methane hydrate: interfacial nucleation

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Methane hydrate: interfacial nucleation. Crystal. Melted under vacuum (300 K), then pressurised under methane (30 atm). Potential Energy (rolling average over 10 ps) (n.b. should divide by 1654 to quote per mole of water. Density profile across interfaces I = 0–0.3 ns II = 9–10 ns. - PowerPoint PPT Presentation

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Methane hydrate: interfacial nucleation

Crystal

Melted under vacuum (300 K), then pressurised under methane

(30 atm)

Time Evolution

Potential Energy (rolling average over 10 ps)

(n.b. should divide by 1654 to quote per mole of water

Density profile across interfaces

I = 0–0.3 ns

II = 9–10 ns

Hydrate Formation: Analysis

upper half of water film (0 – 20 Å)

lower half of water film(-20 – 0 Å)

Methane-Methane radial distribution functions, g(r)

Order parameters: 3-body

• Fluctuations from tetrahedral network

• Average over all triplets, based on central oxygen and “bonding” radius

Order parameters: “4-body”

• Locate a three H-bond chain

• Calculate torsion angle and triple product from “bond” vectors

• Mimic by two-molecules

• Average over coordination shell

Local Phase of Water Molecules• Define local order parameters that distinguish between

bulk phases

• Determine standard deviations, , within stable bulk phases (hydrate/ice)

• Assign individual molecule as hydrate/ice if all its order parameters agree with bulk values to within 2

Environment Liquid Hydrate IceF3 0.10 0.01 0.01F4 0.00 0.70 -0.40F4t 0.26 0.47 0.29

H-bond network angles

H-bond network torsions

Order parameters & melting

• Analysis of melting crystal shows order parameters are consistent

• Analysis of covariance matrix (bulk) shows they are independent

Characterising Molecular Order

• Define vector of three order parameters (f)

• Calculate covariance matrix for each molecule (C–1) for stable phases

• Eigenvalue analysis to de-correlate (y)

1

2

1

2

( )P e

e

f C f

y Λ y

-1

f

Λ U CU

y Uf

Local Phase Assignment

2 2i i i i iy

y Uf

• Calculate f for each molecule in arbitrary system

• Project onto eigenvectors (components of y)

• Compare with : assign “local phase” if all three components within 2(?) standard deviation of for that phase

Water in Hydrate Environment

Fraction of Hydrate-Water

0

0.05

0.1

0.15

0.2

0.25

0.3

0.35

0.4

0 10 20 30 40

time / ns

Control1

Control2

Control3

Distribution of order parameters

1 ns

Difference:22 ns - 1 ns

Animated Nucleation

Simulated Nucleation [ hydrate-waters )

3.3ns2.4ns 4.2ns 5.1ns

6.9ns6.0ns

1.5ns

7.8ns 20ns 40ns

0.6ns

10.5ns

Which hydrate structure?

type II

• Best signature is arrangement of dodecahedra

type I

Which hydrate structure?

• Early appearance of face-sharing dodecahedra

type II

• Oswald’s step rule: form the unstable polymorph first

• Experimental verification: time resolved X-ray powder study (Kuhs, 2002)

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