New evidence of acoustic effects of radiation impacts in deep wells
- Authors: Belyakov A.S.1, Didenkulov I.N.2, Zhigalin A.D.1, Lavrov V.S.1, Malekhanov A.I.2, Nikolaev A.V.1
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Affiliations:
- Schmidt Institute of Physics of the Earth
- Institute of Applied Physics
- Issue: Vol 475, No 1 (2017)
- Pages: 808-810
- Section: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/190323
- DOI: https://doi.org/10.1134/S1028334X1707011X
- ID: 190323
Cite item
Abstract
Passive seismic observations were performed in the Vorotolovskaya deep well in Nizhny Novgorod oblast at a depth of 1400 m and in a well in the vicinity of Ufa at a depth of 500 m. Observations show significantly different acoustic impulse fluxes in these wells: hundreds per second in the Vorotilovskaya deep well and only few impulses per day in the Ufa well. It is supposed that it is the geological conditions that determine the character of seismoacoustic signals. A seismic observation technique is proposed for further studies of acoustic manifestations of radiation fields.
About the authors
A. S. Belyakov
Schmidt Institute of Physics of the Earth
Email: zhigalin.alek@yandex.ru
Russian Federation, Moscow, 123242
I. N. Didenkulov
Institute of Applied Physics
Email: zhigalin.alek@yandex.ru
Russian Federation, Nizhny Novgorod, 603950
A. D. Zhigalin
Schmidt Institute of Physics of the Earth
Author for correspondence.
Email: zhigalin.alek@yandex.ru
Russian Federation, Moscow, 123242
V. S. Lavrov
Schmidt Institute of Physics of the Earth
Email: zhigalin.alek@yandex.ru
Russian Federation, Moscow, 123242
A. I. Malekhanov
Institute of Applied Physics
Email: zhigalin.alek@yandex.ru
Russian Federation, Nizhny Novgorod, 603950
A. V. Nikolaev
Schmidt Institute of Physics of the Earth
Email: zhigalin.alek@yandex.ru
Russian Federation, Moscow, 123242
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