
Tiny solid particles in space, like soot or sand, that absorb and emit radiation.Dust grains are tiny solid particles in space, ranging in size from a few molecules to about a micrometer across, similar to smoke particles or fine sand. They are composed of silicates, carbon compounds, and ices, and they play a surprisingly important role in astrophysics. Despite their small size, dust grains absorb and scatter light, making distant objects appear dimmer and redder — a process called extinction. They also emit their own thermal radiation, which can dominate the infrared spectrum of galaxies.
The existence of interstellar dust was inferred in the early 20th century from the reddening of starlight, but its detailed properties were only revealed with the advent of infrared astronomy in the 1970s and 1980s.
Dust grains form in the outflows of evolved stars, where heavy elements condense into solid particles, and in supernova remnants. In interstellar space, they grow by accreting atoms and molecules onto their surfaces. When ultraviolet light from stars strikes a dust grain, it heats up and re-emits the energy as infrared radiation. Dust grains also act as catalysts for chemical reactions, providing a surface where atoms can meet and form molecules, including complex organic ones.
Understanding dust grains is essential for interpreting observations of star-forming regions, planetary systems, and the cosmic microwave background, as dust emission contaminates these signals.
Dust grains are so efficient at absorbing light that a single grain can block a star's light from reaching us, and they are responsible for the dark patches visible in the Milky Way's band across the night sky.













