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<front>
<journal-meta>
<journal-id journal-id-type="publisher">SED</journal-id>
<journal-title-group>
<journal-title>Solid Earth Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">SED</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Solid Earth Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1869-9537</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/se-2019-48</article-id>
<title-group>
<article-title>Evaluating porosity estimates for sandstones based on X-ray micro-tomographic images</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Nehler</surname>
<given-names>Mathias</given-names>
<ext-link>https://orcid.org/0000-0002-0006-3509</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Stoeckhert</surname>
<given-names>Ferdinand</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Oelker</surname>
<given-names>Anne</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Renner</surname>
<given-names>Jörg</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Saenger</surname>
<given-names>Erik</given-names>
<ext-link>https://orcid.org/0000-0002-2057-4728</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>International Geothermal Centre, Bochum University of Applied Sciences, 44801, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Ruhr-Universität, Bochum, 44801, Germany</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>RWTH Aachen, Aachen, 52062, Germany</addr-line>
</aff>
<pub-date pub-type="epub">
<day>11</day>
<month>03</month>
<year>2019</year>
</pub-date>
<volume>2019</volume>
<fpage>1</fpage>
<lpage>45</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2019 Mathias Nehler et al.</copyright-statement>
<copyright-year>2019</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://se.copernicus.org/preprints/se-2019-48/">This article is available from https://se.copernicus.org/preprints/se-2019-48/</self-uri>
<self-uri xlink:href="https://se.copernicus.org/preprints/se-2019-48/se-2019-48.pdf">The full text article is available as a PDF file from https://se.copernicus.org/preprints/se-2019-48/se-2019-48.pdf</self-uri>
<abstract>
<p>&lt;p&gt;We compare experimentally determined porosity with values derived from X-ray tomography for a suite of eight sandstone varieties covering a porosity range from about 3 to 25&amp;thinsp;%. In addition, we performed conventional stereological analysis of SEM images and examined thin sections. We investigated the sensitivity of segmentation, the conversion of the tomographic gray-value images representing the obtained X-ray attenuation coefficients into binary images, to (a) resolution of the digital images, (b) denoising filters, and (c) seven thresholding methods. Images of sandstones with porosities of 15 to 25&amp;thinsp;% exhibit a bimodal intensity distribution of the attenuation coefficients, enabling unambiguous segmentation that gives porosity values closely matching the laboratory values. For samples with lower porosities, pores and grains do not separate well in the skewed unimodal intensity histograms. For these samples, all tested thresholding methods tend to miscalculate porosity significantly. In addition to absolute porosity, the ratio between pore size and resolution, and mineralogical composition of the rocks affect the biases of the global segmentation methods.&lt;/p&gt;</p>
</abstract>
<counts><page-count count="45"/></counts>
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<funding-source></funding-source>
<award-id>321-8.03.04.03-2012/x</award-id>
</award-group>
</funding-group>
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</front>
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