Hydrochemical evaluation of the Voltaian system-The Afram Plains area, Ghana

Sandow Mark Yidana, Duke Ophori, Bruce Banoeng-Yakubo

Research output: Contribution to journalArticle

38 Citations (Scopus)

Abstract

Inverse geochemical modeling from PHREEQC, and multivariate statistical methods were jointly used to define the genetic origin of chemical parameters of groundwater from the Voltaian aquifers in the Afram Plains area. The study finds, from hierarchical cluster analysis that there are two main hydrochemical facies namely the calcium-sodium-chloride-bicarbonate waters and the magnesium-potassium-sulfate-nitrate waters in the northern and southern sections, respectively, of the Afram Plains area. This facies differentiation is confirmed by the distribution of the SO42-/Cl- ratio, which associates groundwater from the northern and southern sections to areas influenced by contact with evaporites and seawater, respectively. Principal component analysis (PCA) with varimax rotation using the Kaiser criterion identifies four principal sources of variation in the hydrochemistry. Mineral saturation indices calculated from both major ions and trace elements, indicate saturation-supersaturation with respect to calcite, aragonite, k-mica, chlorite, rhodochrosite, kaolinite, sepiolite, and talc, and undersaturation with respect to albite, anorthite, and gypsum in the area. Inverse geochemical modeling along groundwater flowpaths indicates the dissolution of albite, anorthite and gypsum and the precipitation of kaolinite, k-mica, talc, and quartz. Both the PCA and inverse geochemical modeling identify the incongruent weathering of feldspars as the principal factors controlling the hydrochemistry in the Afram Plains area. General phase transfer equations have been developed to characterize the geochemical evolution of groundwater in the area. A very good relationship has been established between calcite and aragonite saturation indices in the Afram Plains area, with R2=1.00.

Original languageEnglish
Pages (from-to)697-707
Number of pages11
JournalJournal of Environmental Management
Volume88
Issue number4
DOIs
StatePublished - 1 Sep 2008

Fingerprint

Groundwater
Hydrochemistry
Talc
groundwater
hydrochemistry
anorthite
Kaolinite
talc
Calcite
Gypsum
Mica
saturation
aragonite
albite
mica
Principal component analysis
gypsum
kaolinite
principal component analysis
calcite

Keywords

  • Afram plains
  • Hierarchical cluster analysis
  • Inverse modeling
  • PHREEQC
  • Principal component analysis

Cite this

Yidana, Sandow Mark ; Ophori, Duke ; Banoeng-Yakubo, Bruce. / Hydrochemical evaluation of the Voltaian system-The Afram Plains area, Ghana. In: Journal of Environmental Management. 2008 ; Vol. 88, No. 4. pp. 697-707.
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Hydrochemical evaluation of the Voltaian system-The Afram Plains area, Ghana. / Yidana, Sandow Mark; Ophori, Duke; Banoeng-Yakubo, Bruce.

In: Journal of Environmental Management, Vol. 88, No. 4, 01.09.2008, p. 697-707.

Research output: Contribution to journalArticle

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