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<front>
<journal-meta>
<journal-id journal-id-type="publisher">NHESSD</journal-id>
<journal-title-group>
<journal-title>Natural Hazards and Earth System Sciences Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">NHESSD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Nat. Hazards Earth Syst. Sci. Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">2195-9269</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/nhessd-2-6475-2014</article-id>
<title-group>
<article-title>Estimate of ULF electromagnetic noise caused by a fluid flow during seismic or volcano activity</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Surkov</surname>
<given-names>V. V.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Pilipenko</surname>
<given-names>V. A.</given-names>
<ext-link>https://orcid.org/0000-0003-3056-7465</ext-link>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>National Research Nuclear University &quot;MEPhI&quot;, Moscow, Russia</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute of Physics of the Earth, Moscow, Russia</addr-line>
</aff>
<pub-date pub-type="epub">
<day>14</day>
<month>10</month>
<year>2014</year>
</pub-date>
<volume>2</volume>
<issue>10</issue>
<fpage>6475</fpage>
<lpage>6497</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2014 V. V. Surkov</copyright-statement>
<copyright-year>2014</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://nhess.copernicus.org/preprints/2/6475/2014/nhessd-2-6475-2014.html">This article is available from https://nhess.copernicus.org/preprints/2/6475/2014/nhessd-2-6475-2014.html</self-uri>
<self-uri xlink:href="https://nhess.copernicus.org/preprints/2/6475/2014/nhessd-2-6475-2014.pdf">The full text article is available as a PDF file from https://nhess.copernicus.org/preprints/2/6475/2014/nhessd-2-6475-2014.pdf</self-uri>
<abstract>
<p>The elaboration of theoretical models, even oversimplified, capable
  to estimate an expected electromagnetic effect during earthquake
  preparation process is not less important than the advancement of
  observational technique to detect seismic-related electromagnetic
  emission. Here possible mechanisms of ULF electromagnetic noise
  associated with seismic or volcanic activity are discussed. The
  electrokinetic (EK) and magnetohydrodynamic (MHD) effects due to an
  irregular flow of conducting rock fluid or magma flow are being
  revised. The conventional theory of EK effect in a water-saturated
  rocks has been advanced by consideration of elliptic-shaped
  channels. A contribution of both mechanisms to observed ULF signal
  on the ground is shown to be dependent on the pore channel size/rock
  permeability.  Estimates of magnetic and telluric perturbations
  caused by magma motion along a volcano throat indicate on the
  important role of the surrounding rock conductivity. These estimates
  have proven that the mechanisms under consideration are able to
  generate ULF electromagnetic emission which could be detected by
  modern magnetometers under favorable conditions.</p>
</abstract>
<counts><page-count count="23"/></counts>
</article-meta>
</front>
<body/>
<back>
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