Iron-mediated mineralogical control of organic matter accumulation in tropical soils
Tropical forest soils contribute disproportionately to the poorly-characterized and persistent deep soil carbon (C) pool. These soils, highly-weathered and often extending one to two meters in depth, may contain an abundance of iron-(Fe) bearing mineral phases. Short-range-order (SRO) minerals are o...
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Published in | Geoderma Vol. 306; pp. 206 - 216 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
15.11.2017
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Subjects | |
Online Access | Get full text |
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