Identification of potential dam sites for severe water crisis management in semi-arid fluoride contaminated region, India

Arijit Ghosh, Biswajit Bera
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Abstract

Pressure on freshwater resources is tremendously increasing due to large-scale global population explosion, socio-economic development, climate change and infrastructural development worldwide. The study area faces severe water crisis, groundwater fluoride contamination, and high drought frequency. Thus, the principal objectives are i) to assess the recent surface and subsurface water dynamics in this plateau fringe using satellite datasets on Google Earth Engine (GEE) and ii) to demarcate the suitable sites for dam construction to manage the severe water crisis and substitute drinking water sources. Satellite datasets such as Sentinel 2 and Gravity Recovery and Climate Experiment (GRACE) have been used to access the surface and groundwater dynamics. Numerous criteria or influencing factors including geology, geomorphology, lineament, elevation, slope, rainfall, land use/land cover, soil, stream density, normalized vegetation index (NDVI), and distance from the river have been considered to demarcate the suitable sites for new dam site suitability. In this study, four advanced machine learning models namely support vector machine (SVM), random forest (RF), logistic regression (LR) and gradient boosting (XGBoost) have been applied to recommend suitable sites for dam construction. Average surface water changes from 157.375 km2 (2012–2016) to 156.185 km2(2017–2022). Estimated water thickness (EWT) values vary from 28.58 cm to −27.07 cm (2002–2017). In case of soil moisture (SM), the lowest value (2.4 cm) was in June 2009, and the highest (21.51 cm) was in September 2003. After the deduction of SM from EWS, it specifies that maximum groundwater storage (9.48 cm) occurred in July 2004 whereas a minimum (-30.21 cm) in March 2016. Dam site suitability results denote that 10% of areas come under the very high suitable for surface and subsurface dam construction. The area under curve (AUC) values of SVM, RF, LR, and XGBoost are 0.94, 0.95, 0.91, and 0.92 respectively. Therefore, the RF model has comparatively higher values regarding model performance. The output of this research will be advantageous to define suitable places for new dam construction and sustainable water resource management in semi-arid environment.

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为印度半干旱氟污染地区严重水危机管理确定潜在坝址
由于全球人口大规模激增、社会经济发展、气候变化和基础设施建设,淡水资源的压力与日俱增。研究地区面临着严重的水危机、地下水氟污染和频繁的干旱。因此,研究的主要目标是 i) 利用谷歌地球引擎(GEE)上的卫星数据集评估该高原边缘地区近期的地表水和地下水动态;ii) 划定合适的水坝建设地点,以应对严重的水危机并替代饮用水源。哨兵 2 号和重力恢复与气候实验(GRACE)等卫星数据集被用来获取地表水和地下水的动态信息。考虑了许多标准或影响因素,包括地质、地貌、线型、海拔、坡度、降雨、土地利用/土地覆盖、土壤、溪流密度、归一化植被指数(NDVI)和与河流的距离,以划定新坝址的合适地点。本研究采用了四种先进的机器学习模型,即支持向量机 (SVM)、随机森林 (RF)、逻辑回归 (LR) 和梯度提升 (XGBoost),来推荐合适的坝址。平均地表水从 157.375 平方公里(2012-2016 年)变为 156.185 平方公里(2017-2022 年)。估计水厚度(EWT)值从 28.58 厘米变化到-27.07 厘米(2002-2017 年)。土壤水分(SM)的最低值(2.4 厘米)出现在 2009 年 6 月,最高值(21.51 厘米)出现在 2003 年 9 月。从 EWS 中扣除土壤水分后,可以看出地下水储量最大值(9.48 厘米)出现在 2004 年 7 月,而最小值(-30.21 厘米)出现在 2016 年 3 月。坝址适宜性结果表明,10% 的区域属于非常适合建造地表和地下大坝的区域。SVM、RF、LR 和 XGBoost 的曲线下面积(AUC)值分别为 0.94、0.95、0.91 和 0.92。因此,RF 模型的模型性能值相对较高。这项研究的成果将有助于在半干旱环境中确定新水坝建设和可持续水资源管理的合适地点。
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