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Updated: Jan 10, 2026

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
13:27

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface

Published on: June 8, 2015

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气候驱动的水文极端会增加石油碳化合物的地下流动性:在半大陆气候条件下的实验研究

Amélie Cavelan1, Fabrice Golfier2, Catherine Lorgeoux2

  • 1Université de Lorraine, CNRS, LIEC, F-54000, Nancy, France; BRGM, F- 45000, Orléans, France.

The Science of the total environment
|November 26, 2025
PubMed
概括

极端的地下水波动显著增加轻非水相液体 (LNAPLs) 的释放和挥发,但也增强了自然衰减. 这影响了污染土壤的长期环境风险和管理策略.

关键词:
衰减减弱化 减弱 减弱气候变化 气候变化 气候变化地下水的地下水.在LNAPL中使用LNAPL.半大陆气候是一个半大陆气候.土壤 土壤土壤.

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