
The fraction of void space in a material, affecting its permeability and density.Porosity is the fraction of a material's volume that is occupied by voids or pores, and it is a key parameter controlling how fluids flow through rocks, soils, and engineered materials. In geophysics, porosity determines the storage capacity of aquifers and oil reservoirs, while in materials science it affects mechanical strength, thermal insulation, and permeability. The study of porous media connects fluid dynamics with solid mechanics, with applications from groundwater remediation to biomedical implants.
The quantitative study of porous media began in the 19th century with Henry Darcy's experiments on water flow through sand, published in 1856, which established the fundamental law governing flow in porous materials.
Porosity is typically measured as the ratio of pore volume to total volume, often expressed as a percentage. The arrangement and connectivity of pores determine permeability, which is how easily a fluid can flow through the material. In saturated porous media, flow is described by Darcy's law, which relates the flow rate to the pressure gradient and the material's permeability. Recent advances in modeling use pore-scale simulations to capture complex behaviors like capillary effects and multiphase flow.
Porosity measurements are used to assess groundwater resources, optimize oil and gas extraction, and design porous implants that release drugs at controlled rates in the human body.
Some porous materials, like certain zeolites, have such precise pore sizes that they can act as molecular sieves, separating molecules by size with remarkable accuracy.













