盐渍化作用
在干旱气候带及高山寒漠带，因降水少、淋溶弱、蒸发强，使母质风化释出的易溶盐不能洗出土体而积聚，也可因其含盐多的地下水上升蒸发而积盐。在滨海地区由于海水含盐量高，通过海水浸淹或矿化度高的地下水上升蒸发，也可造成土壤盐化。上述两种盐分在土壤中积聚过程，称盐渍化作用。
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contributed at 2011-10-13
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Earth System(in Chinese) Soil Science
Detailed Description
| English |
|---|
| Name | salinization |
| Chinese |
|---|
| Name | 盐渍化作用 |
| Description | 在干旱气候带及高山寒漠带，因降水少、淋溶弱、蒸发强，使母质风化释出的易溶盐不能洗出土体而积聚，也可因其含盐多的地下水上升蒸发而积盐。在滨海地区由于海水含盐量高，通过海水浸淹或矿化度高的地下水上升蒸发，也可造成土壤盐化。上述两种盐分在土壤中积聚过程，称盐渍化作用。 |
How to Cite
NNU_Group (2011). 盐渍化作用, Concept & Semantic, OpenGMS,
https://geomodeling.njnu.edu.cn/repository/concept/2d807cf8-adbf-4103-81f0-0bc81b19641e
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