21st Biennial Conference of the APS Topical Group on Shock Compression of Condensed Matter
Volume 64, Number 8
Sunday–Friday, June 16–21, 2019;
Portland, Oregon
Session J6: TMS: First-principles and Molecular Dynamics III
11:00 AM–12:30 PM,
Tuesday, June 18, 2019
Room: Broadway III/IV
Chair: Brian Barnes, ARL
Abstract: J6.00001 : Machine Learning Reactive Force Fields for an Atomistically-Resolved View into Shockwave-Driven Carbon Condensation
11:00 AM–11:30 AM
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Abstract
Author:
Rebecca Lindsey
(Lawrence Livermore Natl Lab)
In this work, we discuss development and application of the Chebyshev
Interaction Model for Efficient Simulations (ChIMES) to the problem of
carbon condensation. Formation of soot particles resulting from strong
shockwave propagation in carbon-rich energetic materials can have
significant implications on material performance and sensitivity. However,
the time and length scales associated with condensate growth (i.e. up to
hundreds of ns and 10's of nm, respectively) make direct investigation
highly challenging. From an experimental standpoint, these scales preclude
formation tracking, leading to what appears to be instantaneous condensate
growth, while for highly predictive quantum-based simulation methods, these
scales are prohibitively large.
Reactive force field-based approaches, capable of multi-million atom
simulations, offer a viable alternative means of studying carbon
condensation. To this effect, we discuss development of the Chebyshev
Interaction Model for Efficient Simulation (ChIMES), a generalized many-body
reactive force field machine-learned to Kohn-Sham Density Functional Theory
(DFT) molecular dynamics trajectories. ChIMES models are linear-scaling with
respect to system size and are thus highly suitable for large-scale problems
requiring atomistic resolution. Strategies for achieving
``quantum-accurate'' descriptions of chemistry in complicated molecular
systems are discussed and broad insights stemming from application to carbon
condensation in liquid carbon monoxide under extreme conditions are
presented. Our results indicate possible mechanisms, timescales, and
chemistry for the ensuing condensate products.
In collaboration with: L.E. Fried, N. Goldman, S. Bastea and M.R. Armstrong
This work is performed under the auspices of the U.S. Department of Energy
by Lawrence Livermore National Laboratory under Contract DE-AC52-07NA27344.
LLNL-ABS-768127