首页> 外文会议>International Soil Conservation Organization Conference vol.2; 20020526-31; Beijing(CN) >Relationships between Crumbing Hills and Rock-Soil Characteristics of Granite Weathering Crusts in South China
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Relationships between Crumbing Hills and Rock-Soil Characteristics of Granite Weathering Crusts in South China

机译:华南花岗岩风化壳碎屑山与岩土特征的关系

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Based on field investigation and laboratory analysis including grain-size analysis, scanning electron microscopy (SEM), chemical composition and X-ray diffraction (XRD), relationships between crumbing hills and rock-soil characteristics of granite weathering crusts are discussed in this paper. The coarse grains are dominant in the crusts which have a loosen structure with lots of cranny, and its strength is influenced mightily by water. In general, there are 5 layers in typical granite weathering mantle with distinct differences in grain-size, chemical composition and structure. The rock-soil characteristics play an important role during forming and developing of crumbing hills.
机译:通过现场调查和实验室分析,包括粒度分析,扫描电镜(SEM),化学成分和X射线衍射(XRD),探讨了碎屑丘陵与花岗岩风化壳岩石-土壤特性之间的关系。地壳中粗粒占主导地位,地壳结构疏松,裂缝很多,其强度受到水的强烈影响。通常,典型的花岗岩风化地幔有5层,在粒度,化学成分和结构上存在明显差异。岩土特性在碎屑山的形成和发展中起着重要作用。

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