In particle physics, the coincidence method (or coincidence technique) is an experimental design through which particle detectors register two or more simultaneous measurements of a particular event through different interaction channels. Detection can be made by sensing the primary particle and/or through the detection of secondary reaction products. Such a method is used to increase the sensitivity of an experiment to a specific particle interaction, reducing conflation with background interactions by creating more degrees of freedom by which the particle in question may interact. The first notable use of the coincidence method was conducted in 1924 by the Bothe–Geiger coincidence experiment.[1]
The higher the rate of interactions or reaction products that can be measured in coincidence, the harder it is to justify such an event occurred from background flux and the higher the experiment's efficiency. As an example, the Cowan and Reines’ neutrino experiment (1956) used a design that featured a four-fold coincidence technique.[2] Particle detectors that rely on measurements of coincidence are often referred to as q-fold, where q is the number of channel measurements which must be triggered to affirm the desired interaction took place.[3] Anti-coincidence counters or "vetos" are often used to filter common backgrounds, such as cosmic rays, from interacting with the primary detection medium. For instance, such a veto is used in the gamma ray observatory COS-B. Detectors relying on coincidence designs are limited by random, chance coincidence events.[4]
Coincidence designs are an essential technique for increasing confidence in signals and reducing random background within a wide range of particle detectors. Common backgrounds include radioactive decay products (beta, alpha, and gamma radiation) and cosmic rays (protons, air showers). Such backgrounds can produce random interactions within a particle detector that may be hard to differentiate from the target particle. If the particle in question is able to trigger multiple channels that are correlated in time or space, it can be determined more likely that the particle is not a background trigger. "Chance" coincidence events may occur, in which all channels are triggered by particles which are not under investigation yet happen to interact with each channel at the same time.[5] In this case, measurements of this chance event may be difficult to separate from measurements of the target events.
A coincidence design must contain two or more measured channels for detecting a particle interaction which can be correlated with each other or the interaction in question over time, space, and/or the properties/products of the interaction. For some experimental setup with q coincidence channels (q-fold coincidence), the rate at which true correlated coincidence events can be measured is given by:
Rq=q\tauq-1
q | |
\prod | |
1 |
Nq
where
Nq
\tau
The rate at which coincidence events are measured
R\rm
R\rm
\epsilon
\epsilon=
R\rm | |
R\rm |
in which case
R\rm
N
R\rm=
q | |
N\prod | |
1 |
\epsilonq
Therefore, the ability of a detector to successfully confirm signals in coincidence is directly proportional to its efficiency.
The use of coincidence detectors in particle physics experiments opened doors to similar methods in nuclear physics, astroparticle physics, and other related fields. A wide variety of operational particle detectors today contain some identifiable form of coincidence or anti-coincidence design.
In 1924, physicists Walther Bothe and Hans Geiger used the coincidence method to probe the Compton scattering of gamma rays and x-rays, a phenomenon whose quantum mechanical nature (see particle-wave duality) with regard to energy conservation was ambiguous at the time.[1] The Bothe–Geiger experiment was the first significant coincidence experiment to test the transfer of energy between the incoming photon and the electron in this process. The experiment utilized two Geiger counters: one to detect the initial recoiling election and one to simultaneously detect a secondary electron recoil caused by the photonic product of the first recoil. This setup included a coincidence circuit which measured the process to
\tau
See main article: Cowan–Reines neutrino experiment.
In 1956, it was known that in order to balance the spin states of a beta decay process, a neutrino of spin 1/2 had to be a product of the reaction
n0 → \nu+p++\beta-
n0
\nu
p+
\beta-
The experiment utilized multiple interaction channels through which the presence of a neutrino (or in this experiment, an antineutrino) could be detected. The antineutrinos would enter a tank of water doped with cadmium chloride and interact with a water molecule's proton. This reaction (
p++\nu- → n0+\beta+
\beta+
\nu-
The invention of the coincidence method enlightened new techniques for measuring high-energy cosmic rays. On such experiment, COS-B, launched in 1975 and featured an anti-coincidence veto for charged particles, as well as three scintillation detectors to measure electron cascades caused by incoming gamma radiation. Therefore, gamma ray interactions could be measured with three-fold coincidence, after having passed a charged particle veto (see Anti-Coincidence).[10]
See main article: Electronic anticoincidence.
The anti-coincidence method, similarly to the coincidence method, helps discriminate background interactions from target signals. However, anti-coincidence designs are used to actively reject non-signal particles rather than affirm signal particles.[14] For instance, anti-coincidence counters can be used to shield charged particles when an experiment is explicitly searching for neutral particles,[15] as in the SuperKamiokande neutrino experiment. These charged particles are often cosmic rays.
Anti-coincidence detectors work by flagging or rejecting any events that trigger one channel of the detector, but not another. For a given rate of coincident particle interactions,
R\rm
R\rm=R\rm-R\rm
where
R\rm
R\rm
Rsuspected
297, 319