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Type: | Resource | |
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Created: | Feb 08, 2023 at 1:48 p.m. | |
Last updated: | Feb 08, 2023 at 1:49 p.m. | |
Citation: | See how to cite this resource |
Sharing Status: | Public |
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Views: | 560 |
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Abstract
Numerical models of ground-water flow within the regional aquifer underlying Lambton County, Ontario, Canada, are constructed by the conjunctive application of methods of regression and inverse analyses. Regression analysis of physiographic and hydraulic head data reveals a distinct relation between ground-water levels and ground-surface topography that is used to condition the aquifer models that are subjected to inverse analysis. Inverse analysis determines the variation of hydraulic head along the perimeter of the region and the distribution of ground-water recharge and discharge within the region that optimally replicate the observed hydraulic head data. The use of physiographic data as a substitute for geologic data in the construction of the aquifer models is defended on the basis of the constraints that apply to the investigation and the opportunity to invoke hydrogeologic judgment in the evaluation of the results. Interpretation of the results of the analyses reveals important characteristics of the hydrogeology of Lambton County, including an area of elevated groundwater recharge and the partitioning of ground-water discharge to the Saint Clair River.
Subject Keywords
Coverage
Spatial
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Additional Metadata
Name | Value |
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DOI | 10.1061/(ASCE)0733-9496(1996)122:1(1) |
Depth | 100 |
Scale | 1 001 - 10 000 km² |
Layers | 1 |
Purpose | Groundwater resources;Scientific investigation (not related to applied problem) |
GroMoPo_ID | 245 |
IsVerified | True |
Model Code | SUTRA |
Model Link | https://doi.org/10.1061/(ASCE)0733-9496(1996)122:1(1) |
Model Time | SS |
Model Year | 1996 |
Model Authors | Piggott, AR; Bobba, AG; Novakowski, KS |
Model Country | Canada |
Data Available | Report/paper only |
Developer Email | NA |
Dominant Geology | Unconsolidated sediments |
Developer Country | Canada |
Publication Title | Regression and inverse analyses in regional ground-water modeling |
Original Developer | No |
Additional Information | Regression analysis is used to find relationship between ground surface and water table. An inverse model is used to replicate hydraulic head data using hydraulic head along the perimeter. |
Integration or Coupling | None of the above |
Evaluation or Calibration | Static water levels |
Geologic Data Availability | No |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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