Management practices differently affect particulate and mineral-associated organic matter and their precursors in arable soils
2020
Abstract Our understanding of soil organic matter (SOM) formation and stabilization mechanisms has evolved recently. The SOM is considered as a continuum from coarse fresh and decomposing plant residues (particulate organic matter, >53 μm; POM) to fine and presumably more stable mineral-associated organic matter (fine organic matter,
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