Atomic-scale modelling of elastic and failure properties of clays

被引:63
|
作者
Hantal, Gyoergy [1 ]
Brochard, Laurent [2 ]
Laubie, Hadrien [1 ]
Ebrahimi, Davoud [1 ]
Pellenq, Roland J. -M. [1 ,3 ,4 ]
Ulm, Franz-Josef [1 ,4 ]
Coasne, Benoit [1 ,4 ]
机构
[1] MIT, Dept Civil & Environm Engn, Cambridge, MA 02139 USA
[2] Univ Paris Est, Lab Navier, CNRS, ENPC,IFSTTAR,UMR 8205, Marne La Vallee, France
[3] CNRS, CINaM, Marseille, France
[4] Joint CNRS MIT Lab, Multiscale Mat Sci Energy & Environm MSE2, Cambridge, MA USA
关键词
elastic properties; reactive molecular simulation; clay; fracture; REACTIVE FORCE-FIELD; DYNAMICS; WATER; MONTMORILLONITE; 1ST-PRINCIPLES; SILICATES; SHALE;
D O I
10.1080/00268976.2014.897393
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
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.
引用
收藏
页码:1294 / 1305
页数:12
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