Response of a coastal hydrogeological system to a rapid decline in sea level; the case of Zuqim springs - The largest discharge area along the Dead Sea coast
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- 作者：Avihu Burga ; burg@gsi.gov.il" class="auth_mail" title="E-mail the corresponding author ; Yoseph Yechielia ; yechieli@gsi.gov.il" class="auth_mail" title="E-mail the corresponding author ; Udi Galilib ; udig30@water.gov.il" class="auth_mail" title="E-mail the corresponding author
- 关键词：Dead sea ; On-shore springs ; Lake-level drop ; Hydrological boundary ; Mud plains ; Water refreshing
- 刊名：Journal of Hydrology
- 出版年：2016
- 出版时间：May 2016
- 年：2016
- 卷：536
- 期：Complete
- 页码：222-235
- 全文大小：2178 K
文摘
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A response of a coastal aquifer to a drop in the level of a nearby lake is described.
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Hydrological system extension is not accompanied by a change in the total discharge.
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There is a clear refreshing of the groundwater due to flushing of trapped brines.
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Lithological facies variations have a pronounced effect on the underground flow.
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Every sub-aquifer has a unique composition determined by a mixing of end-members.