Amount of heat required to change the temperature of one unit of mass by one unit of temperature:
c_m = \frac{\delta Q}{\delta m \cdot \delta T} |
Specific Heat Capacity depends on the way the heat is transferred and as such is not a material property.
The two major heat transfer processes are isobaric and isohoric which define:
Both c_{mp} and c_{mV} are material properties and properly tabulated for the vast majority of materials.
Specific Heat Capacity c_m relates to Volumetric Heat Capacity c_v and density of the matter \rho as:
(1) | c_m = \rho \cdot c_v |
In many technical papers the "m" or "v" index is omitted which leads to confusion between Specific Heat Capacity c_m and Volumetric Heat Capacity c_v.
For multiphase fluid in thermodynamic equilibrium the Specific Heat Capacity c_m is:
(2) | c_m = \frac{\sum_\alpha s_\alpha \rho_\alpha c_{m \alpha}}{\sum_\alpha s_\alpha \rho_\alpha } |
where
s_\alpha | \alpha-phase volume share, subjected to \sum_{\alpha} s_\alpha = 1 |
\rho_\alpha | \alpha-phase Fluid Density |
c_{v \alpha} | \alpha-phase Volumetric Heat Capacity |
See also
Physics / Thermodynamics / Thermodynamic process / Heat Transfer / Heat Capacity
[ Heat ] [ Volumetric Heat Capacity ]