Infrared heaters were used to simulate a 2°C warming of the surface soil temperature. Deep collars (50 cm to exclude root growth) were inserted into soil to measure \u003Cjats:italic>R\u003Cjats:sub>h\u003C\u002Fjats:sub>\u003C\u002Fjats:italic>: \u003Cjats:italic>R\u003Cjats:sub>a\u003C\u002Fjats:sub>\u003C\u002Fjats:italic>, which was calculated by subtracting \u003Cjats:italic>R\u003Cjats:sub>h\u003C\u002Fjats:sub>\u003C\u002Fjats:italic> from \u003Cjats:italic>R\u003Cjats:sub>s\u003C\u002Fjats:sub>\u003C\u002Fjats:italic>. Average \u003Cjats:italic>R\u003Cjats:sub>s\u003C\u002Fjats:sub>\u003C\u002Fjats:italic> and its components (\u003Cjats:italic>R\u003Cjats:sub>a\u003C\u002Fjats:sub>\u003C\u002Fjats:italic> and \u003Cjats:italic>R\u003Cjats:sub>h\u003C\u002Fjats:sub>\u003C\u002Fjats:italic>) were significantly stimulated by 21.5, 27 and 15.6%, respectively, in warmed plots from January 2011 to October 2013. The contribution of \u003Cjats:italic>R\u003Cjats:sub>h\u003C\u002Fjats:sub>\u003C\u002Fjats:italic> to \u003Cjats:italic>R\u003Cjats:sub>s\u003C\u002Fjats:sub>\u003C\u002Fjats:italic> decreased in the warmed plots because of the smaller relative increase in \u003Cjats:italic>R\u003Cjats:sub>h\u003C\u002Fjats:sub>\u003C\u002Fjats:italic> than in \u003Cjats:italic>R\u003Cjats:sub>a\u003C\u002Fjats:sub>\u003C\u002Fjats:italic>. Annual soil C release increased by 263 and 247 g C m\u003Cjats:sup>−2\u003C\u002Fjats:sup> in 2011 and 2012, respectively. Stimulation in \u003Cjats:italic>R\u003Cjats:sub>a\u003C\u002Fjats:sub>\u003C\u002Fjats:italic> and \u003Cjats:italic>R\u003Cjats:sub>h\u003C\u002Fjats:sub>\u003C\u002Fjats:italic> was related to the significant increase in root biomass (0–50 cm) and in labile soil C in the deeper layer (40–50 cm). The temperature sensitivities (\u003Cjats:styled-content style=\"fixed-case\">Q\u003Cjats:sub>10\u003C\u002Fjats:sub>\u003C\u002Fjats:styled-content>) of \u003Cjats:italic>R\u003Cjats:sub>s\u003C\u002Fjats:sub>\u003C\u002Fjats:italic> and its components all increased with larger values in \u003Cjats:italic>R\u003Cjats:sub>a\u003C\u002Fjats:sub>\u003C\u002Fjats:italic>, followed by \u003Cjats:italic>R\u003Cjats:sub>s\u003C\u002Fjats:sub>\u003C\u002Fjats:italic> and \u003Cjats:italic>R\u003Cjats:sub>h\u003C\u002Fjats:sub>\u003C\u002Fjats:italic>. Our results suggest a positive feedback between soil C release and climatic warming in the permafrost region of the \u003Cjats:styled-content style=\"fixed-case\">QTP\u003C\u002Fjats:styled-content>.\u003C\u002Fjats:p>",{"EN":102},"Effects of experimental warming on soil respiration and its components in an alpine meadow in the permafrost region of the Qinghai‐Tibet Plateau",{"VOID":104},"[\"17167761120430101070\"]",{"VOID":106},"10.1111\u002Fejss.12187","PUBLICATION","VERIFIED","2024-09-12T15:09:21.242+00:00","Auto 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Most studies have found that it is possible to estimate chemical properties that are related to surface and solid material composition. This paper focuses on prediction of physical and mechanical properties, with emphasis on the elucidation of possible mechanisms of prediction. Soil physical properties that are based on pore‐space relationships such as bulk density, water retention and hydraulic conductivity cannot be predicted well using MIR spectroscopy. Hydraulic conductivity was measured using a tension‐disc permeameter, excluding the macropore effect, but MIR spectroscopy did not give a good prediction. Properties based on the soil solid composition and surfaces such as clay content and shrink‐swell potential can be predicted reasonably well. Macro‐aggregate stability in water can be predicted reasonably as it has a strong correlation with carbon content in the soil. We found that most of the physical and mechanical properties can be related back to the fundamental soil properties such as clay content, carbon content, cation exchange capacity and bulk density. These connections have been explored previously in pedotransfer functions studies. The concept of a spectral soil inference system is reiterated: linking the spectra to basic soil properties and connecting basic soil properties to other functional soil properties via pedotransfer functions.\u003C\u002Fjats:p>",{"EN":454},"Using soil knowledge for the evaluation of mid‐infrared diffuse reflectance spectroscopy for predicting soil physical and mechanical properties",{"VOID":456},"[]",{"VOID":458},"10.1111\u002Fj.1365-2389.2008.01058.x","2025-02-07T03:45:35.110+00:00",[112],"https:\u002F\u002Fbsssjournals.onlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1365-2389.2008.01058.x",[463,482,499,514],{"id":464,"sortIndex":25,"researcher":24,"roles":465,"affiliations":466,"properties":475},"a3f0a4bf-ec04-4131-b6c0-52fbabcf157e",[],[467],{"id":468,"sortIndex":25,"affiliation":469,"properties":24},"96a67a62-a3aa-4ceb-b080-a311b22fda89",{"id":468,"createTime":24,"updateTime":24,"relativeEntities":470,"slug":24,"properties":471,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":474,"statistic":24},[],{"title":472},{"EN":473},"aFaculty of Agriculture, Food and Natural Resources, University of Sydney, New South Wales 2006, Australia, and \u2028 bDepartment of Environment and Climate Change, Cowra, New South Wales 2794, Australia",[],{"orcid":476,"title":478,"openalex":480},{"VOID":477},"https:\u002F\u002Forcid.org\u002F0000-0002-1182-2371",{"EN":479},"Budiman Minasny",{"VOID":481},"A5051455406",{"id":483,"sortIndex":138,"researcher":24,"roles":484,"affiliations":485,"properties":492},"03752558-0ccd-45dd-bcc4-553bec78bfe4",[],[486],{"id":468,"sortIndex":25,"affiliation":487,"properties":24},{"id":468,"createTime":24,"updateTime":24,"relativeEntities":488,"slug":24,"properties":489,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":491,"statistic":24},[],{"title":490},{"EN":473},[],{"orcid":493,"title":495,"openalex":497},{"VOID":494},"https:\u002F\u002Forcid.org\u002F0000-0003-0913-2643",{"EN":496},"Alex B. 