The Effects of Long‐term Application of Organic Amendments on Soil Organic Carbon Accumulation

Application of organic amendments (e.g., biosolids[BS], composts) to soil may provide an effective method for accumulating considerable amounts of C, but the long term stability of such C is not well known. We investigated study sites in Virginia to determine the amounts of C remaining in soils 7 to...

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Veröffentlicht in:Soil Science Society of America journal 2013-05, Vol.77 (3), p.964-973
Hauptverfasser: Li, Jinling, Evanylo, Gregory K.
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description Application of organic amendments (e.g., biosolids[BS], composts) to soil may provide an effective method for accumulating considerable amounts of C, but the long term stability of such C is not well known. We investigated study sites in Virginia to determine the amounts of C remaining in soils 7 to 27 yr following amending with biosolids and composts. The first study employed a Fauquier silty clay loam (fine, mixed, active, mesic Ultic Hapludalf) to which four treatments (control, poultry litter‐yard waste compost, biosolids compost, and poultry litter) were continuously applied during 2000–2004. The second study was conducted on a Davidson clay loam (fine, kaolinitic, thermic, Rhodic Kandiudult) to which six rates of aerobically digested biosolids (0, 42, 84, 126, 168, and 210 Mg ha–1) were applied in 1984. The third study was on a Pamunkey sandy loam (fine‐loamy, mixed, semiactive, thermic Ultic Hapludalfs) to which five rates of anaerobically digested biosolids (0, 14, 42, 70, and 98 Mg ha–1), with and without sawdust, were applied in 1996. Total soil organic C concentration and bulk density were measured to calculate C accumulation. The organic amendment‐treated soils increased C in the surface soil depth (
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We investigated study sites in Virginia to determine the amounts of C remaining in soils 7 to 27 yr following amending with biosolids and composts. The first study employed a Fauquier silty clay loam (fine, mixed, active, mesic Ultic Hapludalf) to which four treatments (control, poultry litter‐yard waste compost, biosolids compost, and poultry litter) were continuously applied during 2000–2004. The second study was conducted on a Davidson clay loam (fine, kaolinitic, thermic, Rhodic Kandiudult) to which six rates of aerobically digested biosolids (0, 42, 84, 126, 168, and 210 Mg ha–1) were applied in 1984. The third study was on a Pamunkey sandy loam (fine‐loamy, mixed, semiactive, thermic Ultic Hapludalfs) to which five rates of anaerobically digested biosolids (0, 14, 42, 70, and 98 Mg ha–1), with and without sawdust, were applied in 1996. Total soil organic C concentration and bulk density were measured to calculate C accumulation. The organic amendment‐treated soils increased C in the surface soil depth (&lt;15 cm), ranging from 2 to 12% of C across all three sites. Soil C movement was limited to a depth of 15 cm. Evidence of C saturation was revealed in the third study site. These results demonstrate that organic amendments applied over a long time remain in soil and may contribute to C sequestration in the Mid‐Atlantic region.</description><identifier>ISSN: 0361-5995</identifier><identifier>EISSN: 1435-0661</identifier><identifier>DOI: 10.2136/sssaj2012.0306</identifier><identifier>CODEN: SSSJD4</identifier><language>eng</language><publisher>Madison: The Soil Science Society of America, Inc</publisher><subject>Active control ; Agricultural wastes ; Biosolids ; Carbon ; Clay (material) ; Clay loam ; Composting ; Composts ; Decomposition ; Efficiency ; Herbivores ; Litter ; Loams ; Magnesium ; Organic carbon ; Poultry ; Sandy loam ; Sawdust ; Sludge ; Soil (material) ; Soil depth ; Soil surfaces ; Soil treatment ; Solid wastes ; Studies ; Tillage ; Yard waste</subject><ispartof>Soil Science Society of America journal, 2013-05, Vol.77 (3), p.964-973</ispartof><rights>Copyright © by the Soil Science Society of America, Inc.