Transient seawater inflow into seacoast aquifers

Yu. V. Fomin; V. V. Zhmur; A. V. Marchenko

doi:10.1134/S0097807816060026

Transient seawater inflow into seacoast aquifers

Авторы: Fomin Y.V.¹, Zhmur V.V.², Marchenko A.V.³
Учреждения:
1. Shirshov Institute of Oceanology
2. Moscow Institute of Physics and Technology
3. University Center in Svalbard, Longyearbyen
Выпуск: Том 44, № 1 (2017)
Страницы: 61-68
Раздел: Hydrophysical Processes
URL: https://journals.rcsi.science/0097-8078/article/view/174106
DOI: https://doi.org/10.1134/S0097807816060026
ID: 174106

Цитировать

Полный текст

Открытый доступ
Доступ закрыт

Доступ предоставлен
Доступ закрыт

Только для подписчиков

Аннотация
Об авторах
Список литературы
Дополнительные файлы
Статистика

Аннотация

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.