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Report for 1970 Part 2 Rothamsted Experimental Station Harpenden Herts UK.",{},{"id":24,"text":758,"url":24,"identifiers":759},"Williams P.C, 1987, Near‐Infrared Technology in the Agricultural and Food Industries, 143",{},{"id":761,"createTime":762,"updateTime":763,"relativeEntities":764,"slug":765,"properties":766,"entityType":107,"verifyStatus":108,"verifyTime":778,"verifyNote":110,"languages":779,"translateLanguages":24,"viewCount":25,"primaryUrl":780,"fullTextUrl":24,"authors":781,"publicationType":256,"publisherRelationship":801,"citationCount":846,"citationInfo":847,"publishDate":853,"publishYear":848,"citationAnalyzeStatus":585,"lastCitationAnalyze":854,"indexDatabases":855,"openAccess":24,"references":856,"isForceReanalyzing":439},"042e15fa-7785-42e4-8096-d1941f8b3c27","2024-10-08T17:16:42.036+00:00","2025-12-25T20:29:09.443+00:00",[],"An-overview-of-the-permanence-of-soil-organic-carbon-stocks-influence-of-direct-human-induced-indirect-and-natural-effects",{"openalex":767,"mag":769,"abstract":771,"title":773,"gsPaper":775,"doi":776},{"VOID":768},"W2076882771",{"VOID":770},"2076882771",{"EN":772},"\u003Cjats:title>Summary\u003C\u002Fjats:title>\u003Cjats:p>If biospheric sinks, such as soil organic carbon, are to be used to meet obligations for greenhouse gas emission reduction under the Kyoto Protocol, the permanence of these sinks needs to be considered. Further, since only direct human‐induced carbon sinks can be included, and sinks resulting from indirect and natural effects cannot be used, there is a pressing need to separate direct human‐induced effects from indirect and natural effects. Since these effects also influence the permanence of soil organic stocks, this paper attempts to synthesize existing knowledge in soil science, and use models to examine the likely influence of direct, indirect and natural effects on the permanence of soil organic carbon stocks.\u003C\u002Fjats:p>",{"EN":774},"An overview of the permanence of soil organic carbon stocks: influence of direct human‐induced, indirect and natural effects",{"VOID":456},{"VOID":777},"10.1111\u002Fj.1365-2389.2005.00708.x","2024-10-08T17:16:42.035+00:00",[112],"https:\u002F\u002Fbsssjournals.onlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1365-2389.2005.00708.x",[782],{"id":783,"sortIndex":25,"researcher":24,"roles":784,"affiliations":785,"properties":794},"76844678-ebd1-40f1-89f2-4afc8a3315ab",[],[786],{"id":787,"sortIndex":25,"affiliation":788,"properties":24},"be5197be-942b-40c3-b3df-e7bb28f279d0",{"id":787,"createTime":24,"updateTime":24,"relativeEntities":789,"slug":24,"properties":790,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":793,"statistic":24},[],{"title":791},{"EN":792},"School of Biological Sciences, Cruickshank Building, St. Machar Drive, University of Aberdeen, Aberdeen, AB24 3UU, UK",[],{"orcid":795,"title":797,"openalex":799},{"VOID":796},"https:\u002F\u002Forcid.org\u002F0000-0002-3784-1124",{"EN":798},"Pete Smith",{"VOID":800},"A5028843362",{"url":24,"publisher":802,"properties":840},{"id":6,"createTime":7,"updateTime":8,"relativeEntities":803,"slug":10,"properties":804,"entityType":22,"verifyStatus":23,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":25,"subjectFields":809,"manageAffiliations":814,"indexDatabases":825,"url":83,"thumbnailPath":24,"statistic":24,"gsStatistic":24,"type":24,"analyzePriority":24},[],{"country":805,"eissn":806,"issn":807,"title":808},{"VOID":13},{"VOID":15},{"VOID":17},{"EN":19},[810],{"id":28,"createTime":24,"updateTime":24,"relativeEntities":811,"label":812,"description":813,"parentId":24,"standard":24,"scholarHubFieldId":24},[],{"EN":31},{},[815,820],{"id":35,"createTime":24,"updateTime":24,"relativeEntities":816,"slug":24,"properties":817,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":819,"statistic":24},[],{"title":818},{"EN":39},[],{"id":42,"createTime":24,"updateTime":24,"relativeEntities":821,"slug":24,"properties":822,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":824,"statistic":24},[],{"title":823},{"EN":46},[],[826,833],{"id":50,"indexDatabase":827,"url":63,"indexYears":24,"academicFieldIds":832,"indexDatabaseRanking":24},{"id":52,"createTime":24,"updateTime":24,"relativeEntities":828,"label":829,"description":830,"key":59,"publicationTags":831,"standard":24},[],{"EN":55,"VI":55},{"EN":57,"VI":58},[61,62],[65],{"id":67,"indexDatabase":834,"url":78,"indexYears":79,"academicFieldIds":839,"indexDatabaseRanking":82},{"id":69,"createTime":24,"updateTime":24,"relativeEntities":835,"label":836,"description":837,"key":75,"publicationTags":838,"standard":24},[],{"EN":72,"VI":72},{"EN":72,"VI":74},[77],[81],{"issue":841,"pages":842,"volume":844},{"VOID":572},{"VOID":843},"673-680",{"VOID":845},"56",114,{"total":846,"publishYear":848,"statisticByYear":849},2005,{"2012":581,"2013":204,"2014":850,"2015":851,"2016":204,"2017":204,"2018":222,"2019":204,"2020":204,"2021":240,"2022":204,"2023":240,"2024":852},12,8,9,"2005-10-01","2025-12-25T20:29:09.442+00:00",[61,82],[857,860,863,866,870,873,876,879,882,885,888,891,894,897,900,903,906,909,912,915,918,921,924,927,930,933,936,939,942,945,948,951,954,957,960,963,966,969,972,975,978,981],{"id":24,"text":858,"url":24,"identifiers":859},"Arrouays D., 2002, Contribution à la lutte contre l'effet de serre. Stocker du carbone dans les dols agricoles de France?",{},{"id":24,"text":861,"url":24,"identifiers":862},"10.1111\u002Fj.1365-2389.1996.tb01386.x",{"doi":861},{"id":24,"text":864,"url":24,"identifiers":865},"Bazzaz F., 1996, Global Climate Change and Agricultural Production: Direct and Indirect Effects of Changing Hydrological, Pedological and Plant Physiological Processes.",{},{"id":24,"text":867,"url":24,"identifiers":868},"Coleman K., 1996, A model for the turnover of carbon in soil., Evaluation of Soil Organic Matter Models using Existing Long-Term Datasets, 237, 10.1007\u002F978-3-642-61094-3_17",{"doi":869},"10.1007\u002F978-3-642-61094-3_17",{"id":24,"text":871,"url":24,"identifiers":872},"10.1046\u002Fj.1365-2486.1998.00101.x",{"doi":871},{"id":24,"text":874,"url":24,"identifiers":875},"10.1016\u002F0168-1923(86)90054-7",{"doi":874},{"id":24,"text":877,"url":24,"identifiers":878},"10.1016\u002F0016-7061(95)00072-0",{"doi":877},{"id":24,"text":880,"url":24,"identifiers":881},"10.1146\u002Fannurev.arplant.48.1.609",{"doi":880},{"id":24,"text":883,"url":24,"identifiers":884},"10.1111\u002Fj.1475-2743.2003.tb00313.x",{"doi":883},{"id":24,"text":886,"url":24,"identifiers":887},"10.1016\u002Fj.geoderma.2004.01.021",{"doi":886},{"id":24,"text":889,"url":24,"identifiers":890},"Glendining M.J., 1995, Soil Management: Experimental Basis for Sustainability and Environmental Quality, 385",{},{"id":24,"text":892,"url":24,"identifiers":893},"10.1046\u002Fj.1354-1013.2002.00486.x",{"doi":892},{"id":24,"text":895,"url":24,"identifiers":896},"10.1034\u002Fj.1600-0889.1999.00013.x",{"doi":895},{"id":24,"text":898,"url":24,"identifiers":899},"IPCC, 1997, Guidelines for National Greenhouse Gas Inventories. Workbook.",{},{"id":24,"text":901,"url":24,"identifiers":902},"IPCC, 2000, Land Use, Land Use Change, and Forestry",{},{"id":24,"text":904,"url":24,"identifiers":905},"IPCC, 2001, Climate Change: The Scientific Basis",{},{"id":24,"text":907,"url":24,"identifiers":908},"IPCC2003.IPCC meeting on current scientific understanding of the processes affecting terrestrial carbon stocks and human influences upon them. Expert Meeting Report Geneva Switzerland 21–23 