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On the origin of kinking in layered crystalline solids

Plummer, G. (author)
Colorado Sch Mines, CO 80401 USA
Rathod, H. (author)
Texas A&M Univ, TX 77840 USA
Srivastava, A. (author)
Texas A&M Univ, TX 77840 USA
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Radovic, M. (author)
Texas A&M Univ, TX 77840 USA
Ouisse, T. (author)
Univ Grenoble Alpes, France
Yildizhan Özyar, Melike (author)
Linköpings universitet,Tunnfilmsfysik,Tekniska fakulteten
Persson, Per O A (author)
Linköpings universitet,Tunnfilmsfysik,Tekniska fakulteten
Lambrinou, K. (author)
SCK CEN, Belgium; Univ Huddersfield, England
Barsoum, M. W. (author)
Drexel Univ, PA 19104 USA
Tucker, G. J. (author)
Colorado Sch Mines, CO 80401 USA
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 (creator_code:org_t)
Elsevier Science Ltd, 2021
2021
English.
In: Materials Today. - : Elsevier Science Ltd. - 1369-7021 .- 1873-4103. ; 43, s. 45-52
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • Kinking is a deformation mechanism ubiquitous to layered systems, ranging from the nanometer scale in layered crystalline solids, to the kilometer scale in geological formations. Herein, we demonstrate its origins in the former through multiscale experiments and atomistic simulations. When compressively loaded parallel to their basal planes, layered crystalline solids first buckle elastically, then nucleate atomic-scale, highly stressed ripplocation boundaries - a process driven by redistributing strain from energetically expensive in-plane bonds to cheaper out-of-plane bonds. The consequences are far reaching as the unique mechanical properties of layered crystalline solids are highly dependent upon their ability to deform by kinking. Moreover, the compressive strength of numerous natural and engineered layered systems depends upon the ease of kinking or lack there of.

Subject headings

TEKNIK OCH TEKNOLOGIER  -- Materialteknik -- Metallurgi och metalliska material (hsv//swe)
ENGINEERING AND TECHNOLOGY  -- Materials Engineering -- Metallurgy and Metallic Materials (hsv//eng)

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