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The density profile is used in conjunction with the gradient theory, to yield an expression for the surface tension of a saturated fluid as a function of temperature and fluid properties.
The MMP is reported to be a function of temperature and fluid compositions.
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A series of experimental measurements was conducted to evaluate the cavitation threshold as a function of temperature and viscosity/surface tension, for different fluid load media.
In coexisting melts and fluids and in supercritical fluid as a function of temperature (and pressure) in a hydrous Na-aluminosilicate system (data from Mysen 2010a).
c Areas of coexisting melt and fluid normalized to the area of single phase fluid at 800 °C as a function of temperature and pressure.
The local density of drilling fluid as a function of temperature and pressure is evaluated using the available PVT correlations.
Fig. 11 Evolution of Q-species abundance and bulk NBO/T of melt and coexisting fluid as a function of temperature (and pressure, see Table 1).
where keff(L,T, φ) is the effective thermal conductivity of the nanofluid as a function of particle size (L), temperature (T), and particle volume fraction, kl(T) is the thermal conductivity of the base fluid as a function of temperature, and kP L,T) is the thermal conductivity of the particle as a function of particle size and temperature.
Fig. 9 Evolution of CO32 abundance in coexisting fluid and melt as a function of temperature and pressure with concentration, expressed as area of the ~ 1070 cm−1 band normalized to the value for single phase fluid at 800 °C (diamond symbol).
Fig. 5 Zr concentration in fluids as a function of temperature and pressure for the systems indicated.
In hydrous Na-aluminosilicate melts and in silicate-saturated aqueous fluids as a function of temperature (and pressure) (data from Mysen 2012a, b).
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