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This document presents seawater property data from our library (web.mit.edu/seawater). Properties are listed as a function of temperature and salinity for the pressures, P = P0 , 7 MPa and 12 MPa. Here, P0 = 0.101325 MPa for t <= 100°C and for t > 100 °C is the vapor pressure of seawater.
K. Formula by Hardy for viscosity of salt water: ν = ν . Where . + 0 .03338 T + 0 .00018325 T. 0. = 1.052, ν. is the viscosity of seawater at T °C and ν. 0 = 0.001787 Pa s that of fresh water at 0°C. 1.3 Tables Given In 1963. Salinity 3.5% TABLE 3. 1.2.3 Values of Kinematic Viscosity for Fresh Water. 2 . it.
Best-fi tted new correlations are obtained from available data for density, dynamic viscosity, surface tension, boiling point eleva-tion, specifi c enthalpy, specifi c entropy and osmotic coeffi cient after appropriate conversion of temperature and salinity scales to the most recent standards.
Freezing Point of Seawater vs. Pressure and Salinity. Seawater properties like density, saturation pressure, specific heat, electrical conductivity and absolute viscosity.
The viscosity of saline water is a key parameter for fluid flow systems, including those of desalination. Also, heat transfer is a boundary layer phenomenon and is strongly affected by viscosity. The viscosity is important in determining the transport properties of water (Swindellsr et al. 1952).
1.1 Formulae Used by 1978 ITTC Performance Prediction Method: 1.2 Formula Given in 1963: Values of Mass Density for Fresh Water. Values of Mass Density for Salt Water. Values of Kinematic Viscosity for Fresh Water.
For this procedure, only the following properties are provided: density, absolute viscosity, kine-matic viscosity, and vapour pressure. In general, the water properties are a func-tion of temperature (t), pressure (p), and abso-lute salinity (SA). For fresh water, SA = 0.0.
