Name: Simulation of Groundwater Flow and Hydrologic Effects of Groundwater Withdrawals from the Kirkwood-Cohansey Aquifer System in the Pinelands of Souther (en Inglés)
Price: 785.04 MXN
Availability: InStock
Author: Charles, Emmanuel G. ; Nicholson, Robert S.
ISBN: 9781288853175

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portada Simulation of Groundwater Flow and Hydrologic Effects of Groundwater Withdrawals from the Kirkwood-Cohansey Aquifer System in the Pinelands of Souther (en Inglés)

Formato

Libro Físico

Autor

Robert S. Nicholson

Emmanuel G. Charles

Editorial

Bibliogov

Idioma

Inglés

N° páginas

246

Encuadernación

Tapa Blanda

Dimensiones

24.6 x 18.9 x 1.3 cm

Peso

0.44 kg.

ISBN13

9781288853175

Categorías

Política y gobierno

Simulation of Groundwater Flow and Hydrologic Effects of Groundwater Withdrawals from the Kirkwood-Cohansey Aquifer System in the Pinelands of Souther (en Inglés)

Robert S. Nicholson (Autor) · Emmanuel G. Charles (Autor) · Bibliogov · Tapa Blanda

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Origen: Estados Unidos (Costos de importación incluídos en el precio)

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Reseña del libro "Simulation of Groundwater Flow and Hydrologic Effects of Groundwater Withdrawals from the Kirkwood-Cohansey Aquifer System in the Pinelands of Souther (en Inglés)"

The Kirkwood-Cohansey aquifer system is an important source of present and future water supply in southern New Jersey. Because this unconfined aquifer system also supports sensitive wetland and aquatic habitats within the New Jersey Pinelands (Pinelands), water managers and policy makers need up-to-date information, data, and projections that show the effects of potential increases in groundwater withdrawals on these habitats. Finite-difference groundwater flow models (MODFLOW) were constructed for three drainage basins (McDonalds Branch Basin, 14.3 square kilometers (km2); Morses Mill Stream Basin, 21.63 km2; and Albertson Brook Basin, 52.27 km2) to estimate the effects of potential increases in groundwater withdrawals on water levels and the base-flow portion of streamflow, in wetland and aquatic habitats. Three models were constructed for each drainage basin: a transient model consisting of twenty-four 1-month stress periods (October 2004 through September 2006); a transient model to simulate the 5- to 10-day aquifer tests that were performed as part of the study; and a high-resolution, steady-state model used to assess long-term effects of increased groundwater withdrawals on water levels in wetlands and on base flow. All models were constructed with the same eight-layer structure.