The vast majority of experimental evidence for the success of Quantum Field Theory in describing the elementary particles of nature comes from the comparison of particle collisions with calculations of scattering "amplitudes". These amplitudes are numbers which describe the relative importance of various elementary field interactions in contributing to the total process of one particle colliding with (scattering off of) another. The amplitudes are added together and the dependence of their total magnitude on various physical variables, such as scattering angle, is compared with that actually observed. The total amplitude which describes the transition from an initial set of states (the incoming particles) to a final set of states (the outgoing particles) is equivalent to the statistical correlation of the incoming and outgoing states weighted by the exponent of the classical action associated with the fields. Hence we actually compute the dependence of field correlations on physical parameters. It is interesting to note that the total amplitude must be the sum of contributions from every topologically distinct elementary process which obeys the relevant conservation laws.
It is important to understand what the numerical outcomes of measurements depend on:
Quantum Gravity Concept Map Index:
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©1997, Kenneth R. Koehler. All Rights Reserved.