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Shallow Unconfined Flow on a Sloping Base Redux.
1Department of Civil, Environmental and Geo-Engineering, University of Minnesota, Minneapolis, MN, 55455.
Ground Water
|November 10, 2017
Summary
The impact of a sloping base on unconfined aquifer models is determined by saturated thickness relative to base elevation change, not just the slope magnitude. This finding simplifies complex groundwater modeling.
Area of Science:
- Hydrogeology
- Groundwater Modeling
- Mathematical Hydrology
Background:
- Unconfined aquifer analysis often involves complex models to account for sloping bases.
- Existing implicit solutions provide limited insight into the significance of base slope.
- The intuitive understanding of slope impact may be insufficient for accurate modeling.
Purpose of the Study:
- To explicitly solve the unconfined aquifer sloping base problem.
- To determine when complex models are justified based on sloping base impact.
- To offer a more insightful characterization of sloping base effects than existing methods.
Main Methods:
- Utilized recent mathematical advancements, specifically the Lambert W function.
- Developed an explicit analytical solution for the sloping base problem.
- Compared the explicit solution's insights against traditional implicit solutions (Dupuit, Polubarinov-Kochina, Harr, Child).
Main Results:
- The impact of a sloping base is not solely dependent on the slope's magnitude.
- An explicit solution reveals that the ratio of saturated thickness to change in base elevation is the key characterizing factor.
- This ratio provides superior insight compared to implicit solutions.
Conclusions:
- The simplified characterization using saturated thickness and base elevation change is crucial for determining the necessity of complex unconfined aquifer models.
- The explicit solution offers a more robust understanding of sloping base hydraulics.
- This research provides a new criterion for model selection in hydrogeology.
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