Estimation of bare soil evaporation for different depths of water table in the wind-blown sand area of the Ordos Basin, China

Soil surface evaporation is a significant component of the hydrological cycle, occurring at the interface between the atmosphere and vadose zone, but it is affected by factors such as groundwater level, soil properties, solar radiation and others. In order to understand the soil evaporation characte...

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Veröffentlicht in:Hydrogeology journal 2018-08, Vol.26 (5), p.1693-1704
Hauptverfasser: Chen, Li, Wang, Wenke, Zhang, Zaiyong, Wang, Zhoufeng, Wang, Qiangmin, Zhao, Ming, Gong, Chengcheng
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Sprache:eng
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