Report Open Access
Mekonen Gedewon
<?xml version='1.0' encoding='utf-8'?> <oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd"> <dc:creator>Mekonen Gedewon</dc:creator> <dc:date>2025-07-22</dc:date> <dc:description>The development of a balanced plan for water resource utilization necessitates a comprehensive assessment of water resources in terms of quality, quantity, spatial distribution, and the land use and land cover conditions of the entire catchment. The Mekaneselam and its surrounding area, located in the northern part of Ethiopia within the South Wollo Zone, are bordered by the Blue Nile Gorge to the south and the Yeshum River Gorge to the east. This region exhibits two distinct topographic features: the highlands, covering approximately 80% of the area and dominated by the Ashengie Formation, and the lowlands, comprising Quaternary volcanics. The catchment’s annual rainfall, determined through arithmetic averaging of point data from nearby stations, is approximately 1268 mm/year. Using a conventional recharge estimation method, the annual recharge rate of the catchment is calculated to be 230.4 mm/year. The primary aquifers in the area consist of scoria and vesicular basalt. Groundwater recharge, discharge conditions, and flow systems are predominantly influenced by rainfall, topographic features, and structural geology. The groundwater potential of the area is categorized into High, moderate, low, and very low, with the general groundwater flow direction from northeast to southwest, albeit with minor irregularities due to local topographic variations, deep wells, and structural influences. Hydrogeochemical analysis using Aquachem software identified four water types, including Ca-HCO3, Na-Ca-HCO3, Ca-Mg-HCO3, and Ca-Mg-HCO3-Cl. The dominant water type in the region is Ca-Mg-HCO3. Groundwater in the area evolves from Ca-HCO3 and CaMg-HCO3 types in recharge zones to Na-Ca-HCO3 types in discharge zones. This evolutionary trend is governed by processes such as dissolution, precipitation, cation exchange, and hydrolysis of silicate minerals. This study provides insights into groundwater recharge-discharge dynamics, flow systems, and hydrogeochemical evolution to support sustainable water resource planning and emphasizes the importance of implementing land use practices, monitoring water quality variations, and constructing storage facilities to enhance resource utilization in Mekaneselam and similar catchments.</dc:description> <dc:description>Funded by Mekdela Amba University</dc:description> <dc:identifier>https://zenodo.org/record/11619</dc:identifier> <dc:identifier>10.20372/nadre:11619</dc:identifier> <dc:identifier>oai:zenodo.org:11619</dc:identifier> <dc:relation>doi:10.20372/nadre:11618</dc:relation> <dc:relation>url:https://nadre.ethernet.edu.et/communities/mau-community</dc:relation> <dc:rights>info:eu-repo/semantics/openAccess</dc:rights> <dc:rights>http://www.opendefinition.org/licenses/cc-by</dc:rights> <dc:title>Groundwater Quality and Potential Assessment in Mekane Selam and its Surrounding Area, South Wollo, Ethiopia</dc:title> <dc:type>info:eu-repo/semantics/report</dc:type> <dc:type>publication-report</dc:type> </oai_dc:dc>
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