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Hunting Neutrinos in Arizona
A group of researchers in the Physics Department at Stanford,
led by Professor Giorgio
Gratta, are working in collaboration with Caltech and the
University of Alabama on a neutrino oscillation experiment using
neutrinos produced by the Palo Verde Nuclear Generating Station
near Phoenix, Arizona.
Neutrinos are very fundamental, yet little known elementary
particles produced in radioactive beta decay. Among the things
we do not know is whether or not they have a finite mass (if
so, it would be thousands of times smaller than the electron
mass). If they have a small mass, it is predicted that there
would be "oscillations" between different neutrino species.
If discovered, neutrino oscillations would shed light on some
of the most essential issues of modern particle physics, ranging
from a better general understanding of lepton masses to the
exploration of new physics beyond the Standard Model of Elementary
Particles. In addition, the pheonomenon of oscillations would
have important consequences in astrophysics and cosmology.
The neutrino associated with the electron was discovered in
the 1950's by Frederick Reines at the Savannah River Reactor.
Reines, along with Martin Perl of SLAC, who discovered the
tau lepton in the 1970's, was awarded the Nobel Prize last
year. The neutrino associated with the muon was discovered
in the 1960's at Brookhaven National Laboratory by Leon Lederman,
Mel Schwartz and Jack Steinberger, who received the Nobel
Prize for their work in 1988.
Experiments using both particle accelerators and nuclear
reactors have been carried out extensively in the last twenty
years, without finding evidence for neutrino oscillations.
However, recent evidence has been collected on two effects
that could point to oscillations: the solar neutrino puzzle
and the anomaly observed in atmospheric neutrinos. While in
the first case, an interpretation in terms of neutrino oscillations
would lead to mixing parameters too small to be directly observable
in an Earth-based experiment, the atmospheric neutrino anomaly
points to a region in parameter space that is accessible using
MeV-energy neutrinos and a baseline of about one kilometer.
The Palo Verde experiment will use low energy electron (anti)neutrinos
from the 11 GW nuclear reactors. The detector will be located
at about 1 km distance from the reactors in order to explore
very long oscillation lengths and hence, small neutrino masses.
At this distance, the neutrino flux is relatively modest,
and in order to make a measurement, a large detector is needed.
A 12 ton liquid scintillator detector will be used to detect
about 25 neutrinos per day from the reactor. Since the signal
is so low, good shielding is required to protect from cosmic
rays, which can create a false neutrino signature. This requirement
makes it imperative that the detector be placed underground,
shielded by the earth.
A 25 meter deep underground vault has been built, which
is large enough to contain the detector surrounded by pure
water shields and active cosmic ray veto counters. The lab
and its access tunnel are shown in these photographs. Toward
year end, the first part of the detector will be installed
under the Arizona desert. Some preliminary answers to this
quest for neutrino oscillations should be found by the summer
of 1998...stay tuned!
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| Inside the access tunnel to the neutrino lab. |
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| Underground structures of the Alabama-Caltech-Stanford
Neutrino Laboratory. The detector will sit in the concrete
bunker on the left. The long pipe on the right of the
photo is the tunnel used to access the lab. |
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