非重力水沉积
在洞穴中非重力水作用的沉积物。在包气带洞穴中，非重力水主要存在形式是薄膜水和毛细水。岩层微细裂隙、孔隙及粗糙表面是非重力水活动主要场所。洞穴中空气的湿度和运动强度对非重力水沉积物结晶的完美程度及形态有重大影响。非重力水沉积的主要类型有洞穴毛发、石枝(或卷曲石)、珊瑚状物、根须石枝、皮壳、石花、花斑、穴疱等。
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contributed at 2011-10-12
Classification(s)
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Earth System(in Chinese) Karstology
Detailed Description
| English |
|---|
| Name | nongravitational water deposits |
| Chinese |
|---|
| Name | 非重力水沉积 |
| Description | 在洞穴中非重力水作用的沉积物。在包气带洞穴中，非重力水主要存在形式是薄膜水和毛细水。岩层微细裂隙、孔隙及粗糙表面是非重力水活动主要场所。洞穴中空气的湿度和运动强度对非重力水沉积物结晶的完美程度及形态有重大影响。非重力水沉积的主要类型有洞穴毛发、石枝(或卷曲石)、珊瑚状物、根须石枝、皮壳、石花、花斑、穴疱等。 |
How to Cite
NNU_Group (2011). 非重力水沉积, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/a5efe646-4833-4dd5-a78d-44f734ba2516
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