TY - JOUR
T1 - Atomic-scale modelling of elastic and failure properties of clays
AU - Hantal, György
AU - Brochard, Laurent
AU - Laubie, Hadrien
AU - Ebrahimi, Davoud
AU - Pellenq, Roland J.M.
AU - Ulm, Franz Josef
AU - Coasne, Benoit
PY - 2014/5/19
Y1 - 2014/5/19
N2 - The elastic and failure properties of a typical clay, illite, are investigated using molecular simulation. We employ a reactive (ReaxFF) and a non-reactive (ClayFF) force field to assess the elastic properties of the clay. As far as failure is concerned, ReaxFF was used throughout the study; however, some calculations were also performed with ClayFF. A crack parallel to the clay layers is found to have low fracture resistance when submitted to a tensile loading perpendicular to the crack. The mechanism of both yield and fracture failures is decohesion in the interlayer space. In contrast, under shear loading, the nanoscale failure mechanism is a stick-slip between clay layers. No fracture propagation is observed as the clay layers slide on top of each other. The low fracture resistance in mode I and the stick-slip failure in mode II are both the consequence of the lack of chemical bonds between clay layers where the cohesion is provided by non-covalent interactions. This work, which provides a description of the failure of clays at the microscopic scale, is the first step towards describing the failure of clays at a larger scale where the polycrystalline distribution of clay grains must be taken into account.
AB - The elastic and failure properties of a typical clay, illite, are investigated using molecular simulation. We employ a reactive (ReaxFF) and a non-reactive (ClayFF) force field to assess the elastic properties of the clay. As far as failure is concerned, ReaxFF was used throughout the study; however, some calculations were also performed with ClayFF. A crack parallel to the clay layers is found to have low fracture resistance when submitted to a tensile loading perpendicular to the crack. The mechanism of both yield and fracture failures is decohesion in the interlayer space. In contrast, under shear loading, the nanoscale failure mechanism is a stick-slip between clay layers. No fracture propagation is observed as the clay layers slide on top of each other. The low fracture resistance in mode I and the stick-slip failure in mode II are both the consequence of the lack of chemical bonds between clay layers where the cohesion is provided by non-covalent interactions. This work, which provides a description of the failure of clays at the microscopic scale, is the first step towards describing the failure of clays at a larger scale where the polycrystalline distribution of clay grains must be taken into account.
KW - Clay
KW - Elastic properties
KW - Fracture
KW - Reactive molecular simulation
UR - https://www.scopus.com/pages/publications/84901199577
U2 - 10.1080/00268976.2014.897393
DO - 10.1080/00268976.2014.897393
M3 - Article
AN - SCOPUS:84901199577
SN - 0026-8976
VL - 112
SP - 1294
EP - 1305
JO - Molecular Physics
JF - Molecular Physics
IS - 9-10
ER -