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Contribution of water dimers in atmospheric absorption: methodology Ross E. A. Kelly , Matt J. Barber, Jonathan Tennyson Department of Physics and Astronomy, University College London Gerrit C. Groenenboom, Ad van der Avoird Theoretical Chemistry Institute for Molecules and Materials, Radboud University Caviar Consortium Meeting, NPL 29 th September 2010

Contribution of water dimers in atmospheric absorption: methodology

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Contribution of water dimers in atmospheric absorption: methodology. Ross E. A. Kelly , Matt J. Barber, Jonathan Tennyson Department of Physics and Astronomy, University College London Gerrit C. Groenenboom, Ad van der Avoird Theoretical Chemistry Institute for Molecules and Materials, - PowerPoint PPT Presentation

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Page 1: Contribution of water dimers in atmospheric absorption: methodology

Contribution of water dimers in atmospheric absorption: methodology

Ross E. A. Kelly, Matt J. Barber, Jonathan TennysonDepartment of Physics and Astronomy,

University College London

Gerrit C. Groenenboom, Ad van der Avoird Theoretical Chemistry Institute for Molecules and Materials,

Radboud University

Caviar Consortium Meeting, NPL29th September 2010

Page 2: Contribution of water dimers in atmospheric absorption: methodology

• (1) Need to solve the nuclear motion Hamiltonian– 12D problem! Approximations required.

• (2) Fully dimensional potential energy surface required– Huang, Braams and Bowman (HBB) potentials

• 30-40,000 configurations sampled.• Calculated at coupled-cluster, single and double and perturbative

treatment of triple excitations method.• Augmented, correlation consistent, polarized triple zeta basis set.• Polynomial fit with 5227 coefficients.

Water Dimer Method

HBB – X. Huang et al. J. Chem. Phys. 128, 034312 (2008).HBB2 – X. Huang et al. J. Chem. Phys. 130, 144314 (2009).

Page 3: Contribution of water dimers in atmospheric absorption: methodology

(2) Fully Dimensional Water Dimer Potential

Monomer corrected* HBB potential • Corrects for monomer excitation

– Accurate modes for the monomer

* S. V. Shirin et al., J. Chem. Phys. 128, 224306 (2008).R.E.A. Kelly, J. Tennyson, G C. Groenenboom, A. Van der Avoird, JQRST, 111, 1043 (2010).

Page 4: Contribution of water dimers in atmospheric absorption: methodology

• Diffusion Monte Carlo may be used– Start with a number of walkers– Allow them to follow a random walk in space– Propagate in imaginary time– Decide whether to replicate or destroy the walker

(1) Fully Dimensional (12D) Solution

• Only useful for 12D vibrational ground state.

Page 5: Contribution of water dimers in atmospheric absorption: methodology

Solving the 6D intermolecular problem

• Brocks Brocks et alet al. Hamiltonian*. Hamiltonian*

• Monomers fixed in Monomers fixed in – Equilibrium geometry, or Equilibrium geometry, or – Vibrational ground state geometryVibrational ground state geometry

* G. Brocks et al. Mol. Phys. 50, 1025 (1983).

Page 6: Contribution of water dimers in atmospheric absorption: methodology

Solving the 6D intermolecular problemSolving the 6D intermolecular problem

AcceptorTwist (AT)

AcceptorWag (AW)

Donor Torsion (DT)

In PlaneBend (IPB) Stretch

Out-of-PlaneBend (OPB)

Generated by Matt Hodges and Anthony Stone. C. Millot et al. J. Phys. Chem. A 1998,102, 754. http://www-stone.ch.cam.ac.uk/research/water.dimer/modes.html

Page 7: Contribution of water dimers in atmospheric absorption: methodology

1 1

1 1

5 5

5 5

2 2

2 2

6 6

6 6

6 6

6 6

5

5 5

5

4

4

4

4

3

3

3

3

3 3

3 3

4

4

4

4

1 1

1 1

2

2 2

2

Isomorphic to D4h

with Irreducible Elements:

A1

+, A2

+, A1

-, A2

-, B1

+, B2

+, B1

-, B2

-, E+, E-

-> Water Dimer Spectroscopic Labels

Tunneling Splittings

Page 8: Contribution of water dimers in atmospheric absorption: methodology

Tunneling Splittings

Very good agreement with:

• Ground State Tunnelling splittings• Rotational Constants

Not so good agreement with:

• Acceptor Tunnelling

Page 9: Contribution of water dimers in atmospheric absorption: methodology

Solving the 6D intermolecular problem

• Brocks Brocks et alet al. Hamiltonian*. Hamiltonian*

• Monomers fixed in Monomers fixed in – Equilibrium geometry, or Equilibrium geometry, or – Vibrational ground state geometryVibrational ground state geometry

* G. Brocks et al. Mol. Phys. 50, 1025 (1983).

Is there another way to help us probe the 12D problem?

