整合遥感、地球化学建模和同位素约束条件,探测干旱地区有潜力的地下水区。对埃及克纳-卢克索地区的研究

IF 4.9 Q2 ENGINEERING, ENVIRONMENTAL Groundwater for Sustainable Development Pub Date : 2024-07-01 DOI:10.1016/j.gsd.2024.101266
Mohamed Hassan Ramzy , Mustafa Eissa , Shaimaa M. El-Hadidy , Samah Mahmoud Morsy
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引用次数: 0

摘要

埃及的可再生地下水资源仅限于尼罗河附近。在研究地区,尼罗河附近有两个主要的水源承载层:第四纪含水层和始新世含水层。研究采用了遥感技术(ASTER DEM、Landsat-8 和 Sentinal-1 InSAR 图像)、地球化学建模和同位素约束(δ18O 和 δ2H),并与地理信息系统框架相结合,以划定低盐度和可持续地下水区。遥感数据表明,中东部有密集的结构线形,与雷达卫星推断的地下特征在空间上一致,有利于与尼罗河水的水力联系。灌溉区的土壤水分指数、地表温度和盐度指数显示,原地电导率值与卫星光谱指数之间存在密切联系。中东部地区较高的地下水盐度与高线密度区和较高温度区相吻合,导致岩石与水的相互作用加剧,从而导致地下水盐化。第四纪含水层的同位素组成中,δ18O介于-1.30 ‰和+5.53 ‰之间,δ2H介于-11.49 ‰和+34.47 ‰之间。在始新世含水层中,δ18O介于-0.46和+3.45‰之间,而δ2H介于-3.16和+23.50‰之间,这表明地下有尼罗河水补给。质量输运地球化学 NETPATH 模型模拟显示,尼罗河水的混合比在 3.4% 至 93.7% 之间。根据研究结果,该地区被划分为四个等级,等级(1)代表尼罗河水的高导流样本(混合率 50%),等级(2)代表尼罗河水的中等导流样本(混合率 10-50%),等级(3)代表尼罗河水的低导流样本(混合率 1-10%),等级(4)代表水岩相互作用样本。这些发现对于划定尼罗河谷含水层的可持续发展区具有重要意义。
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Integration of remote sensing, geochemical modeling, and isotopic constraints for the detection of promising groundwater zones in arid regions. A study in Qena- Luxor area, Egypt

The renewable groundwater resources in Egypt are restricted close to the Nile River. In the study area, two major water bearings are near the Nile: The Quaternary and the Eocene aquifers. Remote sensing (ASTER DEM, Landsat-8, and Sentinal-1 InSAR images), geochemical modeling, and isotopic constraints (δ18O and δ2H) were employed and integrated with the GIS framework for delineating the low saline and sustainable groundwater zones. Remote sensing data indicates intensive structure lineaments in the middle-eastward part, spatially congruent with subsurface features deduced from radar satellites, facilitating hydraulic connections with the Nile water. The soil moisture index, land surface temperature, and salinity index in irrigated areas, reveal a strong association between in situ electrical conductivity values and satellite-derived spectral indices. The higher groundwater salinity in the middle eastern region coincided with high lineament density zones, and higher temperature zones, leading to increased rock water interaction that leads to groundwater salinization. The isotopic composition of the Quaternary aquifer ranges between −1.30 ‰ and +5.53 ‰ for δ18O, while δ2H ranges between −11.49 ‰ and +34.47 ‰. In the Eocene aquifer, δ18O ranges between −0.46 and +3.45 ‰, while the δ2H ranges between −3.16 ‰ and +23.50 ‰, indicating subsurface recharge from the Nile water. The simulation of the mass transport geochemical NETPATH model revealed mixing ratios from the Nile water ranging from 3.4% to 93.7%. Based on the results, the area is classified into four classes, class (1) represents samples of high conduit with Nile water (<50% mixing), class (2) represents samples of moderate conduit with Nile water (10–50% mixing), class (3) represents samples of low conduit with Nile water (<1–10% mixing), class (4) represents samples of water-rock interaction. The findings would be of great importance for delineating sustainable zones of the Nile Valley aquifers.

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来源期刊
Groundwater for Sustainable Development
Groundwater for Sustainable Development Social Sciences-Geography, Planning and Development
CiteScore
11.50
自引率
10.20%
发文量
152
期刊介绍: Groundwater for Sustainable Development is directed to different stakeholders and professionals, including government and non-governmental organizations, international funding agencies, universities, public water institutions, public health and other public/private sector professionals, and other relevant institutions. It is aimed at professionals, academics and students in the fields of disciplines such as: groundwater and its connection to surface hydrology and environment, soil sciences, engineering, ecology, microbiology, atmospheric sciences, analytical chemistry, hydro-engineering, water technology, environmental ethics, economics, public health, policy, as well as social sciences, legal disciplines, or any other area connected with water issues. The objectives of this journal are to facilitate: • The improvement of effective and sustainable management of water resources across the globe. • The improvement of human access to groundwater resources in adequate quantity and good quality. • The meeting of the increasing demand for drinking and irrigation water needed for food security to contribute to a social and economically sound human development. • The creation of a global inter- and multidisciplinary platform and forum to improve our understanding of groundwater resources and to advocate their effective and sustainable management and protection against contamination. • Interdisciplinary information exchange and to stimulate scientific research in the fields of groundwater related sciences and social and health sciences required to achieve the United Nations Millennium Development Goals for sustainable development.
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