2006
DOI: 10.1016/j.jhydrol.2005.09.003
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Determination of stochastic well head protection zones by direct propagation of uncertainties of particle tracks

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Cited by 19 publications
(18 citation statements)
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References 29 publications
(34 reference statements)
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“…This is a reasonable simplification, since aquifer heterogeneity adds uncertainty in the prediction of transport pathways and duration, but does not change the long-term recharge contribution from septic drainfields and hence does not change the overall size of the source area, only its actual shape and location (Kunstmann and Kastens, 2006). Since our analysis is already probabilistic with respect to the exact shape and location relative to the lot shape, aquifer heterogeneity would not add to the reported uncertainty.…”
Section: Discussionmentioning
confidence: 99%
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“…This is a reasonable simplification, since aquifer heterogeneity adds uncertainty in the prediction of transport pathways and duration, but does not change the long-term recharge contribution from septic drainfields and hence does not change the overall size of the source area, only its actual shape and location (Kunstmann and Kastens, 2006). Since our analysis is already probabilistic with respect to the exact shape and location relative to the lot shape, aquifer heterogeneity would not add to the reported uncertainty.…”
Section: Discussionmentioning
confidence: 99%
“…Subsurface heterogeneity is difficult to assess and typically leads to increased dispersion ("macrodispersion"). Macro-dispersion increases the source area of a well (Kunstmann and Kastens, 2006). Regional groundwater flow direction can typically be retrieved from regional water level contour maps generated by state or federal agencies.…”
Section: Source Area Intersection With Septic Drainfieldsmentioning
confidence: 99%
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“…The source area size per capita is therefore at least 0.1 ha. Uncertainties about actual groundwater flow direction and about aquifer heterogeneity, and the transient flow dynamics due to seasonal influence of nearby large capacity agricultural irrigation wells lead to areas contributing to recharge of a well to be significantly larger than Equation (2) (e.g., [53,54]. Information regarding groundwater flow, location of community wells, soil characteristics, and current areas of agricultural production may contribute to this determination.…”
Section: Determining Recharge Buffer Zone Areamentioning
confidence: 99%