Application of δ<sup>13</sup>C and δ<sup>15</sup>N isotopic signatures of organic matter fractions sequentially separated from adjacent arable and forest soils to identify carbon stabilization mechanisms
Identifying the chemical mechanisms behind soil carbon bound in organo-mineral complexes is necessary to determine the degree to which soil organic carbon is stabilized belowground. Analysis of δ<sup>13</sup>C and δ<sup>15</sup>N isotopic signatures of sta...
| Main Authors: | , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2011-10-01
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| Series: | Biogeosciences |
| Online Access: | http://www.biogeosciences.net/8/2895/2011/bg-8-2895-2011.pdf |