IGSNRR OpenIR
华南花岗岩风化壳岩土特性与崩岗侵蚀关系
王继增1; 吴志峰2
2000
Source Publication水土保持学报
ISSN1009-2242
Volume014Issue:002Pages:31
Abstract在野外调查和室内分析的基础上,探讨了华南花岗岩风化壳岩土特性与崩岗侵蚀的关系。花岗岩风化壳土体粗粒含量较多。结构疏松,裂隙发育,力学性质受水的影响显著。典型的花岗岩风化壳可划分为5个基本层次,各风化层在粒度,成份和结构等方面存在明显差异,表明出相应的物理力学特性,并对崩岗侵蚀的形成和 育产生重要影响。
Language英语
Document Type期刊论文
Identifierhttp://ir.igsnrr.ac.cn/handle/311030/89016
Collection中国科学院地理科学与资源研究所
Affiliation1.广东省生态环境与土壤所
2.中国科学院地理科学与资源研究所
Recommended Citation
GB/T 7714
王继增,吴志峰. 华南花岗岩风化壳岩土特性与崩岗侵蚀关系[J]. 水土保持学报,2000,014(002):31.
APA 王继增,&吴志峰.(2000).华南花岗岩风化壳岩土特性与崩岗侵蚀关系.水土保持学报,014(002),31.
MLA 王继增,et al."华南花岗岩风化壳岩土特性与崩岗侵蚀关系".水土保持学报 014.002(2000):31.
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