Articles | Volume 5, issue 2
https://doi.org/10.5194/se-5-883-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/se-5-883-2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
27 Aug 2014
Research article |
| 27 Aug 2014
Transport processes at quartz–water interfaces: constraints from hydrothermal grooving experiments
K. Klevakina
Institut für Geologie, Mineralogie und Geophysik, Ruhr-Universität Bochum, 44780 Bochum, Germany
J. Renner
Institut für Geologie, Mineralogie und Geophysik, Ruhr-Universität Bochum, 44780 Bochum, Germany
N. Doltsinis
Institut für Chemie, Ruhr-Universität Bochum, 44780 Bochum, Germany
now at: Institut für Festkörpertheorie, Westfälische Wilhelms-Universität, 48149 Münster, Germany
W. Adeagbo
Institut für Chemie, Ruhr-Universität Bochum, 44780 Bochum, Germany
now at: Institut für Physik, Martin-Luther-Universität Halle-Wittenberg, 06120 Halle, Germany
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Short summary
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The technique of X-ray computed tomography (CT) is widely used in multiple disciplines such as medicine, industry and earth sciences. However, quantitative analysis from the reconstructed images are subject to errors due to technical limitations and subsequent evaluation workflows. The paper addresses the uncertainties related to the estimation of porosity from these images and compares the results with laboratory measurements. Accurate porosity estimates are linked to sufficient resolution.
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Solid Earth, 4, 331–345, https://doi.org/10.5194/se-4-331-2013, https://doi.org/10.5194/se-4-331-2013, 2013
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