2022
DOI: 10.1007/s41101-022-00130-7
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Investigation of groundwater potential in quaternary undifferentiated geological formation in Fogera district, Amhara, Ethiopia

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Cited by 5 publications
(2 citation statements)
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“…As a result, it is a crucial component in determining the groundwater potential zone obtained from DEM data. Finding the length of the stream and dividing on to the total area of the basin as shown in the equation of Drainage Density DD=L (length/A (area) and using Archydro program [24]. The drainage-density map (Figure 3) was created by dividing themed river maps produced from a basin-wide flow accumulation (Fac) and stream definition operation [25].…”
Section: Drainage Densitymentioning
confidence: 99%
“…As a result, it is a crucial component in determining the groundwater potential zone obtained from DEM data. Finding the length of the stream and dividing on to the total area of the basin as shown in the equation of Drainage Density DD=L (length/A (area) and using Archydro program [24]. The drainage-density map (Figure 3) was created by dividing themed river maps produced from a basin-wide flow accumulation (Fac) and stream definition operation [25].…”
Section: Drainage Densitymentioning
confidence: 99%
“…As a result, it is a crucial component in determining the groundwater potential zone obtained from DEM data. Finding the length of the stream and dividing on to the total area of the basin as shown in the equation of Drainage Density DD = L (length / A (area) and using Archydro program [21].The drainage-density map was created by dividing themed river maps produced from a basin-wide ow accumulation (Fac) and stream de nition operation [22].…”
Section: Drainage Densitymentioning
confidence: 99%