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EOS of simple Solids for wide Ranges in p and T. Problem: The accuracy of “primary” K(V)-scales is still seriously limited by the present range and precision in measurements of K and V under high p and T. Solution: Semi-empirical EOS with theoretical and experimental input provide - PowerPoint PPT Presentation
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EOS of simple Solids for wide Ranges in p and T
Washington 2007
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
Problem:The accuracy of “primary” K(V)-scales is still seriously limited by the present range and precision in measurements of K and V under high p and T.
Solution:Semi-empirical EOS with theoretical and experimental input provide p(V,T)-relations of many “simple” materials for the determination of p with higher accuracy from measurements of V and T.Comparison of different markers gives estimates of the accuracy!
EOS of simple Solids for wide Ranges in p and T
Washington 2007
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
EOS of “simple” or “regular” solids are well understood theoretically!
All thermo-physical data including the EOS must be modeled by the same thermodynamic potential (the same Gibbs function).
“Cold” (0 K) isotherms can be determined from a priory theoryor from semi-empirical effective potential forms (APL).
Thermal contributions are accurately modeled by thermodynamicswith experimental input from ambient pressure and theoreticalsupport for the volume dependence of the intrinsic anharmonicity.
EOS of simple Solids for wide Ranges in p and T
Washington 2007
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
The approach:
1) Set up a thermodynamic model for the solid with anharmonicity!2) Use Kr and Kr’ values from ultrasonic or Brillouin measurements for one (cold) reference isotherm!3) Use ambient pressure data of Vo(T), αo(T),Cpo(T) and Ko(T) to determine thermo-physical parameters (θo, γo, ...) of the model!4) Refine Kr’ as best fitting Ko(T)!
EOS of simple Solids for wide Ranges in p and T
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
The thermo-physical model for the Gibbs function: Total Free-Energy: F(V,T) = Ec(V) + Fth (V,T) with Ground State Energy Ec(V) and thermal Excitations in Fth(V,T)
Ec(V) from one cold isotherm: pc(V) = pAP2(V,Z,Vo,Ko,K’o)
Fth(V,T) = Fcond.el.(T,TFG(V)) + Fquasi-harm.phonon(V,T) + Fintr.anharm.(V,T)
Quasi-harmonic Phonons are modeled with an optimized pseudo-Debye-Einstein approximation: opDE, Intrinsic Anharmonicity with a Modified Mean Field approach: MMF
Washington 2007
Effective potential forms for cold isotherm
Washington 2007
Mie EOS (Mi3)
Effective Rydberg EOS (ER2)
Adapted Polynomial EOS (AP2)
Thomas-Fermi-limit is modeled by co!
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
m nMi3 0p (3/ n) K x (1 x )
ER 2 0 ER 22
1 xp 3 K exp(c (1 x))
x
ER 2 0c (3/ 2)(K 1)
AP2 0 0 25
1 xp 3 K exp(c (1 x)) 1 c x (1 x)
x
5 / 3FG0 FG 0p a (Z / V ) 0 0 FG0c ln(3 K / p ) 5
FGa 0.02337GPa nm
2 0 0c (3 / 2) (K 3) c
1/ 30x (V / V )
An optimized pseudo-Debye-Einstein model
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
Cold Isotherm:
The Mie-Grüneisen approach for the internal energy gives :
with
An optimized pseudo-Debye-Einstein model for quasi-harmonic phonons
with g=0.068 a=0.0434
and
is conveniently used here!
