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About the Genesis of Brown Tropical Soils with Shallow Nonferrallitic Profile

机译:关于浅浅层晶体剖面棕色热带土壤的成因

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Brown soil with a shallow nonferrallitic profile developing from various parent rocks in conditions of a seasonally humid tropical climate have been studied in Laos. It is found that these soils characterize the mature stage of tropical pedogensis on the rocks that have not been altered by presoil hydrothermal processes: in other world, these soils display all normal features of tropical pedogenesis. Red ferrallitic soils that predominate in humid tropical regions develop from hydrothermal weathering crusts.
机译:在老挝的季节性潮湿的热带气候条件下,棕色土壤具有从各种父岩的浅不流体剖面,在季节性潮湿的热带气候中已经在老挝进行了研究。 结果发现,这些土壤表征了热带佩皮塞斯的成熟阶段,岩石上尚未被PREIOL水热过程改变的岩石:在其他世界中,这些土壤显示了热带基础的所有正常特征。 潮湿的热带地区占优势的红菲尔利氏土壤,从水热风化外壳中产生。

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