Abstract
The results obtained by interfacing a hydrological model with a hydrogeochemical model are presented and compared to the observed data collected from the Turkey Lakes Watershed. The most prominent feature shown in the data is the progressive increase of pH, alkalinity and Ca++ + Mg++ in the downstream direction. Analysis of the model results indicates that the proportion of groundwater input to total runoff in the headwater and downstream areas plays an important role in creating these spatial gradients. The model also reproduces many of the episodic events, both temporal and spatial, shown in the observed data.
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