4
3( ) (1 )
exp( / ) 1E
opDEE
t fu t g g
a g t f t
30
0
3( )
4 (1 )Dh
ED
f gg
( , ) 3 ( ) ( )MG DU V T R V u t / ( )Dt T V
Washington 2007
Intrinsic AnharmonicityClassical Free Volume Approach with Modified Mean Field Potential g(r,V)
J.G. Kirkwood, J. Chem. Phys. 18, 380 (1950) Y. Wang, Phys. Rev. B 61, R11863 (2000)
Prag 2006
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
( , ) ( ) ( ) 2 ( ) ( ) ( )2 C C C C C
b s f rg r V E R r E R r E R E R r E R r
R
w i t h c o r r e l a t i o n p a r a m e t e r :
2,( , ) 4 e x p
B
g r Vv f V T r d r
k T
3
0 0( ) /R V R V V f o r f c c : 6 3
0 02R V
2
3( , ) l n l n ( , )
2 2B
v i b B
m k TF V T N k T v f V T
l n ( , )( , )
l nB
v i b
N k T v f V Tp V T
V V
( , ) 3 l n ( , )( , )
2 l nv i b
v i b B
F V T v f V TS V T N k
T T
3 l n ( , )( , ) ( , ) ( , )
2 l nv i b v i b v i b B
v f V TU V T F V T T S V T N k T
T
2
2
3 l n ( , ) l n ( , )( , )
2 l n ( l n )v i b B
v f V T v f V TC V T N k
T T
Intrinsic AnharmonicityClassical Free Volume Approach with Modified Mean Field Potential g(r,V)
J.G. Kirkwood, J. Chem. Phys. 18, 380 (1950) Y. Wang, Phys. Rev. B 61, R11863 (2000)
Prag 2006
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
l n ( , ) / l n
( 3 / 2 ) l n ( , ) / l n( , ) v i b
b a r i cv i b
p V v f V T V
U v f V T TV T
( , ) v Tt h e r m a l
V
K VV T
C
2
2 2
l n ( , ) / l n l n ( , ) / ( l n l n )( , )
( 3 / 2 ) l n ( , ) / l n l n ( , ) / ( l n )t h e r m a l
v f V T V v f V T V TV T
v f V T T v f V T T
Intrinsic Anharmonicity Two Series Expansions in the Classical Free Volume Approach
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
( , ) ( ) ( ) 2 ( ) ( ) ( )2 C C C C C
b s f rg r V E R r E R r E R E R r E R r
R
1 ) 2 4 62 ( ) 4 ( )
( , ) ( )2 ! 4 !
k V k Vg r V r r O r
22
( )2 ( ) Cb s f E R
k V RR R R
34
4 3
( )4 ( ) Cb s f E R
k V RR R R
2,( , ) 4 e x p
B
g r Vv f V T r d r
k T
4 2 ( )( )
3M P FB
k VV
k b s f m
2 )
4 224 ( ) 2 ( )
( , ) 4 1 e x p4 ! 2 !B B
k V r k V rv f V T r d r
k T k T
3 / 2
2 22( , ) 1 3 ( ) 6 . 3 ( )
2 ( )B
v f v f
k Tv f V T a V T a V T
k V
2
5 4 ( )( )
2 4 2 ( )B
v f
k k Va V
k V
2 2
0 03
0 0 0 0
2
4D D B
M P F
k mb s f
K K V
Washington 2007
Vibrational Free-Energy in the Classical Free-Volume Approachwith linear contributions from and only.
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
vfa avf
3 / 2
2( , ) 1 3 ( )
2 ( )B
v f
k Tv f V T a V T
k V
1 2 ( )( , ) 3 l n l n ( )
2B
v i b B v f
k T k VF V T N k T a V T
m
( , ) 3 1 ( )v i b B v fU V T N k T a V T
3( , ) ( ) ( ) ( )B
v i b v i b v f a v f
N k Tp V T V a V V T
V ( , ) 3 1 2 ( )V B v fC V T N k a V T
ln ( )( )
lnvf
avf
a VV
V
ln ( ) 1 ln 2( )
( )ln 2 ln
V k VV
V VDvib
0 0( ) 2( ) / 2( )D DV k V k V
( , ) ( ) (1 )V T V Tbar vib A
( , ) ( ) (1 2 )V T V Tthm vib A
( ) (1 ( ) / ( ))A vf avf viba V V V
0A Mie-Grüneisen Approximation implies
Washington 2007
Vibrational Grüneisen Parameterin the classical free volume approach
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
A c o n s t a n t c o r r e l a t i o n p a r a m e t e r
/ 0d d V i n t h e M M F - p o t e n t i a l
( , ) ( ) ( ) 2 ( ) ( ) ( )2 C C C C C
b s f rg r V E R r E R r E R E R r E R r
R
r e s u l t s i n 22
