Soil organic carbon losses due to land use change in a semiarid grassland
Background and Aims Knowledge about the effect of land use change on soil organic carbon (OC) in semiarid grassland is essential for understanding C cycles and for forecasting ecosystem C sequestration. Our objectives were (1) to study the effect of land use change on aggregate size distribution, ag...
Gespeichert in:
| Veröffentlicht in: | Plant and soil 2012-06, Vol.355 (1/2), p.299-309 |
|---|---|
| Hauptverfasser: | , , , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 309 |
|---|---|
| container_issue | 1/2 |
| container_start_page | 299 |
| container_title | Plant and soil |
| container_volume | 355 |
| creator | Qiu, Liping Wei, Xiaorong Zhang, Xingchang Cheng, Jimin Gale, William Guo, Chao Long, Tao |
| description | Background and Aims Knowledge about the effect of land use change on soil organic carbon (OC) in semiarid grassland is essential for understanding C cycles and for forecasting ecosystem C sequestration. Our objectives were (1) to study the effect of land use change on aggregate size distribution, aggregate-associated OC concentrations, and aggregate-associated stocks in a semiarid grassland area and (2) to relate changes in the aggregate fractions to changes in total soil OC. Methods Cropland and shrubland plots were established in a semiarid grassland area in 1982. We collected soil samples from adjacent grassland, cropland, and shrubland plots 27 years later and measured OC concentrations in the macroaggregate (>0.25 mm), microaggregate (0.25–0.053 mm) and silt+clay ( |
| doi_str_mv | 10.1007/s11104-011-1099-x |
| format | Article |
| fullrecord | <record><control><sourceid>gale_proqu</sourceid><recordid>TN_cdi_proquest_miscellaneous_1020857902</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A361711813</galeid><jstor_id>24370164</jstor_id><sourcerecordid>A361711813</sourcerecordid><originalsourceid>FETCH-LOGICAL-c440t-6fa39d19d8d410aba3e284f456ef5d1db88c6ef8ed34db8edf6869a2d51e29623</originalsourceid><addsrcrecordid>eNp1kU9rFTEUxYMo-Kx-ABdCQAQ3U3OTTCZZllJtoeBCBXdDXv4885iX1NwZqN_eDFO0CJJFcpPfOZybS8hrYOfA2PABAYDJjgF0wIzp7p-QHfSD6Hom1FOyY0zwjg3m-3PyAvHI1hrUjtx8KWmipR5sTo46W_cl06kgBqR-CXQudLLZ0wUDdT9sPgSaMrUUwynZmjw9VIu4Ii_Js2gnDK8e9jPy7ePV18vr7vbzp5vLi9vOScnmTkUrjAfjtZfA7N6KwLWMslch9h78XmvXjjp4IVsRfFRaGct9D4EbxcUZeb_53tXycwk4j6eELkwtQygLjsA40_1g2Iq-_Qc9lqXmlq5RoKTsGVONOt-og53CmHIsc7WuLd96dCWHmNr9hVAwAGgQTQCbwNX2UTXE8a6mk62_muu4TmPcpjG2aYzrNMb7pnn3EMWis1OsNruEf4S8N4PkRjeObxy2p_bb9XHk_5u_2URHnEv9ayrFsLYpfgNaWaJZ</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1016445006</pqid></control><display><type>article</type><title>Soil organic carbon losses due to land use change in a semiarid grassland</title><source>SpringerNature Journals</source><source>JSTOR Archive Collection A-Z Listing</source><creator>Qiu, Liping ; Wei, Xiaorong ; Zhang, Xingchang ; Cheng, Jimin ; Gale, William ; Guo, Chao ; Long, Tao</creator><creatorcontrib>Qiu, Liping ; Wei, Xiaorong ; Zhang, Xingchang ; Cheng, Jimin ; Gale, William ; Guo, Chao ; Long, Tao</creatorcontrib><description>Background and Aims Knowledge about the effect of land use change on soil organic carbon (OC) in semiarid grassland is essential for understanding C cycles and for forecasting ecosystem C sequestration. Our objectives were (1) to study the effect of land use change on aggregate size distribution, aggregate-associated OC concentrations, and aggregate-associated stocks in a semiarid grassland area and (2) to relate changes in the aggregate fractions to changes in total soil OC. Methods Cropland and shrubland plots were established in a semiarid grassland area in 1982. We collected soil samples from adjacent grassland, cropland, and shrubland plots 27 years later and measured OC concentrations in the macroaggregate (>0.25 mm), microaggregate (0.25–0.053 mm) and silt+clay (<0.053 mm) fractions. Results Total soil OC concentrations and stocks decreased significantly after the grassland was converted to cropland or shrubland. Soil microbial biomass C, root biomass, and root C also declined. The proportion of soil in the macroaggregate fraction decreased after conversion to cropland or shrubland. Decreases in macroaggregate-associated OC stocks accounted for more than half of the OC