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Long-Term Changes in Soil Carbon Stocks in the Brazilian Cerrado Under Commercial Soybean
The net effect of agriculture on soil carbon is not yet fully understood. While a number of studies on shallow profiles have been published, evidence suggests that carbon stock changes occur in deeper layers. In this study we analyzed the effect of agriculture in the Cerrado soil C looking at change...
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Published in: | Land degradation & development 2016-08, Vol.27 (6), p.1586-1594 |
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description | The net effect of agriculture on soil carbon is not yet fully understood. While a number of studies on shallow profiles have been published, evidence suggests that carbon stock changes occur in deeper layers. In this study we analyzed the effect of agriculture in the Cerrado soil C looking at changes in seven different profile depths from 0 to 100 cm in a commercial grain farm. We also used isotopic techniques to distinguish between the original Cerrado C3 carbon and the C4 carbon derived from the grasses used in agriculture. At 0–5 cm depth C stocks significantly decreased with cultivation time. The C stock did not change significantly when it was calculated using the 0–10, 0–20, 0–30, 0–50 or 0–75 cm profile (p > 0·05) but increased with cultivation time when the profile considered was 0–100 cm (p |
doi_str_mv | 10.1002/ldr.2473 |
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While a number of studies on shallow profiles have been published, evidence suggests that carbon stock changes occur in deeper layers. In this study we analyzed the effect of agriculture in the Cerrado soil C looking at changes in seven different profile depths from 0 to 100 cm in a commercial grain farm. We also used isotopic techniques to distinguish between the original Cerrado C3 carbon and the C4 carbon derived from the grasses used in agriculture. At 0–5 cm depth C stocks significantly decreased with cultivation time. The C stock did not change significantly when it was calculated using the 0–10, 0–20, 0–30, 0–50 or 0–75 cm profile (p > 0·05) but increased with cultivation time when the profile considered was 0–100 cm (p < 0·05). A two‐source isotope model revealed that there was a significant increase in carbon derived from C4 grasses for all depths with cultivation time. Annual carbon sequestration rates for the upper 100 cm of soil were 1·1 Mg C ha−1 year−1 for total carbon and 0·8 Mg C4 C ha−1 year−1 for C4 carbon. The oldest area, with 23 years of cultivation, had a soil C stock increase compared to the native Cerrado soil of 17·6%. These findings suggest that commercial grain farms practices may increase soil C stock compared to native Cerrado soil, if a more complete soil profile down to 100 cm is used to assess C stocks. Copyright © 2015 John Wiley & Sons, Ltd.</description><identifier>ISSN: 1085-3278</identifier><identifier>EISSN: 1099-145X</identifier><identifier>DOI: 10.1002/ldr.2473</identifier><identifier>CODEN: LDDEF6</identifier><language>eng</language><publisher>Chichester: Blackwell Publishing Ltd</publisher><subject>Agriculture ; C3 carbon ; C4 carbon ; Carbon ; Cerrado ; Cultivation ; Farms ; Grains ; Grasses ; Raw materials ; Soil (material) ; soil carbon</subject><ispartof>Land degradation & development, 2016-08, Vol.27 (6), p.1586-1594</ispartof><rights>Copyright © 2015 John Wiley & Sons, Ltd.</rights><rights>Copyright © 2016 John Wiley & Sons, Ltd.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3973-1b60fb021aee7979cd2bae3df4a7b9858d62c103d289a3a47aca1cffbeb7a6d83</citedby><cites>FETCH-LOGICAL-c3973-1b60fb021aee7979cd2bae3df4a7b9858d62c103d289a3a47aca1cffbeb7a6d83</cites><orcidid>0000-0002-4259-5028</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Miranda, Eduardo</creatorcontrib><creatorcontrib>Carmo, Janaina</creatorcontrib><creatorcontrib>Couto, Eduardo</creatorcontrib><creatorcontrib>Camargo, Plínio</creatorcontrib><title>Long-Term Changes in Soil Carbon Stocks in the Brazilian Cerrado Under Commercial Soybean</title><title>Land degradation & development</title><addtitle>Land Degrad. Develop</addtitle><description>The net effect of agriculture on soil carbon is not yet fully understood. While a number of studies on shallow profiles have been published, evidence suggests that carbon stock changes occur in deeper layers. In this study we analyzed the effect of agriculture in the Cerrado soil C looking at changes in seven different profile depths from 0 to 100 cm in a commercial grain farm. We also used isotopic techniques to distinguish between the original Cerrado C3 carbon and the C4 carbon derived from the grasses used in agriculture. At 0–5 cm depth C stocks significantly decreased with cultivation time. The C stock did not change significantly when it was calculated using the 0–10, 0–20, 0–30, 0–50 or 0–75 cm profile (p > 0·05) but increased with cultivation time when the profile considered was 0–100 cm (p < 0·05). A two‐source isotope model revealed that there was a significant increase in carbon derived from C4 grasses for all depths with cultivation time. Annual carbon sequestration rates for the upper 100 cm of soil were 1·1 Mg C ha−1 year−1 for total carbon and 0·8 Mg C4 C ha−1 year−1 for C4 carbon. The oldest area, with 23 years of cultivation, had a soil C stock increase compared to the native Cerrado soil of 17·6%. These findings suggest that commercial grain farms practices may increase soil C stock compared to native Cerrado soil, if a more complete soil profile down to 100 cm is used to assess C stocks. Copyright © 2015 John Wiley & Sons, Ltd.