Porosity Formula:
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Porosity is a measure of the void spaces in a material, expressed as a percentage of the total volume. It is an important property in fields like geology, soil science, and materials engineering, indicating how much fluid a material can hold.
The calculator uses the porosity formula:
Where:
Explanation: The formula calculates the proportion of void space by comparing the bulk density (including pores) to the particle density (excluding pores).
Details: Porosity is crucial for understanding fluid storage and transport in porous media. It affects water retention in soils, hydrocarbon recovery in reservoirs, and filtration efficiency in engineered materials.
Tips: Enter bulk density and particle density in g/cm³. Both values must be positive, and bulk density must be less than particle density for valid results.
Q1: What is the difference between bulk density and particle density?
A: Bulk density includes the volume of both solid particles and pore spaces, while particle density refers only to the solid material without pores.
Q2: What are typical porosity values for common materials?
A: Soils typically range from 30-60%, sandstones 5-30%, clays 40-70%, and gravels 20-40% porosity.
Q3: How is porosity measured in laboratory settings?
A: Common methods include mercury intrusion porosimetry, gas expansion techniques, and water saturation methods.
Q4: Does porosity affect material strength?
A: Yes, generally higher porosity reduces material strength as there is less solid material to bear loads.
Q5: Can porosity be greater than 100%?
A: No, porosity is always between 0-100% as it represents a percentage of void space in the total volume.