Let us assume a quantum state formed by an isolated system which consists of a superposition with
equal amplitude of one configuration of mass
with the center of mass at
, and another
configuration of the same mass with the center of mass at
. The semiclassical theory as described by
the semiclassical Einstein equation predicts that the center of mass of the gravitational field of the system is
centered at
. However, one would expect that if we send a succession of test particles to probe
the gravitational field of the above system, half of the time they would react to a gravitational
field of mass
centered at
and half of the time to the field centered at
. The
two predictions are clearly different; note that the fluctuation in the position of the center of
masses is of the order of
. Although this example raises the issue of how to place
the importance of fluctuations to the mean, a word of caution should be added to the effect
that it should not be taken too literally. In fact, if the previous masses are macroscopic, the
quantum system decoheres very quickly [306
, 307
] and instead of being described by a pure
quantum state it is described by a density matrix which diagonalizes in a certain pointer basis. For
observables associated to such a pointer basis, the density matrix description is equivalent to that
provided by a statistical ensemble. The results will differ, in any case, from the semiclassical
prediction.
In other words, one would expect that a stochastic source that describes the quantum fluctuations
should enter into the semiclassical equations. A significant step in this direction was made in [148
],
where it was proposed to view the backreaction problem in the framework of an open quantum
system: the quantum fields seen as the “environment” and the gravitational field as the “system”.
Following this proposal a systematic study of the connection between semiclassical gravity and open
quantum systems resulted in the development of a new conceptual and technical framework where
(semiclassical) Einstein–Langevin equations were derived [44
, 157
, 167
, 58
, 59
, 38
, 202
]. The key
technical factor to most of these results was the use of the influence functional method of Feynman
and Vernon [89
], when only the coarse-grained effect of the environment on the system is of
interest. Note that the word semiclassical put in parentheses refers to the fact that the noise
source in the Einstein–Langevin equation arises from the quantum field, while the background
spacetime is classical; generally we will not carry this word since there is no confusion that
the source which contributes to the stochastic features of this theory comes from quantum
fields.
In the language of the consistent histories formulation of quantum
mechanics [114, 221, 222, 223, 224, 225, 226, 105, 125, 83
, 120
, 122
, 30, 239, 278, 170, 171, 172, 121, 81, 82, 185, 186, 187, 173]
for the existence of a semiclassical regime for the dynamics of the system, one needs two requirements: The
first is decoherence, which guarantees that probabilities can be consistently assigned to histories describing
the evolution of the system, and the second is that these probabilities should peak near histories which
correspond to solutions of classical equations of motion. The effect of the environment is crucial, on the one
hand, to provide decoherence and, on the other hand, to produce both dissipation and noise to the system
through backreaction, thus inducing a semiclassical stochastic dynamics on the system. As shown by
different authors [106
, 303
, 304
, 305
, 306
, 180
, 33
, 279
, 307
, 109
], indeed over a long history predating
the current revival of decoherence, stochastic semiclassical equations are obtained in an open quantum
system after a coarse graining of the environmental degrees of freedom and a further coarse graining in the
system variables. It is expected but has not yet been shown that this mechanism could also work for
decoherence and classicalization of the metric field. Thus far, the analogy could be made formally [206
] or
under certain assumptions, such as adopting the Born–Oppenheimer approximation in quantum
cosmology [237
, 238
].
An alternative axiomatic approach to the Einstein–Langevin equation without invoking the open system
paradigm was later suggested, based on the formulation of a self-consistent dynamical equation for a
perturbative extension of semiclassical gravity able to account for the lowest order stress-energy fluctuations
of matter fields [207
]. It was shown that the same equation could be derived, in this general case, from the
influence functional of Feynman and Vernon [208
]. The field equation is deduced via an effective action
which is computed assuming that the gravitational field is a c-number. The important new element
in the derivation of the Einstein–Langevin equation, and of the stochastic gravity theory, is
the physical observable that measures the stress-energy fluctuations, namely, the expectation
value of the symmetrized bi-tensor constructed with the stress-energy tensor operator: the noise
kernel. It is interesting to note that the Einstein–Langevin equation can also be understood
as a useful intermediary tool to compute symmetrized two-point correlations of the quantum
metric perturbations on the semiclassical background, independent of a suitable classicalization
mechanism [255
].
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