Aquifer Dynamics and Atmospheric Electricity
- 作者: Shuleikin V.1
-
隶属关系:
- Oil and Gas Research Institute, Russian Academy of Sciences
- 期: 卷 54, 编号 7 (2018)
- 页面: 646-653
- 栏目: Article
- URL: https://journals.rcsi.science/0001-4338/article/view/148597
- DOI: https://doi.org/10.1134/S0001433818070125
- ID: 148597
如何引用文章
详细
Measurements of variations in the atmospheric electric field (AEF), soil and atmospheric radon concentration, and hydrogeological parameters have made it possible to establish links between the listed processes. A rise in aquifer levels increases the outflow of soil radon, which decreases the AEF; a decrease in levels leads to the opposite effect. The rise can be caused by the infiltration of precipitation, hydraulic fracturing, and lowering of atmospheric pressure; the fall can be caused by the pumping of artesian waters or by an increase in atmospheric pressure.
作者简介
V. Shuleikin
Oil and Gas Research Institute, Russian Academy of Sciences
编辑信件的主要联系方式.
Email: shvn1947@yandex.ru
俄罗斯联邦, Moscow, 119333