( )2 ( ) Cb s f E R
k V RR R R
a n d
( ) ( 2 / 3 ) ( 1 ) 1( )
2 ( 1 ( 2 / 3 ) ( 1 ) ( ( ) / ( ) ) 6C
v i bC C
K VV
p V K V
V a s h c h e n k o - Z u b a r e v ( 1 9 6 3 ) , B a r t o n - S t a c e y ( 1 9 8 5 )
Washington 2007
A c o n s t a n t c o r r e l a t i o n p a r a m e t e r
/ 0d d V i n t h e M M F - p o t e n t i a l
( , ) ( ) ( ) 2 ( ) ( ) ( )2 C C C C C
b s f rg r V E R r E R r E R E R r E R r
R
r e s u l t s i n 22
( )2 ( ) Cb s f E R
k V RR R R
a n d
( ) ( 2 / 3 ) ( 1 ) 1( )
2 ( 1 ( 2 / 3 ) ( 1 ) ( ( ) / ( ) ) 6C
v i bC C
K VV
p V K V
V a s h c h e n k o - Z u b a r e v ( 1 9 6 3 ) , B a r t o n - S t a c e y ( 1 9 8 5 )
A c o n s t a n t c o r r e l a t i o n p a r a m e t e r
/ 0d d V i n t h e M M F - p o t e n t i a l
( , ) ( ) ( ) 2 ( ) ( ) ( )2 C C C C C
b s f rg r V E R r E R r E R E R r E R r
R
r e s u l t s i n 22
( )2 ( ) Cb s f E R
k V RR R R
a n d
( ) ( 2 / 3 ) ( 1 ) 1( )
2 ( 1 ( 2 / 3 ) ( 1 ) ( ( ) / ( ) ) 6C
v i bC C
K VV
p V K V
V a s h c h e n k o - Z u b a r e v ( 1 9 6 3 ) , B a r t o n - S t a c e y ( 1 9 8 5 )
A c o n s t a n t c o r r e l a t i o n p a r a m e t e r
/ 0d d V i n t h e M M F - p o t e n t i a l
( , ) ( ) ( ) 2 ( ) ( ) ( )2 C C C C C
b s f rg r V E R r E R r E R E R r E R r
R
r e s u l t s i n 22
( )2 ( ) Cb s f E R
k V RR R R
a n d
( ) ( 2 / 3 ) ( 1 ) 1( )
2 ( 1 ( 2 / 3 ) ( 1 ) ( ( ) / ( ) ) 6C
v i bC C
K VV
p V K V
V a s h c h e n k o - Z u b a r e v ( 1 9 6 3 ) , B a r t o n - S t a c e y ( 1 9 8 5 )
Higher Order Corrections in the Free Volume Approach
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
2_ 1 . _ 3c l a s s i c o r d e r a n h a r m o n i c i t y v fF R a T
Q u a n t u m c o r r e c t i o n s + h i g h e r o r d e r :
2( ) ( )3 4 ( ) ( 1 6 )T T
a n h v f D q h v f D q hD D
F R f a u f a u
w i t h q u a s i - h a r m o n i c o p t i m i z e d p s e u d o - D e b y e - E i n s t e i n u q h
q u a r t i c c o r r e c t i o n f a c t o r f 4
a n d h e x i c c o r r e c t i o n f a c t o r f 6
Washington 2007
Heat capacity of Cu at ambient pressure
Prag 2006
Experimental data +, o, x and • from Ly59, Ma60, Gr72 and Ch98
Present fit of Cpo and Cvo: solid and dashed line
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
0 200 400 600 800 1000 12000
0.5
1cpo T( )
cvo T( )
cp1 nc1
cp2 nc2
cp3 nc3
cp4 nc4
T T Tc1 nc1 Tc2 nc2 Tc3 nc3 Tc4 nc4
Cpo(T) 3R
T (K)
Heat capacity of Ag at ambient pressure
Experimental data o, x and • from Mo36, MF41, and Gr72
Present fit of Cpo and Cvo: solid and dashed line
0 200 400 600 800 1000 12000
0.5
1cpo T( )
cvo T( )
cp1 nc1
cp2 nc2
cp3 nc3
T T Tc1 nc1 Tc2 nc2 Tc3 nc3
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
Cpo(T) 3R
T (K)
Heat capacity of Au at ambient pressure
Experimental data x and • from GG52, and Gr72
Present fit of Cpo and Cvo: solid and dashed line
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
0 200 400 600 800 1000 12000
0.5
1cpo T( )
cvo T( )
cp1 nc1
cp2 nc2
cp3 nc3
T T Tc1 nc1 Tc2 nc2 Tc3 nc3 T (K)
Cpo(T) 3R
Vo(T) Vr
T (K)
Vo(T) Vr
x 10000
0 200 400 600 800 1000 12001.5
1
0.5
0
0.5
1
1.5
10 rvnv
D T( )
Tv nv T
0 200 400 600 800 1000 1200
1
1.02
1.04
1.06
vxnv
v0T T( )
Tv nv T
_
