Research Article
Sep 1972
Hele-Shaw Model of Long Island Aquifer System
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VIEW THE REPLYAuthors: Michael A. Collins, AM.ASCE, Lynn W. Gelhar, AM.ASCE, and John L. Wilson IIIAuthor Affiliations
Publication: Journal of the Hydraulics Division
Volume 98, Issue 9
Abstract
An experimental study, using a vertical Hele-Shaw model, is undertaken to determine fresh and salt ground-water flow for various ground-water development schemes on Long Island, N.Y. To satisfy dynamic similitude, some portions of the model are anisotropic. To simulate stream base flow, a significant hydrologic feature along the south shore of the island, an internal weir is incorporated in the model. Liquid silicones simulate fresh and salt water. Verification of the model is achieved by reproduction of long-term water table profiles, the stream base flow, and the double salt-water wedge structure, i.e., two salt-water wedges separated vertically by fresh water, south of the island. Response of the salt water to hydrologic transients on the island is slow. Recharge is effective in arresting or reversing salt-water movement.
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Published In
Journal of the Hydraulics Division
Volume 98 • Issue 9 • September 1972
Pages: 1701 - 1714
Copyright
© 1972 American Society of Civil Engineers.
History
Published in print: Sep 1972
Published online: Feb 3, 2021
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Authors
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Michael A. Collins, AM.ASCE
Asst. Prof., Inst. of Technology, Southern Methodist Univ., Dallas, Tex.
Lynn W. Gelhar, AM.ASCE
Assoc. Prof., Dept. of Civ. Engrg., MIT, Cambridge, Mass.
John L. Wilson III
Research Asst., Dept. of Civ. Engrg., MIT, Cambridge, Mass.
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Terms of Use: ASCE Library Cards are for individual, personal use only. Reselling, republishing, or forwarding the materials to libraries or reading rooms is prohibited.
Terms of Use: ASCE Library Cards are for individual, personal use only. Reselling, republishing, or forwarding the materials to libraries or reading rooms is prohibited.