|
|
|
|
| LEADER |
01823 am a22002773u 4500 |
| 001 |
92762 |
| 042 |
|
|
|a dc
|
| 100 |
1 |
0 |
|a Ebrahimi, Davoud
|e author
|
| 100 |
1 |
0 |
|a Massachusetts Institute of Technology. Department of Civil and Environmental Engineering
|e contributor
|
| 100 |
1 |
0 |
|a Whittle, Andrew
|e contributor
|
| 100 |
1 |
0 |
|a Ebrahimi, Davoud
|e contributor
|
| 100 |
1 |
0 |
|a Pellenq, Roland Jm
|e contributor
|
| 100 |
1 |
0 |
|a Whittle, Andrew
|e contributor
|
| 700 |
1 |
0 |
|a Pellenq, Roland Jm
|e author
|
| 700 |
1 |
0 |
|a Whittle, Andrew
|e author
|
| 245 |
0 |
0 |
|a Nano-Scale Elastic Properties Due to Montmorillonite Water Adsorption
|
| 246 |
3 |
3 |
|a Nanoscale Elastic Properties of Montmorillonite upon Water Adsorption
|
| 260 |
|
|
|b American Chemical Society (ACS),
|c 2015-01-09T15:54:07Z.
|
| 856 |
|
|
|z Get fulltext
|u http://hdl.handle.net/1721.1/92762
|
| 520 |
|
|
|a Smectites are an important group of clay minerals that experience swelling upon water adsorption. This paper uses molecular dynamics with the CLAYFF force field to simulate isothermal isobaric water adsorption of interlayer Wyoming Na-montmorillonite, a member of the smectite group. Nanoscale elastic properties of the clay-interlayer water system are calculated from the potential energy of the model system. The transverse isotropic symmetry of the elastic constant matrix was assessed by calculating Euclidean and Riemannian distance metrics. Simulated elastic constants of the clay mineral are compared with available results from acoustic and nanoindentation measurements.
|
| 520 |
|
|
|a National Science Foundation (U.S.) (National Center for Supercomputing Applications and Texas Advanced Computing Center Grant TG-DMR100028)
|
| 520 |
|
|
|a X-Shale Hub at MIT
|
| 520 |
|
|
|a Singapore-MIT Alliance for Research and Technology
|
| 546 |
|
|
|a en_US
|
| 655 |
7 |
|
|a Article
|
| 773 |
|
|
|t Langmuir
|
