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1DTempPro V2: New Features for Inferring Groundwater/Surface-Water Exchange
Franklin W Koch1, Emily B Voytek2, Frederick D Day-Lewis2
1Contractor to the U.S. Geological Survey, currently at University of Calgary, Department of Geoscience, ES118 2500 University Dr. NW, Calgary, AB T2N 1N4 Canada.
The updated 1DTempPro software enhances groundwater analysis by adding automated parameter estimation and accounting for layer heterogeneity and time-varying specific discharge. This improves assessments of groundwater/surface-water exchange and hydraulic conductivity calculations.
Area of Science:
- Hydrogeology
- Computational Modeling
- Environmental Science
Background:
- Accurate assessment of groundwater/surface-water interactions is crucial for water resource management.
- Estimating hydraulic conductivity often requires sophisticated numerical models.
- Previous versions of 1DTempPro facilitated analysis of one-dimensional temperature profiles.
Purpose of the Study:
- To introduce a new version of the 1DTempPro computer program with enhanced functionalities.
- To extend the capabilities for analyzing vertical one-dimensional temperature profiles under saturated flow conditions.
- To improve the estimation of hydraulic conductivity and assessment of groundwater/surface-water exchange.
Main Methods:
- The enhanced 1DTempPro program serves as an interface to the U.S. Geological Survey's VS2DH model.
- New capabilities include automated parameter estimation.
- The model now incorporates layer heterogeneity and time-varying specific discharge for more realistic simulations.
Main Results:
- The updated software provides advanced tools for analyzing temperature profiles in saturated subsurface flow.
- Automated parameter estimation streamlines the process of determining model parameters.
- Inclusion of layer heterogeneity and time-varying specific discharge allows for more nuanced and accurate modeling.
Conclusions:
- The upgraded 1DTempPro program offers a more powerful and versatile tool for hydrogeological studies.
- It facilitates improved estimation of hydraulic conductivity when hydraulic head is known.
- The enhanced features support better understanding of groundwater/surface-water exchange processes.
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