Long-term impact of fertilizers on soil organic carbon pools and sequestration rates in maize–wheat–cowpea cropping system
We assessed the impact of long-term manuring and fertilization on changes in different SOC fractions over ten years period (1994–2003) in a Typic Haplustept under intensive cropping with maize ( Zea mays L.) — wheat ( Triticum aestivum L.) — cowpea ( Vigna unguiculata) in semi-arid, sub-tropical Ind...
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description | We assessed the impact of long-term manuring and fertilization on changes in different SOC fractions over ten years period (1994–2003) in a Typic Haplustept under intensive cropping with maize (
Zea mays L.) — wheat (
Triticum aestivum L.) — cowpea (
Vigna unguiculata) in semi-arid, sub-tropical India. The application of graded doses of NPK from 50% (130 kg N, 35 kg P and 41.5 kg K ha
−
1
) to 150% (390 kg N, 105 kg P and 124 kg K ha
−
1
) in the cropping system significantly enhanced SOC, particulate organic C (POC) and KMnO
4 oxidizable C (KMnO
4–C) fractions in soil. The increase in these C fractions was greater when farmyard manure (FYM) was applied conjointly with 100% NPK (260 kg N, 70 kg P and 83 kg K ha
−
1
). This treatment showed highest amount of SOC (58.3 Mg C ha
−
1
in 1994 and 72.1 Mg C ha
−
1
in 2003), POC (5.30 Mg C ha
−
1
in 1994 and 6.33 Mg C ha
−
1
in 2003) and KMnO
4-C (10.05 Mg C ha
−
1
in 1994 and 11.2 Mg C ha
−
1
in 2003) in 0–45 cm soil depth. The C sequestration rate in SOC calculated over ten year period (1994–2003) was highest with 100% NPK
+
FYM (997 kg C ha
−
1
yr
−
1
) followed by the 150% NPK (553 kg C ha
−
1
yr
−
1
). It was estimated that 17.1 to 34.0% of the gross C input over ten year period contributed towards the increase in SOC content, while C sequestration efficiency (CSE) in POC (varied between 1.28 and 2.58%) was lower than KMnO
4-C (varied between 1.42 and 3.72%). The CSE was highest in 150% NPK treatment, while 100% NPK
+
FYM showed the lowest CSE. By applying the values of humification constant (
h) and decay constant (
k) in Jenkinson's equation, it is possible to predict SOC level in the year 2003 and the C inputs required to maintain the SOC level in the year 1994 (
A
E) were calculated from Jenkinson's equation. The low
k value in native SOC was responsible for lower requirements of C input required to maintain SOC in equilibrium. Thus increase in SOC concentration under long-term maize–wheat–cowpea cropping was due to the fact that annual C input by the system was higher than
A
E. In semi-arid sub-tropical India, continuous adoption of 100% NPK
+
FYM treatment in maize–wheat–cowpea cropping system might sequester 1.83 Tg C yr
−
1
which corresponds to about 1% of the fossil fuel emissions by India. |
doi_str_mv | 10.1016/j.geoderma.2007.12.006 |
format | Article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_19634423</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0016706107003588</els_id><sourcerecordid>19634423</sourcerecordid><originalsourceid>FETCH-LOGICAL-a396t-103dc734724bafb6f1d74b0c29addc98252ced9bc40a9ff32caba02ea6355ec43</originalsourceid><addsrcrecordid>eNqFkE2O1DAQhS0EEs3AFZA3sEsoO4nT2YFG_EktsYG1VXHKjVuJHVwZRsMCcQduyEnw0ANbVk8ufc_16gnxVEGtQJkXp_pIaaK8YK0B-lrpGsDcEzu173VldDfcFzsoZNWDUQ_FI-ZTefagYSe-H1I8Vltxy7Cs6DaZvPSUtzCHb5RZpig5hVmmfMQYnHSYxzJbU5pZYpwk05cr4i3jFsq8CLEMUS5Y_L9-_Lz-TLgVdel6JZQup3UN8Sj5hjdaHosHHmemJ3d6IT69ef3x8l11-PD2_eWrQ4XNYLZKQTO5vml73Y7oR-PV1LcjOD3gNLlhrzvtaBpG1wIO3jfa4YigCU3TdeTa5kI8P_-75vQnrl0CO5pnjJSu2KrBNG2rmwKaM1iCMmfyds1hwXxjFdjbuu3J_q3b3tZtlbal7mJ8drcB2eHsM0YX-J9bg-r2LUDhXp45Kud-DZQtu0CxxA-Z3GanFP636jeb-Z9B</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>19634423</pqid></control><display><type>article</type><title>Long-term impact of fertilizers on soil organic carbon pools and sequestration rates in maize–wheat–cowpea cropping system</title><source>Access via ScienceDirect (Elsevier)</source><creator>Purakayastha, T.J. ; Rudrappa, L. ; Singh, D. ; Swarup, A. ; Bhadraray, S.