Page 10: Contribution of water dimers in atmospheric absorption: methodology

Adiabatic Separation

• Approximate separation between monomer and dimer modes– Separate intermolecular and intramolecular modes.

mD – water donor vibrational wavefunction

mA – water acceptor vibrational wavefunction

d – dimer VRT wavefunction

dmm AD

Page 11: Contribution of water dimers in atmospheric absorption: methodology

)()(|);,(|)()()( BBAABABBAAmm

eff mmVmmV BA QQRQQQQR

• Now we can vibrationally average the potentialNow we can vibrationally average the potential

• Input for 6D calculationsInput for 6D calculations

donordonor acceptoracceptor

State mState m State nState n

• How well does it perform for |0 0> calculationsHow well does it perform for |0 0> calculations

Solving the 6D intermolecular problem

Page 12: Contribution of water dimers in atmospheric absorption: methodology

• In cm-1

• Red – ab initio potential• Black – experimental

• GS – ground state

• DT – donor torsion

• AW – acceptor wag

• AT – acceptor twist

• DT2 – donor torsion overtone R.E.A. Kelly, J. Tennyson, G C. Groenenboom, A. Van der Avoird, JQRST, 111, 1043 (2010).

Vibrational Averaging

Page 13: Contribution of water dimers in atmospheric absorption: methodology

Vibrational Averaging: 6D Costs!

• Computation:

– typical number of DVR points with different Morse Parameters:

– {9,9,24} gives 1,080 points for monomer

– 1,0802 = 1,166,400 points for both monomers

– 1,166,400 x 2,894,301 intermolecular points

= 3,374,862,926,400 points• Same monomer wavefunctions for all grid points• Distributed computing: Condor 1000 computers, 10 days

But we have a way to probe high frequency dimer spectra

Page 14: Contribution of water dimers in atmospheric absorption: methodology

Full model for high frequency absorption

• Approximate separation between monomer and dimer modes

• Franck-Condon approximation for vibrational fine structure

• Rotational band model

Page 15: Contribution of water dimers in atmospheric absorption: methodology

Adiabatic Separation

• Approximate separation between monomer and dimer modes– Separate intermolecular and intramolecular modes.

mD – water donor vibrational wavefunction

mA – water acceptor vibrational wavefunction

d – dimer VRT wavefunction

dmm AD

Page 16: Contribution of water dimers in atmospheric absorption: methodology

Model for high frequency absorption

• Approximate separation between monomer and dimer modes

• Franck-Condon approximation for vibrational fine structure

• Rotational band model

Page 17: Contribution of water dimers in atmospheric absorption: methodology

2

2121

2fffiii

fi dmmdmmI

22

1122

fifi

mmddmmfi

Franck-Condon Approx for overtone spectra

Assume monomer m1 excited, m2 frozen

m2i = m2

f

I

(2) Franck-Condon factor

(square of overlap integral):

Gives dimer vibrational fine structure

(1) Monomer vibrational band Intensity

Page 18: Contribution of water dimers in atmospheric absorption: methodology

Allowed Transitions in our Model

1. Excited donor 2. Excited acceptor

All transitions from ground monomer vibrational states

Assume excitation localised on one monomer

Page 19: Contribution of water dimers in atmospheric absorption: methodology

Franck-Condon factors

– Overlap between dimer states on adiabatic potential energy surfaces for water monomer initial and final states

– Need the dimer states (based on this model).

Page 20: Contribution of water dimers in atmospheric absorption: methodology

Transitions: Example

Donor – Vibrational ground state (VGS)Acceptor – VGS

Donor –VGS Acceptor – bend

Acceptor Twist (AT)

Acceptor Wag (AW)

Donor Torsion (DT)

Ground State (GS)

Acceptor Twist (AT)

Acceptor Wag (AW)

Donor Torsion (DT)

Ground State (GS)

Page 21: Contribution of water dimers in atmospheric absorption: methodology

Transitions: Example

Acceptor Twist (AT)

Acceptor Wag (AW)

Donor Torsion (DT)

Ground State (GS)

Acceptor Twist (AT)

Acceptor Wag (AW)

Donor Torsion (DT)

Ground State (GS)

Donor – Vibrational ground state (VGS)Acceptor – VGS

Donor –VGS Acceptor – bend

Page 22: Contribution of water dimers in atmospheric absorption: methodology

Transitions: Example

Acceptor Twist (AT)

Acceptor Wag (AW)

Donor Torsion (DT)

Ground State (GS)

Acceptor Twist (AT)

Acceptor Wag (AW)

Donor Torsion (DT)

Ground State (GS)

Donor – Vibrational ground state (VGS)Acceptor – VGS

Donor –VGS Acceptor – bend

Page 23: Contribution of water dimers in atmospheric absorption: methodology

Outline of full problem

• Need to ultimately solve (6D problem)

• H=K+Veff

• Veff sampled on a 6D grid

dd EH • Calculate states for donor

• Calculate states for acceptor

• Vibrationally average potential for each state-state combination– Really only |0j> and |i0>

Page 24: Contribution of water dimers in atmospheric absorption: methodology

(a) 6D averaging:

(b) 3D+3D averaging:

