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        <title type="main" level="a">The use of 2H and 18O isotopes in the study of coastal karstic aquifers</title>
        <author>
          <persName n="1" ref="https://orcid.org/0000-0001-6746-8693" type="ORCID">
            <forename>Diana</forename>
            <surname>Mance</surname>
            <placeName type="affiliation">University of Rijeka, Croatia</placeName>
          </persName>
          <persName n="2">
            <forename>Danijela</forename>
            <surname>Lenac</surname>
            <placeName type="affiliation">University of Rijeka, Croatia</placeName>
          </persName>
          <persName n="3" ref="https://orcid.org/0000-0003-1384-8417" type="ORCID">
            <forename>Maja</forename>
            <surname>Radišić</surname>
            <placeName type="affiliation">University of Rijeka, Croatia</placeName>
          </persName>
          <persName n="4" ref="https://orcid.org/0000-0002-6206-2464" type="ORCID">
            <forename>Davor</forename>
            <surname>Mance</surname>
            <placeName type="affiliation">University of Rijeka, Croatia</placeName>
          </persName>
          <persName n="5" ref="https://orcid.org/0000-0002-5766-804X" type="ORCID">
            <forename>Josip</forename>
            <surname>Rubinić</surname>
            <placeName type="affiliation">University of Rijeka, Croatia</placeName>
          </persName>
        </author>
        <respStmt>
          <resp>This is a section of <title>Ninth International Symposium “Monitoring of Mediterranean Coastal Areas: Problems and Measurement Techniques”</title>(DOI: <idno type="DOI">10.36253/979-12-215-0030-1</idno>) by </resp>
          <name>Laura Bonora, Donatella Carboni, Matteo De Vincenzi, Giorgio Matteucci</name>
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      <publicationStmt>
        <publisher>Firenze University Press</publisher>
        <pubPlace>Firenze</pubPlace>
        <date when="2022">2022</date>
        <idno type="DOI">https://doi.org/10.36253/979-12-215-0030-1.48</idno>
        <availability>
          <p>Available for academic research purposes</p>
          <p>Open Access</p>
          <p>Copyright Author(s)</p>
          <licence source="text" target="https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode">
            <p>Content licence CC BY-NC-SA 4.0</p>
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        <p>This is original content, published for academic research purposes</p>
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      <abstract xml:lang="en">
        <p>Complexity of karst groundwater networks requires implementation of standard hydrogeological monitoring and unconventional methods of investigation. We present the results of isotope composition analysis for three karst springs and rain water collected in their hinterland. During two years, spring water samples were collected on a weekly and rain samples on a monthly basis. The main findings are: winter precipitation of Mediterranean origin dominates springs' recharge, a dual porosity model is a fit for the studied systems, and hinterlands of the springs have different retention capabilities.</p>
      </abstract>
      <textClass>
        <keywords>
          <list>
            <item>Coastal environmental physics</item>
            <item>Coastal karstic aquifer</item>
            <item>Stable isotopes</item>
            <item>Statistical modelling</item>
          </list>
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      <p>It is available online at https://doi.org/10.36253/979-12-215-0030-1.48<ref target="https://doi.org/10.36253/979-12-215-0030-1.48" /></p>
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