July 2003.IPCC – XXI\u002FINF.1 (22.IX.2003) IPCC Twenty‐First Session 3 and 6–7 November 2003 Vienna.",{},{"id":24,"text":910,"url":24,"identifiers":911},"IPCC, 2004, Good Practice Guidance for National Greenhouse Gas Inventories for Land Use, Land‐Use Change and Forestry",{},{"id":24,"text":913,"url":24,"identifiers":914},"10.1016\u002FS0016-7061(97)00044-X",{"doi":913},{"id":24,"text":916,"url":24,"identifiers":917},"Jenkinson D.S., 1988, Russell's Soil Conditions and Plant Growth, 564",{},{"id":24,"text":919,"url":24,"identifiers":920},"Lal R., 1999, Soil management and restoration for C sequestration to mitigate the accelerated greenhouse effect, Progress in Environmental Science, 1, 307",{},{"id":24,"text":922,"url":24,"identifiers":923},"10.1016\u002Fj.geoderma.2004.01.032",{"doi":922},{"id":24,"text":925,"url":24,"identifiers":926},"Lamborg M.R., 1983, CO2 and Plants: The Response of Plants to Rising Levels of Carbon Dioxide, 131",{},{"id":24,"text":928,"url":24,"identifiers":929},"Lisovoi N., 2001, The influence of long‐term fertilization on the crop yield and fertility of the typical chernozem in the left bank forest steppe region of the Ukraine, Agrokhimia, 2, 27",{},{"id":24,"text":931,"url":24,"identifiers":932},"10.1038\u002F18205",{"doi":931},{"id":24,"text":934,"url":24,"identifiers":935},"10.1111\u002Fj.1475-2743.1997.tb00594.x",{"doi":934},{"id":24,"text":937,"url":24,"identifiers":938},"Romanyá J., 2000, Modelling changes in soil organic matter after planting fast‐growing Pinus radiata on Mediterranean agricultural soils, European Journal of Soil Science, 51, 627",{},{"id":24,"text":940,"url":24,"identifiers":941},"Sampson R.N., 2000, Land Use, Land‐Use Change and Forestry, 183",{},{"id":24,"text":943,"url":24,"identifiers":944},"10.1111\u002Fj.1365-2486.1995.tb00008.x",{"doi":943},{"id":24,"text":946,"url":24,"identifiers":947},"10.1038\u002F35102500",{"doi":946},{"id":24,"text":949,"url":24,"identifiers":950},"10.1126\u002Fscience.284.5423.2095",{"doi":949},{"id":24,"text":952,"url":24,"identifiers":953},"10.1111\u002Fj.1475-2743.2004.tb00367.x",{"doi":952},{"id":24,"text":955,"url":24,"identifiers":956},"10.1111\u002Fj.1365-2486.2004.00854.x",{"doi":955},{"id":24,"text":958,"url":24,"identifiers":959},"10.1016\u002Fj.eja.2003.08.002",{"doi":958},{"id":24,"text":961,"url":24,"identifiers":962},"Smith P., 2004, The Global Carbon Cycle: Integrating Humans, Climate, and the Natural World, 479",{},{"id":24,"text":964,"url":24,"identifiers":965},"Smith P., 2005, Limited increase of agricultural soil carbon and nitrogen stocks due to increased atmospheric CO2 concentrations, Journal of Crop Production",{},{"id":24,"text":967,"url":24,"identifiers":968},"10.1126\u002Fscience.287.5452.427e",{"doi":967},{"id":24,"text":970,"url":24,"identifiers":971},"10.1046\u002Fj.1461-0248.2000.00176.x",{"doi":970},{"id":24,"text":973,"url":24,"identifiers":974},"10.1007\u002F978-3-642-61094-3_7",{"doi":973},{"id":24,"text":976,"url":24,"identifiers":977},"10.1023\u002FA:1012617517839",{"doi":976},{"id":24,"text":979,"url":24,"identifiers":980},"Smith P., 2001, Proceedings of Second ESA Symposium on Modelling Cropping Systems, Florence, Italy, July 2001",{},{"id":24,"text":982,"url":24,"identifiers":983},"10.1016\u002FS0959-3780(00)00026-1",{"doi":982},{"id":985,"createTime":986,"updateTime":987,"relativeEntities":988,"slug":989,"properties":990,"entityType":107,"verifyStatus":108,"verifyTime":986,"verifyNote":110,"languages":1005,"translateLanguages":1006,"viewCount":25,"primaryUrl":1008,"fullTextUrl":24,"authors":1009,"publicationType":256,"publisherRelationship":1156,"citationCount":581,"citationInfo":1200,"publishDate":1203,"publishYear":1201,"citationAnalyzeStatus":23,"lastCitationAnalyze":987,"indexDatabases":1204,"openAccess":24,"references":1205,"isForceReanalyzing":439},"9649eab8-77a5-4fe1-a806-8972bbf45ceb","2024-11-25T10:26:55.314+00:00","2025-08-12T03:18:57.625+00:00",[],"Effects-of-microsized-rice-straw-on-soil-clay-dispersibility",{"openalex":991,"abstract":993,"title":996,"gsPaper":999,"keywords":1001,"doi":1003},{"VOID":992},"W4280588622",{"VI":994,"EN":995},"\u003Cjats:title>Tóm tắt\u003C\u002Fjats:title>\u003Cjats:sec>\u003Cjats:label \u002F>\u003Cjats:p>Việc đưa rơm vào đất đã được khuyến khích như một giải pháp thay thế cho việc đốt rơm tại chỗ, điều này đang diễn ra ở nhiều vùng trồng lúa. Tuy nhiên, thực hành này có thể dẫn đến sự thay đổi trong tính chất keo của đất sét, điều này có thể làm tăng cường sự mất mát của đất sét và dinh dưỡng. Nghiên cứu này nhằm chứng minh ảnh hưởng của bột rơm được thiết kế với kích thước vi mô lên các tính chất keo của hai loại đất sét, đó là đất sét illite và kaolinite. Kỹ thuật tán xạ ánh sáng động đã được kết hợp với phương pháp ống nghiệm để đánh giá sự thay đổi theo thời gian về kích thước hạt, điện thế zeta và khả năng phân tán cho các huyền phù của bột rơm và các hỗn hợp của nó với đất sét illite và kaolinite. Dữ liệu từ các thí nghiệm động học trong khoảng thời gian 20 ngày cho thấy bột rơm đã làm tăng đáng kể khả năng phân tán của đất sét. Phát hiện cho thấy các hạt rơm mang điện tích âm; do đó, việc đưa bột rơm vào các huyền phù đất sét đã làm tăng số lượng điện tích âm trong hệ thống, từ đó tăng cường các lực đẩy nội bộ và cuối cùng thúc đẩy sự phân tán của đất sét. Hơn nữa, một số quá trình tương tác, đó là sự phân hủy sinh học và hòa tan của phytolith (silica trong rơm), dẫn đến việc giải phóng chất hữu cơ hòa tan và silicon, điều này làm tăng cường khả năng phân tán của đất sét. Ngoài nhận thức “truyền thống” về tác động của việc đưa rơm vào đất, chẳng hạn như tạo ra môi trường độc hại, môi trường thiếu oxy hoặc tăng lượng phát thải CH\u003Cjats:sub>4\u003C\u002Fjats:sub>, sự thay đổi trong các tính chất keo của đất sét cũng cần được nhấn mạnh. Chúng tôi đề xuất rằng việc đưa rơm vào đất cần có thêm các giải pháp để ngăn ngừa sự mất mát đất sét.