</description><subject>Agriculture</subject><subject>C3 carbon</subject><subject>C4 carbon</subject><subject>Carbon</subject><subject>Cerrado</subject><subject>Cultivation</subject><subject>Farms</subject><subject>Grains</subject><subject>Grasses</subject><subject>Raw materials</subject><subject>Soil (material)</subject><subject>soil carbon</subject><issn>1085-3278</issn><issn>1099-145X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><recordid>eNqN0UtLxDAQB_AiCj7Bj1Dw4qWaR9skR63uqiy-RT2FaTrVaNtosouun96uiqAgeJph-M3A8I-idUq2KCFsu6n8FksFn4uWKFEqoWl2Mz_rZZZwJuRitBzCAyGEilQsRbcj190ll-jbuLiH7g5DbLv4wtkmLsCXru_Hzjx-TMf3GO96eLONhS4u0HuoXHzVVejjwrUtemOh6ZenJUK3Gi3U0ARc-6or0dVg_7I4SEYnw8NiZ5QYrgRPaJmTuiSMAqJQQpmKlYC8qlMQpZKZrHJmKOEVkwo4pAIMUFPXJZYC8krylWjz8-6Td88TDGPd2mCwaaBDNwmaSp7lXKU5-QelVCrGZdrTjV_0wU181z_SKyKYzOWH-jpovAvBY62fvG3BTzUlehaH7uPQszh6mnzSF9vg9E-nR3vnP70NY3z99uAfdS64yPT18VCfHbGL07Oh1AP-Dt2nmcI</recordid><startdate>201608</startdate><enddate>201608</enddate><creator>Miranda, Eduardo</creator><creator>Carmo, Janaina</creator><creator>Couto, Eduardo</creator><creator>Camargo, Plínio</creator><general>Blackwell Publishing Ltd</general><general>Wiley Subscription Services, Inc</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>8FD</scope><scope>C1K</scope><scope>FR3</scope><scope>KR7</scope><scope>SOI</scope><orcidid>https://orcid.org/0000-0002-4259-5028</orcidid></search><sort><creationdate>201608</creationdate><title>Long-Term Changes in Soil Carbon Stocks in the Brazilian Cerrado Under Commercial Soybean</title><author>Miranda, Eduardo ; Carmo, Janaina ; Couto, Eduardo ; Camargo, Plínio</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3973-1b60fb021aee7979cd2bae3df4a7b9858d62c103d289a3a47aca1cffbeb7a6d83</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Agriculture</topic><topic>C3 carbon</topic><topic>C4 carbon</topic><topic>Carbon</topic><topic>Cerrado</topic><topic>Cultivation</topic><topic>Farms</topic><topic>Grains</topic><topic>Grasses</topic><topic>Raw materials</topic><topic>Soil (material)</topic><topic>soil carbon</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Miranda, Eduardo</creatorcontrib><creatorcontrib>Carmo, Janaina</creatorcontrib><creatorcontrib>Couto, Eduardo</creatorcontrib><creatorcontrib>Camargo, Plínio</creatorcontrib><collection>Istex</collection><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><collection>Environment Abstracts</collection><jtitle>Land degradation & development</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Miranda, Eduardo</au><au>Carmo, Janaina</au><au>Couto, Eduardo</au><au>Camargo, Plínio</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Long-Term Changes in Soil Carbon Stocks in the Brazilian Cerrado Under Commercial Soybean</atitle><jtitle>Land degradation & development</jtitle><addtitle>Land Degrad. Develop</addtitle><date>2016-08</date><risdate>2016</risdate><volume>27</volume><issue>6</issue><spage>1586</spage><epage>1594</epage><pages>1586-1594</pages><issn>1085-3278</issn><eissn>1099-145X</eissn><coden>LDDEF6</coden><abstract>The net effect of agriculture on soil carbon is not yet fully understood. While a number of studies on shallow profiles have been published, evidence suggests that carbon stock changes occur in deeper layers. In this study we analyzed the effect of agriculture in the Cerrado soil C looking at changes in seven different profile depths from 0 to 100 cm in a commercial grain farm. We also used isotopic techniques to distinguish between the original Cerrado C3 carbon and the C4 carbon derived from the grasses used in agriculture. At 0–5 cm depth C stocks significantly decreased with cultivation time. The C stock did not change significantly when it was calculated using the 0–10, 0–20, 0–30, 0–50 or 0–75 cm profile (p > 0·05) but increased with cultivation time when the profile considered was 0–100 cm (p < 0·05). A two‐source isotope model revealed that there was a significant increase in carbon derived from C4 grasses for all depths with cultivation time. Annual carbon sequestration rates for the upper 100 cm of soil were 1·1 Mg C ha−1 year−1 for total carbon and 0·8 Mg C4 C ha−1 year−1 for C4 carbon. The oldest area, with 23 years of cultivation, had a soil C stock increase compared to the native Cerrado soil of 17·6%. These findings suggest that commercial grain farms practices may increase soil C stock compared to native Cerrado soil, if a more complete soil profile down to 100 cm is used to assess C stocks. Copyright © 2015 John Wiley & Sons, Ltd.</abstract><cop>Chichester</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1002/ldr.2473</doi><tpages>9</tpages><orcidid>https://orcid.org/0000-0002-4259-5028</orcidid></addata></record> |
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subjects | Agriculture C3 carbon C4 carbon Carbon Cerrado Cultivation Farms Grains Grasses Raw materials Soil (material) soil carbon |
title | Long-Term Changes in Soil Carbon Stocks in the Brazilian Cerrado Under Commercial Soybean |
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