Automatic Calculation of Particle Interaction or Decay - History

History

The idea of automation of the calculations in high-energy physics is not new. It dates back to the 1960s when packages such as SCHOONSCHIP and then REDUCE had been developed.

These are symbolic manipulation codes that automatize the algebraic parts of a matrix element evaluation, like traces on Dirac matrices and contraction of Lorentz indices. Such codes have evolved quite a lot with applications not only optimized for high-energy physics like FORM but also more general purpose programs like Mathematica and Maple.

Generation of QED Feynman graphs at any order in the coupling constant was automatized in the late 70's. One of the first major application of these early developments in this field was the calculation of the anomalous magnetic moments of the electron and the muon. The first automatic system incorporating all the steps for the calculation of a cross section, from Feynman graph generation, amplitude generation through a REDUCE source code that produces a FORTRAN code, phase space integration and event generation with BASES/SPRING is GRAND. It was limited to tree-level processes in QED. In the early nineties, a few groups started to develop packages aiming at the automation in the SM.

Read more about this topic:  Automatic Calculation Of Particle Interaction Or Decay

Famous quotes containing the word history:

    “All history is a record of the power of minorities, and of minorities of one.”
    —Ralph Waldo Emerson (1803–1882)

    “History has neither the venerableness of antiquity, nor the freshness of the modern. It does as if it would go to the beginning of things, which natural history might with reason assume to do; but consider the Universal History, and then tell us,—when did burdock and plantain sprout first?”
    —Henry David Thoreau (1817–1862)

    “If usually the “present age” is no very long time, still, at our pleasure, or in the service of some such unity of meaning as the history of civilization, or the study of geology, may suggest, we may conceive the present as extending over many centuries, or over a hundred thousand years.”
    —Josiah Royce (1855–1916)