T159 Groundwater for the Present and Future in the Mississippi Embayment Aquifer System, South-Central United States

Tuesday, 11 October 2022
8:00 AM - 12:00 PM
405


WATER BUDGET ACCOUNTING IN THE MISSISSIPPI EMBAYMENT REGION AND MISSISSIPPI ALLUVIAL PLAIN, 2000-2020, WITH UNCERTAINTY ANALYSIS, SEASONAL IMPACT OF IRRIGATION ON THE WATER BUDGET, AND ALTERNATE MODEL COMPARISON

Paper number: T159-15
Program: Technical Sessions
Time: 11:30 AM – 11:45 AM


Authors


Abstract

In support of a broad series of investigations into the hydrology of the Mississippi Alluvial Plain aquifer, a USGS Soil-Water-Balance model was constructed and calibrated to better understand the distribution and timing of water budget components from 2000-2020 in the study area. The calibration included history matching with observations of direct runoff, base flow, actual evapotranspiration (AET), and irrigation application. Uncertainty analysis using a Monte Carlo approach showed that the AET had the lowest uncertainty of all the components and the net infiltration had the highest uncertainty. The model analysis illustrated the effect of summer irrigation on the overall water budget in the alluvial plain, which increased the summer AET by 22 percent and total combined runoff and baseflow by 62 percent. The soil-water-balance model uses a rooting zone accounting method, which produces net infiltration estimates higher than groundwater recharge values calculated by means of a MODFLOW model of the study area, likely because of the presence of horizontal clay lenses that block much of the infiltration from reaching the water table. Challenges with determining true base flow from groundwater discharge in such an altered hydrologic system were partly responsible for an over-estimation of potential recharge relative to values estimated through MODFLOW history matching.

Geological Society of America Abstracts with Programs. Vol. 54, No. 6

doi: 10.1130/abs/2022AM-383080

© Copyright 2022 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.