THE EFFECTS OF EVAPORATION on THE CHEMISTRY OF THE OKAVANGO RIVER, NORTHWESTERN BOTSWANA
To isolate the effects of river water-vegetation-sediment interaction on riverine solute evolution, we investigated the effects of evaporation on water from the Okavango River delta. The experimental objective was to assess changes in water chemistry due to direct evaporation. These results can serve as a basis for evaluating the contribution of vegetative evapo-concentration and river water-vegetation-sediment interaction to surface and groundwater chemical evolution. Water was collected from the proximal (Mohembo) and distal (Maun) portions of the delta and evaporated in open containers outdoors under ambient conditions. Temporal measurements of pH, oxidation reduction potential (ORP), total dissolved solids (TDS), alkalinity, silica, dissolved inorganic carbon (DIC) and major ions were made. The values of all measured parameters increased with continued evaporation. Although the initial concentrations of the parameters for the two samples were different, all trends in parameter enrichment were similar, and linearly related to the extent of evaporation. Comparisons of the solute concentrations in the evaporative experiment with spatial river water samples from the Okavango River and shallow groundwater show similar relations. Thus, we infer that vegetative evapo-concentration is a primary mechanism in the evolution of solutes in surface and shallow groundwater in the Okavango River delta.