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利用 Hydrus-1D 在半干旱地区(突尼斯中部的凯鲁万平原)模拟饱和带和非饱和带之间的相互作用。

Modeling interactions between saturated and un-saturated zones by Hydrus-1D in semi-arid regions (plain of Kairouan, Central Tunisia).

机构信息

Faculté des Sciences de Tunis, UR13ES26 Paléo-environnement, Géomatériaux et Risques Géologiques, Université de Tunis El Manar, 2092, Tunis, Tunisie.

Institut National de Recherche en Génie Rural, Eau et Forêts, Rue Hédi EL Karray El Menzah IV, BP 10, Ariana, 2080, Tunisie.

出版信息

Environ Monit Assess. 2018 Feb 24;190(3):170. doi: 10.1007/s10661-018-6544-3.

DOI:10.1007/s10661-018-6544-3
PMID:29478086
Abstract

In semi-arid areas like the Kairouan region, salinization has become an increasing concern because of the constant irrigation with saline water and over use of groundwater resources, soils, and aquifers. In this study, a methodology has been developed to evaluate groundwater contamination risk based on the unsaturated zone hydraulic properties. Two soil profiles with different ranges of salinity, one located in the north of the plain and another one in the south of plain (each 30 m deep) and both characterized by direct recharge of the aquifer, were chosen. Simulations were conducted with Hydrus-1D code using measured precipitation data for the period 1998-2003 and calculated evapotranspiration for both chosen profiles. Four combinations of initial conditions of water content and salt concentration were used for the simulation process in order to find the best match between simulated and measured values. The success of the calibration of Hydrus-1D allowed the investigation of some scenarios in order to assess the contamination risk under different natural conditions. The aquifer risk contamination is related to the natural conditions where it increased while facing climate change and temperature increase and decreased in the presence of a clay layer. Hydrus-1D was a useful tool to predict the groundwater level and quality in the case of a direct recharge and in the absence of any information related to the soil layers except for the texture.

摘要

在半干旱地区,如凯鲁万地区,由于不断用盐水灌溉和过度使用地下水资源、土壤和含水层,盐渍化已成为一个日益令人担忧的问题。在这项研究中,开发了一种基于非饱和带水力特性评估地下水污染风险的方法。选择了两个具有不同盐度范围的土壤剖面,一个位于平原北部,另一个位于平原南部(每个剖面深 30 米),两者均具有含水层的直接补给。使用 Hydrus-1D 代码对 1998-2003 年期间的实测降水数据和为两个选定剖面计算的蒸发蒸腾量进行了模拟。为了找到模拟值与实测值之间的最佳匹配,在模拟过程中使用了四种初始含水量和盐浓度组合。Hydrus-1D 的校准成功允许研究一些情景,以评估在不同自然条件下的污染风险。含水层污染风险与自然条件有关,在气候变化和温度升高的情况下,风险增加,而在存在粘土层的情况下,风险降低。在直接补给且没有与土壤层相关的任何信息的情况下,Hydrus-1D 是预测地下水水位和质量的有用工具,除了质地之外。

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引用本文的文献

1
Numerical simulation to assess potential groundwater recharge and net groundwater use in a semi-arid region.数值模拟评估半干旱地区的潜在地下补给和净地下水利用。
Environ Monit Assess. 2019 May 17;191(6):371. doi: 10.1007/s10661-019-7508-y.