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Transient seawater inflow into seacoast aquifers

  • Hydrophysical Processes
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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.

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Authors and Affiliations

  1. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, 117997, Russia

    Yu. V. Fomin

  2. Moscow Institute of Physics and Technology, Dolgoprudnyi, Moscow oblast, 141700, Russia

    V. V. Zhmur

  3. University Center in Svalbard, Longyearbyen, 9171, Spitsbergen, Norway

    A. V. Marchenko

Authors
  1. Yu. V. Fomin
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  2. V. V. Zhmur
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  3. A. V. Marchenko
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Correspondence to Yu. V. Fomin.

Additional information

Original Russian Text © Yu.V. Fomin, V.V. Zhmur, A.V. Marchenko, 2017, published in Vodnye Resursy, 2017, Vol. 44, No. 1, pp. 19–24.

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Fomin, Y.V., Zhmur, V.V. & Marchenko, A.V. Transient seawater inflow into seacoast aquifers. Water Resour 44, 61–68 (2017). https://doi.org/10.1134/S0097807816060026

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  • DOI: https://doi.org/10.1134/S0097807816060026

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