Comparison of Two Computational Methods for Estimating Transmissivity Based on the Picking Equation
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The PPC-Recovery method offers a time-efficient alternative to PICKINGmodel for estimating transmissivity in low-yielding wells. Both methods, based on the Picking equation, yield statistically similar results for transmissivity.
Area of Science:
- Hydrogeology
- Geophysical Well Logging
Background:
- Accurate estimation of aquifer transmissivity is crucial for managing groundwater resources, especially in low-yielding domestic wells.
- Traditional methods for transmissivity estimation can be time-consuming and require specialized software.
Purpose of the Study:
- To compare the efficacy of two computational methods, PICKINGmodel and PPC-Recovery, for estimating transmissivity using water-level recovery data.
- To evaluate the PPC-Recovery method as a potentially faster and less labor-intensive alternative to PICKINGmodel for low-yielding domestic wells.
Main Methods:
- Pumping tests were conducted in 50 domestic bedrock wells in south-central New York State by the United States Geological Survey (USGS).
- Water-level recovery data from these tests were analyzed using the PICKINGmodel and PPC-Recovery, both based on the Picking equation.
- The PPC-Recovery method was also applied to truncated recovery data to assess its performance under modified conditions.
Main Results:
- Estimated transmissivities ranged from 0.86 to 2900 ft²/d, with a median of 41 ft²/d.
- Statistical comparison showed no significant difference between transmissivity values estimated by PICKINGmodel and PPC-Recovery (95% probability).
- PPC-Recovery applied to truncated data also yielded statistically similar median transmissivity values compared to PICKINGmodel.
Conclusions:
- The PPC-Recovery method provides transmissivity estimates comparable to PICKINGmodel for low-yielding domestic wells.
- Using PPC-Recovery, particularly with truncated data, offers a viable and more efficient alternative for transmissivity estimation, saving time and effort.
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