2013
DOI: 10.1007/s12665-013-2295-1
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Locating suitable sites for the construction of subsurface dams using GIS

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Cited by 43 publications
(20 citation statements)
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“…A major indicator of percolation rate is lithology, which determines the quality of a drainage network. The structure of a drainage network helps gauge the characteristics of a water holding zone [19]. The drainage density of the study area ranges from 0 to 0.58 per km 2 (Figure 3c).…”
Section: Data Usedmentioning
confidence: 99%
See 1 more Smart Citation
“…A major indicator of percolation rate is lithology, which determines the quality of a drainage network. The structure of a drainage network helps gauge the characteristics of a water holding zone [19]. The drainage density of the study area ranges from 0 to 0.58 per km 2 (Figure 3c).…”
Section: Data Usedmentioning
confidence: 99%
“…Nevertheless, the fuzzy model produced suitable results for clustered areas. Another study conducted for the Boda-Kalvsvik Island in Sweden implemented the weighted overlay analysis technique on layers including precipitation, evapotranspiration, potential recharge, piezometric level and geological and geomorphological layers [19]. The study was validated using the topographic wetness index method and groundwater balance.…”
Section: Introductionmentioning
confidence: 99%
“…However, in order to estimate the volumes of ripped and/or excavated material using Assumption 2, with stratigraphy, six typical patterns were assumed based on expert knowledge (Fig. 8) and patterns found in Jamali et al 2013: 1. Rock: In the case where the surface consisted of rock outcrops (pattern 1, Fig.…”
Section: Processing Stepsmentioning
confidence: 99%
“…Segundo Kim (2017), 6 barragens subterrâneas são operadas na Correia desde a década de 80, a maioria construída no início da mesma década. Experiências na região de Boda-Kalvsvik, na Suécia, buscaram através de ferramentas GIS e sensoriamento remoto localizar possíveis áreas para a construção desse tipo de barragem (JAMALI et al, 2013 (JACOMINE et al, 1975). Os solos em Sergipe podem ser de mais de 122 classes diferentes, variando entre areias quartzosas nas faixas litorâneas, litólitos eutróficos no sertão, entre outros (JACOMINE et al, 1975 (Freitas, 2010).…”
Section: Considerações Gerais Sobre As Barragens Subterrâneasunclassified