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  4. Synchrotron-radiation computed tomography of the water drop penetration time test on hydrophobic soils
 
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Synchrotron-radiation computed tomography of the water drop penetration time test on hydrophobic soils

Citation Link: https://doi.org/10.15480/882.15410
Publikationstyp
Journal Article
Date Issued
2025
Sprache
English
Author(s)
Toffoli, Clara M. 
Geotechnik und Baubetrieb B-5  
Milatz, Marius  orcid-logo
Moosmann, Julian Philipp  
Helmholtz-Zentrum Hereon  
Jentschke, Thomas  
Helmholtz-Zentrum Hereon  
Beckmann, Felix  
Helmholtz-Zentrum Hereon  
Grabe, Jürgen  
Geotechnik und Baubetrieb B-5  
TORE-DOI
10.15480/882.15410
TORE-URI
https://hdl.handle.net/11420/56292
Journal
Journal of Rock Mechanics and Geotechnical Engineering  
Volume
17
Issue
8
Start Page
5111
End Page
5121
Citation
Journal of Rock Mechanics and Geotechnical Engineering 17 (8): 5111-5121 (2025)
Publisher DOI
10.1016/j.jrmge.2025.06.003
Scopus ID
2-s2.0-105009691260
Publisher
Elsevier
The water drop penetration time (WDPT) test consists of placing water drops on a material's surface in order to evaluate how long it takes to penetrate the pores. It is used to evaluate the hydrophobicity of materials. This study aims at investigating in more detail the soil-water interaction during the test, exposing its mechanism. For that, a model soil named Hamburg Sand was coated with a hydrophobic fluoropolymer and then a WDPT test was performed while computed tomography (CT) images were taken. Tomography experiments were performed at the P07 high-energy materials science (HEMS) beamline, operated by Helmholtz–Zentrum Hereon, at the storage ring PETRA III at the Deutsches Elektronen-Synchrotron (DESY) in Hamburg. Using synchrotron radiation, a tomogram can be obtained in about 10 min, way less time than regular laboratory X-ray sources usually owned by universities. The faster imaging enables the observation of the drop penetration during time and thus provides insight into the dynamics of the process. After that, digital discrete image correlation is performed to track the displacement of the grains throughout time. From the results one can observe that, as the drop is absorbed at the material's surface, the grains directly around the droplet base are dragged to the liquid-air interface around the drop, revealing grain kinematics during capillary interactions of the penetrating liquid and sand grains.
Subjects
Hydrophobic soil
Synchrotron tomography
Water drop penetration time (WDPT) test
DDC Class
551.3: Surface and Exogenous Processes and their Agents
620.11: Engineering Materials
Lizenz
https://creativecommons.org/licenses/by/4.0/
Publication version
publishedVersion
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