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A framework for sourcing of evaporation between saturated and unsaturated zone in bare soil condition

机译:裸土条件下饱和与非饱和带之间蒸发源的获取框架

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摘要

Sourcing subsurface evaporation (Ess) into groundwater (Eg) and unsaturated zone (Eu) components has received little scientific attention so far, despite its importance in water management and agriculture. We propose a novel sourcing framework, with its implementation in dedicated post-processing software called SOURCE (used along with the HYDRUS1D model), to study evaporation sourcing dynamics, define quantitatively “shallow” and “deep” water table conditions and test the applicability of water table fluctuation (WTF) and “bucket” methods for estimation of Eg and Eu separately.For the “shallow” and “deep” water table we propose Eg > 0.95Ess and Eg = 0 criteria, respectively. Assessment of the WTF method allowed sourcing of very small fluxes otherwise neglected by standard hydrological methods. Sourcing with SOURCE software was more accurate than the standard “bucket” method mainly because of greater flexibility in spatio-temporal discretization. This study emphasized the dry condition relevance of groundwater evaporation which should be analysed by applying coupled flow of heat, vapour and liquid water.
机译:尽管将地下蒸发(Ess)引入地下水(Eg)和非饱和区(Eu)组分中,尽管在水管理和农业中具有重要意义,但迄今为止,该研究很少受到科学关注。我们提出了一种新颖的采购框架,并在称为SOURCE的专用后处理软件(与HYDRUS1D模型一起使用)中实施了该框架,以研究蒸发物供应动力学,定量定义“浅”和“深”地下水位条件并测试水的适用性。地下水位波动(WTF)和“桶”法分别估算Eg和Eu。对于“浅”和“深”水位,我们分别提出Eg> 0.95Ess和Eg = 0标准。对WTF方法的评估允许获得很小的流量,而标准水文学方法却忽略了这些流量。使用SOURCE软件进行采购比标准“存储桶”方法更为准确,主要是因为时空离散化具有更大的灵活性。这项研究强调了地下水蒸发的干燥条件的相关性,应通过应用热,蒸汽和液态水的耦合流来分析。

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