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--------------The apparent particle density (often simply called particle density) is the density of individual particles, including their internal porosity. It is distinct from the skeletal density (which excludes pores) and the bulk density (which includes the voids between different particles).
The fundamental definition is the mass of a single particle divided by its total volume (including internal closed or open pores):
\[ \rho_p = \frac{\text{mass of a particle}}{\text{volume of a particle}} \]

Equation 1: Apparent particle density
It is possible to determine the apparent particle density from the Skeletal density and the internal porosity (pore volume), which are typically measured via gas pycnometry or mercury porosimetry.
\[ \frac{1}{\rho_p} = \frac{1}{\rho_{sk}} + \omega_p \]

Equation 2: Relationship between Apparent Density, Skeletal Density, and Porosity
With:
\(\rho_p\) = apparent particle density (kg/m³)
\(\rho_{sk}\) = skeletal density (kg/m³)
\(\omega_p\) = specific pore volume (m³/kg)
The particle density is critical in applications requiring fluidization of particles or their suspension. It directly influences the terminal velocity of the particles in a gas stream. In cyclone design, pneumatic conveying, and gas-solid separations, the apparent density (not the bulk density) is the governing physical property for aerodynamic behavior.