1 C Leforestier et al, J Chem Phys, 117, 8710 (2002)2 R. E. A. Kelly et al. To submit shortly.

);,()()(

)()(|);,(|)()()(22 RQQQQ

QQRQQQQR

BABBAqq

A

BBAABABBAAeff

Vmm

mmVmmV

BA

);,()(|);,(|)(

)(|);,(|)()(000

0

RQQQRQQQ

QRQQQR

BABBBABB

AABAAAeff

VmVm

mVmV

Averaging Techniques

Page 25: Contribution of water dimers in atmospheric absorption: methodology

Averaging Techniques

• Form of the wavefunction:– (I) Uncoupled free monomer

– (II) Uncoupled perturbed (fixed) monomer

R. E. A. Kelly et al. To submit shortly.

Page 26: Contribution of water dimers in atmospheric absorption: methodology

Problems with Fixed Wavefunction approach (uncoupled methods)

• Donor bend • (Donor) Free OH stretch • (Donor) Bound OH stretch

• (Donor) Free OH stretch • (Donor) Bound OH stretch

Page 27: Contribution of water dimers in atmospheric absorption: methodology

Averaging Techniques

• Form of the wavefunction:– (I) Uncoupled free monomer

– (II) Uncoupled perturbed (fixed) monomer

– (III) Coupled Adiabatic

R. E. A. Kelly et al. To submit shortly.

Page 28: Contribution of water dimers in atmospheric absorption: methodology

Averaging Techniques

• Form of the wavefunction:– (I) Uncoupled free monomer

– (II) Uncoupled perturbed (fixed) monomer

– (III) Coupled Adiabatic

R. E. A. Kelly et al. To submit shortly.

Page 29: Contribution of water dimers in atmospheric absorption: methodology

Averaging Techniques

• Form of the wavefunction:– (I) Uncoupled free monomer

– (II) Uncoupled perturbed (fixed) monomer

– (III) Coupled Adiabatic

R. E. A. Kelly et al. To submit shortly.

Page 30: Contribution of water dimers in atmospheric absorption: methodology

Averaging Techniques

• Form of the wavefunction*:– (I) Uncoupled free monomer– (II) Uncoupled perturbed monomer – (III) Coupled Adiabatic

• Coupled Adiabatic methods are the most suitable– Requires wavefunction calculations at each intermolecular grid

point! 2,893,401 * 2 DVR3D calculations!– So we use cheaper (3+3)D averaging technique.

– Still costs! 500-700 CPUs for 3-4 weeks.

*R. E. A. Kelly et al. To submit shortly.

Page 31: Contribution of water dimers in atmospheric absorption: methodology

Calculating dimer spectra with FC approach

• Solved for monomers • Coupled adiabatic appoach

• Vibrationally averaged potential for donor-acceptor state-state combinations |0j> and |i0>• Input for 6D intermolecular problem

• Now we can solve 6D intermolecular problem• Obtain vibrational fine structure

Page 32: Contribution of water dimers in atmospheric absorption: methodology

Solving the 6D intermolecular problem:Allowed permutations

1 15 5

2 26 6

4

4

3

3

1 1

5 5

2 26 6

6 6

6 6

5

5 5

5

4

4

3

3

3 3

3 3

4

4

4

4

1 1

1 1

2

2 2

2

Page 33: Contribution of water dimers in atmospheric absorption: methodology

1 15 5

2 26 6

4

4

3

3• G16 Symmetry of Hamiltonian for GS monomers

– > replaced with G4 • Greatly increases computational requirements

• Reduced angular basis• Small radial basis• 320 diagonalizations for 0-10,000 cm-1

• Each at 16GB• 8 states per symmetry block

• Leading to 20,480 transitions

Solving the 6D intermolecular problem:Allowed permutations for excited monomers

Page 34: Contribution of water dimers in atmospheric absorption: methodology

Full Vibrational Stick Spectra

1.00E-56

1.00E-50

1.00E-44

1.00E-38

1.00E-32

1.00E-26

1.00E-20

1.00E-14

1.00E-08

1.00E-02

1000 4000 7000 10000

Frequency (cm-1)

Ab

sorp

tio

n (

Hit

ran

un

its)

1.00E-281.00E-271.00E-261.00E-251.00E-241.00E-231.00E-221.00E-211.00E-201.00E-191.00E-181.00E-171.00E-16

1000 4000 7000 10000

Strongest absorption on bend – difficult todistinguish from monomer features

More structure between 6000-9000 cm-1

Page 35: Contribution of water dimers in atmospheric absorption: methodology

Model for high frequency absorption

• Approximate separation between monomer and dimer modes

• Franck-Condon approximation for vibrational fine structure

• Rotational band model – Matt will discuss this

Page 36: Contribution of water dimers in atmospheric absorption: methodology

• We have a new model to probe near IR and visible regions of the water dimer spectra.– With first vibrational fine structure reported.

• Spectra for up to 10,000 cm-1 produced.– Much better agreement with experimental and theoretical work

than our previous calculations.

• We have finished new averaging calculations which will allow us to probe spectra up to 18,000 cm-1

• And all states up to dissociation to be calculated.– Only 8 states per symmetry here (32 states per state-state job)– up to 800, or 3200 per job.

Conclusions