SEAWAT Model of Flow and Chloride Transport in the 1,500-Foot, 2,400-Foot, and 2,800-Foot Sands of the Baton Rouge Area, Louisiana
An updated three-dimensional, groundwater-flow and chloride-transport model (SEAWAT)
of the Southern Hills regional aquifer system in southeastern Louisiana and southwestern
Mississippi was developed to examine the effects of groundwater withdrawals on the rate
and pathways of saltwater migration in the “1,500-foot” sand, “2,400-foot” sand, and
“2,800-foot” sand. New interpretations of stratigraphic correlations amongst geophysical
well logs were utilized to revise a hydrogeologic-framework that delineates the depth and
thickness variations of aquifers and confining units in the Southern Hills regional aquifer
system. Regional groundwater flow throughout the Southern Hills regional aquifer system
was first simulated with MODFLOW, and flow-model parameters were calibrated to 8,810
water levels observed through 2016 with the parameter-estimation code PEST++. Saltwater
transport was subsequently simulated for the “1,500-foot” sand, “2,400-foot” sand, and
“2,800-foot” sand with the variable-density code, SEAWAT. Chloride-concentration
measurements were used as a proxy for the saltwater to formulate the concentration
initial conditions and calibrate the transport-model parameters. Three hypothetical
groundwater management scenarios are included in the archive. These scenarios
simulate the future water levels and chloride concentrations within the “1,500-foot”
sand, “2,400-foot” sand, and “2,800-foot” sand if groundwater withdrawals were to
continue at 2016 rates or if one of two proposed modifications to the 2016 withdrawals
from the “1,500-foot” sand or “2,800-foot” sand were to be enacted. The model was
calibrated to water levels measured in aquifers beneath the “400-foot” sand, and water
levels simulated in these aquifers could be used for various purposes, including predicting
the effects of changing pumping rates. Water planners and managers need additional
knowledge about the effects of groundwater withdrawals on the rate and pathways of
saltwater migration and a tool to assess possible management strategies that could
control further saltwater encroachment in the Baton Rouge area. This USGS data release
contains all of the input and output files for the simulations described in the associated
model documentation report (https://doi.org/10.3133/sir20195102).
Complete Metadata
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| contactPoint |
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|
| description | An updated three-dimensional, groundwater-flow and chloride-transport model (SEAWAT) of the Southern Hills regional aquifer system in southeastern Louisiana and southwestern Mississippi was developed to examine the effects of groundwater withdrawals on the rate and pathways of saltwater migration in the “1,500-foot” sand, “2,400-foot” sand, and “2,800-foot” sand. New interpretations of stratigraphic correlations amongst geophysical well logs were utilized to revise a hydrogeologic-framework that delineates the depth and thickness variations of aquifers and confining units in the Southern Hills regional aquifer system. Regional groundwater flow throughout the Southern Hills regional aquifer system was first simulated with MODFLOW, and flow-model parameters were calibrated to 8,810 water levels observed through 2016 with the parameter-estimation code PEST++. Saltwater transport was subsequently simulated for the “1,500-foot” sand, “2,400-foot” sand, and “2,800-foot” sand with the variable-density code, SEAWAT. Chloride-concentration measurements were used as a proxy for the saltwater to formulate the concentration initial conditions and calibrate the transport-model parameters. Three hypothetical groundwater management scenarios are included in the archive. These scenarios simulate the future water levels and chloride concentrations within the “1,500-foot” sand, “2,400-foot” sand, and “2,800-foot” sand if groundwater withdrawals were to continue at 2016 rates or if one of two proposed modifications to the 2016 withdrawals from the “1,500-foot” sand or “2,800-foot” sand were to be enacted. The model was calibrated to water levels measured in aquifers beneath the “400-foot” sand, and water levels simulated in these aquifers could be used for various purposes, including predicting the effects of changing pumping rates. Water planners and managers need additional knowledge about the effects of groundwater withdrawals on the rate and pathways of saltwater migration and a tool to assess possible management strategies that could control further saltwater encroachment in the Baton Rouge area. This USGS data release contains all of the input and output files for the simulations described in the associated model documentation report (https://doi.org/10.3133/sir20195102). |
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| identifier | http://datainventory.doi.gov/id/dataset/USGS_047b61a0-31c1-486b-b92c-620fb841723e |
| keyword |
[
"Ascension Parish",
"Avoyelles Parish",
"Baton Rouge",
"Concordia Parish",
"East Baton Rouge Parish",
"East Feliciana Parish",
"Groundwater",
"Groundwater Model",
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"salinity",
"usgsgroundwatermodel",
"water budget",
"water use"
]
|
| modified | 2020-11-17T00:00:00Z |
| publisher |
{
"name": "U.S. Geological Survey",
"@type": "org:Organization"
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|
| spatial | -91.915925, 30.242934, -90.447555, 31.337561 |
| theme |
[
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|
| title | SEAWAT Model of Flow and Chloride Transport in the 1,500-Foot, 2,400-Foot, and 2,800-Foot Sands of the Baton Rouge Area, Louisiana |