Transient seawater inflow into seacoast aquifers


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Abstract

The coastal zone of the sea is a boundary domain between seawater and land, making most processes within it to show specific features. Seawater can penetrate into aquifers in the land part of the shore through the underwater part of the sea–shore interface and move over considerable distances from the shoreline, mixing with fresh groundwater. This process is of critical importance for the construction of oil and gas pipelines in permafrost areas.

About the authors

Yu. V. Fomin

Shirshov Institute of Oceanology

Author for correspondence.
Email: yury.fomin88@gmail.com
Russian Federation, Moscow, 117997

V. V. Zhmur

Moscow Institute of Physics and Technology

Email: yury.fomin88@gmail.com
Russian Federation, Dolgoprudnyi, Moscow oblast, 141700

A. V. Marchenko

University Center in Svalbard, Longyearbyen

Email: yury.fomin88@gmail.com
Norway, Spitsbergen, 9171

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