Questions and Answers about Neutrinos
and the Super-Kamiokande Discovery
prepared by
John Learned,
University of Hawaii professor of physics, Super-Kamiokande collaborator
WHAT ARE NEUTRINOS?
Neutrinos are the least
massive elementary particle in the set of building blocks of nature,
which include six quarks (down, up, strange, charmed, bottom and
top) and leptons. Neutrinos have no charge and are in the family of
neutral leptons. They do not feel the strong force that binds quarks
into protons and neutrons, and protons and neutrons into
nuclei.
There are three kinds, or "flavors" as they
are called, of neutrinos electron, muon and tau. There are also
three anti-neutrinos of the same flavors. The neutrinos get their
names from their charged lepton brethren in order of increasing
mass, the electron, muon and tau. Many theoreticians have thought
the mass of neutrinos to be zero. The findings of such small values
is both a mystery and undoubtedly a clue.
WHERE DO NEUTRINOS COME FROM?
Neutrinos are
produced in many circumstances. The ones we are concerned with here
are the result of cosmic rays hitting the earth's atmosphere.
The primary cosmic rays make a spray of secondary particles, all
traveling close to the same direction and at nearly the speed of
light. Some of these secondaries (mostly pi and K mesons, and
tertiary muons) decay, resulting in neutrinos.
The charged
particles and photons get absorbed in the atmosphere or ground.
There are quite a few of these neutrinos, despite being down the
decay chain from the incoming cosmic rays‹of the energies we are
concerned with, about 100 of the cosmic-ray induced neutrinos from
the atmosphere pass through you each second. (Yet there is only a
one in 10 chance that one will hit a nucleon in your body during
your lifetime.)
HOW ARE NEUTRINOS DETECTED?
Neutrinos generally go
right through the earth unscattered, but occasionally one interacts
in the Super-Kamiokande detector, typically striking a quark in the
nucleus of an oxygen atom within a water molecule and snatching a
plus or minus charge to become either a muon or an electron. That
charged particle travels some distance in the water. As it moves at
high speed, it radiates Cherenkov light, which is detected with the
photomultipliers. Muons travel relatively straight and produce a
rather clean ring image on the wall. Electrons are distinguished as
they scatter and make fuzzier images, which can be recognized with
about 98 percent accuracy. On average, Super-Kamiokande catches one
atmospheric neutrino every 90 minutes.
WHAT IS THE ATMOSPHERIC NEUTRINO ANOMALY?
Because of the
well known nature of neutrino production, we knew that the there
should have been twice as many muon neutrinos as electron neutrinos
from the atmosphere. Yet, in observations first made more than ten
years ago in the IMB and Kamioka detectors and later confirmed, the
ratio of muon to electron neutrino interactions was closer to
1:1.
Many explanations have been proposed for this
"atmospheric neutrino anomaly." Hypotheses included
greater abundance of electron neutrinos (perhaps from some
unexpected though seemingly unlikely extraterrestrial source or
nucleon decay), a problem with calculations of the neutrino flux or
neutrino interaction rates or some problem unique to water
detectors. Scientists suspected that oscillations might be the
cause, but had no compelling, exclusive arguments. Some
experimenters thought the problem would be resolved as an
experimental artifact.
HOW WAS THE ANOMALY RESOLVED?
The new
Super-Kamiokande data show the anomaly is due specifically to a
deficit in the muon neutrinos--more come from "overhead"
than come "up" through the earth. Super-Kamiokande
analysis shows this can only be the result of the muon neutrino
oscillating into another type of neutrino during long flight
paths. Neutrinos coming through the earth (13,000 km) travel further
and have greater distance in which to change from a muon neutrino to
another neutrino and back again, through many cycles at typical
energies. Neutrinos coming from overhead (20 km) have not had time
to oscillate before reaching the detector. Neutrinos of higher
energies oscillate more slowly. The net result is that we see muon
neutrinos disappearing in proportion to their flight path and
inversely proportional to their energy. This is the hallmark of the
hypothesized oscillation phenomenon.
WHAT ARE OSCILLATIONS?
Neutrino oscillations are a
peculiar quantum mechanical effect. It's hard to find a good
macroscopic analogy as it has to do with the particle-wave duality
of fundamental matter.
We only know what a particle is
by the way it is produced or interacts; that is how we name
it. When a pion decays, it results in a muon and a muon
(anti)neutrino; when a neutron decays, it results in a proton, an
electron and an electron (anti)neutrino. When a muon is produced by
a neutrino we know it was produced by a muon neutrino. And so
on.
