Determining Age And Vertical Contribution Of Ground Water Pumped From Wells In A Small Coastal River Basin PDF Download

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Determining Age and Vertical Contribution of Ground Water Pumped from Wells in a Small Costal River Basin

Determining Age and Vertical Contribution of Ground Water Pumped from Wells in a Small Costal River Basin
Author:
Publisher:
Total Pages: 5
Release: 2005
Genre:
ISBN:

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The age and vertical contribution of ground water flowing into four municipal supply wells were determined under pumping conditions in order to better understand the source of water to the wells. Vertical flowrate inside the wells, located in the Sweetwater River drainage basin of San Diego County, California, was measured at selected depths using a dye-injection technique. Flowmeter results indicate that as much as about half the pumped water comes from the alluvial deposits and half from the underlying San Diego Formation. Chemical analysis of water samples collected at specific depths support this vertical distribution of pumped water. Tritium and carbon-14 data indicate that ground water from the alluvial deposits was recharged less than 50 years ago, and ground water from the San Diego Formation is thousands of years old, some as much as 16,000 years old.


Scientific Investigations Report

Scientific Investigations Report
Author: Sharon E. Kroening
Publisher:
Total Pages: 122
Release: 2004
Genre: Earth sciences
ISBN:

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Seawater Intrusion in Coastal Aquifers

Seawater Intrusion in Coastal Aquifers
Author: Jacob Bear
Publisher: Springer Science & Business Media
Total Pages: 652
Release: 2013-03-09
Genre: Science
ISBN: 9401729697

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Coastal aquifers serve as major sources for freshwater supply in many countries around the world, especially in arid and semi-arid zones. Many coastal areas are also heavily urbanized, a fact that makes the need for freshwater even more acute. Coastal aquifers are highly sensitive to disturbances. Inappropriate management of a coastal aquifer may lead to its destruction as a source for freshwater much earlier than other aquifers which are not connected to the sea. The reason is the threat of seawater intrusion. In many coastal aquifers, intrusion of seawater has become one of the major constraints imposed on groundwater utilization. As sea water intrusion progresses, existing pumping wells, especially those close to the coast, become saline and have to be abandoned. Also, the area above the intruding seawater wedge is lost as a source of natural replenishment to the aquifer. Despite the importance of this subject, so far there does not exist a book that integrates our present knowledge of seawater intrusion, its occurrences, physical mechanism, chemistry, exploration by geo physical and geochemical techniques, conceptual and mathematical modeling, analytical and numerical solution methods, engineering measures of combating seawater intrusion, management strategies, and experience learned from case studies. By presenting this fairly comprehensive volume on the state-of-the-art of knowledge and ex perience on saltwater intrusion, we hoped to transfer this body of knowledge to the geologists, hydrologists, hydraulic engineers, water resources planners, managers, and governmental policy makers, who are engaged in the sustainable development of coastal fresh ground water resources.


Simulated Ground-water Flow at the Fairmount Site, Sussex County, Delaware (USA), with Implications for Nitrate Transport

Simulated Ground-water Flow at the Fairmount Site, Sussex County, Delaware (USA), with Implications for Nitrate Transport
Author: Joshua W. Kasper
Publisher:
Total Pages: 145
Release: 2007
Genre:
ISBN:

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Results of this study illustrate the utility of a numerical-modeling approach to evaluate ground water-surface water interactions. The results also suggest several implications for watershed management in Coastal Plain settings where stream discharge is dominated by baseflow. The significant "lag" time required for recharged ground water (and associated contaminants) to flush out of the system is an important consideration for the protection of surface-water quality. As previously noted by others, the temporal and spatial aspects of ground-water flow within the source area must be taken into account when evaluating baseflow and ground-water chemistry. Finally, source areas in Coastal Plain settings are dynamic in size and shape and can be significantly influenced by stresses imposed on the ground-water system by artificial recharge.