2018
DOI: 10.1016/j.iswcr.2018.07.003
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A GIS-based approach for identifying potential sites for harvesting rainwater in the Western Desert of Iraq

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Cited by 118 publications
(87 citation statements)
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“…This parameter is determined by the terrain ratio, which denotes the ratio of the height difference between two points divided by the horizontal straight line distance between them [18,31]. The slope parameter has an effect on the runoff, sedimentation ratio, recharge, surface water velocity, and the number of materials essential to creating dams [25]. The DEM with a 30 m resolution was used to generate the slope map, and the area was then divided into four classes ( Figure 2c).…”
Section: Slope Mapmentioning
confidence: 99%
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“…This parameter is determined by the terrain ratio, which denotes the ratio of the height difference between two points divided by the horizontal straight line distance between them [18,31]. The slope parameter has an effect on the runoff, sedimentation ratio, recharge, surface water velocity, and the number of materials essential to creating dams [25]. The DEM with a 30 m resolution was used to generate the slope map, and the area was then divided into four classes ( Figure 2c).…”
Section: Slope Mapmentioning
confidence: 99%
“…The profiles of the dams are based on the method described throughout this paper. Nevertheless, some of the proposed dam heights may not be feasible in practice because of some other factors such as the movement of material, or the dam's width [25]. In addition to the five criteria used in this study, there are other criteria not considered in this study such as geology and socio-economic aspects [18].…”
Section: Sites Proposed For Small and Medium Damsmentioning
confidence: 99%
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“…Low stream orders have high permeability as compared to the high stream orders. The low stream orders also have high infiltration rates as compared to the high stream orders [24]. Stream orders are essential in the planning of conservation measures in terms of storage and capacity [25].…”
Section: Stream Ordermentioning
confidence: 99%
“…The recharge of groundwater occurs when rainfall or snowmelt water infiltrates into the aquifer [6,7]. The occurrence and movement of groundwater are determined by physical edifices, topographic condition, lithological difference, gradient, soil, drainage form and climate [8][9][10]. Hence, it is necessary to consider all these factors, to understand groundwater recharge potential of an area.…”
Section: Introductionmentioning
confidence: 99%