2022
DOI: 10.3390/w14040648
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Assessing the Groundwater Reserves of the Udaipur District, Aravalli Range, India, Using Geospatial Techniques

Abstract: Population increase has placed ever-increasing demands on the available groundwater (GW) resources, particularly for intensive agricultural activities. In India, groundwater is the backbone of agriculture and drinking purposes. In the present study, an assessment of groundwater reserves was carried out in the Udaipur district, Aravalli range, India. It was observed that the principal aquifer for the availability of groundwater in the studied area is quartzite, phyllite, gneisses, schist, and dolomitic marble, … Show more

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Cited by 18 publications
(2 citation statements)
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“…The main factor contributing to the high landslides in the study area is the slope. In other words, surface topography is one such landscape characteristic that helps understand why some places are comparatively more vulnerable to landslides than others [61][62][63][64]. The topography has a significant effect on landslide kinematics [65].…”
Section: Landslide Early Warning System (Lews) and Land System Proces...mentioning
confidence: 99%
“…The main factor contributing to the high landslides in the study area is the slope. In other words, surface topography is one such landscape characteristic that helps understand why some places are comparatively more vulnerable to landslides than others [61][62][63][64]. The topography has a significant effect on landslide kinematics [65].…”
Section: Landslide Early Warning System (Lews) and Land System Proces...mentioning
confidence: 99%
“…Considering the water resources as a limiting factor for socio-economic development, especially in arid/semi-arid regions, Shyam et al [8] carried out the assessment of groundwater reserves, which was carried out in the Udaipur district, Aravalli range, India using an integrated approach of remote sensing, GIS, and field-based spatial modeling. Results show that the principal aquifer for the availability of groundwater in the studied area is quartzite, phyllite, gneisses, schist, and dolomitic marble, which occur in unconfined to semi-confined zones.…”
mentioning
confidence: 99%