![]() ![]() Online calculator, figures and tables showing dynamic (absolute) and kinematic viscosity of gasous and liquid ammonia at temperatures ranging from -73 to 425☌ (-100 to 800☏) at pressure ranging from 1 to 1000 bara (14.5 - 14500 psia) - SI and Imperial Units.Īmmonia - Prandtl Number vs. Minor loss (pressure or head loss) coefficients for air duct components.Īmmonia - Dynamic and Kinematic Viscosity vs. Thermal properties of air at different temperatures - density, viscosity, critical temperature and pressure, triple point, enthalpi and entropi, thermal conductivity and diffusivity and more.Īir Duct Components - Minor Dynamic Loss Coefficients ![]() Temperature and Pressureįigures and tables withdry air thermal diffusivity vs. SI and imperial units.Īir - Thermal Diffusivity vs. Online calculator with figures and tables showing air thermal conductivity vs. ![]() SI and imperial units.Īir - Thermal Conductivity vs. Online calculator with figures and tables showing specific heat (Cp and Cv) of dry air vs. Pressure at Constant Temperatureįigures and tables with isobaric (Cp) and isochoric (Cv) specific heat of air at constant temperature and pressure ranging 0.01 to 10000 bara.Īir - Specific Heat vs. An air phase diagram included.Īir - Specific Heat vs. Properties of air change along the boiling and condensation curves (temperature and pressure between triple point and critical point conditions). ![]() temperature and pressure.Īir - Properties at Gas-Liquid Equilibrium Conditions Online calculator, figures and tables with dynamic (absolute) and kinematic viscosity for air at temperatures ranging -100 to 1600☌ (-150 to 2900☏) and at pressures ranging 1 to 10 000 bara (14.5 - 145000 psia) - SI and Imperial Units.ĭry air is a mixture of gases where the average molecular weight (or molar mass) can be calculated by adding the weight of each component. Online calculator, figures and tables showing density, specific weight and thermal expansion coefficients of air at temperatures ranging -100 to 1600 ☌ (-140 to 2900 ☏) at atmospheric and higher pressure - Imperial and SI Units.Īir - Diffusion Coefficients of Gases in Excess of Airĭiffusion coefficients (D 12) for gases in large excess of air at temperatures ranging 0 - 400 ☌. Pressure and TemperaturesĪir density at pressure ranging 1 to 10 000 bara (14.5 - 145000 psi) and constant selected temperatures.Īir - Density, Specific Weight and Thermal Expansion Coefficient vs. Altitudeĭensity and specific volume of air varies with elevation above sea level.Īir - Density vs. Phase diagram included.ĭry air is a mechanical mixture of nitrogen, oxygen, argon and several other gases in minor amounts.Īir - Density and Specific Volume vs. Online calculator, figures and tables showing density and specific weight of acetone at temperatures ranging from -95 to 275 ☌ (-138 to 530 ☏) at atmospheric and higher pressure - Imperial and SI Units.Ĭhemical, physical and thermal properties of acetone, also called 2-propanone, dimethyl ketone and pyroacetic acid. and Brulé M.: "Phase Behavior", SPE Monograph Series vol.Absolute or Dynamic Viscosity Online ConverterĬonvert between dynamic or absolute viscosity units - Poiseuille, Poise, centPoise and more. International Journal of Greenhouse Gas Control", Volume 5, Issue 6, 2011,Pages 1460-1477,ISSN 1750-5836 Stenby,"Measurement and modeling of CO2 solubility in NaCl brine and CO2–saturated NaCl brine density, and Whitson, C.H.: "Peng-Robinson Predictions for Hydrocarbons,ĬO2, N2 and H2S With Pure Water and NaCl-Brines," Fluid Phase Increasing pressure change in the under-saturated state: The summary is based on Chapter 9 of Whitson and Brulé\(\) is calculated for an This section explains how correlations can be used to estimate the water density and viscosity which is relevant for reservoir simulation and pipe-flow calculations. The amount of gas in solution in water can also be included as a fourth variable. Water PVT and viscosity can be computed as a function of pressure, temperature, and salinity. Water PVT Computing Water Properties from Correlations Introduction Computing Water Properties from CorrelationsĬomputing Water Properties Using an EOS Model ![]()
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