
8.5 The Discovery of the Neutrino 191
uranium isotope triggers nuclear fission, producing energy plus two or three free
neutrons. These free neutrons can multiply the fission process. If this basic process
is uncontrolled, a bomb is obtained; otherwise, one has a peaceful reactor producing
energy. Each neutron produced in a fission process, if not captured by another
uranium nucleus, decays producing antineutrinos.
During the war, the research center in Los Alamos in the United States existed as
a secret military laboratory where the Manhattan project was developed. After the
war, it became a center of excellence for research in nuclear and particle physics. In
particular, F. Reines and C. Cowan initiated a research project to detect neutrinos in
1951 (Cowan died in 1974; Reines was honored with the Nobel Prize in 1995). It
was called the Poltergeist Project.
As explained before, a large neutrino flux and a method of discriminating the
signal from the background were needed. The initial project, which solved both of
these problems, was to use the explosion of a nuclear bomb to detect neutrinos. The
bomb would produce:
• An intense neutrino flux calculated from the explosion power
• An impulsive neutrino flux in such a small time interval that the signal to noise
ratio would have been very large. The noise, in this case, would be due to the
detected environmental radioactivity
The explosion of a 20-kiloton bomb would generate an antineutrino flux high
enough to be detected with an apparatus located about 50 m underground below
the explosion point. The bomb would be placed on a tower about 30 m high, and
the experiment control room would be (of course) placed at a remote distance. The
possible detector was a huge container filled with a liquid scintillator, which was
called “El Mostro” (the monster).
In 1952, it became clear that a better way was offered by the steady
e
flux
(less intense with respect to the flux produced by a bomb) from a nuclear reactor.
The remaining problem was to detect the reaction (8.19) over the background
due to environmental radioactivity. The new idea was to measure not only the
annihilation of the positron, but also the possible capture of the neutron. The
neutron, once moderated (i.e., slowed down by elastic collisions with other nuclei)
can be captured with high probability by some nuclei (for instance, Cadmium). After
neutron capture, the nuclear isotope is unstable and emits a -ray. The experimental
technique is illustrated in Fig. 8.6. As Cowan said, “instead of detecting a burst of
neutrinos in a second or two coming from the fury of a nuclear explosion, we would
now be able to watch patiently near a reactor and catch one every few hours or so.
And there are many hours available for watching in a month–or a year!”
The Savannah River nuclear reactor, with a power of 150 MW, was chosen for the
experiment. It was possible to install the detector (shown in Fig. 8.7) at about 11 m
from the reactor core, and about 12 m deep. The detector consisted of two containers
of 200 l of water placed between three liquid scintillator containers, each with a
capacity of 1,400 l. This is a small detector compared to the scale of the current
experiments: today, Super-Kamiokande (Sect. 12.8) uses 50,000 tons of water!