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2012 Summer School on Computational Materials Science Quantum Monte Carlo: Theory and Fundamentals July 23–-27, 2012 • University of Illinois at Urbana–Champaign http://www.mcc.uiuc.edu/summerschool/2012/ Equations of State Ronald Cohen Geophysical Laboratory Carnegie Institution of Washington [email protected] 2012 Summer School on Computational Materials Science Quantum Monte Carlo: Theory and Fundamentals July 23–-27, 2012 • University of Illinois at Urbana–Champaign http://www.mcc.uiuc.edu/summerschool/2012/ QMC Summer School 2012 UIUC
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Equations of State Ronald Cohen Geophysical Laboratory Carnegie Institution of Washington

Feb 23, 2016

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2012 Summer School on Computational Materials Science Quantum Monte Carlo: Theory and Fundamentals July 23–-27, 2012 • University of Illinois at Urbana–Champaign http://www.mcc.uiuc.edu /summerschool/ 2012/. Equations of State Ronald Cohen Geophysical Laboratory - PowerPoint PPT Presentation
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Page 1: Equations of State Ronald Cohen Geophysical Laboratory Carnegie Institution of Washington

Equations of StateRonald Cohen

Geophysical LaboratoryCarnegie Institution of Washington

[email protected]

2012 Summer School on Computational Materials Science Quantum Monte Carlo: Theory and FundamentalsJuly 23–-27, 2012 • University of Illinois at Urbana–Champaignhttp://www.mcc.uiuc.edu/summerschool/2012/

QMC Summer School 2012 UIUC

Page 2: Equations of State Ronald Cohen Geophysical Laboratory Carnegie Institution of Washington

Need for Equations of State

• QMC gives us the energy at a set of points for different structures and volumes

• To predict phase stability and to compare with experiment we need the pressure

• The most stable phase has the lowest free energy, or at zero temperature, the lowest enthapy.

• The relationship among E, V, P, and T is the equation of state.

• Also enthalpy H=E+PV and free energy G=H-TS

CohenQMC Summer School 2012 UIUC 2

Cohen, R. E. & Gulseren, O. Thermal equation of state of tantalum. Phys. Rev. B 63, 224101-224111 (2000).

Ta Thermal equation of state

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Pressure vs. volumeTa isotherms

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Residuals for T=0 isotherm:Evidence for electronic transition

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Ta bands and DOS

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V=12.66 Å3 (5 GPa)

V=9.3 Å3 (460 GPa)

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Vinet parameters vs. temperature

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Thermal pressure vs. V

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Thermal pressure vs. T

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Average Thermal Pressure

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QMC Summer School 2012 UIUC

Simple Equation of State for Ta

• P (GPa) = P0K+Pth • P0K is Vinet equation:• x=(V/V0)1/3• P=3 K0 (1-x) exp (3/2 (K0’-1) (1-x))/x2• with V0=123.632 K0=190.95 K0'=3.98 • Pth = 0.00441 T• This should be good to better than ±5 GPa to 9000 K and for V>80 bohr3

(35% compression).

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Page 12: Equations of State Ronald Cohen Geophysical Laboratory Carnegie Institution of Washington

QMC Summer School 2012 UIUC

An accurate high temperature global equation of state

• T=0 Vinet isotherm• V dependent Thermal Pressure• Heat Capacity

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3

112

10922

82

72

65

20

21

00

0

31

0

0

1123exp3135

12

14

GPa)in K and Rydin E(for 75614710

T+PTT+P)+PxTx+PT+PTT+P=V(PE

)))(x-(K'-(-x))-K'(x-+)()(K'-kV-(

K'-kP+=eE

./k=K

VVx

+EE=E

th

th

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Global free energy fit

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cBN Raman Frequencies

• Within harmonic approx. DFT frequency is reasonable

• But, cBN Raman mode is quite anharmonic

• With anharmonic corrections, DFT frequencies are not so good.

• Compute energy vs. displacement with DMC and do 4th-order fit. Solve 1D Schrodinger eq. to get frequency

• Anharmonic DMC frequency is correct to within statistical error

Cohen QMC Summer School 2012 UIUC 19

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Summary

• Fit your DFT and QMC results to equations of state, carefully.

• Much can be learned from the equation of state, and the parameterizations are very useful, particularly for comparing with experiments or input to other studies.

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