<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     caa a22        4500</leader>
  <controlfield tag="001">475813936</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20180406123805.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">170329e20000501xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1007/PL00001118</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)springer-10.1007/PL00001118</subfield>
  </datafield>
  <datafield tag="245" ind1="0" ind2="0">
   <subfield code="a">Characterization of Electrical Daily Variations Induced by Capillary Flow in the Non-saturated Zone</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[F. Perrier, P. Morat]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">—Electrical daily variations without an associated magnetic field were observed for a period of six weeks on independent parallel dipoles during the one-year electrode inter comparison experiment that took place in Garchy, France, from April 1995 to April 1996. These daily variations appeared suddenly during summer when the soil was dry on the surface. Their amplitude ranged from 0.1 to 1.5 mV for 50-m long dipoles, and characteristic relative phases. The amplitude of the variations was found to be related to soil temperature. These daily variations are accounted for in a model where streaming potentials are produced by coherent capillary flow in the non-saturated zone. Such daily variations are important to control in long-period magnetotelluric sounding and may be of practical use for agricultural applications. As their amplitude strongly depends on time-varying soil conditions, they may also lead to erroneous interpretations as earthquake precursors.</subfield>
  </datafield>
  <datafield tag="540" ind1=" " ind2=" ">
   <subfield code="a">Birkhäuser Verlag Basel,, 2000</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Key Words: Spontaneous potential, capillary flow, soil physics, magnetotelluric sounding, streaming potentials, earthquake precursors</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Perrier</subfield>
   <subfield code="D">F.</subfield>
   <subfield code="u">Laboratoire de Détection et de Géophsique, Commissariat à l'Energie Atomique, B.P. 12, F-91680, Bruyères-le-Châtel, France. E-mail: perrier@ldg.bruyeres.cea.fr, FR</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Morat</subfield>
   <subfield code="D">P.</subfield>
   <subfield code="u">Laboratoire de Géomagnétisme, Institut de Physique du Globe de Paris, 4, Place Jussieu, F-75252, Paris Cedex 05, France., FR</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="0">
   <subfield code="u">https://doi.org/10.1007/PL00001118</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="908" ind1=" " ind2=" ">
   <subfield code="D">1</subfield>
   <subfield code="a">research-article</subfield>
   <subfield code="2">jats</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">856</subfield>
   <subfield code="E">40</subfield>
   <subfield code="u">https://doi.org/10.1007/PL00001118</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Perrier</subfield>
   <subfield code="D">F.</subfield>
   <subfield code="u">Laboratoire de Détection et de Géophsique, Commissariat à l'Energie Atomique, B.P. 12, F-91680, Bruyères-le-Châtel, France. E-mail: perrier@ldg.bruyeres.cea.fr, FR</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Morat</subfield>
   <subfield code="D">P.</subfield>
   <subfield code="u">Laboratoire de Géomagnétisme, Institut de Physique du Globe de Paris, 4, Place Jussieu, F-75252, Paris Cedex 05, France., FR</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="900" ind1=" " ind2="7">
   <subfield code="a">Metadata rights reserved</subfield>
   <subfield code="b">Springer special CC-BY-NC licence</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="898" ind1=" " ind2=" ">
   <subfield code="a">BK010053</subfield>
   <subfield code="b">XK010053</subfield>
   <subfield code="c">XK010000</subfield>
  </datafield>
  <datafield tag="949" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="F">NATIONALLICENCE</subfield>
   <subfield code="b">NL-springer</subfield>
  </datafield>
 </record>
</collection>
