TIP4P/FQ model of water: Difference between revisions
		
		
		
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==Melting point==  | |||
The [[Ice Ih]]-[[water]] melting point has been calculated to be <math>303\pm 8~K</math> <ref>[http://dx.doi.org/10.1016/j.jcrysgro.2006.04.077  Benjamin F. Nicholson, Paulette Clancy and Steven W. Rick "The interface response function and melting point of the prism interface of ice Ih using a fluctuating charge model (TIP4P-FQ)", Journal of Crystal Growth '''293''' pp. 78-85 (2006)] </ref>.  | |||
==References==  | ==References==  | ||
<references/>  | <references/>  | ||
[[category: water]]  | [[category: water]]  | ||
[[category: models]]  | [[category: models]]  | ||
Latest revision as of 16:29, 15 June 2011
The TIP4P/FQ model [1] is a variant of the TIP4P model, which now incorporates fluctuating charges.
Parameters[edit]

| (Å) | HOH , deg | (Å) | (K) | q(O) (e) | q(H) (e) | q(M) (e) | (Å) | 
| --- | --- | --- | --- | --- | --- | --- | --- | 
Melting point[edit]
The Ice Ih-water melting point has been calculated to be [2].
References[edit]
- ↑ Steven W. Rick, Steven J. Stuart, and B. J. Berne "Dynamical fluctuating charge force fields: Application to liquid water", Journal of Chemical Physics 101 pp. 6141-6156 (1994)
 - ↑ Benjamin F. Nicholson, Paulette Clancy and Steven W. Rick "The interface response function and melting point of the prism interface of ice Ih using a fluctuating charge model (TIP4P-FQ)", Journal of Crystal Growth 293 pp. 78-85 (2006)