\u003C\u002Fjats:p>\u003C\u002Fjats:sec>\u003Cjats:sec>\u003Cjats:title>Nổi bật\u003C\u002Fjats:title>\u003Cjats:p>\u003Cjats:list list-type=\"bullet\">\n\u003Cjats:list-item>\u003Cjats:p>Bột rơm đã được kiểm tra về khả năng ảnh hưởng đến các tính chất keo của đất sét\u003C\u002Fjats:p>\u003C\u002Fjats:list-item>\n\u003Cjats:list-item>\u003Cjats:p>Phát hiện rằng các hạt rơm mang điện tích âm\u003C\u002Fjats:p>\u003C\u002Fjats:list-item>\n\u003Cjats:list-item>\u003Cjats:p>Việc đưa bột rơm vào tăng cường lực đẩy và tạo điều kiện cho sự phân tán của đất sét\u003C\u002Fjats:p>\u003C\u002Fjats:list-item>\n\u003Cjats:list-item>\u003Cjats:p>Vi sinh vật, \u003Cjats:italic>B. amyloliquefaciens\u003C\u002Fjats:italic>, tăng cường hiệu ứng của bột rơm\u003C\u002Fjats:p>\u003C\u002Fjats:list-item>\n\u003C\u002Fjats:list>\u003C\u002Fjats:p>\u003C\u002Fjats:sec>","\u003Cjats:title>Abstract\u003C\u002Fjats:title>\u003Cjats:sec>\u003Cjats:label \u002F>\u003Cjats:p>The incorporation of straw into soil has been encouraged as an alternative straw‐disposal strategy to the on‐site burning that occurs in many paddy regions. However, this practice may lead to changes in the colloidal properties of soil clays that potentially intensify clay and nutrient losses. This study aimed to demonstrate the effect of engineered microsized straw powder on the colloidal properties of two soil clays, that is, illitic and kaolinitic soil clays. Dynamic light scattering was coupled with the test tube method to evaluate time‐resolved changes in the particle size, zeta potential and dispersibility for the suspensions of straw powder and its mixtures with illitic and kaolinitic soil clays. Data from kinetic experiments over a time span of 20 days revealed that straw powder remarkably increased the dispersibility of soil clays. It was found that straw particles carried negative charges; thus, the introduction of straw powder into the clay suspensions increased the number of negative charges in the system, thereby increasing internal repulsive forces and eventually favouring clay dispersion. Moreover, certain mutual processes, that is, the biodegradation and dissolution of phytoliths (silica in straw), resulted in the release of dissolved organic matter and silicon, which aggravated clay dispersibility. In addition to the “traditional” awareness of the impacts of straw incorporation, for example, creating toxic, reduced environments or increasing CH\u003Cjats:sub>4\u003C\u002Fjats:sub> emissions, the changes in the colloidal properties of soil clays should also be highlighted. We propose that the incorporation of straw requires additional solutions for the prevention of clay loss.\u003C\u002Fjats:p>\u003C\u002Fjats:sec>\u003Cjats:sec>\u003Cjats:title>Highlights\u003C\u002Fjats:title>\u003Cjats:p>\u003Cjats:list list-type=\"bullet\">\n\u003Cjats:list-item>\u003Cjats:p>Straw powder was examined for possible effect on colloidal properties of soil clays\u003C\u002Fjats:p>\u003C\u002Fjats:list-item>\n\u003Cjats:list-item>\u003Cjats:p>It was found that straw particles carried negative charges\u003C\u002Fjats:p>\u003C\u002Fjats:list-item>\n\u003Cjats:list-item>\u003Cjats:p>Introduction of straw powder increase repulsive forces and favor clay dispersion\u003C\u002Fjats:p>\u003C\u002Fjats:list-item>\n\u003Cjats:list-item>\u003Cjats:p>Microorganism, \u003Cjats:italic>B. amyloliquefaciens\u003C\u002Fjats:italic>, enhances the effect of straw powder\u003C\u002Fjats:p>\u003C\u002Fjats:list-item>\n\u003C\u002Fjats:list>\u003C\u002Fjats:p>\u003C\u002Fjats:sec>",{"EN":997,"VI":998},"Effects of microsized rice straw on soil clay dispersibility","Ảnh hưởng của rơm gạo kích thước vi mô đến khả năng phân tán của đất sét",{"VOID":1000},"6353683104836671030",{"VI":1002},"",{"VOID":1004},"10.1111\u002Fejss.13246",[112],[1007],"VI","https:\u002F\u002Fbsssjournals.onlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fejss.13246",[1010,1029,1044,1069,1086,1105,1122,1139],{"id":1011,"sortIndex":25,"researcher":24,"roles":1012,"affiliations":1013,"properties":1022},"db788e26-d8a9-4781-aee6-a0307102e60a",[],[1014],{"id":1015,"sortIndex":25,"affiliation":1016,"properties":24},"cb8894d6-3b2f-490c-9aaa-749147eb87d4",{"id":1015,"createTime":24,"updateTime":24,"relativeEntities":1017,"slug":24,"properties":1018,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":1021,"statistic":24},[],{"title":1019},{"VI":1020},"Faculty of Environmental Sciences, University of Science, Vietnam National University, Hanoi, Vietnam",[],{"title":1023,"gsAuthor":1025,"openalex":1027},{"EN":1024},"Thu T.T. 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Etat d’avancement et premiers résultats., Etude et Gestion des Sols, 13, 149",{},{"id":24,"text":1640,"url":24,"identifiers":1641},"10.2136\u002Fsssaj2002.6400a",{"doi":1640},{"id":24,"text":1643,"url":24,"identifiers":1644},"10.1016\u002Fj.agee.2007.01.002",{"doi":1643},{"id":24,"text":1646,"url":24,"identifiers":1647},"10.1016\u002Fj.chemolab.2008.06.003",{"doi":1646},{"id":24,"text":1649,"url":24,"identifiers":1650},"R Development Core Team, 2005, R: A Language and Environment for Statistical Computing.",{},{"id":24,"text":1652,"url":24,"identifiers":1653},"10.1016\u002Fj.geoderma.2009.04.005",{"doi":1652},{"id":24,"text":1655,"url":24,"identifiers":1656},"10.1180\u002Fclaymin.1979.014.2.03",{"doi":1655},{"id":24,"text":1658,"url":24,"identifiers":1659},"10.1111\u002Fj.1365-2486.2008.01658.x",{"doi":1658},{"id":24,"text":1661,"url":24,"identifiers":1662},"10.2136\u002Fsssaj2002.9880",{"doi":1661},{"id":24,"text":1664,"url":24,"identifiers":1665},"Silverstein R.M., 1998, Spectrometric Identification of Organic Compounds",{},{"id":24,"text":1667,"url":24,"identifiers":1668},"10.1016\u002Fj.geoderma.2007.12.009",{"doi":1667},{"id":24,"text":1670,"url":24,"identifiers":1671},"10.1346\u002FCCMN.1997.0450605",{"doi":1670},{"id":24,"text":1673,"url":24,"identifiers":1674},"10.1016\u002Fj.ecolind.2009.05.001",{"doi":1673},{"id":24,"text":1676,"url":24,"identifiers":1677},"10.1201\u002F9780203912546",{"doi":1676},{"id":24,"text":749,"url":24,"identifiers":1679},{"doi":749},{"id":24,"text":1681,"url":24,"identifiers":1682},"10.1016\u002Fj.jaridenv.2004.03.027",{"doi":1681},{"id":24,"text":1684,"url":24,"identifiers":1685},"10.1016\u002Fj.soilbio.2006.07.010",{"doi":1684},{"id":1687,"createTime":1688,"updateTime":1688,"relativeEntities":1689,"slug":1690,"properties":1691,"entityType":107,"verifyStatus":108,"verifyTime":1702,"verifyNote":110,"languages":1703,"translateLanguages":24,"viewCount":25,"primaryUrl":1704,"fullTextUrl":24,"authors":1705,"publicationType":256,"publisherRelationship":1742,"citationCount":1788,"citationInfo":1789,"publishDate":1792,"publishYear":1790,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":1793,"openAccess":24,"references":1794,"isForceReanalyzing":439},"ef0a1425-cae6-4479-b671-a9d6404ee759","2025-02-07T03:45:14.682+00:00",[],"Particle-packing-and-organization-of-the-textural-porosity-in-clay-silt-sand-mixtures",{"openalex":1692,"mag":1694,"abstract":1696,"title":1698,"doi":1700},{"VOID":1693},"W1989624750",{"VOID":1695},"1989624750",{"EN":1697},"\u003Cjats:title>Summary\u003C\u002Fjats:title>\u003Cjats:p>The packing of elementary particles in soil largely determines the properties that depend on the textural soil pore space, but is studied little. The relations between packing and size and nature of soil particles were studied using fractions of clay, silt and sand, mixed when wet and then dried. Ternary mixtures (clay:silt:sand) were compared with binary mixtures (clay:silt, clay:sand). The pore space of the