Interpretation of Measurement Results of the Potential Difference in Lake Baikal


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A model is proposed in which the electrical voltage measured between the electrodes in Lake Baikal is a consequence of two effects: electrochemical processes near the electrodes and a positive charge current flowing through the lake. The electrochemical component of the voltage in the case of lead electrodes arises due to the difference in concentrations of carbonate anion—\({\text{CO}}_{3}^{{2 - }}\) at different depths. In the case of the use of chlorine-silver electrodes, only the effect of the positive charge current flowing through the lake is measured. We proposed an interpretation of an increase of electrical voltage registered in Lake Baikal during an earthquake in August 2008. The reason for the increase in voltage is the release of positively charged hydrogen-containing gases from the Earth’s interior.

作者简介

L. Bezrukov

Institute for Nuclear Research of Russian Academy of Sciences

编辑信件的主要联系方式.
Email: bezrukov@inr.ac.ru
俄罗斯联邦, Moscow

V. Zavarzina

Institute for Nuclear Research of Russian Academy of Sciences

Email: bezrukov@inr.ac.ru
俄罗斯联邦, Moscow

I. Karpikov

Institute for Nuclear Research of Russian Academy of Sciences

Email: bezrukov@inr.ac.ru
俄罗斯联邦, Moscow

A. Kurlovich

Institute for Nuclear Research of Russian Academy of Sciences

Email: bezrukov@inr.ac.ru
俄罗斯联邦, Moscow

B. Lubsandorzhiev

Institute for Nuclear Research of Russian Academy of Sciences

Email: bezrukov@inr.ac.ru
俄罗斯联邦, Moscow

A. Mezokh

Institute for Nuclear Research of Russian Academy of Sciences

Email: bezrukov@inr.ac.ru
俄罗斯联邦, Moscow

V. Morgaluk

A.N. Nesmeyanov Institute of Organoelement Compounds of Russian Academy of Sciences

Email: bezrukov@inr.ac.ru
俄罗斯联邦, Moscow

V. Sinev

Institute for Nuclear Research of Russian Academy of Sciences

Email: bezrukov@inr.ac.ru
俄罗斯联邦, Moscow

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