Hydrogeologic framework and borehole yields in Ghana
Autor: | P. Gyau-Boakye, S. Dapaah-Siakwan |
---|---|
Rok vydání: | 2000 |
Předmět: | |
Zdroj: | Hydrogeology Journal. 8:405-416 |
ISSN: | 1435-0157 1431-2174 |
DOI: | 10.1007/pl00010976 |
Popis: | In Ghana, 68% of the population live in rural communities, which are scattered and remote. Groundwater is the most feasible source of potable water supply for most of these dispersed and remote settlements. To meet the present and future challenges of population expansion vis-a-vis the observed declining rainfall in most parts of Africa including Ghana, it is necessary to assess, efficiently manage, and utilize the groundwater resources. The objective of this paper is therefore to describe the hydrogeologic framework and analyze borehole yields as part of the groundwater-resources assessment of Ghana. The hydrogeologic units are broadly categorized as: (1) the Basement Complex (crystalline rocks), which underlies about 54% of the country; (2) the Voltaian System, which underlies about 45%; and (3) the Cenozoic, Mesozoic, and Paleozoic sedimentary strata (Coastal Provinces), which underlie the remaining 1% of the country. The Basement Complex and the Coastal Provinces have higher groundwater potential than the Voltaian System. This is particularly significant, because the Basement Complex and the Coastal Provinces underlie the most densely populated areas of the country and can hence be tapped for human use. The average borehole yields of the Basement Complex, the Coastal Provinces and the Voltaian System range from 2.7–12.7, 3.9–15.6, and 6.2–8.5 m3/h, respectively. |
Databáze: | OpenAIRE |
Externí odkaz: |