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首页> 外文期刊>极地科学进展(英文版) >Softs of Fildes Peninsula, King George Island, the maritime Antarctic: Part I. Formation processes and pedogenetic particularities
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Softs of Fildes Peninsula, King George Island, the maritime Antarctic: Part I. Formation processes and pedogenetic particularities

机译：南极海洋国王乔治岛的菲尔德斯半岛软岩：第一部分。形成过程和成岩特殊性

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摘要

Based on the data obtained from tens of the investigated soil profiles scattered over the Fildes Peninsula, King George Island, the maritime Antarctic, the soil-forming processes were discussed. It was concluded that on the weathering crusts resulted from various physical courses, the strong freeze-thaw action within regolith, significant organic matter accumulation, evident leaching and illuviation, as well as initial argillification dominated the formation and development of the soils on the Fildes Peninsula. Furthermore, this study indicated that the juvenility of genesis, poor profile-expression, variation in column thickness, etc. characterized the pedogenetic features of the soils of the Fildes Peninsula.
机译：根据从几十个分布在菲尔德半岛，国王乔治岛，海洋南极的调查土壤剖面中获得的数据，讨论了土壤形成过程。结论是，在各种物理过程中形成的风化硬皮上，砾石内部强烈的冻融作用，大量的有机物质积累，明显的浸出和溶蚀作用，以及初始的泥凝作用主导了菲尔德斯半岛土壤的形成和发展。 。此外，这项研究表明，成因的少年性，不良的剖面表达，柱厚的变化等是菲尔德斯半岛土壤的成岩特征。

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