| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5162756 | Organic Geochemistry | 2011 | 12 Pages |
Abstract
⺠Organic matter compound distribution in physical fractions of soils with similar mineralogy but varying carbon contents. ⺠Lignin-derived phenols were protected from oxidation in silt-size fractions. ⺠Polymethylene compounds and peptides accumulated in clay-size fractions. ⺠Organic acids > C20 accumulated in silt- and clay-size fractions. ⺠Chemical structure exerts stronger control than environment on accumulation of organic matter in minerals.
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Authors
Joyce S. Clemente, Andre J. Simpson, Myrna J. Simpson,