Evaluation of the Saq aquifer groundwater resources in Al Ula, Saudi Arabia

IF 2.4 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Hydrogeology Journal Pub Date : 2024-09-03 DOI:10.1007/s10040-024-02817-8
Etienne Buscarlet, Jean-François Desprats, Yamen Ouerghi, Pierre Séraphin
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Abstract

Regional sandstone aquifers in arid areas provide prolific water resources that can meet human water demands, but their sustainability is at risk where recharge is very low and significant withdrawals occur. The Saq sandstone aquifer in the Al Ula area (Saudi Arabia) has been investigated through a field survey that included groundwater level measurement, groundwater sampling and analysis, crop inventory mapping and irrigation practice enquiries to assess groundwater abstractions. A groundwater model has been built to assimilate the collected data and investigate the aquifer response under various abstractions scenarios to meet future agricultural and domestic water demand. Since the 1960’s, water levels have dropped by 5–20 m within the Al Ula Valley, with maximum water level drawdowns reaching 30–40 m in Al Ula City. Present water level drawdown rates range from 0.5 to 2 m year–1 in the agricultural areas of the valley. Less than half of the sampled groundwater is in compliance with regulatory guidelines for drinking water purpose, and high groundwater nitrate concentrations are observed in agricultural areas. Predictive scenarios of decreasing abstractions suggest a reduction in the water level decline by 2050 but do not reverse the current decreasing trend. The estimated recharge is much lower than groundwater abstraction rates and current withdrawals are effectively mining the groundwater reserves. Further challenges arise from a water quality standpoint, due to the presence of radionuclide activities (mostly 228Ra) in the aquifer above the WHO guidelines.

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沙特阿拉伯乌拉萨克含水层地下水资源评估
干旱地区的区域性砂岩含水层提供了丰富的水资源,可以满足人类的用水需求,但在补给量极低和大量取水的地方,含水层的可持续性就会受到威胁。对 Al Ula 地区(沙特阿拉伯)的 Saq 砂岩含水层进行了实地调查,包括地下水位测量、地下水取样和分析、作物清单测绘以及灌溉方法调查,以评估地下水的抽取量。建立了一个地下水模型,以吸收收集到的数据,并研究含水层在各种取水方案下的反应,以满足未来的农业和生活用水需求。自 20 世纪 60 年代以来,乌拉河谷的水位下降了 5-20 米,乌拉市的最大水位下降幅度达到 30-40 米。目前,河谷农业区的水位下降率为每年 0.5 至 2 米。采样的地下水中只有不到一半符合饮用水的监管准则,在农业区观察到的地下水硝酸盐浓度较高。减少取水量的预测方案表明,到 2050 年,水位下降的幅度会减小,但不会扭转目前的下降趋势。估计的补给量远远低于地下水的抽取率,目前的抽取量实际上是在开采地下水储备。从水质角度看,由于含水层中放射性核素(主要是 228Ra)的含量超过了世界卫生组织的标准,因此面临着进一步的挑战。
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来源期刊
Hydrogeology Journal
Hydrogeology Journal 地学-地球科学综合
CiteScore
5.40
自引率
7.10%
发文量
128
审稿时长
6 months
期刊介绍: Hydrogeology Journal was founded in 1992 to foster understanding of hydrogeology; to describe worldwide progress in hydrogeology; and to provide an accessible forum for scientists, researchers, engineers, and practitioners in developing and industrialized countries. Since then, the journal has earned a large worldwide readership. Its peer-reviewed research articles integrate subsurface hydrology and geology with supporting disciplines: geochemistry, geophysics, geomorphology, geobiology, surface-water hydrology, tectonics, numerical modeling, economics, and sociology.
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