Overview
Radiation pressure is the mechanical pressure exerted on a surface by electromagnetic radiation. Photons carry momentum as well as energy, and when light or other electromagnetic waves strike matter they transfer some of that momentum. The resulting force per unit area can be observed in controlled experiments and plays a measurable role in many natural and technological settings. For a concise definition see radiation pressure.
How it arises and basic formula
In classical terms the flow of electromagnetic energy is described by the Poynting vector, and the momentum flux is related to that energy flux. A simple, widely used expression links intensity I (energy per unit area per unit time) to pressure p: for perfect absorption the pressure is p = I/c, where c is the speed of light; for perfect reflection the momentum change is doubled and p = 2I/c. Real materials produce intermediate values depending on reflectivity and scattering. For a compact summary of the energetics and momentum transfer see energy and momentum in light.
Historical measurements and demonstrations
The idea that electromagnetic radiation can exert pressure follows from electromagnetic theory developed in the 19th century. Direct laboratory measurements came later, when sensitive torsion balances and radiometers were used to detect the tiny forces involved. Some early devices, including the Crookes radiometer, are often discussed in this context; the radiometer's spinning vanes are driven primarily by thermal effects on residual gas molecules rather than by photon pressure itself. For accessible experimental descriptions consult experimental studies of light pressure.
Examples and applications
Although radiation pressure is negligible for most everyday forces, it becomes important where light intensities are large or over long distances. Notable examples include:
- Solar sails: spacecraft that use sunlight momentum to produce continuous thrust without propellant.
- Astrophysics: radiation pressure influences the structure of stellar atmospheres, drives stellar winds in massive stars, and helps shape comet tails by pushing dust away from the Sun.
- Optical manipulation: focused laser beams can trap and move microscopic particles (optical tweezers) and contribute to laser cooling techniques.
- Laboratory physics: precision experiments can use radiation pressure to measure properties of light and matter or to actuate micro- and nano-mechanical devices.
Related phenomena and important distinctions
Radiation pressure should be distinguished from other radiative forces and effects. Scattering and absorption by particles involve momentum exchange but depend on size, composition, and angle. For charged particles, radiation can exert forces indirectly through induced currents or by Compton and Thomson scattering. In orbital dynamics, subtle effects such as the Poynting–Robertson drag arise when sunlight both exerts pressure and changes a particle's orbital energy. For further reading on related concepts see related radiation effects.
Practical note: the magnitude of radiation pressure at Earth from sunlight is small (on the order of micro- to milli-Newtons per square meter under ordinary conditions), but it accumulates over time or becomes significant in domains where conventional forces are absent or tiny, making it a useful and sometimes dominant influence in space and in precision optical systems.


