Analysis of Local Creep Strain Field and Cracking Process in Claystone by X-Ray Micro-Tomography and Digital Volume Correlation
X-ray micro-tomography (XMT) is an efficient technique for non-destructive imaging of morphological structures. It is suitable for monitoring local displacement fields of heterogeneous materials. Digital volume correlation (DVC) methods are widely used for the quantification of local strain fields f...
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| Veröffentlicht in: | Rock mechanics and rock engineering 2021-04, Vol.54 (4), p.1937-1952 |
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| container_end_page | 1952 |
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| container_issue | 4 |
| container_start_page | 1937 |
| container_title | Rock mechanics and rock engineering |
| container_volume | 54 |
| creator | Shi, Hai-Ling Hosdez, Jerome Rougelot, Thomas Xie, Shou-Yi Shao, Jian-Fu Talandier, Jean |
| description | X-ray micro-tomography (XMT) is an efficient technique for non-destructive imaging of morphological structures. It is suitable for monitoring local displacement fields of heterogeneous materials. Digital volume correlation (DVC) methods are widely used for the quantification of local strain fields from highly contrasted XMT images. The aim of this work is to investigate strain localization and cracking process in a hard clayey rock. For this purpose, three-dimensional images have been taken by in situ X-ray micro-tomography on a tested sample under different loading levels and time steps. These images are analyzed with a DVC based method to calculate both local strain fields and averaged global strains. In particular, the progressive localization of strain field with applied stress and creep time is investigated in relation with material heterogeneities. It is found that the strain field localization as well as the cracking process is clearly influenced by the presence of stiff inclusions, pores, weak clayey zones and layered microscopic structure of claystone. |
| doi_str_mv | 10.1007/s00603-021-02375-5 |
| format | Article |
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It is suitable for monitoring local displacement fields of heterogeneous materials. Digital volume correlation (DVC) methods are widely used for the quantification of local strain fields from highly contrasted XMT images. The aim of this work is to investigate strain localization and cracking process in a hard clayey rock. For this purpose, three-dimensional images have been taken by in situ X-ray micro-tomography on a tested sample under different loading levels and time steps. These images are analyzed with a DVC based method to calculate both local strain fields and averaged global strains. In particular, the progressive localization of strain field with applied stress and creep time is investigated in relation with material heterogeneities. 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It is found that the strain field localization as well as the cracking process is clearly influenced by the presence of stiff inclusions, pores, weak clayey zones and layered microscopic structure of claystone.</description><subject>Applied geology</subject><subject>Civil Engineering</subject><subject>Correlation</subject><subject>Cracking (chemical engineering)</subject><subject>Creep (materials)</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Engineering Sciences</subject><subject>Fields</subject><subject>Geophysics</subject><subject>Geophysics/Geodesy</subject><subject>Inclusions</subject><subject>Localization</subject><subject>Mechanics</subject><subject>Nondestructive testing</subject><subject>Original Paper</subject><subject>Sciences of the Universe</subject><subject>Solid mechanics</subject><subject>Solifluction</subject><subject>Strain analysis</subject><subject>Strain localization</subject><subject>Tomography</subject><subject>X ray microtomography</subject><subject>X rays</subject><issn>0723-2632</issn><issn>1434-453X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kU1r3DAQhkVpINukfyAnQU89KJU0khwfFzcfhS0t-Si5iZFX3ij1WlvJW_Apf71KXJpbD8PAzPO-MPMSciL4qeC8-pQ5NxwYl6IUVJrpN2QhFCimNNy_JQteSWDSgDwk73J-5Lwsq7MFeVoO2E85ZBo7uoot9rRJ3u_ozZgwDPQi-H5NcViXMbY_w7Ch31Nsfc60bJsepzzGwVM30Xt2jRP9GtoU2W3cxk3C3cP0ov0cNmEs1j9iv9962sSUfI9jiMMxOeiwz_79335E7i7Ob5srtvp2-aVZrlgLdTWyNRhwktet450xci0kGJRn0KJ0KKRBVYMzBj1wBVq61inslFBOgKyclnBEPs6-D9jbXQpbTJONGOzVcmWfZ1ypWmsjf4vCfpjZXYq_9j6P9jHuU_lTtlJzI4SuoC6UnKlyb87Jd_9sBbfPodg5FFtCsS-hWF1EMItygYeNT6_W_1H9AQG_jhQ</recordid><startdate>20210401</startdate><enddate>20210401</enddate><creator>Shi, Hai-Ling</creator><creator>Hosdez, Jerome</creator><creator>Rougelot, Thomas</creator><creator>Xie, Shou-Yi</creator><creator>Shao, Jian-Fu</creator><creator>Talandier, Jean</creator><general>Springer Vienna</general><general>Springer Nature B.V</general><general>Springer Verlag</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TN</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>M2P</scope><scope>M7S</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>Q9U</scope><scope>1XC</scope><scope>VOOES</scope><orcidid>https://orcid.org/0000-0002-6632-8207</orcidid><orcidid>https://orcid.org/0000-0003-3602-674X</orcidid></search><sort><creationdate>20210401</creationdate><title>Analysis of Local Creep Strain Field and Cracking Process in Claystone by X-Ray Micro-Tomography and Digital Volume Correlation</title><author>Shi, Hai-Ling ; 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It is suitable for monitoring local displacement fields of heterogeneous materials. Digital volume correlation (DVC) methods are widely used for the quantification of local strain fields from highly contrasted XMT images. The aim of this work is to investigate strain localization and cracking process in a hard clayey rock. For this purpose, three-dimensional images have been taken by in situ X-ray micro-tomography on a tested sample under different loading levels and time steps. These images are analyzed with a DVC based method to calculate both local strain fields and averaged global strains. In particular, the progressive localization of strain field with applied stress and creep time is investigated in relation with material heterogeneities. 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| ispartof | Rock mechanics and rock engineering, 2021-04, Vol.54 (4), p.1937-1952 |
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| subjects | Applied geology Civil Engineering Correlation Cracking (chemical engineering) Creep (materials) Earth and Environmental Science Earth Sciences Engineering Sciences Fields Geophysics Geophysics/Geodesy Inclusions Localization Mechanics Nondestructive testing Original Paper Sciences of the Universe Solid mechanics Solifluction Strain analysis Strain localization Tomography X ray microtomography X rays |
| title | Analysis of Local Creep Strain Field and Cracking Process in Claystone by X-Ray Micro-Tomography and Digital Volume Correlation |
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