mixtures was studied using mercury porosimetry and scanning electron microscopy. In all the mixtures the textural pore space was divided into two compartments: (1) lacunar pores due to the presence of skeleton particles and to the shrinkage of the clay phase between these particles, and (2) the clay–fabric pores due to the packing of the clay. In the ternary mixtures, lacunar pores could be divided into two classes: (1) those due to sand particles within the clay–slit phase considered as a single phase, and (2) those due to silt particles within this same phase. For certain mixtures, lacunar pores, referred to as hidden lacunar pores, were not interconnected but were occluded. This occurred both for hidden pores caused by the presence of sand and occluded by the clay–slit phase, and for hidden pores caused by the presence of silt and occluded by the clay phase. The relations between these types of textural pores and the proportions of different size fractions in the mixtures provide guidelines for making optimum use of the particle‐size characteristics of the soil to determine its properties.\u003C\u002Fjats:p>",{"EN":1699},"Particle packing and organization of the textural porosity in clay–silt–sand mixtures",{"VOID":1701},"10.1046\u002Fj.1365-2389.1998.4940557.x","2025-02-07T03:45:14.681+00:00",[112],"https:\u002F\u002Fbsssjournals.onlinelibrary.wiley.com\u002Fdoi\u002F10.1046\u002Fj.1365-2389.1998.4940557.x",[1706,1723],{"id":1707,"sortIndex":25,"researcher":24,"roles":1708,"affiliations":1709,"properties":1718},"b79ea5c0-dffd-452d-8683-e807dceefb46",[],[1710],{"id":1711,"sortIndex":25,"affiliation":1712,"properties":24},"572812c5-1e97-4599-9936-167af3753ad2",{"id":1711,"createTime":24,"updateTime":24,"relativeEntities":1713,"slug":24,"properties":1714,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":1717,"statistic":24},[],{"title":1715},{"EN":1716},"INRA, Unité de Science du Sol, Centre de Recherche d'Avignon, Site Agroparc, 84914 Avignon Cedex 9, France",[],{"title":1719,"openalex":1721},{"EN":1720},"J.C. 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D., 2011, The significant climate warming in the northern Tibetan Plateau and its possible causes, International Journal of Climatology, 31, 1257",{},{"id":24,"text":2142,"url":24,"identifiers":2143},"10.1007\u002Fs11104-013-1855-1",{"doi":2142},{"id":24,"text":2145,"url":24,"identifiers":2146},"10.1002\u002Fjpln.201000397",{"doi":2145},{"id":24,"text":2148,"url":24,"identifiers":2149},"IPCC, 2013, Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change",{},{"id":24,"text":2151,"url":24,"identifiers":2152},"IUSS Working Group WRB2006.World Reference Base for Soil Resources–a Framework for International Classification Correlation and Communication. World Soil Resources Report No 103 FAO Rome.",{},{"id":24,"text":2154,"url":24,"identifiers":2155},"10.1007\u002Fs00248-003-1037-4",{"doi":2154},{"id":24,"text":2157,"url":24,"identifiers":2158},"10.1016\u002Fj.soilbio.2013.10.041",{"doi":2157},{"id":24,"text":2160,"url":24,"identifiers":2161},"10.1111\u002Fj.1574-6941.2008.00620.x",{"doi":2160},{"id":24,"text":2163,"url":24,"identifiers":2164},"10.1111\u002Fj.1365-2486.1997.gcb136.x",{"doi":2163},{"id":24,"text":2166,"url":24,"identifiers":2167},"10.2134\u002Fjeq1998.00472425002700050036x",{"doi":2166},{"id":24,"text":2169,"url":24,"identifiers":2170},"10.1111\u002Fj.2006.0030-1299.14337.x",{"doi":2169},{"id":24,"text":2172,"url":24,"identifiers":2173},"Nelson D.W., 1996, Methods of Soil Analysis Part II, 539",{},{"id":24,"text":2175,"url":24,"identifiers":2176},"Oksanen J.2013.Multivariate Analysis of Ecological Communities in R: Vegan Tutorial[WWW document]. URLhttp:\u002F\u002Fcc.oulu.fi\u002F∼jarioksa\u002Fopetus\u002Fmetodi\u002Fvegantutor.pdf[accessed on 20 January 2015].",{},{"id":24,"text":2178,"url":24,"identifiers":2179},"10.1016\u002Fj.soilbio.2005.12.009",{"doi":2178},{"id":24,"text":2181,"url":24,"identifiers":2182},"10.1111\u002Fj.1365-2486.2006.01263.x",{"doi":2181},{"id":24,"text":2184,"url":24,"identifiers":2185},"10.1007\u002Fs11104-010-0391-5",{"doi":2184},{"id":24,"text":2187,"url":24,"identifiers":2188},"Rutherford P.M., 2006, Soil Sampling and Methods of Analysis, 267",{},{"id":24,"text":2190,"url":24,"identifiers":2191},"10.1016\u002F0038-0717(87)90052-6",{"doi":2190},{"id":24,"text":2193,"url":24,"identifiers":2194},"10.1016\u002FS0038-0717(02)00274-2",{"doi":2193},{"id":24,"text":2196,"url":24,"identifiers":2197},"10.1007\u002Fs12665-013-2523-8",{"doi":2196},{"id":24,"text":2199,"url":24,"identifiers":2200},"10.1128\u002FAEM.01063-10",{"doi":2199},{"id":24,"text":2202,"url":24,"identifiers":2203},"10.1016\u002F0038-0717(90)90046-3",{"doi":2202},{"id":24,"text":2205,"url":24,"identifiers":2206},"10.1038\u002Fismej.2011.124",{"doi":2205},{"id":24,"text":2208,"url":24,"identifiers":2209},"10.1111\u002Fj.1365-2486.2005.00902.x",{"doi":2208},{"id":24,"text":2211,"url":24,"identifiers":2212},"10.1038\u002Fnclimate1331",{"doi":2211},{"id":24,"text":2214,"url":24,"identifiers":2215},"10.2136\u002Fsssaj1997.03615995006100020015x",{"doi":2214},{"id":2217,"createTime":2218,"updateTime":2218,"relativeEntities":2219,"slug":2220,"properties":2221,"entityType":107,"verifyStatus":108,"verifyTime":2218,"verifyNote":110,"languages":2232,"translateLanguages":24,"viewCount":25,"primaryUrl":2233,"fullTextUrl":24,"authors":2234,"publicationType":256,"publisherRelationship":2326,"citationCount":2371,"citationInfo":2372,"publishDate":2375,"publishYear":2373,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":2376,"openAccess":24,"references":2377,"isForceReanalyzing":439},"cd1b0510-7d80-43f8-a0c1-bfa89fdefcd1","2025-02-05T11:32:09.087+00:00",[],"Mechanisms-of-solute-transport-affect-small-scale-abundance-and-function-of-soil-microorganisms-in-the-detritusphere",{"openalex":2222,"mag":2224,"abstract":2226,"title":2228,"doi":2230},{"VOID":2223},"W2038431903",{"VOID":2225},"2038431903",{"EN":2227},"\u003Cjats:title>Summary\u003C\u002Fjats:title>\u003Cjats:p>In the detritusphere, particulate organic matter offers new sites for microorganisms, whereas soluble substrates are transported into the adjacent soil. We investigated how mechanisms of solute transport affect microbial abundance and function in the detritusphere. In a first experiment, transport was restricted to diffusion, whereas in a second experiment it was dominated by convection. Two soil moisture contents were established in each experiment. When diffusion was the exclusive transport mechanism, the addition of maize litter induced distinct gradients in enzyme activities, soil organic C content and microbial biomass to a depth of 1.5–2.8 mm. Convection enlarged these gradients to 2.5–3.0 mm. The moisture regime modified the temporal