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Tracer Transport through Seepage Lakes
Residence times of tracers in rectangular seepage lakes with wind-driven circulation are investigated in this paper. The key dimensionless parameters are and , in which is the diffusion coefficient transverse to the wind direction, is the dimension of the lake aligned with the direction of groundwater inflow/outflow, is the specific discharge of groundwater entering and leaving the lake, and are the lake dimensions in the wind direction and transverse to the wind direction, respectively, and V is the wind speed. The well-mixed approximation in rectangular lakes is reasonable when and . Under these conditions, tracer particles are distributed uniformly over the outflow surface, and the probability distribution of tracer residence times can be estimated theoretically without the need to develop a numerical mixing model for the lake.
Tracer Transport through Seepage Lakes
Residence times of tracers in rectangular seepage lakes with wind-driven circulation are investigated in this paper. The key dimensionless parameters are and , in which is the diffusion coefficient transverse to the wind direction, is the dimension of the lake aligned with the direction of groundwater inflow/outflow, is the specific discharge of groundwater entering and leaving the lake, and are the lake dimensions in the wind direction and transverse to the wind direction, respectively, and V is the wind speed. The well-mixed approximation in rectangular lakes is reasonable when and . Under these conditions, tracer particles are distributed uniformly over the outflow surface, and the probability distribution of tracer residence times can be estimated theoretically without the need to develop a numerical mixing model for the lake.
Tracer Transport through Seepage Lakes
Chin, David A. (Autor:in)
17.03.2016
Aufsatz (Zeitschrift)
Elektronische Ressource
Unbekannt
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