losses that occurred when grassland was converted to cropland. The decreases in macroaggregate-associated OC stocks were due to declines in both macroaggregation and macroaggregate-associated OC concentrations after conversion to cropland. In contrast, decreases in microaggregate-associated OC stocks accounted for more than half of the OC losses when grassland was converted to shrubland. The declines in microaggregate-associated OC stocks were primarily due to a decrease in microaggregate-associated OC concentrations after conversion to shrubland. Conclusions Land use changed caused significant decreases in soil OC stocks. Conversion to cropland soil resulted in large decreases in macroaggregate-associated OC stocks whereas conversion to shrubland resulted in large decreases in microaggregate-associated OC stocks. Any changes in land use in semiarid grasslands could cause the grassland soil to become a source of atmospheric CO2; therefore extreme caution should be taken to avoid this hazard.</description><identifier>ISSN: 0032-079X</identifier><identifier>EISSN: 1573-5036</identifier><identifier>DOI: 10.1007/s11104-011-1099-x</identifier><identifier>CODEN: PLSOA2</identifier><language>eng</language><publisher>Dordrecht: Springer</publisher><subject>Agricultural land ; Agricultural soils ; Agronomy. Soil science and plant productions ; Animal, plant and microbial ecology ; Biological and medical sciences ; Biomass ; Biomedical and Life Sciences ; Carbon ; Carbon content ; Carbon dioxide ; Carbon sequestration ; Chemical, physicochemical, biochemical and biological properties ; China ; Desert soils ; Ecology ; Environment ; Environmental aspects ; Farmlands ; Fundamental and applied biological sciences. Psychology ; General agronomy. Plant production ; Geochemistry ; Grassland soils ; Grasslands ; Land use ; Land use change ; Life Sciences ; Organic carbon ; Organic matter ; Physics, chemistry, biochemistry and biology of agricultural and forest soils ; Plant Physiology ; Plant Sciences ; Plant-soil relationships ; Regular Article ; Roots ; Semiarid grasslands ; Shrublands ; Size distribution ; Soil ; Soil aggregation ; Soil depth ; Soil science ; Soil Science & Conservation ; Soil-plant relationships. Soil fertility ; Soil-plant relationships. Soil fertility. Fertilization. Amendments ; Soils ; Soils (organic)</subject><ispartof>Plant and soil, 2012-06, Vol.355 (1/2), p.299-309</ispartof><rights>Springer Science+Business Media B.V. 2012</rights><rights>2015 INIST-CNRS</rights><rights>COPYRIGHT 2012 Springer</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c440t-6fa39d19d8d410aba3e284f456ef5d1db88c6ef8ed34db8edf6869a2d51e29623</citedby><cites>FETCH-LOGICAL-c440t-6fa39d19d8d410aba3e284f456ef5d1db88c6ef8ed34db8edf6869a2d51e29623</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/24370164$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/24370164$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,780,784,803,27924,27925,41488,42557,51319,58017,58250</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=25974298$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Qiu, Liping</creatorcontrib><creatorcontrib>Wei, Xiaorong</creatorcontrib><creatorcontrib>Zhang, Xingchang</creatorcontrib><creatorcontrib>Cheng, Jimin</creatorcontrib><creatorcontrib>Gale, William</creatorcontrib><creatorcontrib>Guo, Chao</creatorcontrib><creatorcontrib>Long, Tao</creatorcontrib><title>Soil organic carbon losses due to land use change in a semiarid grassland</title><title>Plant and soil</title><addtitle>Plant Soil</addtitle><description>Background and Aims Knowledge about the effect of land use change on soil organic carbon (OC) in semiarid grassland is essential for understanding C cycles and for forecasting ecosystem C sequestration. Our objectives were (1) to study the effect of land use change on aggregate size distribution, aggregate-associated OC concentrations, and aggregate-associated stocks in a semiarid grassland area and (2) to relate changes in the aggregate fractions to changes in total soil OC. Methods Cropland and shrubland plots were established in a semiarid grassland area in 1982. We collected soil samples from adjacent grassland, cropland, and shrubland plots 27 years later and measured OC concentrations in the macroaggregate (>0.25 