Fracturing of migmatite monitored by acoustic emission and ultrasonic sounding
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F19%3A00494576" target="_blank" >RIV/67985530:_____/19:00494576 - isvavai.cz</a>
Alternative codes found
RIV/67985831:_____/19:00494576 RIV/00216208:11310/19:10472519
Result on the web
<a href="https://link.springer.com/article/10.1007%2Fs00603-018-1590-2" target="_blank" >https://link.springer.com/article/10.1007%2Fs00603-018-1590-2</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s00603-018-1590-2" target="_blank" >10.1007/s00603-018-1590-2</a>
Alternative languages
Result language
angličtina
Original language name
Fracturing of migmatite monitored by acoustic emission and ultrasonic sounding
Original language description
Here, we present an experimental study of the fracturing of anisotropic migmatite with plane-parallel structure (foliation). Four specimens, with different dips of foliation, including subhorizontal (13 degrees), subvertical (86 degrees), and oblique (47 degrees, 67 degrees), were uniaxially loaded up to failure. Acoustic emission monitoring and ultrasonic sounding were applied for fracturing characterization. In case of subhorizontal and subvertical foliation, the tensile source type played an important role before reaching nucleation stress when shearing became dominant. The dominance of non-tension microcracking was characteristic for oblique foliation. The uniaxial loading of migmatite resulted in triaxial stress state regardless of the foliation dip. The minimum stress axis was in the subhorizontal direction of the foliation dip. The triaxial stress state caused the preferential orientation of induced shear and tension microcracks that had the same azimuthal orientation as the foliation. Preferential microcracking resulted in preferential orientation of the failure plane. Based on the anisotropic behavior of migmatite's characteristic mechanical properties, as well as its mechanism of failure that is typical for anisotropic rocks, the obtained conclusions may be generalized for other types of metamorphic anisotropic rocks with a plane-parallel structure.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10507 - Volcanology
Result continuities
Project
<a href="/en/project/GA16-03950S" target="_blank" >GA16-03950S: Solid body fracturing mode by shear-tensile source model: acoustic emission laboratory study</a><br>
Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2019
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Rock Mechanics and Rock Engineering
ISSN
0723-2632
e-ISSN
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Volume of the periodical
52
Issue of the periodical within the volume
1
Country of publishing house
AT - AUSTRIA
Number of pages
13
Pages from-to
47-59
UT code for WoS article
000456673000004
EID of the result in the Scopus database
2-s2.0-85053439932