MODFLOW2005 model used to simulate the effects of groundwater withdrawals from aquifers in Ocean County and vicinity, New Jersey

A three-dimensional groundwater flow model was developed to simulate the effects of withdrawals on the groundwater-flow systems of five aquifers in and around Ocean County, New Jersey—the unconfined Kirkwood-Cohansey aquifer system and Vincentown aquifer, and three confined aquifers--the Rio Grande water-bearing zone, the Atlantic City 800-foot sand, and the Piney Point aquifer. A transient model was used to simulate conditions that represent no groundwater withdrawals, 2000–2003 groundwater withdrawals, and maximum-allocation groundwater withdrawals. Particle-tracking analysis, using results from two steady-state simulations, determine flow paths and travel times to near-shore wells screened in the unconfined Kirkwood-Cohansey aquifer system, the Rio Grande water-bearing zone, and the Atlantic City 800-foot sand. Sources of water to wells in both unconfined and confined aquifers and travel times based on particle-tracking analysis are used to assess the susceptibility of selected wells to saltwater intrusion from bay or ocean water. 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/sir20165035).

Data and Resources

Field Value
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identifier USGS:b03b8693-c302-4d1b-a207-23c003f44171
metadata_type geospatial
modified 20201117
old-spatial -74.634006, 39.432992, -73.901659, 40.239449
publisher U.S. Geological Survey
publisher_hierarchy Department of the Interior > U.S. Geological Survey
resource-type Dataset
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spatial {"type": "Polygon", "coordinates": [[[-74.634006, 39.432992], [-74.634006, 40.239449], [ -73.901659, 40.239449], [ -73.901659, 39.432992], [-74.634006, 39.432992]]]}
theme {geospatial}
Groups
  • AmeriGEOSS
  • National Provider
  • North America
Tags
  • amerigeo
  • amerigeoss
  • atlantic-city-800-foot-sand
  • burlington-county
  • ckan
  • environment
  • geo
  • geoscientificinformation
  • geoss
  • groundwater
  • groundwater-model
  • inlandwaters
  • kirkwood-cohansey-aquifer-system
  • modflow
  • modflow2005
  • modpath6
  • monmouth-county
  • national
  • new-jersey
  • north-america
  • ocean-county
  • pinelands
  • piney-point-aquifer
  • rio-grande-water-bearing-zone
  • united-states
  • usgs-b03b8693-c302-4d1b-a207-23c003f44171
  • usgsgroundwatermodel
isopen False
license_id notspecified
license_title License not specified
maintainer NJ Water Science Center Chief
maintainer_email dc_nj@usgs.gov
metadata_created 2025-11-22T01:57:49.392652
metadata_modified 2025-11-22T01:57:49.392656
notes A three-dimensional groundwater flow model was developed to simulate the effects of withdrawals on the groundwater-flow systems of five aquifers in and around Ocean County, New Jersey—the unconfined Kirkwood-Cohansey aquifer system and Vincentown aquifer, and three confined aquifers--the Rio Grande water-bearing zone, the Atlantic City 800-foot sand, and the Piney Point aquifer. A transient model was used to simulate conditions that represent no groundwater withdrawals, 2000–2003 groundwater withdrawals, and maximum-allocation groundwater withdrawals. Particle-tracking analysis, using results from two steady-state simulations, determine flow paths and travel times to near-shore wells screened in the unconfined Kirkwood-Cohansey aquifer system, the Rio Grande water-bearing zone, and the Atlantic City 800-foot sand. Sources of water to wells in both unconfined and confined aquifers and travel times based on particle-tracking analysis are used to assess the susceptibility of selected wells to saltwater intrusion from bay or ocean water. 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/sir20165035).
num_resources 2
num_tags 27
title MODFLOW2005 model used to simulate the effects of groundwater withdrawals from aquifers in Ocean County and vicinity, New Jersey