</creator><creatorcontrib>Purakayastha, T.J. ; Rudrappa, L. ; Singh, D. ; Swarup, A. ; Bhadraray, S.</creatorcontrib><description>We assessed the impact of long-term manuring and fertilization on changes in different SOC fractions over ten years period (1994–2003) in a Typic Haplustept under intensive cropping with maize (
Zea mays L.) — wheat (
Triticum aestivum L.) — cowpea (
Vigna unguiculata) in semi-arid, sub-tropical India. The application of graded doses of NPK from 50% (130 kg N, 35 kg P and 41.5 kg K ha
−
1
) to 150% (390 kg N, 105 kg P and 124 kg K ha
−
1
) in the cropping system significantly enhanced SOC, particulate organic C (POC) and KMnO
4 oxidizable C (KMnO
4–C) fractions in soil. The increase in these C fractions was greater when farmyard manure (FYM) was applied conjointly with 100% NPK (260 kg N, 70 kg P and 83 kg K ha
−
1
). This treatment showed highest amount of SOC (58.3 Mg C ha
−
1
in 1994 and 72.1 Mg C ha
−
1
in 2003), POC (5.30 Mg C ha
−
1
in 1994 and 6.33 Mg C ha
−
1
in 2003) and KMnO
4-C (10.05 Mg C ha
−
1
in 1994 and 11.2 Mg C ha
−
1
in 2003) in 0–45 cm soil depth. The C sequestration rate in SOC calculated over ten year period (1994–2003) was highest with 100% NPK
+
FYM (997 kg C ha
−
1
yr
−
1
) followed by the 150% NPK (553 kg C ha
−
1
yr
−
1
). It was estimated that 17.1 to 34.0% of the gross C input over ten year period contributed towards the increase in SOC content, while C sequestration efficiency (CSE) in POC (varied between 1.28 and 2.58%) was lower than KMnO
4-C (varied between 1.42 and 3.72%). The CSE was highest in 150% NPK treatment, while 100% NPK
+
FYM showed the lowest CSE. By applying the values of humification constant (
h) and decay constant (
k) in Jenkinson's equation, it is possible to predict SOC level in the year 2003 and the C inputs required to maintain the SOC level in the year 1994 (
A
E) were calculated from Jenkinson's equation. The low
k value in native SOC was responsible for lower requirements of C input required to maintain SOC in equilibrium. Thus increase in SOC concentration under long-term maize–wheat–cowpea cropping was due to the fact that annual C input by the system was higher than
A
E. In semi-arid sub-tropical India, continuous adoption of 100% NPK
+
FYM treatment in maize–wheat–cowpea cropping system might sequester 1.83 Tg C yr
−
1
which corresponds to about 1% of the fossil fuel emissions by India.</description><identifier>ISSN: 0016-7061</identifier><identifier>EISSN: 1872-6259</identifier><identifier>DOI: 10.1016/j.geoderma.2007.12.006</identifier><identifier>CODEN: GEDMAB</identifier><language>eng</language><publisher>Amsterdam: Elsevier B.V</publisher><subject>Agronomy. Soil science and plant productions ; Biological and medical sciences ; Carbon sequestration ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Farmyard manure ; Fundamental and applied biological sciences. Psychology ; Geochemistry ; Long-term fertilizer experiment ; Microbial biomass C, NPK fertilizer ; Particulate organic C ; Root biomass ; Soil and rock geochemistry ; Soil organic C ; Soils ; Surficial geology ; Triticum aestivum ; Vigna unguiculata ; Zea mays</subject><ispartof>Geoderma, 2008-03, Vol.144 (1), p.370-378</ispartof><rights>2007 Elsevier B.V.