mm), microaggregate (0.25–0.053 mm) and silt+clay (<0.053 mm) fractions. Results Total soil OC concentrations and stocks decreased significantly after the grassland was converted to cropland or shrubland. Soil microbial biomass C, root biomass, and root C also declined. The proportion of soil in the macroaggregate fraction decreased after conversion to cropland or shrubland. Decreases in macroaggregate-associated OC stocks accounted for more than half of the OC losses that occurred when grassland was converted to cropland. The decreases in macroaggregate-associated OC stocks were due to declines in both macroaggregation and macroaggregate-associated OC concentrations after conversion to cropland. In contrast, decreases in microaggregate-associated OC stocks accounted for more than half of the OC losses when grassland was converted to shrubland. The declines in microaggregate-associated OC stocks were primarily due to a decrease in microaggregate-associated OC concentrations after conversion to shrubland. Conclusions Land use changed caused significant decreases in soil OC stocks. Conversion to cropland soil resulted in large decreases in macroaggregate-associated OC stocks whereas conversion to shrubland resulted in large decreases in microaggregate-associated OC stocks. Any changes in land use in semiarid grasslands could cause the grassland soil to become a source of atmospheric CO2; therefore extreme caution should be taken to avoid this hazard.</description><subject>Agricultural land</subject><subject>Agricultural soils</subject><subject>Agronomy. Soil science and plant productions</subject><subject>Animal, plant and microbial ecology</subject><subject>Biological and medical sciences</subject><subject>Biomass</subject><subject>Biomedical and Life Sciences</subject><subject>Carbon</subject><subject>Carbon content</subject><subject>Carbon dioxide</subject><subject>Carbon sequestration</subject><subject>Chemical, physicochemical, biochemical and biological properties</subject><subject>China</subject><subject>Desert soils</subject><subject>Ecology</subject><subject>Environment</subject><subject>Environmental aspects</subject><subject>Farmlands</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>General agronomy. Plant production</subject><subject>Geochemistry</subject><subject>Grassland soils</subject><subject>Grasslands</subject><subject>Land use</subject><subject>Land use change</subject><subject>Life Sciences</subject><subject>Organic carbon</subject><subject>Organic matter</subject><subject>Physics, chemistry, biochemistry and biology of agricultural and forest soils</subject><subject>Plant Physiology</subject><subject>Plant Sciences</subject><subject>Plant-soil relationships</subject><subject>Regular Article</subject><subject>Roots</subject><subject>Semiarid grasslands</subject><subject>Shrublands</subject><subject>Size distribution</subject><subject>Soil</subject><subject>Soil aggregation</subject><subject>Soil depth</subject><subject>Soil science</subject><subject>Soil Science & Conservation</subject><subject>Soil-plant relationships. Soil fertility</subject><subject>Soil-plant relationships. Soil fertility. Fertilization. Amendments</subject><subject>Soils</subject><subject>Soils (organic)</subject><issn>0032-079X</issn><issn>1573-5036</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1kU9rFTEUxYMo-Kx-ABdCQAQ3U3OTTCZZllJtoeBCBXdDXv4885iX1NwZqN_eDFO0CJJFcpPfOZybS8hrYOfA2PABAYDJjgF0wIzp7p-QHfSD6Hom1FOyY0zwjg3m-3PyAvHI1hrUjtx8KWmipR5sTo46W_cl06kgBqR-CXQudLLZ0wUDdT9sPgSaMrUUwynZmjw9VIu4Ii_Js2gnDK8e9jPy7ePV18vr7vbzp5vLi9vOScnmTkUrjAfjtZfA7N6KwLWMslch9h78XmvXjjp4IVsRfFRaGct9D4EbxcUZeb_53tXycwk4j6eELkwtQygLjsA40_1g2Iq-_Qc9lqXmlq5RoKTsGVONOt-og53CmHIsc7WuLd96dCWHmNr9hVAwAGgQTQCbwNX2UTXE8a6mk62_muu4TmPcpjG2aYzrNMb7pnn3EMWis1OsNruEf4S8N4PkRjeObxy2p_bb9XHk_5u_2URHnEv9ayrFsLYpfgNaWaJZ</recordid><startdate>20120601</startdate><enddate>20120601</enddate><creator>Qiu, Liping</creator><creator>Wei, Xiaorong</creator><creator>Zhang, Xingchang</creator><creator>Cheng, Jimin</creator><creator>Gale, William</creator><creator>Guo, Chao</creator><creator>Long, Tao</creator><general>Springer</general><general>Springer Netherlands</general><general>Springer Nature