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Forest river plants and water quality in Ghana
Swaine, M.D.; Adomako, J.; Ameka, G.; de Graft-Johnston, K.A.A.; Cheek, M. (2006). Forest river plants and water quality in Ghana. Aquat. Bot. 85(4): 299-308. https://dx.doi.org/10.1016/j.aquabot.2006.06.007
In: Aquatic Botany. Elsevier Science: Tokyo; Oxford; New York; London; Amsterdam. ISSN 0304-3770; e-ISSN 1879-1522, more
Peer reviewed article  

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Keywords
    Environments > Tropical environment
    Forests
    Land use
    Management > Ecosystem management > River basin management
    Topographic features > Banks (topography) > River banks
    Water > River water
    Water quality
    Ghana [Marine Regions]
    Fresh water
Author keywords
    aquatic macrophytes; land use; river chemistry; tropical freshwater

Authors  Top 
  • Swaine, M.D.
  • Adomako, J.
  • Ameka, G.
  • de Graft-Johnston, K.A.A.
  • Cheek, M.

Abstract
    River plants and water chemistry in wet and dry seasons were sampled in a wide range of rivers with variable catchments in the forest zone of Ghana, in order to examine the relationships between the floristic composition within the river and river water and catchment environmental variables. Plant species occurring in the river or on its seasonally flooded banks along 500 m sample stretches were listed in 26 sites. Sample species richness was low (1-17 species per sample, mean 5.9). Only nine species were recorded that are confined to rivers. Cluster analysis defined five floristic groups which differed in catchment area, geology, turbidity and dissolved minerals. Analysis of water chemistry variables by principal components analysis revealed a strong principal gradient (42% of total variance) related to annual rainfall with low ionic concentrations under high rainfall. The second component described seasonal differences in water chemistry. Nitrate and chloride were more concentrated in the dry season, but sulphate and calcium were more concentrated in the wet season. Catchments with higher forest cover yielded more oligotrophic and less turbid water. Catchment geology influenced water chemistry so that sandstone areas yielded clear water, and ancient peneplain areas with bauxitic soil were characterised by exceptionally low silicon concentrations. The association of macrophyte composition with river chemistry and catchment conditions was somewhat tenuous, due to the low number of species, but the low turbidity, oligotrophic rivers under high rainfall and with a high percentage of species-rich forest cover were the more species rich. Prediction of river water quality at the scale of this study are more readily made from a knowledge of catchment rainfall and forest cover than from assessments of river plant composition.

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