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Tables B-1 and B-2 present data for saturated liquid and saturated vapor. Table B-1 is presented information at regular intervals of temperature while Table B-2 is presented at regular intervals of pressure. Table B-3 presents data for superheated vapor over a matrix of temperatures and pressures.
Online calculator, figures and tables showing heat of vaporization of water, at temperatures from 0 - 370 °C (32 - 700 °F) - SI and Imperial units.
Table A–1 Molar mass, gas constant, and critical-point properties Table A–2 Ideal-gas specific heats of various common gases Table A–3 Properties of common liquids, solids, and foods Table A–4 Saturated water—Temperature table Table A–5 Saturated water—Pressure table Table A–6 Superheated water Table A–7 Compressed liquid water Table A–8 Saturated ice–water vapor
Air flow in the soil is laminar or diffusive. And it has a greater heat capacity and density than air, so it alters how heat is transferred between the biosphere and atmosphere. It is a complex medium, being a reservoir of roots, water, organic matter, microbes, soil fauna, nutrients, minerals and gases.
Water - Heat of Vaporization vs. Temperature Online calculator, figures and tables showing heat of vaporization of water, at temperatures from 0 - 370 °C (32 - 700 °F) - SI and Imperial units. Water - Ionization Constant, pKw, of Normal and Heavy Water
Tablesareprovidedforthedensity,enthalpy,entropy,andvolumeofwaterand steam calculated from the lAPWS Formulation1995 forthe Thermodynamic Properties of Ordinary Water Substance for General and Scientific Use.This
The properties listed here (except the vapor density) can be used at any pressures with negligible error except at temperatures near the critical-point value. Note 2: The unit kJ/kg· C for specific heat is equivalent to kJ/kg·K, and the unit W/m· C for thermal conductivity is equivalent to W/m·K.
