湿陷性黄土

被水浸湿后在自重和外部荷载作用下结构迅速破坏而发生显著下沉的黄土。一般规定湿陷系数δs≥0.015的黄土为湿陷性黄土;δs<0.015时,定为非湿陷性黄土。

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Contributor(s)

Initial contribute: 2011-10-12

Classification(s)

Geographic semantic resource libraryEarth System(in Chinese)Geology of loess

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English
Name collapsing loess
Chinese
Name 湿陷性黄土
Description 被水浸湿后在自重和外部荷载作用下结构迅速破坏而发生显著下沉的黄土。一般规定湿陷系数δs≥0.015的黄土为湿陷性黄土;δs<0.015时,定为非湿陷性黄土。

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NNU_Group (2011). 湿陷性黄土, Concept & Semantic, OpenGMS, https://geomodeling.njnu.edu.cn/repository/concept/972e796b-6f20-42be-9eb0-f6f5ae1ba358
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Contributor(s)

Initial contribute : 2011-10-12

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