Salinity Distribution And Ground-Water Circulation Beneath The Coastal Plain Of Delaware And The Adjacent Continental Shelf

Author(s)Groot, J.J.
Date Accessioned2008-06-02T13:19:42Z
Date Available2008-06-02T13:19:42Z
Publication Date1983-05
AbstractThe possibility of salt-water encroachment into the aquifers of the Coastal Plain of Delaware from saline-water bodies (Chesapeake and Delaware Canal, Delaware Bay, Atlantic Ocean) has received considerable attention (e.g., Sundstrom et al., 1967, 1971, 1976; Woodruff, 1969). These authors have shown that, so far, little encroachment has taken place. It is also known that a large body of highly saline water occurs at depth beneath the Coastal Plain (Upson, 1966; Back, 1966; Brown and Reid, 1976) and the adjacent continental shelf, but no reports have been published about its origin and shape, and the salinity distribution and flow pattern within it. Yet, this saline-water body has a bearing on the development of fresh-water resources throughout Delaware, the feasibility of constructing injection wells for the disposal of liquid wastes, and radioactive waste disposal in the crystalline rocks beneath the Coastal Plain sediments, and upon the occurrence or migration of hydrocarbons (Bredehoeft and Maini, 1981). It is, therefore, important to study this body of saline water.en_US
URLhttp://udspace.udel.edu/handle/19716/3234
Languageen_USen_US
PublisherNewark, DE: Delaware Geological Survey, University of Delawareen_US
Part of SeriesOpen File Reporten_US
Part of Series26en_US
Keywordssalt-water encroachmenten_US
Keywordsaquifers of the Coastal Plain of Delawareen_US
Keywordssaline-water bodiesen_US
Keywordsinjection wellsen_US
TitleSalinity Distribution And Ground-Water Circulation Beneath The Coastal Plain Of Delaware And The Adjacent Continental Shelfen_US
TypeTechnical Reporten_US
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