method

gravitational wave interferometry

Technique using laser interferometers to measure tiny length changes from passing gravitational waves.
27 related articles

Description

Gravitational wave interferometry is the technique that made the first direct detection of gravitational waves possible in 2015. It uses large-scale laser interferometers, like LIGO and Virgo, to measure minuscule changes in the distance between mirrors—changes as small as a thousandth of the width of a proton. When a gravitational wave passes, it stretches and squeezes spacetime, causing the arms of the interferometer to change length slightly, which alters the interference pattern of the laser light.

History

The concept was proposed in the 1960s by Soviet scientists Gertsenshtein and Pustovoit, and independently by Rainer Weiss in 1972. The first detection was made by LIGO in September 2015, announced in February 2016.

How it works

A laser beam is split into two perpendicular paths, each traveling to a mirror and back. The two beams are then recombined, and their interference pattern is measured. If the arm lengths are equal, the beams cancel out (destructive interference). A passing gravitational wave changes the relative arm lengths, causing a tiny signal to appear. To achieve the required sensitivity, the interferometers use high-power lasers, suspended mirrors to isolate from seismic noise, and multiple reflections to increase the effective path length.

In practice

It is used to observe gravitational waves from merging black holes and neutron stars, opening a new window into astrophysics and testing general relativity in strong-field regimes.

Fun fact

The LIGO detectors are so sensitive that they can measure a change in length smaller than the size of an atom's nucleus over a 4-kilometer arm.

Concept graph →

Related articles · 27

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