岩溶水包气带
又称岩溶水渗流带。丰水期地下水位以上、大气降水或地表水沿可溶岩的裂隙、管道运动的地带。此带水流常不具静水压力，且不连续。常形成近于垂直的洞穴。在局部非可溶岩层之上可形成上层滞水及相应的水平洞穴。
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contributed at 2011-10-12
Classification(s)
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Earth System(in Chinese) Karstology
Detailed Description
| English |
|---|
| Name | karst water aeration zone,karst water vadose zone |
| Chinese |
|---|
| Name | 岩溶水包气带 |
| Description | 又称岩溶水渗流带。丰水期地下水位以上、大气降水或地表水沿可溶岩的裂隙、管道运动的地带。此带水流常不具静水压力，且不连续。常形成近于垂直的洞穴。在局部非可溶岩层之上可形成上层滞水及相应的水平洞穴。 |
How to Cite
NNU_Group (2011). 岩溶水包气带, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/da4fba63-cc00-4c54-8635-356a22585403
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