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Groundwater Evapotranspiration — Underestimated Role of Tree Transpiration and Bare Soil Evaporation in Groundwater Balances of Dry Lands

机译:地下水蒸发 - 树木蒸腾和裸土壤蒸发在干旱地下水平衡中的低估作用

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This paper analyzes and emphasizes the importance of groundwater evapotranspiration (ETg) in groundwater balances. The ETg diminishes the net groundwater recharge that constrains groundwater flow and replenishment of groundwater resources. The ETg consists of two different components, groundwater transpiration (Tg) and groundwater evaporation (Eg), both not yet well identified in hydrogeology. The ETg values are the largest in dry locations with shallow groundwater table. The significance of the ETg however is the largest when its relative contribution to groundwater balance is high i.e. when its rate is comparable with groundwater recharge.
机译:本文分析并强调地下水蒸散(ETG)在地下水平衡中的重要性。 ETG减少了限制地下水流量和地下水资源补充的净地下水补给。 ETG由两种不同的组分,地下水蒸腾(Tg)和地下水蒸发(例如),尚未在水文地质中尚未识别。 ETG值是具有浅地下水位的干燥位置中最大的值。然而,ETG的重要性是当其对地下水平衡的相对贡献很高,即当其速率与地下水充电相当时。

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