B.V</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7SN</scope><scope>7ST</scope><scope>7T7</scope><scope>7X2</scope><scope>88A</scope><scope>8FD</scope><scope>8FE</scope><scope>8FH</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BBNVY</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>HCIFZ</scope><scope>LK8</scope><scope>M0K</scope><scope>M7P</scope><scope>P64</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>RC3</scope><scope>SOI</scope><scope>7U6</scope></search><sort><creationdate>20120601</creationdate><title>Soil organic carbon losses due to land use change in a semiarid grassland</title><author>Qiu, Liping ; Wei, Xiaorong ; Zhang, Xingchang ; Cheng, Jimin ; Gale, William ; Guo, Chao ; Long, Tao</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c440t-6fa39d19d8d410aba3e284f456ef5d1db88c6ef8ed34db8edf6869a2d51e29623</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Agricultural land</topic><topic>Agricultural soils</topic><topic>Agronomy. Soil science and plant productions</topic><topic>Animal, plant and microbial ecology</topic><topic>Biological and medical sciences</topic><topic>Biomass</topic><topic>Biomedical and Life Sciences</topic><topic>Carbon</topic><topic>Carbon content</topic><topic>Carbon dioxide</topic><topic>Carbon sequestration</topic><topic>Chemical, physicochemical, biochemical and biological properties</topic><topic>China</topic><topic>Desert soils</topic><topic>Ecology</topic><topic>Environment</topic><topic>Environmental aspects</topic><topic>Farmlands</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>General agronomy. Plant production</topic><topic>Geochemistry</topic><topic>Grassland soils</topic><topic>Grasslands</topic><topic>Land use</topic><topic>Land use change</topic><topic>Life Sciences</topic><topic>Organic carbon</topic><topic>Organic matter</topic><topic>Physics, chemistry, biochemistry and biology of agricultural and forest soils</topic><topic>Plant Physiology</topic><topic>Plant Sciences</topic><topic>Plant-soil relationships</topic><topic>Regular Article</topic><topic>Roots</topic><topic>Semiarid grasslands</topic><topic>Shrublands</topic><topic>Size distribution</topic><topic>Soil</topic><topic>Soil aggregation</topic><topic>Soil depth</topic><topic>Soil science</topic><topic>Soil Science & Conservation</topic><topic>Soil-plant relationships. Soil fertility</topic><topic>Soil-plant relationships. Soil fertility. Fertilization. Amendments</topic><topic>Soils</topic><topic>Soils (organic)</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Qiu, Liping</creatorcontrib><creatorcontrib>Wei, Xiaorong</creatorcontrib><creatorcontrib>Zhang, Xingchang</creatorcontrib><creatorcontrib>Cheng, Jimin</creatorcontrib><creatorcontrib>Gale, William</creatorcontrib><creatorcontrib>Guo, Chao</creatorcontrib><creatorcontrib>Long, Tao</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Ecology Abstracts</collection><collection>Environment Abstracts</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Agricultural Science Collection</collection><collection>Biology Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>Biological Science Collection</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>SciTech Premium Collection</collection><collection>ProQuest Biological Science Collection</collection><collection>Agricultural Science Database</collection><collection>Biological Science Database</collection><collection>Biotechnology and BioEngineering Abstracts</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Genetics Abstracts</collection><collection>Environment Abstracts</collection><collection>Sustainability Science Abstracts</collection><jtitle>Plant and soil</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Qiu, Liping</au><au>Wei, Xiaorong</au><au>Zhang, Xingchang</au><au>Cheng, Jimin</au><au>Gale, William</au><au>Guo, Chao</au><au>Long, Tao</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Soil organic carbon losses due to land use change in a semiarid grassland</atitle><jtitle>Plant and soil</jtitle><stitle>Plant Soil</stitle><date>2012-06-01</date><risdate>2012</risdate><volume>355</volume><issue>1/2</issue><spage>299</spage><epage>309</epage><pages>299-309</pages><issn>0032-079X</issn><eissn>1573-5036</eissn><coden>PLSOA2</coden><abstract>Background and Aims Knowledge about the effect of land use change on soil organic carbon (OC) in