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  <rdf:Description rdf:about="https://doi.org/10.1046/j.1529-8817.2003.00722.x">
    <dct:isReferencedBy>IMPACT4SOIL</dct:isReferencedBy>
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    <dct:license>Open Access</dct:license>
    <dct:created>2004-12-24</dct:created>
    <dc:description>Abstract&lt;p&gt;Conversion of former agricultural land to grassland and forest ecosystems is a suggested option for mitigation of increased atmospheric CO2. A Sharpsburg prairie loess soil (fine, smectitic, mesic Typic Argiudoll) provided treatments to study the impact of long&#65506;&#65408;&#65424;term land use on soil organic carbon (SOC) content and composition for a 130&#65506;&#65408;&#65424;year&#65506;&#65408;&#65424;old cropped, pasture and forest comparison. The forest and pasture land use significantly retained more SOC, 46% and 25%, respectively, compared with cropped land use, and forest land use increased soil C content by 29% compared with the pasture. Organic C retained in the soils was a function of the soil N content (r=0.98,P&amp;lt;0.001) and the soil carbohydrate (CH) concentration (r=0.96,P&amp;lt;0.001). Statistical analyses found that soil aggregation processes increased as organic C content increased in the forest and pasture soils, but not in the cropped soil. SOC was composed of similar percentages of CHs (49%, 42% and 51%), amino acids (22%, 15% and 18%), lipids (2.3%, 2.3% and 2.9%) and unidentified C (21%, 29% and 27%), but differed for phenolic acids (PAs) (5.7%, 11.6% and 1.0%) for the pasture, forest and cropped soils, respectively. The results suggested that the majority of the surface soil C sequestered in the long&#65506;&#65408;&#65424;term pasture and forest soils was identified as C of plant origin through the use of CH and PA biomarkers, although the increase in amino sugar concentration of microbial origin indicates a greater increase in microbial inputs in the three subsoils. The practice of permanent pastures and afforestation of agricultural land showed long&#65506;&#65408;&#65424;term potential for potential mitigation of atmospheric CO2.&lt;/p&gt;</dc:description>
    <dc:subject>2. Zero hunger</dc:subject>
    <dc:subject>amino acids</dc:subject>
    <dc:subject>550</dc:subject>
    <dc:subject>Plant Sciences</dc:subject>
    <dc:subject>carbohydrates</dc:subject>
    <dc:subject>lignin</dc:subject>
    <dc:subject>organic C</dc:subject>
    <dc:subject>04 agricultural and veterinary sciences</dc:subject>
    <dc:subject>15. Life on land</dc:subject>
    <dc:subject>630</dc:subject>
    <dc:subject>6. Clean water</dc:subject>
    <dc:subject>land-use change</dc:subject>
    <dc:subject>lipids</dc:subject>
    <dc:subject>13. Climate action</dc:subject>
    <dc:subject>0401 agriculture, forestry, and fisheries</dc:subject>
    <dc:subject>phenolic acids</dc:subject>
    <dc:creator>Martens, Dean A., Reedy, Thomas E., Lewis, David T., (retired), </dc:creator>
    <dc:date>2003-12-19</dc:date>
    <dc:type>journalpaper</dc:type>
    <dct:abstract>Abstract&lt;p&gt;Conversion of former agricultural land to grassland and forest ecosystems is a suggested option for mitigation of increased atmospheric CO2. A Sharpsburg prairie loess soil (fine, smectitic, mesic Typic Argiudoll) provided treatments to study the impact of long&#65506;&#65408;&#65424;term land use on soil organic carbon (SOC) content and composition for a 130&#65506;&#65408;&#65424;year&#65506;&#65408;&#65424;old cropped, pasture and forest comparison. The forest and pasture land use significantly retained more SOC, 46% and 25%, respectively, compared with cropped land use, and forest land use increased soil C content by 29% compared with the pasture. Organic C retained in the soils was a function of the soil N content (r=0.98,P&amp;lt;0.001) and the soil carbohydrate (CH) concentration (r=0.96,P&amp;lt;0.001). Statistical analyses found that soil aggregation processes increased as organic C content increased in the forest and pasture soils, but not in the cropped soil. SOC was composed of similar percentages of CHs (49%, 42% and 51%), amino acids (22%, 15% and 18%), lipids (2.3%, 2.3% and 2.9%) and unidentified C (21%, 29% and 27%), but differed for phenolic acids (PAs) (5.7%, 11.6% and 1.0%) for the pasture, forest and cropped soils, respectively. The results suggested that the majority of the surface soil C sequestered in the long&#65506;&#65408;&#65424;term pasture and forest soils was identified as C of plant origin through the use of CH and PA biomarkers, although the increase in amino sugar concentration of microbial origin indicates a greater increase in microbial inputs in the three subsoils. The practice of permanent pastures and afforestation of agricultural land showed long&#65506;&#65408;&#65424;term potential for potential mitigation of atmospheric CO2.&lt;/p&gt;</dct:abstract>
    <dc:title>Soil Organic Carbon Content And Composition Of 130-Year Crop, Pasture And Forest Land-Use Managements</dc:title>
    <dc:identifier>10.1046/j.1529-8817.2003.00722.x</dc:identifier>
    <dct:references>https://doi.org/10.1046/j.1529-8817.2003.00722.x</dct:references>
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