Kortatsi, B.K.Anku, Y.S.A.Anornu, G.K.2019-04-182019-04-182009-09Kortatsi, B.K., Anku, Y.S.A. & Anornu, G.K. Environ Geol (2009) 58: 1349. https://doi.org/10.1007/s00254-008-1638-9Volume 58, Issue 6, pp 1349–1359https://doi.org/10.1007/s00254-008-1638-9http://ugspace.ug.edu.gh/handle/123456789/29393Groundwater composition in the Kulpawn basin is largely controlled by aluminosilicates dissolution and cation exchange resulting in mainly Ca-Mg-HCO3 and NaHCO3 water types. Principal component analysis, Piper graphical classification, and stable isotope (18O and 2H) of groundwater and surface-water samples were used to delineate geochemical processes and groundwater facies. The groundwater is mildly acid to neutral and low in conductivity. Chemical constituents except HCO3- and SiO2 have low concentration. No cation shows clear majority, however, the order of relative abundance is Na+ > Ca2+ > Mg2+ > K+. HCO3- is the predominant anion and the order of abundance is HCO3- > NO3- > SO42- > Cl-. SiO2 concentration is high compared with the major cations. Dissolution of plagioclase, pyroxene and biotite and cation exchange are responsible for groundwater composition. Isotopic data suggest integrative, smooth and rapid recharge from meteoric origin. The groundwater quality is generally good for domestic usage; however, 18 and 47% of boreholes respectively have NO3- and F- levels outside WHO recommended limits suggesting potential physiological problems in some localities. The groundwater has low sodium absorption ratio and low to moderate salinity hazard but significant magnesium hazard partially limiting its use for irrigation. © Springer-Verlag 2008.enAluminosilicates weatheringCation exchangeGhana Kulpawn BasinPrincipal component analysisArticle