Relative atomic volume of Cu at ambient pressure
Experimental data • from TK75 and present fit as solid line
0 200 400 600 800 1000 1200
0 200 400 600 800 1000 1200
1
1.02
1.04
1.06
vxnv
v0T T( )
Tv nv T
0 200 400 600 800 1000 12001.5
1
0.5
0
0.5
1
1.5
10 rvnv
D T( )
Tv nv T
Vo(T) Vr
T (K)
Relative atomic volume of Ag at ambient pressure
Experimental data • from TK75 and present fit as solid line
0 200 400 600 800 1000 1200
Vo(T) Vr
x 10000
0 200 400 600 800 1000 1200
1
1.02
1.04
vxnv
v0T T( )
Tv nv T
0 200 400 600 800 1000 12001.5
1
0.5
0
0.5
1
1.5
10 rvnv
D T( )
Tv nv TT (K)
Relative atomic volume of Au at ambient pressure
Experimental data • from TK75 and present fit as solid line
Vo(T) Vr
x 10000
Vo(T) Vr
0 200 400 600 800 1000 1200
Ko(T) (GPa)
T (K)
0 200 400 600 800 1000 1200
100
120
140
KoT1 nK1
KoT2 nK2
K0a T( )
Koo T( )
TK1 nK1 TK2 nK2 T
Isothermal bulk modulus of Cu at ambient pressure
Experimental data o from CH66 and • from VT79
Present fit with and without anharmonic contributions: solid and dashed line
Isothermal bulk modulus of Ag at ambient pressure
Experimental data • from CH66 and o from BV81
Present fit with and without anharmonic contributions: solid and dashed line
0 200 400 600 800 1000 1200
80
100KoT1 nK1
KoT2 nK2
K0a T( )
Koo T( )
TK1 nK1 TK2 nK2 T
Ko(T) (GPa)
T (K)
0 200 400 600 800 1000 1200
120
140
160
180
KoT1 nK1
KoT2 nK2
K0a T( )
Koo T( )
TK1 nK1 TK2 nK2 TT (K)
Ko(T) (GPa)
Isothermal bulk modulus of Au at ambient pressure
Experimental data • BV81 and o from CH66
Present fit with and without anharmonic contributions: solid and dashed line
0 200 400 600 800 1000 12005
5.5
6
6.5
Ksotot T( )
KosT1 nK1
KosT31
T TK1 nK1 KosT30
Pressure derivative of the isothermal bulk modulus
for Cu at ambient pressure
Temperature dependent data • from VT79 with additional data for 300 K.
Present fit with anharmonic contributions: solid line
T (K)
K´o(T)
0 200 400 600 800 1000 12005.5
6
6.5
7
7.5
8
Ksotot T( )
KosT1 nK2
KosT31
T TK2 nK2 KosT30
Pressure derivative of the isothermal bulk modulus
for Ag at ambient pressure
Temperature dependent data • from BV81 with additional data for 300 K.
Present fit with anharmonic contributions: solid line
T (K)
K´o(T)
T 5 105 1305
0 200 400 600 800 1000 12005.5
6
6.5
7
7.5
Ksotot T( )
KosT1 nK1
KosT31
T TK1 nK1 KosT30
Pressure derivative of the isothermal bulk modulus
for Au at ambient pressure
Temperature dependent data • from BV81 with additional data for 300 K.
Present fit with anharmonic contributions: solid line
T (K)
K´o(T)
Hierarchy of Parameters in the Refinements
1. Fit of Cpo(T) at low T by Refinement of TDo and TDh
2. Fit of Vo(T) at low T by Refinement of r
3. Fit of Cpo(T) and Vo(T) at higher T by Refinement of Anharmonicity Parameters f4 and f6
4. Minor Refinement of K’r to improve Fit of Ko(T)
5. Final Check of Step 2. and 3.
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
Vr(cnm)
Kr(GPa)
TDo(K)
K’r
TDh(K)
r
f6
1000xAph
f4
A
TFeff(K)
Z
M
f2
q
AgCu Au29 47 7964 108 197
57213 62220 5562611,814 17,056 16,964133,1 101,0 166,45,40 6,20 6,21330 214 160328 223 183
2,00 2,46 3,112,11 3,07 3,878,00 0,80 1,580,36 0,34 0,290,60 0,72 -1,310,30 0,48 0,671,03 1,48 2,27
