首页> 外文期刊>Journal of Hydrology >Reply to 'comment on a model for soil surface evaporation based on Campbell's retention curve by Zarei et al.' by M. Sadeghi
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Reply to 'comment on a model for soil surface evaporation based on Campbell's retention curve by Zarei et al.' by M. Sadeghi

机译:回复“对Zarei等人基于坎贝尔保留曲线的土壤表面蒸发模型的评论”。由M.Sadeghi

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摘要

Sadeghi (2015) has been commented on an analytical solution we derived for evaporation from bare soils with a descending shallow groundwater table (Zarei et al., 2010). The evaporation rate in this solution was described as a function of shallow water table depth drawdown using the parameters of Campbell's soil water retention model. Sadeghi (2015) took issue with a simplifying assumption in the derivation about the pressure head distribution above the water table that allowed us to obtain the approximate solution. This response aims to demonstrate that the derivation of Zarei et al. (2010) works reasonably well in the presence of a shallow water table by providing a more detailed discussion and additional experimental evidence. (C) 2015 Elsevier B.V. All rights reserved.
机译:Sadeghi(2015年)对我们从地下水浅层下降的裸露土壤蒸发得出的分析解决方案进行了评论(Zarei等,2010年)。使用坎贝尔土壤保水模型的参数,该溶液中的蒸发速率被描述为浅水位深度下降的函数。 Sadeghi(2015)在推导地下水位上方的压头分布时采用了简化的假设,这使我们能够获得近似解。此响应旨在证明Zarei等人的推论。 (2010年)通过提供更详细的讨论和其他实验证据,在存在浅水位的情况下可以很好地工作。 (C)2015 Elsevier B.V.保留所有权利。

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