Another way to know a particle is by weight, as expressed by
speed given a certain amount of energy and also as it is attracted
by gravity. Usually these identifications are the same for each
particle, but muon neutrinos appear to be very mixed up.
If we
create a muon neutrino beam at an accelerator and pass it through a
kilometer of earth and iron shielding to eliminate all the charged
particles, we see muons occasionally produced in a detector, in the
right direction and just after the particle beam pulse strikes the
production target. Neutrinos are well known particles in this sense,
and their interactions have been studied at the particle
accelerators, underground and at reactors for more than 30
years.
The strange situation for neutrinos, different from all
the other elementary particles, is that the state of the particle
which we call the muon neutrino may not be the same as the particle
mass state. Neutrinos are a Dr. Jekyll and Mr. Hyde sort of
affair. The muon neutrino is apparently composed of two different
masses.
The muon neutrino may be composed of half each of two
states of slightly different mass that oscillate in and out of phase
with each other as they travel along, alternately interacting as a
muon neutrino and then making a tau neutrino. Which is observed
depends on where the detector intercepts the beam.
We have yet
to do this experimentally using beams of neutrinos‹the distance
for oscillations (hundreds of miles) has been too long. New
experiments are being proposed based upon the information we are
finding, however.
WHAT DO OTHER STUDIES SHOW ABOUT NEUTRINO MASS AND
OSCILLATIONS?
The mass of neutrinos and the possibility of
their oscillations has eluded researchers for many
years. Accelerator-based experiments and others using reactors and
radioactive sources have so far only yielded upper limits on
neutrino masses, and no oscillations have been firmly observed.
Many experiments have sought to directly measure neutrino mass,
which is very difficult. We know neutrinos are light, far less than
the mass of the electron. Indeed, many theoreticians have thought
neutrino mass would prove to be zero.
WHAT DOES SUPER-KAMIOKANDE DATA SHOW?
Every proposed
alternate hypothesis explaining the atmospheric neutrino anomaly
(detector systematics, input physics, alternative physics
explanations) has been definitively ruled out. The Super-Kamiokande
team spent the last year carefully examining every possible problem
in the data that might confound their result; none was
found. Only the hypothesis of muon neutrino oscillations fits
the data, and it fits very well.
The paper being submitted to
Physical Review Letters contains results based upon analysis
of 4,700 neutrino interactions collected over 537 days that meets
the rules of probability for a correct hypothesis. All systematic
parameters lie within expectations; the results are robust
insensitive to variations in event selection criteria, data sets,
fitting algorithms and multiple independent analyses. In June 2000
the Collabortatoin updated the oscillations analysis with 1144 days of
data, with the conclusions becoming statistically even stronger.
WHAT DO THE MUON NEUTRINOS OSCILLATE WITH?
Our data
tell us unambiguously that muon neutrinos are oscillating, though we
could not at first be sure with what other neutrino state. Various
tests, which will be published in late 2000, now inidicate that the
oscillating partner of the muon neutrino is NOT a new sterile
neutrino, but is entirely consistent with being the tau neutrino.
It remains to identify the appearance of the tau neutrino, but
preliminary indications are encouraging.
ARE THE NEW FINDINGS CONSISTENT WITH OTHER DATA?
For
the very same reason we only obtained these results in 1998, there
is not much other data which could directly confront these
results. Preliminary results suggest consistency with re-analysis of
data from the IMB experiment. Moreover in 1998 and 1999 there
appeared strongly supporting evidence now from the Soudan II
(Minnesota, USA) and MACRO (Gran Sasso, Italy) experiments. In
summary, no data which gainsays the results reported and there is
supportive evidence.
ACKNOWLEDGMENTS
Super-Kamiokande research was mostly
funded by Japan's Mombusho (Ministry of Education, Science, Sports
and Culture) and the U.S. Department of Energy, Division of High
Energy Physics. The project was made possible by significant support
from the Kamioka Mining and Smelting Company and many other
corporations and individuals.
Locally, we particularly acknowledge significant support from the
University of Hawaii, particularly the Department of Physics and
Astronomy and the dean of the School of Natural Sciences. Many
colleagues in the department, the Institute for Astronomy and the
School of Ocean and Earth Sciences at UH have contributed to this
work in various supportive ways over many years.