pattern of diffusive C transport, microbial growth and enzyme release by inducing faster transport at large water contents. Convective transport seemed to be unaffected by soil moisture content. Using a convective‐diffusive transport model with first‐order decay, it was possible to simulate the observed activity profiles. The results indicate that the spatial dimension of the detritusphere is governed by the ratio between decay rate of available substrates and transport rate. Bacteria and fungi showed differing utilization strategies as revealed by coupling phospholipid fatty acid (PLFA) analysis with stable isotope techniques. Fungi assimilated C directly in the litter, whereas bacteria took up the substrates in the soil and therefore depended more on transport processes than fungi. Our results demonstrate the impact of physicochemical conditions on the abundance and function of microorganisms in the detritusphere. Furthermore, the combination of enzymatic measurements and mathematical transport modelling may offer a new way to measure substrate decay rates in soil.\u003C\u002Fjats:p>",{"EN":2229},"Mechanisms of solute transport affect small‐scale abundance and function of soil microorganisms in the detritusphere",{"VOID":2231},"10.1111\u002Fj.1365-2389.2006.00835.x",[112],"https:\u002F\u002Fbsssjournals.onlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1365-2389.2006.00835.x",[2235,2254,2273,2290,2309],{"id":2236,"sortIndex":25,"researcher":24,"roles":2237,"affiliations":2238,"properties":2247},"1ad6c084-f578-4ab2-9401-3bebdada749a",[],[2239],{"id":2240,"sortIndex":25,"affiliation":2241,"properties":24},"0fbc5915-d5f3-4a0f-acd9-d1fedb16abc7",{"id":2240,"createTime":24,"updateTime":24,"relativeEntities":2242,"slug":24,"properties":2243,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":2246,"statistic":24},[],{"title":2244},{"EN":2245},"Institute of Soil Science and Land Evaluation, Soil Biology Section, University of Hohenheim, Emil‐Wolff‐Straße 27, 70599 Stuttgart, Germany,",[],{"orcid":2248,"title":2250,"openalex":2252},{"VOID":2249},"https:\u002F\u002Forcid.org\u002F0000-0002-9674-4447",{"EN":2251},"Christian Poll",{"VOID":2253},"A5091068098",{"id":2255,"sortIndex":138,"researcher":24,"roles":2256,"affiliations":2257,"properties":2266},"cd73a5ad-c1c0-49ab-bc4f-9bf98101555c",[],[2258],{"id":2259,"sortIndex":25,"affiliation":2260,"properties":24},"5abe9f84-995e-4e9d-b241-94aeae19be53",{"id":2259,"createTime":24,"updateTime":24,"relativeEntities":2261,"slug":24,"properties":2262,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":2265,"statistic":24},[],{"title":2263},{"EN":2264},"Institute of Soil Science and Land Evaluation, Biogeophysics Section, University of Hohenheim, Emil-Wolff-Straße 27, 70599 Stuttgart, Germany,",[],{"orcid":2267,"title":2269,"openalex":2271},{"VOID":2268},"https:\u002F\u002Forcid.org\u002F0000-0001-6208-1991",{"EN":2270},"Joachim Ingwersen",{"VOID":2272},"A5073798718",{"id":2274,"sortIndex":164,"researcher":24,"roles":2275,"affiliations":2276,"properties":2285},"6a62596c-2095-47fd-bdff-62a024248247",[],[2277],{"id":2278,"sortIndex":25,"affiliation":2279,"properties":24},"8a5aa60f-42ca-4c00-b0d5-a09dafb44068",{"id":2278,"createTime":24,"updateTime":24,"relativeEntities":2280,"slug":24,"properties":2281,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":2284,"statistic":24},[],{"title":2282},{"EN":2283},"Institute for Plant Protection, Products Evaluation and Authorisation, Austrian Agency for Health and Food Safety, Spargelfeldstraße 191, 1226 Vienna, Austria, and",[],{"title":2286,"openalex":2288},{"EN":2287},"M. Stemmer",{"VOID":2289},"A5111611922",{"id":2291,"sortIndex":182,"researcher":24,"roles":2292,"affiliations":2293,"properties":2302},"5c2c52f4-bf42-4169-ad92-c6e7bbd176e8",[],[2294],{"id":2295,"sortIndex":25,"affiliation":2296,"properties":24},"cefe7d59-9504-4d77-9d34-e0e4d6140760",{"id":2295,"createTime":24,"updateTime":24,"relativeEntities":2297,"slug":24,"properties":2298,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":2301,"statistic":24},[],{"title":2299},{"EN":2300},"Institute of Soil Science, University of Natural Resources and Applied Life Sciences, Gregor‐Mendel‐Strasse 33, 1180 Vienna, Austria",[],{"orcid":2303,"title":2305,"openalex":2307},{"VOID":2304},"https:\u002F\u002Forcid.org\u002F0000-0002-3307-8416",{"EN":2306},"Martin H. 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T.W., 1986, Perspectives in Microbial Ecology, 493",{},{"id":24,"text":2424,"url":24,"identifiers":2425},"10.1016\u002FS0038-0717(03)00155-X",{"doi":2424},{"id":24,"text":2427,"url":24,"identifiers":2428},"10.1016\u002F0038-0717(93)90113-P",{"doi":2427},{"id":24,"text":2430,"url":24,"identifiers":2431},"10.1016\u002FS0038-0717(02)00241-9",{"doi":2430},{"id":24,"text":2433,"url":24,"identifiers":2434},"10.1046\u002Fj.1365-2389.1999.00266.x",{"doi":2433},{"id":24,"text":2436,"url":24,"identifiers":2437},"10.1002\u002F(SICI)1097-0231(19990715)13:13\u003C1278::AID-RCM649>3.0.CO;2-N",{"doi":2436},{"id":24,"text":2439,"url":24,"identifiers":2440},"10.1104\u002Fpp.102.4.1287",{"doi":2439},{"id":24,"text":2442,"url":24,"identifiers":2443},"10.1016\u002FS0016-7061(02)00363-4",{"doi":2442},{"id":24,"text":2445,"url":24,"identifiers":2446},"Griffin D.M., 1981, Water Potential Relations in Soil Microbiology, 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Band",{},{"id":24,"text":2472,"url":24,"identifiers":2473},"10.1016\u002F0169-7722(91)90038-3",{"doi":2472},{"id":24,"text":2475,"url":24,"identifiers":2476},"Macey R., 2000, Berkeley Madonna User's Guide 8.0",{},{"id":24,"text":2478,"url":24,"identifiers":2479},"10.1016\u002FS0038-0717(01)00079-7",{"doi":2478},{"id":24,"text":2481,"url":24,"identifiers":2482},"10.1039\u002Ftf9615701200",{"doi":2481},{"id":24,"text":2484,"url":24,"identifiers":2485},"10.1016\u002FS0038-0717(99)00047-4",{"doi":2484},{"id":24,"text":2487,"url":24,"identifiers":2488},"10.1111\u002Fj.1574-6941.2000.tb00669.x",{"doi":2487},{"id":24,"text":2490,"url":24,"identifiers":2491},"10.1016\u002Fj.soilbio.2003.12.005",{"doi":2490},{"id":24,"text":2493,"url":24,"identifiers":2494},"10.1111\u002Fj.1365-2389.2004.00639.x",{"doi":2493},{"id":24,"text":2496,"url":24,"identifiers":2497},"10.1016\u002FS0016-7061(98)00084-6",{"doi":2496},{"id":24,"text":2499,"url":24,"identifiers":2500},"10.1016\u002Fj.soilbio.2003.10.015",{"doi":2499},{"id":2502,"createTime":2503,"updateTime":2503,"relativeEntities":2504,"slug":2505,"properties":2506,"entityType":107,"verifyStatus":108,"verifyTime":2503,"verifyNote":110,"languages":2517,"translateLanguages":24,"viewCount":25,"primaryUrl":2518,"fullTextUrl":24,"authors":2519,"publicationType":256,"publisherRelationship":2584,"citationCount":2629,"citationInfo":2630,"publishDate":2633,"publishYear":2631,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":2634,"openAccess":24,"references":2635,"isForceReanalyzing":439},"517367aa-e399-4179-a1c2-0b1b28d9760d","2025-02-01T02:39:19.542+00:00",[],"Changes-in-the-amount-and-distribution-of-neutral-monosaccharides-of-savanna-soils-after-plantation-of-i-Pinus-i-and-i-Eucalyptus-i-in-the-Congo",{"openalex":2507,"mag":2509,"abstract":2511,"title":2513,"doi":2515},{"VOID":2508},"W2083313460",{"VOID":2510},"2083313460",{"EN":2512},"\u003Cjats:title>Summary\u003C\u002Fjats:title>\u003Cjats:p>In