2001
DOI: 10.1016/s0899-5362(01)80069-5
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Pedological characteristics related to groundwater occurrence in the Tarkwa area, Ghana

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Cited by 26 publications
(18 citation statements)
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“…Most groundwaters in southern Ghana, in particular, fall within that range and the reasons are likely related to local geology. Kuma & Younger (2001) reported that the pH of the soils in the Tarkwa area varies from very acidic to moderately acidic, a condition attributed to the tropical climate and lush vegetation. Arsenic concentrations in the groundwaters ranged from < 0.1 µg l -1 to 4 µg l -1 (Table 1).…”
Section: Resultsmentioning
confidence: 99%
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“…Most groundwaters in southern Ghana, in particular, fall within that range and the reasons are likely related to local geology. Kuma & Younger (2001) reported that the pH of the soils in the Tarkwa area varies from very acidic to moderately acidic, a condition attributed to the tropical climate and lush vegetation. Arsenic concentrations in the groundwaters ranged from < 0.1 µg l -1 to 4 µg l -1 (Table 1).…”
Section: Resultsmentioning
confidence: 99%
“…Thus, a health risk to the people of Tarkwa consuming Mn-contami-nated water is of great concern. The geology of the Tarkwa area consists of Tarkwaian and Birimian systems (Kuma & Younger, 2001) and manganese-bearing horizons are quite ubiquitous in rocks of the Birimian suite.…”
Section: Concentration (µG ℓ -1 )mentioning
confidence: 99%
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“…The area is highly dissected and has moderate relief with a general decrease in elevation southwards (Kuma, 2007). The main types of soil in the area are the forest oxysols in the south and the forest ochrosol-oxysol in the north (Asklund & Eldvall, 2005), and consists mostly of silty-sands with minor patches of laterite (mainly on the hilly areas) and underlain by the Banket Series and Tarkwa Phyllite rocks (Kuma & Younger, 2001;Kortatsi, 2004).…”
Section: Study Area Descriptionmentioning
confidence: 99%
“…The analyzed data was used as input for the Hydrus-1D Computer code (Šimunek et al, 2005) and the modelling of bottom fluxes in the estimation of the potential recharge. Soil properties representing the four main soil types (Huni, Tarkwa Phyllite, Banket and Kawere) were determined for each of the profile components in describing the soil profile using the results of infiltration tests technique used by Kuma and Younger (2001). The soil hydraulic parameters, as presented in Table 1, were estimated using the pedo-transfer function model, Rosetta (Schaap et al, 2001).…”
Section: Meteorological Datamentioning
confidence: 99%