1990
DOI: 10.1007/bf00008442
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A review of some characteristics of freshwater and coastal ecosystems in Ghana

Abstract: Data collected over a ten year period have been used to review some characteristics of freshwater and coastal ecosystems in Ghana. Studies were conducted on two recently formed man-made lakes, one river, five coastal lagoons and waters along the ocean front.Freshwaters had near neutral pH while coastal waters were alkaline. In both ecosystems the pH of sediments were lower than those of corresponding waters. While the transparency of coastal waters varied within narrow limits, large variations were observed in… Show more

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Cited by 28 publications
(26 citation statements)
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“…The temperature recorded for the entire study ranged from 27.4 to 31.8°C. According to Biney (1990), this is typical of shallow coastal waters in Ghana, where ambient temperatures remain within a narrow range of 25-35°C. An average temperature of 29.3°C was recorded during the study period which is comparable to that obtained by Biney (1986) in the Kpeshi lagoon 29.4°C.…”
Section: Resultsmentioning
confidence: 99%
“…The temperature recorded for the entire study ranged from 27.4 to 31.8°C. According to Biney (1990), this is typical of shallow coastal waters in Ghana, where ambient temperatures remain within a narrow range of 25-35°C. An average temperature of 29.3°C was recorded during the study period which is comparable to that obtained by Biney (1986) in the Kpeshi lagoon 29.4°C.…”
Section: Resultsmentioning
confidence: 99%
“…The mean water temperatures varied from 29.0 to 29.8 o C and 27.8 to 28.1 o C for Sakumo II and Muni lagoons, respectively. This is typical of shallow coastal waters in Ghana, where ambient temperatures remain within a narrow range of 25-35 o C (Biney, 1990).…”
Section: Physical Parametersmentioning
confidence: 90%
“…Dominance of Ca and Mg ions in lake water is linked primarily with parent rock material present in the catchment area [85]. It is also apparent that the dominance of Cl − over SO4 2− could be due to the large amount of domestic and sewage water being discharged into tributary waters [86]. The primary source of major ions in the river and lake waters is atmospheric deposition, dissolution of evaporates (halite, gypsum), and weathering of carbonates and silicates by sulphuric acid or carbonic acid and anthropogenic activities.…”
Section: Discriminant Analysismentioning
confidence: 99%