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A multilayered sharp interface model of coupled freshwater and saltwater flow in coastal systems: model development and application
A quasi three-dimensional, finite difference model, that simulates freshwater and saltwater flow separated by a sharp interface, has been developed to study layered coastal aquifer systems. The model allows for regional simulation of coastal groundwater conditions, including the effects of saltwater...
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Published in: | Water resources research 1990-07, Vol.26 (7), p.1431-1454 |
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container_end_page | 1454 |
container_issue | 7 |
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container_title | Water resources research |
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creator | Essaid, H.I. (U.S. Geological Survey, Menlo Park, CA) |
description | A quasi three-dimensional, finite difference model, that simulates freshwater and saltwater flow separated by a sharp interface, has been developed to study layered coastal aquifer systems. The model allows for regional simulation of coastal groundwater conditions, including the effects of saltwater dynamics on the freshwater system. Vertically integrated freshwater and saltwater flow equations incorporating the interface boundary condition are solved within each aquifer. Leakage through confining layers is calculated by Darcy's law, accounting for density differences across the layer. The locations of the interface tip and toe, within grid blocks, are tracked by linearly extrapolating the position of the interface. The model has been verified using available analytical solutions and experimental results. Application of the model to the Soquel-Aptos basin, Santa Cruz County. California, illustrates the use of the quasi three-dimensional, sharp interface approach for the examination of freshwater-saltwater dynamics in regional systems. Simulation suggests that the interface, today, is still responding to long-term Pleistocene sea level fluctuations and has not achieved equilibrium with present day sea level conditions |
doi_str_mv | 10.1029/WR026i007p01431 |
format | article |
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Application of the model to the Soquel-Aptos basin, Santa Cruz County. California, illustrates the use of the quasi three-dimensional, sharp interface approach for the examination of freshwater-saltwater dynamics in regional systems. Simulation suggests that the interface, today, is still responding to long-term Pleistocene sea level fluctuations and has not achieved equilibrium with present day sea level conditions</description><identifier>ISSN: 0043-1397</identifier><identifier>EISSN: 1944-7973</identifier><identifier>DOI: 10.1029/WR026i007p01431</identifier><language>eng</language><publisher>Blackwell Publishing Ltd</publisher><subject>AGUA DULCE ; AGUA SALINA ; AGUAS SUBTERRANEAS ; CALIFORNIA ; CALIFORNIE ; COSTA ; COTES ; DEBIT ; EAU DOUCE ; EAU SALINE ; EAU SOUTERRAINE ; GASTO ; HIDRODINAMICA ; HYDRODYNAMIQUE ; MODELE ; MODELOS</subject><ispartof>Water resources research, 1990-07, Vol.26 (7), p.1431-1454</ispartof><rights>This paper is not subject to U.S. copyright. 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The locations of the interface tip and toe, within grid blocks, are tracked by linearly extrapolating the position of the interface. The model has been verified using available analytical solutions and experimental results. Application of the model to the Soquel-Aptos basin, Santa Cruz County. California, illustrates the use of the quasi three-dimensional, sharp interface approach for the examination of freshwater-saltwater dynamics in regional systems. Simulation suggests that the interface, today, is still responding to long-term Pleistocene sea level fluctuations and has not achieved equilibrium with present day sea level conditions</description><subject>AGUA DULCE</subject><subject>AGUA SALINA</subject><subject>AGUAS SUBTERRANEAS</subject><subject>CALIFORNIA</subject><subject>CALIFORNIE</subject><subject>COSTA</subject><subject>COTES</subject><subject>DEBIT</subject><subject>EAU DOUCE</subject><subject>EAU SALINE</subject><subject>EAU SOUTERRAINE</subject><subject>GASTO</subject><subject>HIDRODINAMICA</subject><subject>HYDRODYNAMIQUE</subject><subject>MODELE</subject><subject>MODELOS</subject><issn>0043-1397</issn><issn>1944-7973</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1990</creationdate><recordtype>article</recordtype><recordid>eNqFkUFv1DAQRi0EEkvhjMQpJ26hnjiJY27dFSxIVZFKqyIu1qwzpgYnTu0sy5754xhSceDCXEajeW8O3zD2HPgr4JU6vbnkVes4lxOHWsADtgJV16VUUjxkK85rUYJQ8jF7ktJXnpmmlSv286wY9n52Ho8UqS_SLcapcONM0aKhYgg9-SLYwoT95DNgI6XbA-Z9gWPm0c_LZH04ZDGDmGb0RTqmmYb0-v5ET9_Jh2mgcf4j4jR5Z3B2YXzKHln0iZ7d9xN2_fbN1eZdef5h-35zdl6iAKhKBS30pjU97XZKygarru5AdtYIo1TXgFRc0Q5ykamMbY2yoq9qgC6Du16csJfL3SmGuz2lWQ8uGfIeRwr7pKGr6o7LLoOnC2hiSCmS1VN0A8ajBq5_h63_CTsbzWIcnKfj__A8by4brqrslYvnclg__noYv-lWCtnom4utXm_lxef1pyu9zvyLhbcYNH6JLunrjyr_VnEQvwBZj5xr</recordid><startdate>199007</startdate><enddate>199007</enddate><creator>Essaid, H.I. 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(U.S. Geological Survey, Menlo Park, CA)</creatorcontrib><collection>AGRIS</collection><collection>Istex</collection><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><jtitle>Water resources research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Essaid, H.I. (U.S. Geological Survey, Menlo Park, CA)</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A multilayered sharp interface model of coupled freshwater and saltwater flow in coastal systems: model development and application</atitle><jtitle>Water resources research</jtitle><addtitle>Water Resour. Res</addtitle><date>1990-07</date><risdate>1990</risdate><volume>26</volume><issue>7</issue><spage>1431</spage><epage>1454</epage><pages>1431-1454</pages><issn>0043-1397</issn><eissn>1944-7973</eissn><abstract>A quasi three-dimensional, finite difference model, that simulates freshwater and saltwater flow separated by a sharp interface, has been developed to study layered coastal aquifer systems. The model allows for regional simulation of coastal groundwater conditions, including the effects of saltwater dynamics on the freshwater system. Vertically integrated freshwater and saltwater flow equations incorporating the interface boundary condition are solved within each aquifer. Leakage through confining layers is calculated by Darcy's law, accounting for density differences across the layer. The locations of the interface tip and toe, within grid blocks, are tracked by linearly extrapolating the position of the interface. The model has been verified using available analytical solutions and experimental results. Application of the model to the Soquel-Aptos basin, Santa Cruz County. California, illustrates the use of the quasi three-dimensional, sharp interface approach for the examination of freshwater-saltwater dynamics in regional systems. Simulation suggests that the interface, today, is still responding to long-term Pleistocene sea level fluctuations and has not achieved equilibrium with present day sea level conditions</abstract><pub>Blackwell Publishing Ltd</pub><doi>10.1029/WR026i007p01431</doi><tpages>24</tpages></addata></record> |
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ispartof | Water resources research, 1990-07, Vol.26 (7), p.1431-1454 |
issn | 0043-1397 1944-7973 |
language | eng |
recordid | cdi_proquest_miscellaneous_18248078 |
source | Wiley-Blackwell Journals |
subjects | AGUA DULCE AGUA SALINA AGUAS SUBTERRANEAS CALIFORNIA CALIFORNIE COSTA COTES DEBIT EAU DOUCE EAU SALINE EAU SOUTERRAINE GASTO HIDRODINAMICA HYDRODYNAMIQUE MODELE MODELOS |
title | A multilayered sharp interface model of coupled freshwater and saltwater flow in coastal systems: model development and application |
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