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*It happens that the online record has the thermal conductivity at 30 Kelvins and to the c axis posted at 1.36 W⋅cm −1 K −1 and 78.0 Btu hr −1 ft −1 F −1 which is incorrect.
Thermal conductivity: 0.6065 ... [37] Above 4 °C, however, thermal expansion ... The required potential for the electrolysis of pure water is 1.23 V at 25 °C. ...
The values below 0 °C refer to supercooled water. Viscosity [11] 1.7921 mPa·s at 0 °C 0.5494 mPa·s at 50 °C 1.5188 mPa·s at 5 °C 0.5064 mPa·s at 55 °C 1.3077 mPa·s at 10 °C 0.4688 mPa·s at 60 °C 1.1404 mPa·s at 15 °C 0.4355 mPa·s at 65 °C 1.0050 mPa·s at 20 °C 0.4061 mPa·s at 70 °C 0.8937 mPa·s at 25 °C
For instance, when ice melts to form liquid water at 0 °C, the thermal conductivity changes from 2.18 W/(m⋅K) to 0.56 W/(m⋅K). [24] Even more dramatically, the thermal conductivity of a fluid diverges in the vicinity of the vapor-liquid critical point. [25]
Table of specific heat capacities at 25 °C (298 K) unless otherwise noted. [citation needed] Notable minima and maxima are shown in maroon. Substance Phase Isobaric mass heat capacity c P J⋅g −1 ⋅K −1 Molar heat capacity, C P,m and C V,m J⋅mol −1 ⋅K −1 Isobaric volumetric heat capacity C P,v J⋅cm −3 ⋅K −1 Isochoric ...
The thermal conductivity of seawater is 0.6 W/mK at 25 °C and a salinity of 35 g/kg. [28] The thermal conductivity decreases with increasing salinity and increases with increasing temperature. [ 29 ]
Thermal conductivity, frequently represented by k, is a property that relates the rate of heat loss per unit area of a material to its rate of change of temperature. Essentially, it is a value that accounts for any property of the material that could change the way it conducts heat. [ 1 ]
All values refer to 25 °C and to the thermodynamically stable standard state at that temperature unless noted. Values from CRC refer to "100 kPa (1 bar or 0.987 standard atmospheres )". Lange indirectly defines the values to be standard atmosphere of "1 atm (101325 Pa)", although citing the same NBS and JANAF sources among others.