Classical physics from quantum fields
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Ross, Alasdair
Abstract
Gravitational wave physics is now well established as an experimental science,
no longer existing only in the minds and blackboards of the theorist. There
is an abundance of events being detected with a very high accuracy by the
LIGO/Virgo/KAGRA collaboration. This necessitates the development of
innovative techniques for producing very high precision calculations. Motivated
by the Double Copy, a relation between scattering amplitudes in gauge theory and
gravity, an amplitudes based approach seems to be a promising avenue to pursue.
Yet amplitudes are quantum objects and gravitational waves are classical; there
must be a bridge between these two regimes. This leads us to the topic of this
thesis - how can we extract classical observable quantities directly from quantum
scattering amplitudes.
We begin by reviewing the KMOC formalism for computing classical observables
from amplitudes. We investigate how, by imposing classically sensible minimal
uncertainty constraints on observables, we can learn about amplitudes in the
classical limit. Black holes in general will spin, and so including spin effects into
the calculations of gravitational waveforms is important. Motivated by this we
apply the KMOC formalism to a theory of scalars carrying an SU(N) colour
charge. In this theory we compute changes in and radiation of momentum and
also colour charge. This requires a detour into the study of coherent states which
are another key tool to study classical from quantum.
An older approach to semi-classical physics is the eikonal method which has
recently received a surge of interest. It allows one to easily compute the scattering
angle and impulse during a scattering event. We review the eikonal resummation
and use to describe the final state after such a (conservative) scattering event.
Returning to coherent states we propose an ansatz for a quantum final state,
parametrised only by the eikonal phase and a coherent state parameter, which
captures all the necessary data to compute the radiation in the classical limit.
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