-2,87 -3,94 -5,45
Thermo-physical Parameters for
Discussion
1. Perfect representation of all thermo-physical data at ambient P(for “regular” Solids only!)
2. Uncertainties in (V) and Aph(V) are reduced by MMF-calculation(No experimental data give better constraints!)
3. Reliable basis for the calculation of thermo-physical data at any P
4. Perfect agreement with Shock Wave Data
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
Comment on Parametric EOS
If the cold isotherm pc(V) is represented by pAP2(V,Vo,Ko,K’o)
(or by any other second order parametric EOS)
no other isotherm is perfectly represented by the same formeven with best fitted “effective values” for Vr, Kr, K’r
deviating from the thermodynamic values!
Accurate representations of the present thermodynamic EOS by parametric EOS
need higher order forms with “effective” parameters!
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
PPT2 5 C3
2 PPT
5 5 C35
PPT8 5 C3
8
R3 v tf( ) r3 v tf C3tf
0 100 200 300 400 500 600
0.01
0.005
0
0.005
0.01
R3 v 10( )
N v( )
R3 v 5( )
R3 v 0( )
pAP3 xv v( )( )
Difference between thermodynamic and parametric EOS for Cu a) pAP2 b) pAP3
0 100 200 300 400 500 600
0.01
0.005
0
0.005
0.01
Reff v 10( )
N v( )
Reff v 5( )
Reff v 0( )
r500 v( )
pAP3 xv v( )( )
0 100 200 300 400 500 600
0.01
0.005
0
0.005
0.01.011
.011
rT v 10( )
N v( )
rT v 5( )
rT v 0( )
60010 pAP3 xv v( )( )
p
p
p
p
p / GPa
c) pAP2 + pAP3with data point from HHS-01 for 500K
p / GPa
0 K
500 K HHS 01: 500 K1000 K
0 K
500 K 1000 K
0 K
500 K
1000 K
0 100 200 300 400 500 600
0.01
0.005
0
0.005
0.01
rT v 10( )
N v( )
rT v 5( )
rT v 0( )
pAP3 xv v( )( )
0 100 200 300 400 500 600
0.015
0.01
0.005
0
0.005
Reff v 10( )
N v( )
Reff v 5( )
Reff v 0( )
r500 v( )
pAP3 xv v( )( )
0 100 200 300 400 500 600
0.01
0.005
0
0.005
0.01
rT v 10( )
N v( )
rT v 5( )
rT v 0( )
pAP3 xv v( )( )
0 100 200 300 400 500 600
0.015
0.01
0.005
0
0.005
Reff v 10( )
N v( )
Reff v 5( )
Reff v 0( )
r500 v( )
pAP3 xv v( )( )
0 100 200 300 400 500 600
0.015
0.01
0.005
0
0.005
Reff v 10( )
N v( )
Reff v 5( )
Reff v 0( )
r500 v( )
pAP3 xv v( )( )
p
p
p / GPap / GPa
Differences between thermodynamic and parametric EOS using pAP2+pAP3 for Ag and Au
Data from HHS 01 for 500K are given for comparison
0 K
500 K
1000 K
HHS 01: 500 K
0 K
500 K
1000 K
HHS 01: 500 K
0 11,695 141,7 5,25 5,29 0,45100 11,711 140,2 5,29 5,32 0,30200 11,758 136,8 5,34 5,36 0,15300 11,814 133,1 5,40 5,40 -0,01400 11,875 129,4 5,46 5,44 -0,19500 11,938 125,6 5,52 5,49 -0,40600 12,005 121,7 5,60 5,54 -0,63700 12,074 117,8 5,67 5,59 -0,89800 12,146 113,8 5,76 5,64 -1,19900 12,222 109,7 5,86 5,71 -1,55
1000 12,301 105,5 5,98 5,77 -1,97
Reference data for the parametric EOS of Cu
T Vr Kr K’r K’reff c33 310 nmK GPa
Reference data for parametric EOS of Ag
T Vr Kr K’r K’reff c33 310 nmK GPa
0 16,841 110,68 5,92 6,01 0,88100 16,879 108,56 6,00 6,06 0,58200 16,963 104,89 6,10 6,12 0,27300 17,056 101,11 6,20 6,19 -0,06400 17,156 97,28 6,31 6,27 -0,40500 17,260 93,41 6,42 6,35 -0,76600 17,369 89,51 6,55 6,43 -1,11700 17,484 85,58 6,67 6,52 -1,48800 17,604 81,63 6,81 6,62 -1,84900 17,731 77,64 6,95 6,72 -2,20
1000 17,864 73,64 7,11 6,83 -2,55
Reference data for parametric EOS of Au
T Vr Kr K’r K’reff c33 310 nmK GPa
0 16,791 180,6 5,89 6,00 1,52100 16,825 177,2 5,98 6,06 0,97200 16,892 172,0 6,10 6,13 0,39300 16,964 166,7 6,21 6,20 -0,17400 17,040 161,5 6,33 6,27 -0,72500 17,118 156,3 6,44 6,34 -1,24600 17,198 151,1 6,56 6,42 -1,75700 17,281 145,8 6,68 6,49 -2,26800 17,367 140,7 6,81 6,57 -2,79900 17,456 135,5 6,95 6,66 -3,38
1000 17,548 130,2 7,11 6,75 -4,11
EOS for Solids with Mean-Field Anharmonicity
Prag 2006
Software and Supportavailable on Request!
