Based on the experience from runoff and groundwater recharge simulation a model system has been developed for terrestrial, hydrochemical, and hydrological simulations. The system emphasizes the role of temporary or long term storage in the aquifers of a basin and, separately, accounts for each rainfall or snowmelt event from its entrance into the ground until mixing in the river system. The model is primarily intended for simulation of natural short term variations in alkalinity and pH in running waters. -from Authors
CITATION STYLE
Bergstrom, S., Carlsson, B., Sandberg, G., & Maxe, L. (1985). Integrating modelling of runoff, alkalinity, and pH on a daily basis. Nordic Hydrology, 16(2), 89–104. https://doi.org/10.2166/nh.1985.0008
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