<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     caa a22        4500</leader>
  <controlfield tag="001">475796896</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20180406123727.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">170329e20000101xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1007/PL00001501</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)springer-10.1007/PL00001501</subfield>
  </datafield>
  <datafield tag="100" ind1="1" ind2=" ">
   <subfield code="a">Pham</subfield>
   <subfield code="D">D. C.</subfield>
   <subfield code="u">National Center for Natural Science and Technology, Vien Co hoc, 224 Doi Can, Hanoi, Vietnam, and Institute of General Mechanics, Templergraben 64, Aachen, Germany e-mail: pdchinh@im01.ac.vn, VN</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="245" ind1="1" ind2="0">
   <subfield code="a">Hierarchical unsymmetrical effective medium approximations for the electrical conductivity of water-saturated porous rocks</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[D. C. Pham]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">Abstract.: A two-level unsymmetrical effective medium approximation scheme is developed to model the electrical conductivity of sedimentary rocks with pore space interconnected and water-filled. The scheme takes into account certain observed features of the rock geometry, which appears to be a suspension of open water sphere-like pockets, or platelet-like cracks of secondary porosity, in the mass of solid grains surrounded by the thin water films. The pockets contribute much to the porosity but little to the conductivity in contrast with the thin films surrounding the grains, or the cracks and fractures of secondary porosity, the latest are the most conducting effective. The models are flexible enough to explain the behavior of the rocks described by the empirical Archie's law.</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. Electrical conductivity, effective medium approximation, porous rock</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="0">
   <subfield code="u">https://doi.org/10.1007/PL00001501</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/PL00001501</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">100</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Pham</subfield>
   <subfield code="D">D. C.</subfield>
   <subfield code="u">National Center for Natural Science and Technology, Vien Co hoc, 224 Doi Can, Hanoi, Vietnam, and Institute of General Mechanics, Templergraben 64, Aachen, Germany e-mail: pdchinh@im01.ac.vn, VN</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>
