z-logo
open-access-imgOpen Access
GPU-accelerated discrete element modeling of geological faults
Author(s) -
Vadim Lisitsa,
V. Tchebverda,
V. Volianskaia
Publication year - 2019
Publication title -
journal of physics. conference series
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.21
H-Index - 85
eISSN - 1742-6596
pISSN - 1742-6588
DOI - 10.1088/1742-6596/1392/1/012070
Subject(s) - discrete element method , classification of discontinuities , element (criminal law) , computer science , algorithm , computational science , point (geometry) , parallel computing , geometry , mathematics , mechanics , physics , mathematical analysis , political science , law
In this paper, we present an original algorithm for the numerical simulation of tectonic movements and the related formation of geological faults. The approach is based on the use of Discrete Element Method, where the geological media is represented as an agglomeration of discrete particles which interact as elastic, visco-elastic, or elasto-plastic bodies. This approach naturally allows accounting for large deformations and discontinuities in the geological media; thus, allows simulation of faults formation. Implementation of the algorithm is based on the use of Graphical Processor Units. The Discrete Element Method requires a high number of floating point operations and logical operations per a single particle (degree of freedom) per time step; whereas the number of memory access operations is relatively low. Thus, the use of GPUs decreases the computational time substantially.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here