Structural analysis of carbonaceous solids using an adapted reverse Monte Carlo algorithm

Carbon ◽  
2003 ◽  
Vol 41 (12) ◽  
pp. 2403-2411 ◽  
Author(s):  
Tim Petersen ◽  
Irene Yarovsky ◽  
Ian Snook ◽  
Dougal G McCulloch ◽  
George Opletal
2005 ◽  
Vol 17 (17) ◽  
pp. 2605-2616 ◽  
Author(s):  
G Opletal ◽  
T C Petersen ◽  
D G McCulloch ◽  
I K Snook ◽  
I Yarovsky

2005 ◽  
Vol 44 (6A) ◽  
pp. 3808-3812 ◽  
Author(s):  
Norikazu Tabuchi ◽  
Toshio Kawahara ◽  
Takashi Arai ◽  
Jun Morimoto ◽  
Hideki Matsumura

1997 ◽  
Vol 11 (24) ◽  
pp. 1047-1055 ◽  
Author(s):  
M. Andrecut

A simple Reverse Monte Carlo algorithm for structure simulations of multi-component amorphous solids is presented. The described algorithm is based on the standard reverse Monte Carlo method,1,2 developed for the monoatomic case, the application for poliatomic case being assured by using the Warren–Krutter–Morningstar approximation.3 An application for metal-metalloid glasses is also presented.


2018 ◽  
Vol 495 ◽  
pp. 27-34 ◽  
Author(s):  
Atul Khanna ◽  
Margit Fábián ◽  
Hirdesh ◽  
P.S.R. Krishna ◽  
Christopher J. Benmore ◽  
...  

1996 ◽  
Vol 29 (3) ◽  
pp. 285-290 ◽  
Author(s):  
W. Montfrooij ◽  
R. L. McGreevy ◽  
R. Hadfield ◽  
N. H. Andersen

A Monte Carlo algorithm for the analysis of powder diffraction patterns is presented. One aim of this algorithm, which can be used as a supplement to the regular Rietveld refinement, is to provide a self-consistent determination of the thermal displacements of the atoms. This is achieved by modelling the total scattered intensity, comprising both the Bragg peak intensity and the diffuse contribution to the spectrum from the scattering density of an assembly of atoms. This assembly, which is constructed by the reverse Monte Carlo technique so as to yield a best fit with the data, is then used to calculate the average atomic thermal displacements. This allows for a refinement that, in principle, no longer requires angle-dependent background parameters, and that is well suited for dealing with highly anisotropic Debye–Waller factors and split atomic sites.


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