</rights><rights>2008 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a396t-103dc734724bafb6f1d74b0c29addc98252ced9bc40a9ff32caba02ea6355ec43</citedby><cites>FETCH-LOGICAL-a396t-103dc734724bafb6f1d74b0c29addc98252ced9bc40a9ff32caba02ea6355ec43</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/j.geoderma.2007.12.006$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,3550,27924,27925,45995</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=20158400$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Purakayastha, T.J.</creatorcontrib><creatorcontrib>Rudrappa, L.</creatorcontrib><creatorcontrib>Singh, D.</creatorcontrib><creatorcontrib>Swarup, A.</creatorcontrib><creatorcontrib>Bhadraray, S.</creatorcontrib><title>Long-term impact of fertilizers on soil organic carbon pools and sequestration rates in maize–wheat–cowpea cropping system</title><title>Geoderma</title><description>We assessed the impact of long-term manuring and fertilization on changes in different SOC fractions over ten years period (1994–2003) in a Typic Haplustept under intensive cropping with maize (
Zea mays L.) — wheat (
Triticum aestivum L.) — cowpea (
Vigna unguiculata) in semi-arid, sub-tropical India. The application of graded doses of NPK from 50% (130 kg N, 35 kg P and 41.5 kg K ha
−
1
) to 150% (390 kg N, 105 kg P and 124 kg K ha
−
1
) in the cropping system significantly enhanced SOC, particulate organic C (POC) and KMnO
4 oxidizable C (KMnO
4–C) fractions in soil. The increase in these C fractions was greater when farmyard manure (FYM) was applied conjointly with 100% NPK (260 kg N, 70 kg P and 83 kg K ha
−
1
). This treatment showed highest amount of SOC (58.3 Mg C ha
−
1
in 1994 and 72.1 Mg C ha
−
1
in 2003), POC (5.30 Mg C ha
−
1
in 1994 and 6.33 Mg C ha
−
1
in 2003) and KMnO
4-C (10.05 Mg C ha
−
1
in 1994 and 11.2 Mg C ha
−
1
in 2003) in 0–45 cm soil depth. The C sequestration rate in SOC calculated over ten year period (1994–2003) was highest with 100% NPK
+
FYM (997 kg C ha
−
1
yr
−
1
) followed by the 150% NPK (553 kg C ha
−
1
yr
−
1
). It was estimated that 17.1 to 34.0% of the gross C input over ten year period contributed towards the increase in SOC content, while C sequestration efficiency (CSE) in POC (varied between 1.28 and 2.58%) was lower than KMnO
4-C (varied between 1.42 and 3.72%). The CSE was highest in 150% NPK treatment, while 100% NPK
+
FYM showed the lowest CSE. By applying the values of humification constant (
h) and decay constant (
k) in Jenkinson's equation, it is possible to predict SOC level in the year 2003 and the C inputs required to maintain the SOC level in the year 1994 (
A
E) were calculated from Jenkinson's equation. The low
k value in native SOC was responsible for lower requirements of C input required to maintain SOC in equilibrium. Thus increase in SOC concentration under long-term maize–wheat–cowpea cropping was due to the fact that annual C input by the system was higher than
A
E. In semi-arid sub-tropical India, continuous adoption of 100% NPK
+
FYM treatment in maize–wheat–cowpea cropping system might sequester 1.83 Tg C yr
−
1
