Transient seawater inflow into seacoast aquifers
- 作者: Fomin Y.V.1, Zhmur V.V.2, Marchenko A.V.3
- 
							隶属关系: 
							- Shirshov Institute of Oceanology
- Moscow Institute of Physics and Technology
- University Center in Svalbard, Longyearbyen
 
- 期: 卷 44, 编号 1 (2017)
- 页面: 61-68
- 栏目: Hydrophysical Processes
- URL: https://journals.rcsi.science/0097-8078/article/view/174106
- DOI: https://doi.org/10.1134/S0097807816060026
- ID: 174106
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详细
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.
作者简介
Yu. Fomin
Shirshov Institute of Oceanology
							编辑信件的主要联系方式.
							Email: yury.fomin88@gmail.com
				                					                																			                												                	俄罗斯联邦, 							Moscow, 117997						
V. Zhmur
Moscow Institute of Physics and Technology
														Email: yury.fomin88@gmail.com
				                					                																			                												                	俄罗斯联邦, 							Dolgoprudnyi, Moscow oblast, 141700						
A. Marchenko
University Center in Svalbard, Longyearbyen
														Email: yury.fomin88@gmail.com
				                					                																			                												                	挪威, 							Spitsbergen, 9171						
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