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Type: | Resource | |
Storage: | The size of this resource is 1.5 KB | |
Created: | Feb 08, 2023 at 4:26 p.m. | |
Last updated: | Feb 08, 2023 at 4:27 p.m. | |
Citation: | See how to cite this resource |
Sharing Status: | Public |
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Views: | 460 |
Downloads: | 232 |
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Abstract
A new inverse technique for modelling groundwater flow, based on a functional minimization technique, has been used to calibrate a groundwater flow model of a subregion of the Port Willunga aquifer within the Willunga Basin in South Australia. The Willunga Basin is the location of extensive viticulture, irrigated primarily by groundwater, the levels and quality of which have declined significantly over the last 40 years. The new method is able to generate estimates of transmissivity, storativity and groundwater recharge over the whole subregion as a time-varying continuous surface; previous methods estimate local discrete parameter values at specific times. The new method has also been shown to produce accurate head values for the subregion and very good estimates of groundwater recharge. Its ultimate goal will be to provide a new and invaluable tool for significantly improved groundwater resource management.
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Additional Metadata
Name | Value |
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DOI | 10.1007/s10040-007-0189-6 |
Depth | |
Scale | |
Layers | |
Purpose | Groundwater resources |
GroMoPo_ID | 352 |
IsVerified | True |
Model Code | Unknown |
Model Link | https://doi.org/10.1007/s10040-007-0189-6 |
Model Time | 1998-1999 |
Model Year | 2007 |
Model Authors | Knowles, I; Teubner, M; Yan, A; Rasser, P; Lee, JW |
Model Country | Australia |
Data Available | Report/paper only |
Developer Email | mteubner@maths.adelaide.edu.au |
Dominant Geology | Unconsolidated sediments |
Developer Country | Australia; USA |
Publication Title | Inverse groundwater modelling in the Willunga Basin, South Australia |
Original Developer | No |
Additional Information | |
Integration or Coupling | None of the above |
Evaluation or Calibration | Unsure |
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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