which corresponds to about 1% of the fossil fuel emissions by India.</description><subject>Agronomy. Soil science and plant productions</subject><subject>Biological and medical sciences</subject><subject>Carbon sequestration</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Farmyard manure</subject><subject>Fundamental and applied biological sciences. Psychology</subject><subject>Geochemistry</subject><subject>Long-term fertilizer experiment</subject><subject>Microbial biomass C, NPK fertilizer</subject><subject>Particulate organic C</subject><subject>Root biomass</subject><subject>Soil and rock geochemistry</subject><subject>Soil organic C</subject><subject>Soils</subject><subject>Surficial geology</subject><subject>Triticum aestivum</subject><subject>Vigna unguiculata</subject><subject>Zea mays</subject><issn>0016-7061</issn><issn>1872-6259</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2008</creationdate><recordtype>article</recordtype><recordid>eNqFkE2O1DAQhS0EEs3AFZA3sEsoO4nT2YFG_EktsYG1VXHKjVuJHVwZRsMCcQduyEnw0ANbVk8ufc_16gnxVEGtQJkXp_pIaaK8YK0B-lrpGsDcEzu173VldDfcFzsoZNWDUQ_FI-ZTefagYSe-H1I8Vltxy7Cs6DaZvPSUtzCHb5RZpig5hVmmfMQYnHSYxzJbU5pZYpwk05cr4i3jFsq8CLEMUS5Y_L9-_Lz-TLgVdel6JZQup3UN8Sj5hjdaHosHHmemJ3d6IT69ef3x8l11-PD2_eWrQ4XNYLZKQTO5vml73Y7oR-PV1LcjOD3gNLlhrzvtaBpG1wIO3jfa4YigCU3TdeTa5kI8P_-75vQnrl0CO5pnjJSu2KrBNG2rmwKaM1iCMmfyds1hwXxjFdjbuu3J_q3b3tZtlbal7mJ8drcB2eHsM0YX-J9bg-r2LUDhXp45Kud-DZQtu0CxxA-Z3GanFP636jeb-Z9B</recordid><startdate>20080315</startdate><enddate>20080315</enddate><creator>Purakayastha, T.J.</creator><creator>Rudrappa, L.</creator><creator>Singh, D.</creator><creator>Swarup, A.</creator><creator>Bhadraray, S.</creator><general>Elsevier B.V</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7TV</scope><scope>7U6</scope><scope>C1K</scope><scope>F1W</scope><scope>H98</scope><scope>L.G</scope></search><sort><creationdate>20080315</creationdate><title>Long-term impact of fertilizers on soil organic carbon pools and sequestration rates in maize–wheat–cowpea cropping system</title><author>Purakayastha, T.J. ; Rudrappa, L. ; Singh, D. ; Swarup, A. ; Bhadraray, S.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a396t-103dc734724bafb6f1d74b0c29addc98252ced9bc40a9ff32caba02ea6355ec43</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2008</creationdate><topic>Agronomy. Soil science and plant productions</topic><topic>Biological and medical sciences</topic><topic>Carbon sequestration</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Farmyard manure</topic><topic>Fundamental and applied biological sciences. Psychology</topic><topic>Geochemistry</topic><topic>Long-term fertilizer experiment</topic><topic>Microbial biomass C, NPK fertilizer</topic><topic>Particulate organic C</topic><topic>Root biomass</topic><topic>Soil and rock geochemistry</topic><topic>Soil organic C</topic><topic>Soils</topic><topic>Surficial geology</topic><topic>Triticum aestivum</topic><topic>Vigna unguiculata</topic><topic>Zea mays</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Purakayastha, T.J.</creatorcontrib><creatorcontrib>Rudrappa, L.</creatorcontrib><creatorcontrib>Singh, D.</creatorcontrib><creatorcontrib>Swarup, A.</creatorcontrib><creatorcontrib>Bhadraray, S.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Pollution Abstracts</collection><collection>Sustainability Science Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Aquaculture Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Geoderma</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Purakayastha, T.J.</au><au>Rudrappa, L.</au><au>Singh, D.</au><au>Swarup, A.</au><au>Bhadraray, S.