On the origin of kinking in layered crystalline solids

Gabriel Plummer; Hemant J. Rathod; Ankit Srivastava; Miladin Radovic; T. Ouisse; Melike Mercan Yildizhan; Per O. A. Persson; Konstantza Lambrinou; Michel W. Barsoum; Garritt J. Tucker

doi:10.1016/j.mattod.2020.11.014

On the origin of kinking in layered crystalline solids

Gabriel Plummer, Hemant J. Rathod, Ankit Srivastava, Miladin Radovic, T. Ouisse, Melike Mercan Yildizhan, Per O. A. Persson, Konstantza Lambrinou, Michel W. Barsoum, Garritt J. Tucker

Research output › peer-review

Abstract

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.

Original language	English
Pages (from-to)	45-52
Number of pages	8
Journal	Materials Today
Volume	43
DOIs	https://doi.org/10.1016/j.mattod.2020.11.014
State	Published - Mar 2021

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Cite this

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title = "On the origin of kinking in layered crystalline solids",

abstract = "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.",

keywords = "MAX phases, Deformation behaviour, Kinking, Layered crystalline solids",

author = "Gabriel Plummer and Rathod, {Hemant J.} and Ankit Srivastava and Miladin Radovic and T. Ouisse and Yildizhan, {Melike Mercan} and Persson, {Per O. A.} and Konstantza Lambrinou and Barsoum, {Michel W.} and Tucker, {Garritt J.}",

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doi = "10.1016/j.mattod.2020.11.014",

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T1 - On the origin of kinking in layered crystalline solids

AU - Plummer, Gabriel

AU - Rathod, Hemant J.

AU - Srivastava, Ankit

AU - Radovic, Miladin

AU - Ouisse, T.

AU - Yildizhan, Melike Mercan

AU - Persson, Per O. A.

AU - Lambrinou, Konstantza

AU - Barsoum, Michel W.

AU - Tucker, Garritt J.

N1 - Score=10

PY - 2021/3

Y1 - 2021/3

N2 - 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.

AB - 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.

KW - MAX phases

KW - Deformation behaviour

KW - Kinking

KW - Layered crystalline solids

UR - https://ecm.sckcen.be/OTCS/llisapi.dll/open/42348179

U2 - 10.1016/j.mattod.2020.11.014

DO - 10.1016/j.mattod.2020.11.014

M3 - Article

SN - 1369-7021

VL - 43

SP - 45

EP - 52

JO - Materials Today

JF - Materials Today

ER -