<?xml version="1.0" encoding="UTF-8"?>
<modsCollection xmlns="http://www.loc.gov/mods/v3" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-3.xsd">
  <mods>
    <titleInfo>
      <title>Quantitative assessment of in-situ salt karstification using shear wave velocity, Dead Sea</title>
    </titleInfo>
    <name type="personnal">
      <namePart type="family">Ezersky</namePart>
      <namePart type="given">M.</namePart>
      <role>
        <roleTerm type="text">auteur</roleTerm>
        <roleTerm type="code" authority="marcrelator">aut</roleTerm>
      </role>
      <affiliation>IRD</affiliation>
    </name>
    <name type="personnal">
      <namePart type="family">Legchenko</namePart>
      <namePart type="given">Anatoli</namePart>
      <role>
        <roleTerm type="text">auteur</roleTerm>
        <roleTerm type="code" authority="marcrelator">aut</roleTerm>
      </role>
      <affiliation>IRD</affiliation>
    </name>
    <typeOfResource>text</typeOfResource>
    <genre authority="local">journalArticle</genre>
    <language>
      <languageTerm type="code" authority="iso639-2b">eng</languageTerm>
    </language>
    <physicalDescription>
      <internetMediaType>text/pdf</internetMediaType>
      <digitalOrigin>born digital</digitalOrigin>
      <reformattingQuality>access</reformattingQuality>
    </physicalDescription>
    <abstract>The Dead Sea (DS) coastal areas have been dramatically affected by sinkhole formation since around 1990. Such sinkholes along both Israeli and Jordanian shores are linked to karst cavities that form through slow salt dissolution. A quantitative estimate of such in-situ salt karstification would be an important indicator of sinkhole hazard. One of the indications of salt karstification is its increased hydraulic conductivity, caused by the development of dissolution cavities forming conducting channels within the salt layer. We measured the hydraulic conductivity (K) versus shear-wave velocity (Vs) of DS salt in situ for estimating the actual salt karstification in areas of sinkhole development. These parameters were measured with the Magnetic Resonance Sounding (MRS) and Multichannel Analysis of Surface Waves (MASW) methods, respectively. Understanding of the field relationships was augmented by similar inter-relations obtained in the laboratory on samples of DS salt. In-situ salt velocities Vs vary from 750 m/s to over 1650 m/s, while hydraulic conductivity (K) in the same zones varies between about 10(-4) m/s to slightly over 10(-8) m/s. Both field and laboratory K and Vs values fit the exponential function In(K) = -0.0045 * V-s - 5.416 with a determination coefficient (R-2) of 0.88.A classification based on Vs and K was generated for salt conditions and the corresponding degrees of sinkhole hazard, which was verified in the Mineral Beach sinkhole development area. The mapping of sinkhole sites shows that they form within highly conductive zones with K &gt;= 5.5.10(-5). It is suggested that this methodology, with some modification, can be used for evaluating the conductive properties of karstified rock and associated sinkhole hazards.</abstract>
    <targetAudience authority="marctarget">specialized</targetAudience>
    <subject>
      <topic>Dead Sea</topic>
      <topic>karst</topic>
      <topic>MRS</topic>
      <topic>MASW</topic>
      <topic>salt</topic>
      <topic>Vs</topic>
    </subject>
    <subject authority="local">
      <geographic>ISRAEL</geographic>
      <geographic>JORDANIE</geographic>
    </subject>
    <classification authority="local">064</classification>
    <classification authority="local">062</classification>
    <relatedItem type="host">
      <titleInfo>
        <title>Geomorphology</title>
      </titleInfo>
      <part>
        <detail type="volume">
          <number>221</number>
        </detail>
        <extent unit="pages">
          <list> 150-163</list>
        </extent>
      </part>
      <originInfo>
        <dateIssued>2014</dateIssued>
      </originInfo>
      <identifier type="issn">0169-555X</identifier>
    </relatedItem>
    <identifier type="uri">https://www.documentation.ird.fr/hor/PAR00012226</identifier>
    <identifier type="doi">10.1016/j.geomorph.2014.06.014</identifier>
    <identifier type="issn">0169-555X</identifier>
    <location>
      <shelfLocator>[F B010062461]</shelfLocator>
      <url usage="primary display" access="object in context">https://www.documentation.ird.fr/hor/PAR00012226</url>
      <url access="row object">https://www.documentation.ird.fr/intranet/publi/2014/09/010062461.pdf</url>
    </location>
    <accessCondition type="restriction access" displayLabel="Accès réservé">Accès réservé (Intranet de l'IRD)</accessCondition>
    <recordInfo>
      <recordContentSource>IRD - Base Horizon / Pleins textes</recordContentSource>
      <recordCreationDate encoding="w3cdtf">2014-10-02</recordCreationDate>
      <recordChangeDate encoding="w3cdtf">2017-08-23</recordChangeDate>
      <recordIdentifier>PAR00012226</recordIdentifier>
      <languageOfCataloging>
        <languageTerm authority="iso639-2b">fre</languageTerm>
      </languageOfCataloging>
    </recordInfo>
  </mods>
</modsCollection>