Cooperation welcome!
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
[WR57] J.M. Walsh, M.H. Rice, R.G. McQueen, and F.L. Yarger, Phys. Rev. 108 196 (1957)
[KK72] R.N. Keeler, and G.C. Kennedy, American Institut of Physics Handbook, 4938, ed. D.E. Gray, New York: McGraw Hill (1972)
[MB78] H.K. Mao, P.M. Bell, J.W. Shaner, and D.J. Steinberg, J. Appl. Phys. 49 3276 (1978)
[AM85] R.C.Albers, A.K. McMahan, and J.E. Miller, Phys. Rev. B31 3435 (1985)
[AB87] L.V. Al'tshuler, S.E. Brusnikin, and E.A. Kuz'menkov, J. Appl. Mech. and Tech. Phys. 28 129 (1987)
[NM88] W.J. Nellis, J.A. Moriarty, A.C. Mitchell, M. Ross, R.G. Dandrea, N.W. Ashcroft, N.C. Holmes, and G.R. Gathers,Phys. Rev. Lett. 60, 1414 (1988)
[Mo95] J.A. Moriarty, High Pressure Res. 13 343 (1995)
[WC000] Yi Wang, Dongquan Chen, and Xinwei Zhang, Phys. Rev. Lett. 84 3220-3223 (2000)
SESAME (provided by D.Young with permission)
Comparison of EOS data for Cu
0 100 200 300 400 500 600-0.15
-0.10
-0.05
-0.00
0.05
0.10
0.15Cup/p
p(GPa)
W R 5 7K K 72M B 78
A M 85A B 87N M 8 8
S E S A M E
W C 0 00
M o 95
1 .1sc
0 .9 sc
0 .15K
0 .15K
Relative deviations of different EOS data for Cu at 300 K with respect to an AP2 form using Ko=132.2 GPa and K’o=5.40 used by HH2002
Comparison of EOS data for Ag
WR57KK72
MB78AB87
[WR57] J.M. Walsh, M.H. Rice, R.G. McQueen, and F.L. Yarger, Phys. Rev. 108 196 (1957)
[KK72] R.N. Keeler, and G.C. Kennedy, American Institut of Physics Handbook, 4938, ed. D.E. Gray, New York: McGraw Hill (1972)
[MB78] H.K. Mao, P.M. Bell, J.W. Shaner, and D.J. Steinberg, J. Appl. Phys. 49 3276 (1978)
[AB87] L.V. Al'tshuler, S.E. Brusnikin, and E.A. Kuz'menkov, J. Appl. Mech. and Tech. Phys. 28 129 (1987)
0 100 200 300 400 500 600p(GPa)
-0.15
-0.10
-0.05
-0.00
0.05
0.10
0.15p/p Ag
sc0.9.15K '
0
.15K '0
sc1.1
Relative deviations of different EOS data for Ag at 300 K with respect to an AP2 form using Ko=101.1 GPa and K’o=6.15 used by HH2002
Comparison of EOS data for Au
KK7 2JF82
AB87GN92
AI8 9
[KK72] R.N. Keeler, and G.C. Kennedy, American Institut of Physics Handbook, 4938, ed. D.E. Gray, New York: McGraw Hill (1972)
[JF82] J.C. Jamieson, J.N. Fritz, and M.H. Manghnani in: High Pressure Research in Geophysics, ed. S. Akimoto, M.H. Manghnani Center for Acad. Public., Tokyo (1992)
[AB87] L.V. Al'tshuler, S.E. Brusnikin, and E.A. Kuz'menkov, J. Appl. Mech. and Tech. Phys. 28 129 (1987)
[GN92] B.K. Godwal, A.Ng, R. Jeanloz, High Pressure Res. 10 7501 (1992)
[AI89] O.L. Anderson, D.G. Isaak, S. Yamamoto, J. Appl. Phys. 65 1534 (1989)
.15K '0
0 100 200 300 400 500 600p(GPa)
-0.15
-0.10
-0.05
-0.00
0.05
0.10
0.15p/p Au
sc 0.9
sc1.1
5.1K '0
Relative deviations of different EOS data for Au at 300 K with respect to an AP2 form using Ko=166.7 GPa and K’o=6.20 used by HH2002
