Non-archived models are typically older models with little to no computer files or models with a limited extent. For these models, a link to the published report on the USGS publication warehouse website is available.
Below are other science projects associated with this project.
APPL-RASA
Below are publications associated with this project.
Analytical methods, numerical modeling, and monitoring strategies for evaluating the effects of ground-water withdrawals on unconfined aquifers in the New Jersey Coastal Plain
Digital-simulation model of the Wenonah-Mount Laurel Aquifer in the coastal plain of New Jersey
Digital computer simulation model of the Englishtown aquifer in the northern coastal plain of New Jersey
Digital-simulation and projection of head changes in the Potomac-Raritan-Magothy aquifer system, coastal plain, New Jersey
Steady-state computer model of the water-table aquifer in the Mullica River basin, the Pine Barrens, New Jersey
Geohydrology and digital-simulation model of the Farrington aquifer in the northern coastal plain of New Jersey
Below are partners associated with this project.
- Overview
Non-archived models are typically older models with little to no computer files or models with a limited extent. For these models, a link to the published report on the USGS publication warehouse website is available.
- Science
Below are other science projects associated with this project.
APPL-RASA
Hydrogeology and Groundwater Flow, Fractured Mesozoic Structural-Basin Rocks, Stony Brook, Beden Brook, and Jacobs Creek Drainage Basins, West Central New Jersey - Publications
Below are publications associated with this project.
Analytical methods, numerical modeling, and monitoring strategies for evaluating the effects of ground-water withdrawals on unconfined aquifers in the New Jersey Coastal Plain
Analytical and numerical solutions of ground-water withdrawals in the unconfined part of the Kirkwood-Cohansey aquifer system of the Coastal Plain of New Jersey were evaluated for their usefulness in predicting the area of influence of a pumped well and in determining hydraulic characteristics of an aquifer. Additionally, simulations of ground-water withdrawal using a finite-difference model proviDigital-simulation model of the Wenonah-Mount Laurel Aquifer in the coastal plain of New Jersey
A digital computer-simulation model of the Wenonah-Mount Laurel aquifer is used to evaluate the aquifer's capabilities of meeting the projected future demands and to study the cause of the rapidly declining water levels. The modelled area includes 1,500 square miles (3,885 square kilometres) of the New Jersey Coastal Plain and includes all the important centers of pumping in Monmouth, Burlington,Digital computer simulation model of the Englishtown aquifer in the northern coastal plain of New Jersey
Continued decline of water levels in the Englishtown aquifer, in New Jersey, has caused considerable concern regarding the ability of the aquifer to meet future yield demands. A detailed study of the capability of the aquifer to yield water entailed the use of a digital computer simulation model to evaluate aquifer and confining layer coefficients and to test alternative concepts of the hydrodynamDigital-simulation and projection of head changes in the Potomac-Raritan-Magothy aquifer system, coastal plain, New Jersey
The Potomac-Raritan-Magothy aquifer system of Cretaceous age, which is the principal source of water to the major population and industrial centers in the Coastal Plain of New Jersey, has undergone continuous and widespread reduction in head. The reduced head, already below sea level throughout most of the aquifer system, in conjunction with encroachment of salty water toward centers of pumping, tSteady-state computer model of the water-table aquifer in the Mullica River basin, the Pine Barrens, New Jersey
A two-dimensional steady-state model of the water-table aquifer of the Mullica River basin was made to evaluate the flow system and data required to simulate it. The Mullica River basin covers 570 sq mi and is drained by numerous shallow streams. The water-table aquifer consists of sand and gravel intermixed with clay and silt. The computer model is based on a finite-difference method with stream-Geohydrology and digital-simulation model of the Farrington aquifer in the northern coastal plain of New Jersey
A two-dimensional digital-computer flow model was developed to simulate the Farrington aquifer in the northern part of the Coastal Plain of New Jersey. The area of detailed study includes approximately 500 square miles in Middlesex and Monmouth Couties where the aquifer provides a large part of the municipal and industrial water supply. The area modeled is much larger, extending seaward as well as - Partners
Below are partners associated with this project.