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Long-term impact of fertilizers on soil organic carbon pools and sequestration rates in maize–wheat–cowpea cropping system</atitle><jtitle>Geoderma</jtitle><date>2008-03-15</date><risdate>2008</risdate><volume>144</volume><issue>1</issue><spage>370</spage><epage>378</epage><pages>370-378</pages><issn>0016-7061</issn><eissn>1872-6259</eissn><coden>GEDMAB</coden><abstract>We assessed the impact of long-term manuring and fertilization on changes in different SOC fractions over ten years period (1994–2003) in a Typic Haplustept under intensive cropping with maize (
Zea mays L.) — wheat (
Triticum aestivum L.) — cowpea (
Vigna unguiculata) in semi-arid, sub-tropical India. The application of graded doses of NPK from 50% (130 kg N, 35 kg P and 41.5 kg K ha
−
1
) to 150% (390 kg N, 105 kg P and 124 kg K ha
−
1
) in the cropping system significantly enhanced SOC, particulate organic C (POC) and KMnO
4 oxidizable C (KMnO
4–C) fractions in soil. The increase in these C fractions was greater when farmyard manure (FYM) was applied conjointly with 100% NPK (260 kg N, 70 kg P and 83 kg K ha
−
1
). This treatment showed highest amount of SOC (58.3 Mg C ha
−
1
in 1994 and 72.1 Mg C ha
−
1
in 2003), POC (5.30 Mg C ha
−
1
in 1994 and 6.33 Mg C ha
−
1
in 2003) and KMnO
4-C (10.05 Mg C ha
−
1
in 1994 and 11.2 Mg C ha
−
1
in 2003) in 0–45 cm soil depth. The C sequestration rate in SOC calculated over ten year period (1994–2003) was highest with 100% NPK
+
FYM (997 kg C ha
−
1
yr
−
1
) followed by the 150% NPK (553 kg C ha
−
1
yr
−
1
). It was estimated that 17.1 to 34.0% of the gross C input over ten year period contributed towards the increase in SOC content, while C sequestration efficiency (CSE) in POC (varied between 1.28 and 2.58%) was lower than KMnO
4-C (varied between 1.42 and 3.72%). The CSE was highest in 150% NPK treatment, while 100% NPK
+
FYM showed the lowest CSE. By applying the values of humification constant (
h) and decay constant (
k) in Jenkinson's equation, it is possible to predict SOC level in the year 2003 and the C inputs required to maintain the SOC level in the year 1994 (
A
E) were calculated from Jenkinson's equation. The low
k value in native SOC was responsible for lower requirements of C input required to maintain SOC in equilibrium. Thus increase in SOC concentration under long-term maize–wheat–cowpea cropping was due to the fact that annual C input by the system was higher than
A
E. In semi-arid sub-tropical India, continuous adoption of 100% NPK
+
FYM treatment in maize–wheat–cowpea cropping system might sequester 1.83 Tg C yr
−
1
which corresponds to about 1% of the fossil fuel emissions by India.</abstract><cop>Amsterdam</cop><pub>Elsevier B.V</pub><doi>10.1016/j.geoderma.2007.12.006</doi><tpages>9</tpages></addata></record> |
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subjects | Agronomy. Soil science and plant productions Biological and medical sciences Carbon sequestration Earth sciences Earth, ocean, space Exact sciences and technology Farmyard manure Fundamental and applied biological sciences. Psychology Geochemistry Long-term fertilizer experiment Microbial biomass C, NPK fertilizer Particulate organic C Root biomass Soil and rock geochemistry Soil organic C Soils Surficial geology Triticum aestivum Vigna unguiculata Zea mays |
title | Long-term impact of fertilizers on soil organic carbon pools and sequestration rates in maize–wheat–cowpea cropping system |
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