侧蚀作用
又称旁蚀作用、侧方侵蚀作用。指流水对河岸的侵蚀作用。由于横向输沙的不平衡，水流不断地冲刷河岸，河岸就不断后退，例如由于弯道环流的作用，引起凹岸冲刷、凸岸堆积。这种凹岸冲刷作用即侧蚀作用，结果使河床更加弯曲、加长，河谷加宽。
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Alias
Contributor
contributed at 2011-10-12
Classification(s)
●
Earth System(in Chinese) External dynamic geology
Detailed Description
| English |
|---|
| Name | lateral erosion |
| Chinese |
|---|
| Name | 侧蚀作用 |
| Description | 又称旁蚀作用、侧方侵蚀作用。指流水对河岸的侵蚀作用。由于横向输沙的不平衡，水流不断地冲刷河岸，河岸就不断后退，例如由于弯道环流的作用，引起凹岸冲刷、凸岸堆积。这种凹岸冲刷作用即侧蚀作用，结果使河床更加弯曲、加长，河谷加宽。 |
How to Cite
NNU_Group (2011). 侧蚀作用, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/4a070894-ef7b-4752-938a-07ef152f2886
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