Betül Pamuk
Phil Allen
Marivi Fernández-Serra
Stony Brook University
Computational Condensed Matter Group
DOE Early Career grant DE-SC0003871
March Meeting 2011
Outline
Ice Ih structure
Zero Point Phonon Energy & Grüneisen parameter
Motivation: Normal Isotope Shift Zero Point
Expansion
Experiments: Anomaly in Ice Ih Zero Point
Contraction
Results
Lattice parameters
Bulk modulus
Dispersion curves
Preliminary Results with Ice Ic
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Ice Ih Structure
a
c
a
Ice = O is tetrahedrally coordinated making two covalent
bonds with 2 H’s of the molecule and two H-bonds with the
nearest molecule.
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Phonon Contribution to Zero-Point
The volume dependence of energy at zero point. [1]
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Grüneisen Parameter
The zero-point correction to the lattice parameter:
Grüneisen parameter [2]
Bulk modulus
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20Ne
22Ne
Frozen crystal
lattice constant
a0 = 4.255 Å [2]
Bolz and Mauer, 1962
Batchelder, Losee, and Simmons, 1968
Phil Allen, 1994
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Unit Cell Volume Experiments of Ice Ih
Zero Point
Contraction
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D2O
H2O
Röttger
et al.,
1994.
[3]
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Ice Ih d(O---O) = 2.75 Å
Slope: Γ negative!!!
E. Libowitzky,
1999
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[4]
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Tip4P-flexible
Tip4P-flexible does NOT show zero
point volume contraction
C. P. Herrero, R. Ramirez (2011) [5]
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rOH (Ang)
B. Pamuk et. al.
work in progress
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Electronic Energy vs. Unit Cell Volume
Experiment
10 K
DFT: SIESTA
GGA: PBE
revPBE
+ vdW
Predict water
density nicely
(Jue et. al, 2011)[6]
PBE
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PBE-vdW
revPBE
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revPBE-vdW
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Asymmetric
stretching
4 molecules/cell
Symmetric
stretching
Bending
Libration
Stretching of H-bonds
Frequency less than 0
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Ice Ih Ice XI
Non pure ice Ih : (KOH, defects needed) (Y. Tajima, T.
Matsuo, and H. Suga, 1982)
Phase transition at ~ 73 K
Angle on x-y plane different than 60o
Vector lengths on x-y plane a≠b
a = 4.5019 Å, b = 7.7978 Å, and c = 7.3280 Å
(A. J. Leadbetter, R. C. Ward, J. W. Clark, P. A. Tucker,
T. Matsuo and S. Suga, 1985)
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Contribution to the Shift
The sign of
the slope will
determine the
sign of Γ.
Work in
progress…
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Preliminary Results with Ice Ic
PBE
High
frequency
modes have
negative Γ!!!
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Low
frequency
modes are
different with
different
fcn’als
High
frequency
modes have
similar
behaviour
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Comparing Functionals
PBE predicts ~ 10% zero
point contraction on
H2O and 3% reverse
isotope effect on the
volume.
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PBE-vdW ~ 7% zero point
contraction on H2O and 2.5%
reverse isotope effect on the
volume. The experimental
reverse isotope effect is 0.009%.
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Conclusion
Take into account the zero point phonon effects for
lattice parameters.
Isotope shift in ice
Understand the most stable structure
Calculate volume dependency of frequencies
precisely
Understand how different functionals explain
ice
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References
[1] P. B. Allen, Optical and Vibrational Spectroscopies
Symposium Talk, 2010
[2] P. B. Allen, Phil. Mag. B 70, 527 (1994)
[3] K. Röttger et al. Acta Cryst. B50, 644-648 (1994).
[4] E. Libowitzky, Monatshefte für Chemie (1999)
[5] C. P. Herrero, R. Ramirez, J. Chem. Phys. 134,
094510 (2011)
[6] J. Wang, G. Román-Pérez, J. M. Soler, E. Artacho,
and M.-V. Fernández-Serra, J. Chem. Phys. 134, 024516
(2011)
Thank You
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12 molecules/cell
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Phase Diagram
http://www.thefullwiki.org/Ice_harvesting
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Lattice Parameters
and Unit Cell Volume
Experiments of ice Ih
Röttger et al., 1994.
Lattice parameters a,
and c as a function of
temperature for ice Ih
between 10 K and 265 K.
[4]
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D2O
H 2O
Röttger et al., 1994. Unit-cell volume of ice Ih between
10 and 265 K. [4]
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Lattice Parameter
PBE
revPBE
PBE-vdW
revPBE-vdW
Measurement
(10 K) [4]
a (Å)
4.39
4.52
4.44
4.56
4.49693
c (Å)
7.17
7.39
7.24
7.43
7.32109
c/a
1.633
1.635
1.631
1.629
1.628
B0 (GPa)
17.614
12.867
15.957
14.711
12.1
I. Hamada, 2010.
Results of binding
energy, lattice
parameters, volume
per molecule and
bulk moduli;
comparing different
functionals. [6]
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