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Dislocation avalanches are like earthquakes on the micron scale

. 2022 Apr 13 ; 13 (1) : 1975. [epub] 20220413

Status PubMed-not-MEDLINE Language English Country Great Britain, England Media electronic

Document type Journal Article

Grant support
TKP2020-IKA-05 Emberi Eroforrások Minisztériuma (Ministry of Human Capacities)
NKFIH-K-119561 Nemzeti Kutatási, Fejlesztési és Innovációs Hivatal (NKFI Office)
NKFIH-FK-138975 Nemzeti Kutatási, Fejlesztési és Innovációs Hivatal (NKFI Office)
NKFIH-K-119561 Nemzeti Kutatási, Fejlesztési és Innovációs Hivatal (NKFI Office)
NKFIH-FK-138975 Nemzeti Kutatási, Fejlesztési és Innovációs Hivatal (NKFI Office)
NKFIH-K-119561 Nemzeti Kutatási, Fejlesztési és Innovációs Hivatal (NKFI Office)
NKFIH-K-119561 Nemzeti Kutatási, Fejlesztési és Innovációs Hivatal (NKFI Office)
NKFIH-FK-138975 Nemzeti Kutatási, Fejlesztési és Innovációs Hivatal (NKFI Office)
NKFIH-K-119561 Nemzeti Kutatási, Fejlesztési és Innovációs Hivatal (NKFI Office)
19-22604S Grantová Agentura České Republiky (Grant Agency of the Czech Republic)

Links

PubMed 35418187
PubMed Central PMC9007997
DOI 10.1038/s41467-022-29044-7
PII: 10.1038/s41467-022-29044-7
Knihovny.cz E-resources

Compression experiments on micron-scale specimens and acoustic emission (AE) measurements on bulk samples revealed that the dislocation motion resembles a stick-slip process - a series of unpredictable local strain bursts with a scale-free size distribution. Here we present a unique experimental set-up, which detects weak AE waves of dislocation slip during the compression of Zn micropillars. Profound correlation is observed between the energies of deformation events and the emitted AE signals that, as we conclude, are induced by the collective dissipative motion of dislocations. The AE data also reveal a two-level structure of plastic events, which otherwise appear as a single stress drop. Hence, our experiments and simulations unravel the missing relationship between the properties of acoustic signals and the corresponding local deformation events. We further show by statistical analyses that despite fundamental differences in deformation mechanism and involved length- and time-scales, dislocation avalanches and earthquakes are essentially alike.

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