Aquifer Dynamics and Atmospheric Electricity
- Autores: Shuleikin V.1
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Afiliações:
- Oil and Gas Research Institute, Russian Academy of Sciences
- Edição: Volume 54, Nº 7 (2018)
- Páginas: 646-653
- Seção: Article
- URL: https://journals.rcsi.science/0001-4338/article/view/148597
- DOI: https://doi.org/10.1134/S0001433818070125
- ID: 148597
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Resumo
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.
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Sobre autores
V. Shuleikin
Oil and Gas Research Institute, Russian Academy of Sciences
Autor responsável pela correspondência
Email: shvn1947@yandex.ru
Rússia, Moscow, 119333