岩溶饱水带
又称潜流带(underflow zone)。岩溶含水层枯水期地下水位以下的地带。它的上限及厚度与补给排泄区的相对位置和高差有关。水流常具有连续性和静水压力。按其在地下水面以下的深度，可分浅饱水带和深饱水带。浅饱水带常常是岩溶强烈发育的地带。一些近于水平的洞穴，常发育在当时此带的地下水面附近，深饱水带与深部缓流带成渐变关系。
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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 saturation zone, karst phreatic zone |
| Chinese |
|---|
| Name | 岩溶饱水带 |
| Description | 又称潜流带(underflow zone)。岩溶含水层枯水期地下水位以下的地带。它的上限及厚度与补给排泄区的相对位置和高差有关。水流常具有连续性和静水压力。按其在地下水面以下的深度，可分浅饱水带和深饱水带。浅饱水带常常是岩溶强烈发育的地带。一些近于水平的洞穴，常发育在当时此带的地下水面附近，深饱水带与深部缓流带成渐变关系。 |
How to Cite
NNU_Group (2011). 岩溶饱水带, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/8ac687ab-b420-462d-a15d-3312b1673b00
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