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Methane hydrate: interfacial nucleation Crystal Melted under vacuum (300 K), then pressurised under methane (30 atm)

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Presentation on theme: "Methane hydrate: interfacial nucleation Crystal Melted under vacuum (300 K), then pressurised under methane (30 atm)"— Presentation transcript:

1 Methane hydrate: interfacial nucleation Crystal Melted under vacuum (300 K), then pressurised under methane (30 atm)

2 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

3 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)

4 Order parameters: 3-body Fluctuations from tetrahedral network Average over all triplets, based on central oxygen and “bonding” radius

5 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

6 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  H-bond network angles H-bond network torsions

7 Order parameters & melting Analysis of melting crystal shows order parameters are consistent Analysis of covariance matrix (bulk) shows they are independent

8 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)

9 Local Phase Assignment 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

10 Water in Hydrate Environment

11 Distribution of order parameters 1 ns Difference: 22 ns - 1 ns

12 Animated Nucleation

13 Simulated Nucleation [ hydrate-waters ) 3.3ns2.4ns4.2ns5.1ns 6.9ns6.0ns 1.5ns 7.8ns20ns40ns 0.6ns 10.5ns

14 Which hydrate structure? type II Best signature is arrangement of dodecahedra type I

15 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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