semiarid grassland is essential for understanding C cycles and for forecasting ecosystem C sequestration. Our objectives were (1) to study the effect of land use change on aggregate size distribution, aggregate-associated OC concentrations, and aggregate-associated stocks in a semiarid grassland area and (2) to relate changes in the aggregate fractions to changes in total soil OC. Methods Cropland and shrubland plots were established in a semiarid grassland area in 1982. We collected soil samples from adjacent grassland, cropland, and shrubland plots 27 years later and measured OC concentrations in the macroaggregate (>0.25 mm), microaggregate (0.25–0.053 mm) and silt+clay (<0.053 mm) fractions. Results Total soil OC concentrations and stocks decreased significantly after the grassland was converted to cropland or shrubland. Soil microbial biomass C, root biomass, and root C also declined. The proportion of soil in the macroaggregate fraction decreased after conversion to cropland or shrubland. Decreases in macroaggregate-associated OC stocks accounted for more than half of the OC losses that occurred when grassland was converted to cropland. The decreases in macroaggregate-associated OC stocks were due to declines in both macroaggregation and macroaggregate-associated OC concentrations after conversion to cropland. In contrast, decreases in microaggregate-associated OC stocks accounted for more than half of the OC losses when grassland was converted to shrubland. The declines in microaggregate-associated OC stocks were primarily due to a decrease in microaggregate-associated OC concentrations after conversion to shrubland. Conclusions Land use changed caused significant decreases in soil OC stocks. Conversion to cropland soil resulted in large decreases in macroaggregate-associated OC stocks whereas conversion to shrubland resulted in large decreases in microaggregate-associated OC stocks. Any changes in land use in semiarid grasslands could cause the grassland soil to become a source of atmospheric CO2; therefore extreme caution should be taken to avoid this hazard.</abstract><cop>Dordrecht</cop><pub>Springer</pub><doi>10.1007/s11104-011-1099-x</doi><tpages>11</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0032-079X |
| ispartof | Plant and soil, 2012-06, Vol.355 (1/2), p.299-309 |
| issn | 0032-079X 1573-5036 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_1020857902 |
| source | SpringerNature Journals; JSTOR Archive Collection A-Z Listing |
| subjects | Agricultural land Agricultural soils Agronomy. Soil science and plant productions Animal, plant and microbial ecology Biological and medical sciences Biomass Biomedical and Life Sciences Carbon Carbon content Carbon dioxide Carbon sequestration Chemical, physicochemical, biochemical and biological properties China Desert soils Ecology Environment Environmental aspects Farmlands Fundamental and applied biological sciences. Psychology General agronomy. Plant production Geochemistry Grassland soils Grasslands Land use Land use change Life Sciences Organic carbon Organic matter Physics, chemistry, biochemistry and biology of agricultural and forest soils Plant Physiology Plant Sciences Plant-soil relationships Regular Article Roots Semiarid grasslands Shrublands Size distribution Soil Soil aggregation Soil depth Soil science Soil Science & Conservation Soil-plant relationships. Soil fertility Soil-plant relationships. Soil fertility. Fertilization. Amendments Soils Soils (organic) |
| title | Soil organic carbon losses due to land use change in a semiarid grassland |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-26T20%3A09%3A52IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-gale_proqu&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Soil%20organic%20carbon%20losses%20due%20to%20land%20use%20change%20in%20a%20semiarid%20grassland&rft.jtitle=Plant%20and%20soil&rft.au=Qiu,%20Liping&rft.date=2012-06-01&rft.volume=355&rft.issue=1/2&rft.spage=299&rft.epage=309&rft.pages=299-309&rft.issn=0032-079X&rft.eissn=1573-5036&rft.coden=PLSOA2&rft_id=info:doi/10.1007/s11104-011-1099-x&rft_dat=%3Cgale_proqu%3EA361711813%3C/gale_proqu%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1016445006&rft_id=info:pmid/&rft_galeid=A361711813&rft_jstor_id=24370164&rfr_iscdi=true |