Abstract
Light-absorption curves are given of organic matter extracted from different horizons of humus-iron podzols and brown podzolic soils on liparitic tuff and brown forest and gray-brown podzolic soils, latosols and acid brown earths on andesitic tuff, in support of theories on the role of organic matter in soil-forming processes under a humid tropical climate. (Abstract retrieved from CAB Abstracts by CABI’s permission)
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