Q-TIP4P/F model of water: Difference between revisions

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The '''q-TIP4P/F''' model
The '''q-TIP4P/F''' model
<ref>[http://dx.doi.org/10.1063/1.3167790 Scott Habershon, Thomas E. Markland, and David E. Manolopoulos "Competing quantum effects in the dynamics of a flexible water model", Journal of Chemical Physics '''131''' 024501 (2009)]</ref>
<ref>[http://dx.doi.org/10.1063/1.3167790 Scott Habershon, Thomas E. Markland, and David E. Manolopoulos "Competing quantum effects in the dynamics of a flexible water model", Journal of Chemical Physics '''131''' 024501 (2009)]</ref>

Latest revision as of 14:49, 16 October 2017

The q-TIP4P/F model [1] is a flexible version of the TIP4P/2005 model of water designed for use in path integral simulations.

Melting point[edit]

The melting point was found to be 251±1.5K at 1 bar via direct coexistence calculations, and at 257K from calculations of the Gibbs energy function [2].

Isotope effects[edit]

Melting point (extract from the Ice Ih page)

Tm (D20) Pressure Water model/technique Reference
257.5(5)K 1 bar q-TIP4P/F [3]
276.83±0.02K 1 bar experimental value [4]
Tm (T20) Pressure Water model/technique Reference
259.2(5)K 1 bar q-TIP4P/F [3]
277.64K 0.6629 kPa experimental value [5]

It is worth pointing out that the calculations presented in the work of Ramírez and Herrero [3] used the melting point of the q-TIP4P/F model as its "reference state". It is perhaps more fruitful to examine the relative changes upon isotopic substitution: ΔTm(D2O−H20)=6.5K (experimental value: 3.68 K) and ΔTm(T2O−H20)=8.2K (experimental value: 4.49 K).

Ice Ih[edit]

Isotope effects have also been studied for ice Ih [6].

References[edit]