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<article xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:oasis="http://docs.oasis-open.org/ns/oasis-exchange/table" xml:lang="en" dtd-version="3.0" article-type="abstract"><?xmltex \bartext{S11: Transport processes of radionuclides in radioactive waste repositories}?>
  <front>
    <journal-meta><journal-id journal-id-type="publisher">SaND</journal-id><journal-title-group>
    <journal-title>Safety of Nuclear Waste Disposal</journal-title>
    <abbrev-journal-title abbrev-type="publisher">SaND</abbrev-journal-title><abbrev-journal-title abbrev-type="nlm-ta">Saf. Nucl. Waste Disposal</abbrev-journal-title>
  </journal-title-group><issn pub-type="epub">2749-4802</issn><publisher>
    <publisher-name>Copernicus Publications</publisher-name>
    <publisher-loc>Göttingen, Germany</publisher-loc>
  </publisher></journal-meta>
    <article-meta>
      <article-id pub-id-type="doi">10.5194/sand-2-165-2023</article-id><title-group><article-title>Permeability and diffusion of tritium in bentonite</article-title><alt-title>Permeability and diffusion of tritium in bentonite</alt-title>
      </title-group><?xmltex \runningtitle{Permeability and diffusion of tritium in bentonite}?><?xmltex \runningauthor{G.~Uroi\'{c} et al.}?>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes" rid="aff1">
          <name><surname>Uroić</surname><given-names>Galla</given-names></name>
          <email>galla.uroic@fond-nek.hr</email>
        <ext-link>https://orcid.org/0000-0003-4114-5225</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2">
          <name><surname>Veinović</surname><given-names>Želimir</given-names></name>
          
        <ext-link>https://orcid.org/0000-0002-1572-2191</ext-link></contrib>
        <contrib contrib-type="author" corresp="no" rid="aff3">
          <name><surname>Barešić</surname><given-names>Jadranka</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2">
          <name><surname>Herceg</surname><given-names>Vjekoslav</given-names></name>
          
        </contrib>
        <aff id="aff1"><label>1</label><institution>Fund for financing the decommissioning of the Krško Nuclear Power Plant and the disposal of Krško NPP radioactive waste and spent nuclear fuel, Zagreb 10000, Croatia</institution>
        </aff>
        <aff id="aff2"><label>2</label><institution>Department of Mining Engineering and Geotechnics, Faculty of Mining, geology and Petroleum Engineering, University of Zagreb, Zagreb 10000, Croatia</institution>
        </aff>
        <aff id="aff3"><label>3</label><institution>Laboratory for Low-level Radioactivities, Division of Experimental
Physics, <?xmltex \hack{\break}?> Ruđer Bošković Institute, Zagreb 10000, Croatia</institution>
        </aff>
      </contrib-group>
      <author-notes><corresp id="corr1">Galla Uroić (galla.uroic@fond-nek.hr)</corresp></author-notes><pub-date><day>6</day><month>September</month><year>2023</year></pub-date>
      
      <volume>2</volume>
      <fpage>165</fpage><lpage>166</lpage>
      <history>
        <date date-type="received"><day>28</day><month>March</month><year>2023</year></date>
           <date date-type="accepted"><day>23</day><month>May</month><year>2023</year></date>
      </history>
      <permissions>
        <copyright-statement>Copyright: © 2023 Galla Uroić et al.</copyright-statement>
        <copyright-year>2023</copyright-year>
      <license license-type="open-access"><license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri" xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p></license></permissions><self-uri xlink:href="https://sand.copernicus.org/articles/2/165/2023/sand-2-165-2023.html">This article is available from https://sand.copernicus.org/articles/2/165/2023/sand-2-165-2023.html</self-uri><self-uri xlink:href="https://sand.copernicus.org/articles/2/165/2023/sand-2-165-2023.pdf">The full text article is available as a PDF file from https://sand.copernicus.org/articles/2/165/2023/sand-2-165-2023.pdf</self-uri>
      <abstract><title>Abstract</title>

      <p id="d1e117">As a part of the Croatian RD&amp;D (research, development, and demonstration) program within the Program for LILW (low- and intermediate-level waste) and SNF (spent nuclear fuel) disposal, research of permeability and the diffusion of tritium in bentonite was organized, as part of the research of the future engineering barriers for repositories of LILW and SNF. Two types of materials were prepared, namely pure sodium bentonite and a mixture of sodium bentonite (12 %) with quartz sand (88 %). Compaction of materials was conducted with a modified Proctor test, and the apparatus was designed and made at the Faculty of Mining, Geology and Petroleum Engineering at the University of Zagreb, utilizing fused deposition modeling 3D printer and PETG (polyethylene terephthalate glycol) material.</p>

