Q-TIP4P/F model of water

The q-TIP4P/F model is a flexible version of the TIP4P/2005 model of water designed for use in path integral simulations. The melting point was found to be $251\pm 1.5~K$ at 1 bar via direct coexistence calculations.

Isotope effects

Melting point (extract from the Ice Ih page)

$T_{m}$ (D20)	Pressure	Water model/technique	Reference
$257.5(5)~K$	1 bar	q-TIP4P/F
Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle 276.83 \pm 0.02 K}	1 bar	experimental value

Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle T_m} (T20)	Pressure	Water model/technique	Reference
Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle 259.2(5)~K}	1 bar	q-TIP4P/F
Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle 277.64 K}	0.6629 kPa	experimental value

It is worth pointing out that the calculations presented in the work of Ramírez and Herrero 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: Failed to parse (SVG (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://wikimedia.org/api/rest_v1/":): {\displaystyle \Delta T_m (D_2O - H_2 0) = 6.5 K} (experimental value: 3.68 K) and $\Delta T_{m}(T_{2}O-H_{2}0)=8.2K$ (experimental value: 4.49 K).