TY - JOUR
T1 - Determination of the mineral stability field of evolving groundwater in the Lake Bosumtwi impact crater and surrounding areas
AU - Loh, Yvonne Sena Akosua
AU - Yidana, Sandow Mark
AU - Banoeng-Yakubo, Bruce
AU - Sakyi, Patrick Asamoah
AU - Addai, Millicent Obeng
AU - Asiedu, Daniel Kwadwo
N1 - Publisher Copyright:
© 2016 Elsevier Ltd
PY - 2016/9/1
Y1 - 2016/9/1
N2 - Conventional graphical techniques, mass balance geochemical modelling, and multivariate statistical methods were jointly applied to hydrogeochemical data of groundwater from the fractured rock aquifer system, and surface water in the Bosumtwi and surrounding areas to reveal evolutionary trends and the characteristics of evolving groundwater in the area. Four clusters distinguished from the Q-mode hierarchical cluster analysis (HCA) comprised three main groundwater associations and one surface water group (lake water). Although both water resources are of low mineralization (TDS < 1000 mg/l), it was observed that the groundwater from the upper catchment with hydrochemical facies dominated by [Formula presented]3−, evolves to [Formula presented] and mixed cations HCO3− water types at the lower reaches. The lake water on the other hand is [Formula presented]3− water type. Results from principal component analyses (PCA) and other geochemical interpretations distinguished three sources of variations in the hydrochemistry. Saturation indices of possible reactive mineral phases show groundwater undersaturation relative to albite, anorthite, aragonite, barite, calcite, chlorite, chrysotile, dolomite, gypsum, k-felspar and talc, and supersaturation with respect to gibbsite, kaolinite, Ca-montmorillonite and k-mica in the area. The PCA and other geochemical interpretation identify weathering of feldspars and carbonate mineral dissolution as predominantly influencing the hydrochemistry of the groundwater. Hydrolysis of the aluminosilicates causes the groundwater to reach equilibrium with kaolinite. In addition to dissolution of silicates, the chemical composition of the lake water has been influenced by evaporation and consequent carbonate saturation.
AB - Conventional graphical techniques, mass balance geochemical modelling, and multivariate statistical methods were jointly applied to hydrogeochemical data of groundwater from the fractured rock aquifer system, and surface water in the Bosumtwi and surrounding areas to reveal evolutionary trends and the characteristics of evolving groundwater in the area. Four clusters distinguished from the Q-mode hierarchical cluster analysis (HCA) comprised three main groundwater associations and one surface water group (lake water). Although both water resources are of low mineralization (TDS < 1000 mg/l), it was observed that the groundwater from the upper catchment with hydrochemical facies dominated by [Formula presented]3−, evolves to [Formula presented] and mixed cations HCO3− water types at the lower reaches. The lake water on the other hand is [Formula presented]3− water type. Results from principal component analyses (PCA) and other geochemical interpretations distinguished three sources of variations in the hydrochemistry. Saturation indices of possible reactive mineral phases show groundwater undersaturation relative to albite, anorthite, aragonite, barite, calcite, chlorite, chrysotile, dolomite, gypsum, k-felspar and talc, and supersaturation with respect to gibbsite, kaolinite, Ca-montmorillonite and k-mica in the area. The PCA and other geochemical interpretation identify weathering of feldspars and carbonate mineral dissolution as predominantly influencing the hydrochemistry of the groundwater. Hydrolysis of the aluminosilicates causes the groundwater to reach equilibrium with kaolinite. In addition to dissolution of silicates, the chemical composition of the lake water has been influenced by evaporation and consequent carbonate saturation.
KW - Anthropogenic
KW - Crater
KW - Lake Bosumtwi
KW - Multivariate statistical analysis
KW - Weathering
UR - http://www.scopus.com/inward/record.url?scp=84975853495&partnerID=8YFLogxK
U2 - 10.1016/j.jafrearsci.2016.06.007
DO - 10.1016/j.jafrearsci.2016.06.007
M3 - Review article
AN - SCOPUS:84975853495
SN - 1464-343X
VL - 121
SP - 286
EP - 300
JO - Journal of African Earth Sciences
JF - Journal of African Earth Sciences
ER -