-0,2
-0,1
0,0
0,1
0,2
0 100 200 300 400 500 600
p(GPa)
pp
AP2JF82AI89HJ84MoDE2
Au
Relative deviations of different EOS data for Au at 1000 K with respect to the MoDE2 modelused by HH2002. Deviations with respect to their effective AP2 form are shown by the thin line.
EOS parameters for diamond from different fitsof theoretical E(V)-data with a fixed best value for Vor
Washington 2007
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
The approach:
1) Set up a thermodynamic model for the solid with anharmonicity!2) Use Kr and Kr’ values from ultrasonic or Brillouin measurements for one (cold) reference isotherm!3) Use ambient pressure data of Vo(T), αo(T),Cpo(T) and Ko(T) to determine thermo-physical parameters (θo, γo, ...) of the model!4) Refine Kr’ as best fitting Ko(T)!
Ko (GPa) K'o STD
AP3 433,17 3,69 0,003BE3 439,35 3,56 0,017AP2 443,34 3,50 0,032H02 444,21 3,45 0,036BE2 432,81 3,64 0,050ER2 419,77 3,92 0,087
EOS of simple Solids for wide Ranges in p and T
Washington 2007
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
The approach:
1) Set up a thermodynamic model for the solid with anharmonicity!2) Use Kr and Kr’ values from ultrasonic or Brillouin measurements for one (cold) reference isotherm!3) Use ambient pressure data of Vo(T), αo(T),Cpo(T) and Ko(T) to determine thermo-physical parameters (θo, γo, ...) of the model!4) Refine Kr’ as best fitting Ko(T)!
Fit of Ko(T) for Diamond
Washington 2007
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
The approach:
1) Set up a thermodynamic model for the solid with anharmonicity!2) Use Kr and Kr’ values from ultrasonic or Brillouin measurements for one (cold) reference isotherm!3) Use ambient pressure data of Vo(T), αo(T),Cpo(T) and Ko(T) to determine thermo-physical parameters (θo, γo, ...) of the model!4) Refine Kr’ as best fitting Ko(T)!
0 1000 2000 3000 4000
350
400
450K0R TK1 m Koo T( )
K0a T( )
K0qh T( )
K0S TK1 m K0L TK1 m K0R TK1 m K0H TK1 m
TK1 m T T T TK1 m TK1 m
SK1
0
nK1m 1
m
K0a TK1m K0R TK1
m 2
Fit of Ko(T) for Diamond
Washington 2007
Wilfried B. Holzapfel Department Physik Universität-Paderborn Germany <[email protected]>
The approach:
1) Set up a thermodynamic model for the solid with anharmonicity!2) Use Kr and Kr’ values from ultrasonic or Brillouin measurements for one (cold) reference isotherm!3) Use ambient pressure data of Vo(T), αo(T),Cpo(T) and Ko(T) to determine thermo-physical parameters (θo, γo, ...) of the model!4) Refine Kr’ as best fitting Ko(T)!
0 1000 2000 3000 4000
350
400
450K0R TK1 m Koo T( )
K0a T( )
K0qh T( )
K0S TK1 m K0L TK1 m K0R TK1 m K0H TK1 m
TK1 m T T T TK1 m TK1 m
SK1
0
nK1m 1
m
K0a TK1m K0R TK1
m 2