Abstract:Mineralogical determinations and the suggested genesis of two proposed Nardin soils described in the first paper of this series are presented. Weathered and unweathered material of the clayey Wellington formation, Permian Redbeds were also studied to create two models showing that the proposed Nardin soils formed in either Permian Redbeds or Post‐Permian sediments. Cation‐exchange capacity, nonexchangeable K, ethylene glycol retention, and clay mineralogy based on X‐ray diffraction and differential thermal ana… Show more
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