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 <front>
  <journal-meta>
   <journal-id journal-id-type="publisher-id">Russian Journal of Earth Sciences</journal-id>
   <journal-title-group>
    <journal-title xml:lang="en">Russian Journal of Earth Sciences</journal-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Russian Journal of Earth Sciences</trans-title>
    </trans-title-group>
   </journal-title-group>
   <issn publication-format="online">1681-1208</issn>
  </journal-meta>
  <article-meta>
   <article-id pub-id-type="publisher-id">46697</article-id>
   <article-categories>
    <subj-group subj-group-type="toc-heading" xml:lang="ru">
     <subject>ОРИГИНАЛЬНЫЕ СТАТЬИ</subject>
    </subj-group>
    <subj-group subj-group-type="toc-heading" xml:lang="en">
     <subject>ORIGINAL ARTICLES</subject>
    </subj-group>
    <subj-group>
     <subject>ОРИГИНАЛЬНЫЕ СТАТЬИ</subject>
    </subj-group>
   </article-categories>
   <title-group>
    <article-title xml:lang="en">Implications of electrokinetic processes for the intensity of geoacoustic emission in the time vicinity of a tectonic earthquake: A theoretical study</article-title>
    <trans-title-group xml:lang="ru">
     <trans-title>Implications of electrokinetic processes for the intensity of geoacoustic emission in the time vicinity of a tectonic earthquake: A theoretical study</trans-title>
    </trans-title-group>
   </title-group>
   <contrib-group content-type="authors">
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Panteleev</surname>
       <given-names>I A</given-names>
      </name>
      <name xml:lang="en">
       <surname>Panteleev</surname>
       <given-names>I A</given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-1"/>
    </contrib>
    <contrib contrib-type="author">
     <name-alternatives>
      <name xml:lang="ru">
       <surname>Gavrilov</surname>
       <given-names>V A</given-names>
      </name>
      <name xml:lang="en">
       <surname>Gavrilov</surname>
       <given-names>V A</given-names>
      </name>
     </name-alternatives>
     <xref ref-type="aff" rid="aff-2"/>
    </contrib>
   </contrib-group>
   <aff-alternatives id="aff-1">
    <aff>
     <institution xml:lang="ru">Institute of Continuous Media Mechanics, Ural Branch, Russian Academy of Sciences, Perm, Russia</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Institute of Continuous Media Mechanics, Ural Branch, Russian Academy of Sciences, Perm, Russia</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <aff-alternatives id="aff-2">
    <aff>
     <institution xml:lang="ru">Institute of Volcanology and Seismology, Far Eastern Branch, Russian Academy of Sciences, Petropavlovsk-Kamchatskii, Russia</institution>
     <country>ru</country>
    </aff>
    <aff>
     <institution xml:lang="en">Institute of Volcanology and Seismology, Far Eastern Branch, Russian Academy of Sciences, Petropavlovsk-Kamchatskii, Russia</institution>
     <country>ru</country>
    </aff>
   </aff-alternatives>
   <volume>15</volume>
   <issue>4</issue>
   <fpage>1</fpage>
   <lpage>14</lpage>
   <history>
    <date date-type="received" iso-8601-date="2021-10-29T13:41:11+03:00">
     <day>29</day>
     <month>10</month>
     <year>2021</year>
    </date>
   </history>
   <self-uri xlink:href="https://rjes.ru/en/nauka/article/46697/view">https://rjes.ru/en/nauka/article/46697/view</self-uri>
   <abstract xml:lang="ru">
    <p>We present the results of the work which continues our previous studies of the geoacoustic emission (GAE) responses to the weak impacts from the varying electromagnetic fields. In this paper, we analyze the probable influence exerted on the amplitude of GAE responses by the electrokinetic processes associated with the activation of filtration flows during the preparation of a tectonic earthquake of moderate magnitude. Based on the consolidation model of an earthquake source developed by I.~P.~Dobrovolsky, we suggest the model describing the generation of electrokinetic currents in response to the change in the volumetric strain in the source area of the future earthquake. Our model takes into account the physico-mechanical properties of the medium in the region of the measurement borehole and the physical properties and chemical composition of water in the measurement borehole itself. Using this model, we carry out the numerical experiments on simulating the evolution of the specific density of electrokinetic current in the time vicinity of a considered seismic event. The calculated variations in the specific density of electrokinetic current qualitatively coincide with the variations in the amplitude envelope of GAE responses.</p>
   </abstract>
   <trans-abstract xml:lang="en">
    <p>We present the results of the work which continues our previous studies of the geoacoustic emission (GAE) responses to the weak impacts from the varying electromagnetic fields. In this paper, we analyze the probable influence exerted on the amplitude of GAE responses by the electrokinetic processes associated with the activation of filtration flows during the preparation of a tectonic earthquake of moderate magnitude. Based on the consolidation model of an earthquake source developed by I.~P.~Dobrovolsky, we suggest the model describing the generation of electrokinetic currents in response to the change in the volumetric strain in the source area of the future earthquake. Our model takes into account the physico-mechanical properties of the medium in the region of the measurement borehole and the physical properties and chemical composition of water in the measurement borehole itself. Using this model, we carry out the numerical experiments on simulating the evolution of the specific density of electrokinetic current in the time vicinity of a considered seismic event. The calculated variations in the specific density of electrokinetic current qualitatively coincide with the variations in the amplitude envelope of GAE responses.</p>
   </trans-abstract>
   <kwd-group xml:lang="ru">
    <kwd>Geoacoustic emission</kwd>
    <kwd>electrokinetic processes</kwd>
    <kwd>electrical double layers</kwd>
    <kwd>electromagnetic radiation</kwd>
    <kwd>preparation of a tectonic earthquake</kwd>
    <kwd>borehole</kwd>
   </kwd-group>
   <kwd-group xml:lang="en">
    <kwd>Geoacoustic emission</kwd>
    <kwd>electrokinetic processes</kwd>
    <kwd>electrical double layers</kwd>
    <kwd>electromagnetic radiation</kwd>
    <kwd>preparation of a tectonic earthquake</kwd>
    <kwd>borehole</kwd>
   </kwd-group>
  </article-meta>
 </front>
 <body>
  <p></p>
 </body>
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