A theory treating matter quantum mechanically while spacetime remains classical, used to study black hole evaporation.Semiclassical gravity is a theoretical framework that treats matter and fields quantum mechanically while keeping spacetime itself classical, described by Einstein's general relativity. It is the standard approach for studying phenomena where quantum effects are significant but the gravitational field is not yet quantized, such as black hole evaporation, the early universe, and the behavior of quantum fields in curved spacetime. The theory predicts that quantum fields can influence the geometry of spacetime through their energy-momentum tensor, leading to effects like Hawking radiation.
The framework was developed in the 1970s, notably by Bryce DeWitt and others, as a stepping stone toward a full theory of quantum gravity. It gained prominence with Stephen Hawking's 1974 calculation of black hole radiation, which used semiclassical methods.
In semiclassical gravity, the Einstein field equations are modified to include the expectation value of the quantum energy-momentum tensor as the source of curvature. This means that the quantum state of matter determines the classical spacetime metric, and the metric in turn defines the background on which the quantum fields evolve. The back-reaction of quantum fields on the geometry is computed self-consistently, often using approximations like the large-N expansion or perturbation theory.
It is used in theoretical studies of black hole thermodynamics, cosmological inflation, and the information loss paradox, as well as in quantum field theory in curved spacetime.
Semiclassical gravity predicts that black holes emit thermal radiation and eventually evaporate, but the final stage of evaporation remains unresolved because quantum gravity effects become dominant.