      <p id="d1e120">Water enriched with <inline-formula><mml:math id="M1" display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">3</mml:mn></mml:msup></mml:math></inline-formula>H has been prepared by dilution of the National Institute of Standards and Technology (NIST) <inline-formula><mml:math id="M2" display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">3</mml:mn></mml:msup></mml:math></inline-formula>H standard (4926<inline-formula><mml:math id="M3" display="inline"><mml:mi>e</mml:mi></mml:math></inline-formula>) to 6 L. The activity of the prepared enriched water was <inline-formula><mml:math id="M4" display="inline"><mml:mrow><mml:mn mathvariant="normal">49</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mn mathvariant="normal">700</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">180</mml:mn></mml:mrow></mml:math></inline-formula> TU. One part of the device was filled with <inline-formula><mml:math id="M5" display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">3</mml:mn></mml:msup></mml:math></inline-formula>H-free water and
the other with <inline-formula><mml:math id="M6" display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">3</mml:mn></mml:msup></mml:math></inline-formula>H-spiked water (0.6 L volume for each part). In total, five devices with bentonite and five devices with a sand–bentonite mixture were prepared this way. The devices were thoroughly sealed to avoid loss of sample and isotopic exchange with the atmosphere and put horizontally in holders. The water for <inline-formula><mml:math id="M7" display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">3</mml:mn></mml:msup></mml:math></inline-formula>H activity measurements was sampled monthly or bimonthly. A total of 8 mL of the sample was taken by syringe and transferred to a measurement vial. Each vial was additionally filled with 12 mL of a scintillator (Ultima Gold LLT, PerkinElmer) and thoroughly mixed. <inline-formula><mml:math id="M8" display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">3</mml:mn></mml:msup></mml:math></inline-formula>H activity was determined by a liquid scintillation counter (LSC; Quantulus 1220) at the Laboratory for Low-level Radioactivities, Ruđer Bošković Institute, Zagreb. Due to the penetration of bentonite from the barrier into the water samples, tritium-free water has relatively high activity after 2 months of the experiment (average value was <inline-formula><mml:math id="M9" display="inline"><mml:mrow><mml:mn mathvariant="normal">5560</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">240</mml:mn></mml:mrow></mml:math></inline-formula> TU). In the final sampling, after a 2-month time span, the activity reached <inline-formula><mml:math id="M10" display="inline"><mml:mrow><mml:mn mathvariant="normal">9670</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">2490</mml:mn></mml:mrow></mml:math></inline-formula> TU. Later, sampling and measurement were not possible due to the high bentonite amount within the samples. Tritium-free
samples from the sand–bentonite mixture device were stable, and the first analyses (1 month after the experiment setup) showed an average activity of <inline-formula><mml:math id="M11" display="inline"><mml:mrow><mml:mn mathvariant="normal">533</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">31</mml:mn></mml:mrow></mml:math></inline-formula> TU, while the final (5-month time span from the first sampling) average activity was <inline-formula><mml:math id="M12" display="inline"><mml:mrow><mml:mn mathvariant="normal">12</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mn mathvariant="normal">800</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">3430</mml:mn></mml:mrow></mml:math></inline-formula> TU. The increase in the concentration from the beginning to the end of the experiment was almost exponential. Spiked samples from the bentonite device had an average activity of <inline-formula><mml:math id="M13" display="inline"><mml:mrow><mml:mn mathvariant="normal">36</mml:mn><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mn mathvariant="normal">950</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">2550</mml:mn></mml:mrow></mml:math></inline-formula> TU at the first sampling and <inline-formula><mml:math id="M14" display="inline"><mml:mrow><mml:mn mathvariant="normal">17</mml:mn><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mn mathvariant="normal">580</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">13</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mn mathvariant="normal">320</mml:mn></mml:mrow></mml:math></inline-formula> TU after a 1-month time leg. Later, sampling was not possible. Spiked samples from sand–bentonite mixture showed a decrease in tritium activity from the first sampling (<inline-formula><mml:math id="M15" display="inline"><mml:mrow><mml:mn mathvariant="normal">43</mml:mn><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mn mathvariant="normal">390</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">1310</mml:mn></mml:mrow></mml:math></inline-formula> TU) to <inline-formula><mml:math id="M16" display="inline"><mml:mrow><mml:mn mathvariant="normal">27</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mn mathvariant="normal">210</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">285</mml:mn></mml:mrow></mml:math></inline-formula> TU (5 months after the first sampling). Considering the penetration of bentonite material into the water samples, only the sand–bentonite mixture can be considered for further analyses through the calculation of the diffusion.</p>
  </abstract>
    </article-meta>
  </front>
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