the Congo, near Pointe‐Noire, \u003Cjats:italic>Pinus\u003C\u002Fjats:italic> and \u003Cjats:italic>Eucalyptus\u003C\u002Fjats:italic> were planted on the savanna for 30 years. We have characterized the effects of this change on land‐use on the composition of carbohydrates in whole soil and particle‐size fractions of the soil. Carbohydrates represent variable proportions of the total soil organic carbon (TOC) of various particle size fractions. The largest proportions of sugar‐C were found in the savanna soil with as much as 250 mg g\u003Cjats:sup>−1\u003C\u002Fjats:sup> TOC in the coarsest plant remains and approximately 190 mg g\u003Cjats:sup>−1\u003C\u002Fjats:sup> TOC in the finest organo‐mineral fractions, whereas there was always less sugar in plantation soils. The monosaccharide xylose and mannose have different distributions: xylose appears to be the marker of the vegetal inheritance, whereas the dominance of mannose in the clay fraction bears the signature of current microbial sugar synthesis.\u003C\u002Fjats:p>\u003Cjats:p>The quantitative and qualitative evolution of the whole soil carbohydrates was studied as a function of plantation age. Carbohydrate‐C represents 131 mg g\u003Cjats:sup>−1\u003C\u002Fjats:sup> of the soil organic carbon in the savanna soil, but decreases to an average value of 75 mg g\u003Cjats:sup>−1\u003C\u002Fjats:sup> in plantations more than 6 years old. This appears to be due mainly to the stimulation of the mineralization of the glucose, which represented 60% of the total sugars in savanna soil and only 45–48% in tree plantations. The ratio [arabinose + galactose + fucose]\u002F[rhamnose + xylose], which is the largest in the oldest plantations, is significant for evaluating the replacement of carbohydrates of the original grass savanna by those of the trees.\u003C\u002Fjats:p>",{"EN":2514},"Changes in the amount and distribution of neutral monosaccharides of savanna soils after plantation of \u003Ci>Pinus\u003C\u002Fi> and \u003Ci>Eucalyptus\u003C\u002Fi> in the Congo",{"VOID":2516},"10.1111\u002Fj.1365-2389.1996.tb01371.x",[112],"https:\u002F\u002Fbsssjournals.onlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1365-2389.1996.tb01371.x",[2520,2537,2552,2569],{"id":2521,"sortIndex":25,"researcher":24,"roles":2522,"affiliations":2523,"properties":2532},"a35321a2-8dfb-4707-b06b-5cd15c508ff2",[],[2524],{"id":2525,"sortIndex":25,"affiliation":2526,"properties":24},"6de1e48b-3d78-40b7-aa32-82769f223b9a",{"id":2525,"createTime":24,"updateTime":24,"relativeEntities":2527,"slug":24,"properties":2528,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":2531,"statistic":24},[],{"title":2529},{"EN":2530},"Université d'Orléans‐CNRS URA 724, Laboratoire de Géochimie Organique, BP 6759, 45067 Orléans Cedex 02, France",[],{"title":2533,"openalex":2535},{"EN":2534},"Claire Trouvé",{"VOID":2536},"A5000759131",{"id":2538,"sortIndex":138,"researcher":24,"roles":2539,"affiliations":2540,"properties":2547},"f408620a-3093-4c74-9cb9-920d76603dfb",[],[2541],{"id":2525,"sortIndex":25,"affiliation":2542,"properties":24},{"id":2525,"createTime":24,"updateTime":24,"relativeEntities":2543,"slug":24,"properties":2544,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":2546,"statistic":24},[],{"title":2545},{"EN":2530},[],{"title":2548,"openalex":2550},{"EN":2549},"J‐R. 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In:Pé dologie. 2‐Constituants et Proprié té s du Sol. (edsM.BonneauandB.Souchier) pp.109–142. Masson Paris.",{},{"id":24,"text":2640,"url":24,"identifiers":2641},"10.1016\u002F0038-0717(87)90120-9",{"doi":2640},{"id":24,"text":2643,"url":24,"identifiers":2644},"10.1016\u002FS0031-9422(00)84324-1",{"doi":2643},{"id":24,"text":2646,"url":24,"identifiers":2647},"10.1038\u002F329708a0",{"doi":2646},{"id":24,"text":2649,"url":24,"identifiers":2650},"10.1016\u002F0016-7037(90)90267-O",{"doi":2649},{"id":24,"text":2652,"url":24,"identifiers":2653},"10.1016\u002F0038-0717(92)90230-U",{"doi":2652},{"id":24,"text":2655,"url":24,"identifiers":2656},"Cerri C.C., 1985, Application du traćage isotopique naturel en 13C, àľon;étude de la dynamique de la matière organique dans les sols, Comptes Rendus de ľon;Académie des Sciences, Paris, 300, 423",{},{"id":24,"text":2658,"url":24,"identifiers":2659},"Cheshire M.V., 1979, Nature and Origin of Carbohydrates in Soils",{},{"id":24,"text":2661,"url":24,"identifiers":2662},"10.1111\u002Fj.1365-2389.1981.tb01733.x",{"doi":2661},{"id":24,"text":2664,"url":24,"identifiers":2665},"10.1007\u002FBF00013103",{"doi":2664},{"id":24,"text":2667,"url":24,"identifiers":2668},"10.1111\u002Fj.1365-2389.1990.tb00042.x",{"doi":2667},{"id":24,"text":2670,"url":24,"identifiers":2671},"10.1111\u002Fj.1365-2389.1973.tb00741.x",{"doi":2670},{"id":24,"text":2673,"url":24,"identifiers":2674},"10.2136\u002Fsssaj1988.03615995005200050029x",{"doi":2673},{"id":24,"text":2676,"url":24,"identifiers":2677},"10.1016\u002FB978-0-444-41780-0.50015-8",{"doi":2676},{"id":24,"text":2679,"url":24,"identifiers":2680},"10.1021\u002Fac60111a017",{"doi":2679},{"id":24,"text":2682,"url":24,"identifiers":2683},"10.1007\u002FBF00378547",{"doi":2682},{"id":24,"text":2685,"url":24,"identifiers":2686},"Feller C., 1991, Nature des matières organiques associées aux fractions argileuses ?on;un sol ferrallitique, Complex Rendus de ľon;Académic des Sciences, Paris, 312, 1491",{},{"id":24,"text":2688,"url":24,"identifiers":2689},"Feller C., 1991, Comparaison de différentes méthodes ?on;hydrolyse acide en vue du dosage des glucoses totaux dans les sols, Science du Sol, 29, 13",{},{"id":24,"text":2691,"url":24,"identifiers":2692},"Girardin C., 1991, Analyseisotopiquedu 13C en abondance naturelle dans le carbone organique: un système automatique avec robot préparateur, Cahiers ORSTOM, Série Pédologie, 26, 371",{},{"id":24,"text":2694,"url":24,"identifiers":2695},"Goodwin T.W., 1983, Introduction to Plant Biochemistry",{},{"id":24,"text":2697,"url":24,"identifiers":2698},"Guckert A., 1974, Biodegradation et Humification, 116",{},{"id":24,"text":2700,"url":24,"identifiers":2701},"Guggenberger G., 1994, Land‐use effectsonthecompositionof organic matterinparticle‐size separates of soil: I. Lignin and carbohydrates signature, European Journal of Soil Science, 45, 449, 10.1111\u002Fj.1365-2389.1994.tb00530.x",{"doi":2702},"10.1111\u002Fj.1365-2389.1994.tb00530.x",{"id":24,"text":2704,"url":24,"identifiers":2705},"Jamet R.