</rights><rights>Copyright American Society of Agronomy May 2013</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3876-4309cdb842c4defffcf2f36a92d2817cb41158d6188ffda9ce71ac1c7c232833</citedby><cites>FETCH-LOGICAL-c3876-4309cdb842c4defffcf2f36a92d2817cb41158d6188ffda9ce71ac1c7c232833</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.2136%2Fsssaj2012.0306$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.2136%2Fsssaj2012.0306$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,27924,27925,45574,45575</link.rule.ids></links><search><creatorcontrib>Li, Jinling</creatorcontrib><creatorcontrib>Evanylo, Gregory K.</creatorcontrib><title>The Effects of Long‐term Application of Organic Amendments on Soil Organic Carbon Accumulation</title><title>Soil Science Society of America journal</title><description>Application of organic amendments (e.g., biosolids[BS], composts) to soil may provide an effective method for accumulating considerable amounts of C, but the long term stability of such C is not well known. We investigated study sites in Virginia to determine the amounts of C remaining in soils 7 to 27 yr following amending with biosolids and composts. The first study employed a Fauquier silty clay loam (fine, mixed, active, mesic Ultic Hapludalf) to which four treatments (control, poultry litter‐yard waste compost, biosolids compost, and poultry litter) were continuously applied during 2000–2004. The second study was conducted on a Davidson clay loam (fine, kaolinitic, thermic, Rhodic Kandiudult) to which six rates of aerobically digested biosolids (0, 42, 84, 126, 168, and 210 Mg ha–1) were applied in 1984. The third study was on a Pamunkey sandy loam (fine‐loamy, mixed, semiactive, thermic Ultic Hapludalfs) to which five rates of anaerobically digested biosolids (0, 14, 42, 70, and 98 Mg ha–1), with and without sawdust, were applied in 1996. Total soil organic C concentration and bulk density were measured to calculate C accumulation. 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We investigated study sites in Virginia to determine the amounts of C remaining in soils 7 to 27 yr following amending with biosolids and composts. The first study employed a Fauquier silty clay loam (fine, mixed, active, mesic Ultic Hapludalf) to which four treatments (control, poultry litter‐yard waste compost, biosolids compost, and poultry litter) were continuously applied during 2000–2004. The second study was conducted on a Davidson clay loam (fine, kaolinitic, thermic, Rhodic Kandiudult) to which six rates of aerobically digested biosolids (0, 42, 84, 126, 168, and 210 Mg ha–1) were applied in 1984. The third study was on a Pamunkey sandy loam (fine‐loamy, mixed, semiactive, thermic Ultic Hapludalfs) to which five rates of anaerobically digested biosolids (0, 14, 42, 70, and 98 Mg ha–1), with and without sawdust, were applied in 1996. Total soil organic C concentration and bulk density were measured to calculate C accumulation. The organic amendment‐treated soils increased C in the surface soil depth (&lt;15 cm), ranging from 2 to 12% of C across all three sites. Soil C movement was limited to a depth of 15 cm. Evidence of C saturation was revealed in the third study site. These results demonstrate that organic amendments applied over a long time remain in soil and may contribute to C sequestration in the Mid‐Atlantic region.</abstract><cop>Madison</cop><pub>The Soil Science Society of America, Inc</pub><doi>10.2136/sssaj2012.0306</doi><tpages>10</tpages></addata></record>
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source Wiley Journals
subjects Active control
Agricultural wastes
Biosolids
Carbon
Clay (material)
Clay loam
Composting
Composts
Decomposition
Efficiency
Herbivores
Litter
Loams
Magnesium
Organic carbon
Poultry
Sandy loam
Sawdust
Sludge
Soil (material)
Soil depth
Soil surfaces
Soil treatment
Solid wastes
Studies
Tillage
Yard waste
title The Effects of Long‐term Application of Organic Amendments on Soil Organic Carbon Accumulation
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