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  <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-2-53-2023</article-id><title-group><article-title>A note on the duration of claystone exploration programs</article-title><alt-title>A note on the duration of claystone exploration programs</alt-title>
      </title-group><?xmltex \runningtitle{A note on the duration of claystone exploration programs}?><?xmltex \runningauthor{T.~Mann et al.}?>
      <contrib-group>
        <contrib contrib-type="author" corresp="yes">
          <name><surname>Mann</surname><given-names>Thomas</given-names></name>
          <email>thomas.mann@bgr.de</email>
        <ext-link>https://orcid.org/0000-0002-9182-2741</ext-link></contrib>
        <contrib contrib-type="author" corresp="no">
          <name><surname>Schuck</surname><given-names>Bernhard</given-names></name>
          
        <ext-link>https://orcid.org/0000-0001-7987-3821</ext-link></contrib>
        <contrib contrib-type="author" corresp="no">
          <name><surname>Kneuker</surname><given-names>Tilo</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no">
          <name><surname>Pollok</surname><given-names>Lukas</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no">
          <name><surname>Bornemann</surname><given-names>André</given-names></name>
          
        <ext-link>https://orcid.org/0000-0003-4341-2366</ext-link></contrib>
        <contrib contrib-type="author" corresp="no">
          <name><surname>Erbacher</surname><given-names>Jochen</given-names></name>
          
        </contrib>
        <aff id="aff1"><institution>Federal Institute for Geosciences and Natural Resources (BGR), Hanover 30655, Germany</institution>
        </aff>
      </contrib-group>
      <author-notes><corresp id="corr1">Thomas Mann (thomas.mann@bgr.de)</corresp></author-notes><pub-date><day>6</day><month>September</month><year>2023</year></pub-date>
      
      <volume>2</volume>
      <fpage>53</fpage><lpage>52</lpage>
      <history>
        <date date-type="received"><day>4</day><month>April</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 Thomas Mann 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/2/53/2023/sand-2-53-2023.html">This article is available from https://sand.copernicus.org/articles/2/53/2023/sand-2-53-2023.html</self-uri><self-uri xlink:href="https://sand.copernicus.org/articles/2/53/2023/sand-2-53-2023.pdf">The full text article is available as a PDF file from https://sand.copernicus.org/articles/2/53/2023/sand-2-53-2023.pdf</self-uri>
      <abstract><title>Abstract</title>

      <p id="d1e117">In a recent report, the German Federal Company for Radioactive Waste Disposal (BGE) estimated the probable duration of exploration activities within potential siting regions (BGE, 2022). Based on many years of expertise regarding the exploration of the subsurface, we outline in this contribution that the BGE (2022) likely underestimates the time necessary to characterize claystones within potential siting regions. Our latest experience originates from two research projects that developed sequence stratigraphic frameworks for the largely homogenous claystone successions of the Lower Cretaceous in northern Germany (Thöle et al., 2020) and the Middle Jurassic in southern Germany, respectively. Although the specific study areas are not considered in the site selection procedure, both stratigraphic units are reviewed to potentially host a nuclear waste repository. Accordingly, our hands-on experience might constitute a highly relevant contribution to the ongoing debate. Within each study area, drill cores were extracted from four boreholes with a total length of <inline-formula><mml:math id="M1" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">660</mml:mn></mml:mrow></mml:math></inline-formula> m (northern Germany) and <inline-formula><mml:math id="M2" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">930</mml:mn></mml:mrow></mml:math></inline-formula> m (southern Germany). After the drilling campaigns, each having taken approx. 5–6 weeks, the cores were split, photographed in high resolution, lithologically described, scanned with an X-Ray fluorescence (XRF) core scanner (10 mm scan interval) to determine the elemental distribution, and sampled for lithological, mineralogical and geochemical analyses at a resolution of 1 m, which took approx. 12 months. However, the most time-consuming steps were the analysis and interpretation of the stratigraphy and particularly the mineralogical investigations. With a sampling resolution of 1 m, an analysis time of approx. 6 months per 250 core meters is a robust reference. We reckoned a total duration of 5 years for the workload in each of the abovementioned research projects. Obviously, the duration of claystone exploration will vary, depending on the number and length of the core drillings per siting region, in addition to the sampling resolution. However, if BGE aims to characterize claystones with a degree of detail comparable to our
projects, the estimated 42 months (see Table 3 in BGE, 2022) will likely be
insufficient.</p>
  </abstract>
    </article-meta>
  </front>
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    <back><ref-list>
    <title>References</title>

      <ref id="bib1.bib1"><label>1</label><?label 1?><mixed-citation>BGE: Zeitliche Betrachtung des Standortauswahlverfahrens aus Sicht
der BGE. Rahmenterminplanung für Schritt 2 der Phase I bis zum Vorschlag
der Standortregionen und zeitliche Abschätzungen für Phase II und
III, <uri>https://www.bge.de/fileadmin/user_upload/Standortsuche/Wesentliche_Unterlagen/05_-_Meilensteine/Zeitliche_Betrachtung_des_Standortauswahlverfahrens_2022/20221216_Zeitliche_Betrachtung_StandAW-48_barrierefrei.pdf</uri> (last access: 22 June 2023), 2022.
</mixed-citation></ref><?xmltex \hack{\newpage}?>
      <ref id="bib1.bib2"><label>2</label><?label 1?><mixed-citation>
Thöle, H., Bornemann, A., Heimhofer, U., Luppold, F. W., Blumenberg, M.,
Dohrmann, R., and Erbacher, J.: Using high-resolution XRF analyses
as a sequence stratigraphic tool in a mudstone-dominated succession (Early
Cretaceous, Lower Saxony Basin, Northern Germany), The Depositional Record,
6, 236–258, 2020.</mixed-citation></ref>

  </ref-list></back>
    <!--<article-title-html>A note on the duration of claystone exploration programs</article-title-html>
<abstract-html/>
<ref-html id="bib1.bib1"><label>1</label><mixed-citation>
      
BGE: Zeitliche Betrachtung des Standortauswahlverfahrens aus Sicht
der BGE. Rahmenterminplanung für Schritt 2 der Phase I bis zum Vorschlag
der Standortregionen und zeitliche Abschätzungen für Phase II und
III, <a href="https://www.bge.de/fileadmin/user_upload/Standortsuche/Wesentliche_Unterlagen/05_-_Meilensteine/Zeitliche_Betrachtung_des_Standortauswahlverfahrens_2022/20221216_Zeitliche_Betrachtung_StandAW-48_barrierefrei.pdf" target="_blank"/> (last access: 22 June 2023), 2022.


    </mixed-citation></ref-html>
<ref-html id="bib1.bib2"><label>2</label><mixed-citation>
      
Thöle, H., Bornemann, A., Heimhofer, U., Luppold, F. W., Blumenberg, M.,
Dohrmann, R., and Erbacher, J.: Using high-resolution XRF analyses
as a sequence stratigraphic tool in a mudstone-dominated succession (Early
Cretaceous, Lower Saxony Basin, Northern Germany), The Depositional Record,
6, 236–258, 2020.

    </mixed-citation></ref-html>--></article>
