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| Created: | Feb 08, 2023 at 3:36 p.m. | |
| Last updated: | Mar 23, 2023 at 6:29 p.m. | |
| Citation: | See how to cite this resource |
| Sharing Status: | Public |
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| Views: | 581 |
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Abstract
Alluvial aquifers by nature are complex caused by varied depositional environments. Developing a reliable groundwater model to represent an alluvial aquifer is non-trivial. Also, relying on a single best calibrated model may not be sufficient because of an inadequate choice of model parameter values. To better understand groundwater dynamics and improve model prediction reliability, this study presents a Bayesian multi-model uncertainty quantification (BMMUQ) framework to account for model parameter uncertainty in complex alluvial groundwater modeling. The methodology was applied to the agriculturally intensive Mississippi River alluvial aquifer (MRAA), Northeast Louisiana. An aquifer architecture was first constructed using 7,259 well logs in the MRAA area which covers three fluvial deposits (alluvium, braided-stream terrace, and braided-stream terrace-loess). A 12-layer MODFLOW model was then developed to address the alluvial aquifer complexity and well calibrated through a genetic algorithm. This study quantified model parameter uncertainty in hydraulic conductivity and specific storage of sand facies. Bayesian model averaging (BMA) with the Expectation Maximization (EM) algorithm was adopted to derive posterior model weights and head variances of 50 alternative conceptual groundwater flow models, and thereby obtains BMA ensemble model predictions instead of only relying on the best calibrated conceptual model. Results show that an estimated around 950 million m(3) of groundwater storage loss occurs in 2015 with respect to the beginning of 2004, due to high groundwater demand for irrigation in the MRAA area. Explicitly quantifying model uncertainty can produce more reliable groundwater level predictions from BMA ensemble model. The presented groundwater modeling framework improves our understanding of the MRAA and provides a valuable tool to assist agricultural water management.
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Additional Metadata
| Name | Value |
|---|---|
| DOI | 10.1016/j.jhydrol.2021.126682 |
| Depth | 70 |
| Scale | 10 001 - 100 000 km² |
| Layers | 12 |
| Purpose | Groundwater resources |
| GroMoPo_ID | 317 |
| IsVerified | True |
| Model Code | MODFLOW |
| Model Link | https://doi.org/10.1016/j.jhydrol.2021.126682 |
| Model Time | 2004-2015 |
| Model Year | 2021 |
| Model Authors | Yin, JN; Tsai, FTC; Kao, SC |
| Model Country | United States |
| Data Available | Report/paper only |
| Developer Email | jnyin@hhu.edu.cn; ftsai@lsu.edu; kaos@ornl.gov |
| Dominant Geology | Unconsolidated sediments |
| Developer Country | Peoples R China; USA |
| Publication Title | Accounting for uncertainty in complex alluvial aquifer modeling by Bayesian multi-model approach |
| Original Developer | No |
| Additional Information | |
| Integration or Coupling | |
| Evaluation or Calibration | Dynamic 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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