Abstract:
This research evaluates groundwater potential and quality in (Sinako-Yekalo watershed
Tekezie Basin, Ethiopia). The study area is generally characterized by various topographic
features. The high land area is covered by Tarmaber Formation and the remaining area
consists of Ashangi Formation and Aiba basalt. Insufficient water resources, lack of
hydrogeological investigation, and increasing demand for water resources for different
purposes are the main problems in the study area. Therefore, this study aims to identify the
groundwater potential zone, aquifer system, and suitability of groundwater for drinking and
irrigation purposes. Different approaches have been used to quantify hydrometeorological
components and estimate the recharge amount in the study area. The annual rainfall of point
data from different nearby stations of the area were analyzed by using two methods (Thiessen
polygon and Isohetal). The annual recharge in the study area is estimated by using soil water
balance (SWB) method considering different meteorological components (areal depth of
rainfall, evapotranspiration, temperature, wind speed, sunshine hour, and relative humidity).
The groundwater potential zone was delineated from seven thematic layers (rainfall, geology,
slope, land use land cover, drainage density, lineament density, and soil) by weighted overlay
using the analytical hierarchy process (AHP) tool of the multi-criteria decision analysis
(MCDA) technique. The groundwater potential zone map in the study area is categorized into
five different zones. These are very low (0.4%), low (5%), moderate (56%), high (36.6%), and
very high (2%). The aquifer system in the study area can be categorized into low (0.5-2 l/s),
moderate (2-5 l/s), high (5-25 l/s), and very high (>25 l/s) productive aquifers based on wells
and springs yield. The water types in the study area includes Ca-HCO
3
IV
, Ca-Mg-HCO
3
, NaNO
3
-HCO
3
, Na-Ca-HCO
3
, Ca-Na-HCO
3
, and Ca-Na-Mg-HCO
3
. The water sources from
boreholes, rivers, and springs except for 12.5% of water points are suitable for drinking and
irrigation purposes.