&Rieffel J.M.1976.Notice ?on;explication no 65. Carte pédologique du Congo. Feuille Pointe‐Noire feuille Loubomo à 1\u002F200000. ORSTOM‐Paris.",{},{"id":24,"text":2707,"url":24,"identifiers":2708},"Mariotti A., 1991, Le carbone 13 en abondance naturelle, traceur de la dynamique de la matière organique des sols et de lcar;SeAvolution des paléoenvironnements continentaux, Cahiers ORSTOM, Série Pédologie, 26, 299",{},{"id":24,"text":2710,"url":24,"identifiers":2711},"10.1016\u002F0009-2541(90)90218-V",{"doi":2710},{"id":24,"text":2713,"url":24,"identifiers":2714},"Martin A., 1990, Estimate of organic matter turnover rate in a savanna soil by 13C naturalabundance measurements, Soil Biologyand Biochemistry, 22, 517, 10.1016\u002F0038-0717(90)90188-6",{"doi":2715},"10.1016\u002F0038-0717(90)90188-6",{"id":24,"text":2717,"url":24,"identifiers":2718},"10.1080\u002F00380768.1984.10434702",{"doi":2717},{"id":24,"text":2720,"url":24,"identifiers":2721},"10.1007\u002FBF02205590",{"doi":2720},{"id":24,"text":2723,"url":24,"identifiers":2724},"10.2136\u002Fsssaj1983.03615995004700030023x",{"doi":2723},{"id":24,"text":2726,"url":24,"identifiers":2727},"Trouvé C.1992.Apport de la géochimie isotopique (δ13C) àľon;étude du renouvellement des matières organiques et des sucres neuters dans les sols tropicaux soumis à des changements ?on;écosystèmes. Thèse Université?on;Orldèans.",{},{"id":24,"text":2729,"url":24,"identifiers":2730},"Trouvé C., 1991, Etude par le traçagenaturel en 13C de la dynamique du renouvellement des matières organiques des sols de savane après plantation de pins et dcar;Eucalyptus au Congo, Cahiers ORSTOM, Série Pédologie, 26, 357",{},{"id":24,"text":2732,"url":24,"identifiers":2733},"10.1016\u002F0038-0717(94)90169-4",{"doi":2732},{"id":24,"text":2735,"url":24,"identifiers":2736},"10.1016\u002F0016-7061(79)90005-3",{"doi":2735},{"id":2738,"createTime":2739,"updateTime":2739,"relativeEntities":2740,"slug":2741,"properties":2742,"entityType":107,"verifyStatus":108,"verifyTime":2739,"verifyNote":110,"languages":2752,"translateLanguages":24,"viewCount":25,"primaryUrl":2753,"fullTextUrl":24,"authors":2754,"publicationType":256,"publisherRelationship":2808,"citationCount":2853,"citationInfo":2854,"publishDate":2864,"publishYear":2855,"citationAnalyzeStatus":23,"lastCitationAnalyze":24,"indexDatabases":2865,"openAccess":24,"references":2866,"isForceReanalyzing":439},"af743808-bb9d-43d1-a0ca-9804dae25e5e","2025-02-01T02:39:15.136+00:00",[],"Land-use-effects-on-the-composition-of-organic-matter-in-particle-size-separates-of-soil-I-Lignin-and-carbohydrate-signature",{"openalex":2743,"mag":2745,"abstract":2747,"title":2749,"doi":2751},{"VOID":2744},"W2061455793",{"VOID":2746},"2061455793",{"EN":2748},"\u003Cjats:title>Summary\u003C\u002Fjats:title>\u003Cjats:p>Soil from Eutrochrept A horizons under long‐term spruce forest (Sf), mixed deciduous forest (Df), permanent grassland (Gp) and arable rotation (Ar) was fractionated according to particle size and analysed for contents of C, N, lignin‐derived phenols and carbohydrates.\u003C\u002Fjats:p>\u003Cjats:p>Whole soil from Sf, Df, Gp and Ar contained 84, 59, 73 and 25 g C kg\u003Cjats:sup>−1\u003C\u002Fjats:sup> soil, respectively. For all sites, the C content declined and C\u002FN ratio increased in the order: clay (<2 μm), silt (2–20 μm), sand (20–2000 μm). Clay and silt were significantly lower in C in Ar than in Sf, Df and Gp, C associated with sand being substantially lower under arable rotation.\u003C\u002Fjats:p>\u003Cjats:p>The yield of lignin‐derived phenols decreased and carboxyl functionality and methoxyl demethylation of lignin derivatives increased with decreasing particle size, indicating a progressive lignin alteration. Whole soil from Sf and Gp was substantially higher in vanillyl (V), syringyl (S) and cinnamyl (C) units (VSC) than soil from Df and Ar. Compared to whole soil, clay was depleted and sand enriched in VSC. Only sand appeared to be affected significantly by land use. Sand from Ar and Df was more enriched in VSC than sand from Gp and Sf.\u003C\u002Fjats:p>\u003Cjats:p>Whole soil carbohydrates decreased in the order: Gp>Ar>Df>Sf. Sand‐ and clay‐sized separates were enriched in carbohydrates compared to silt. Carbohydrates in sand were mainly of plant origin whereas microbially‐derived sugars accounted for a larger proportion in the clay. Compared to Sf, Df and Gp, clay from Ar was enriched and sand depleted in microbial sugars.\u003C\u002Fjats:p>\u003Cjats:p>Lignin and carbohydrate distribution patterns indicate that organic matter was in a more advanced stage of decomposition in the sand separates from forest than from agricultural A horizons. The forest soils also show a higher degree of oxidative changes in lignin associated with clay. In contrast, differences between silt from the four A horizons were small.\u003C\u002Fjats:p>",{"EN":2750},"Land‐use effects on the composition of organic matter in particle‐size separates of soil: I. Lignin and carbohydrate signature",{"VOID":2702},[112],"https:\u002F\u002Fbsssjournals.onlinelibrary.wiley.com\u002Fdoi\u002F10.1111\u002Fj.1365-2389.1994.tb00530.x",[2755,2774,2793],{"id":2756,"sortIndex":25,"researcher":24,"roles":2757,"affiliations":2758,"properties":2767},"496bcbb8-bef4-4018-b619-2b833d3a24da",[],[2759],{"id":2760,"sortIndex":25,"affiliation":2761,"properties":24},"3983e64f-204c-4da2-8b36-ae44ee9e57d3",{"id":2760,"createTime":24,"updateTime":24,"relativeEntities":2762,"slug":24,"properties":2763,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":2766,"statistic":24},[],{"title":2764},{"VI":2765},"Institute of Soil Science and Soil Geography, University of Bayreuth, 95440 Bayreuth, Germany",[],{"orcid":2768,"title":2770,"openalex":2772},{"VOID":2769},"https:\u002F\u002Forcid.org\u002F0000-0002-6962-8264",{"EN":2771},"Georg Guggenberger",{"VOID":2773},"A5072191320",{"id":2775,"sortIndex":138,"researcher":24,"roles":2776,"affiliations":2777,"properties":2786},"0a405e23-68b7-45f7-94fd-09fd40a5575a",[],[2778],{"id":2779,"sortIndex":25,"affiliation":2780,"properties":24},"f121a921-3c03-495a-acf5-278e907e60be",{"id":2779,"createTime":24,"updateTime":24,"relativeEntities":2781,"slug":24,"properties":2782,"entityType":24,"verifyStatus":24,"verifyTime":24,"verifyNote":24,"languages":24,"translateLanguages":24,"viewCount":24,"url":24,"parentIds":2785,"statistic":24},[],{"title":2783},{"EN":2784},"Department of Plant Nutrition and Physiology, Research Centre Foulum, P.O. 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