Power producing nuclear reactors are technological and engineering
facilities, whose primary purpose has nothing to do with basic research.
However, they turned out to be indispensible in one area of probing Nature’s
innermost secrets, namely to find out whether or not the neutrino has a
non-zero rest mass.
Neutrinos are one of the most elusive particles in nature. They are
neutral (lack electric charge) and interact with matter extremely weakly; they
can even penetrate the whole Earth without a noticeable chance of being
absorbed. For the very same reason, they are extremely difficult to detect.
They exist in three different forms (in elementary physics jargon called
”flavours”): electron-, muon- and tauneutrinos.
For a long time, one believed that neutrinos, just as photons, have no
rest mass. But there have also been speculations, as well as some indirect
indications, that they might have a non-zero, even if exceedingly small, rest
mass. According to theory, these three types of neutrinos are built up from three
different mass states. If these three masses are different, then the three
different flavours should oscillate among each other. If one can observe oscillations
between two neutrino types, it means that they have different masses, hence at
least one of them must be larger than zero.
The simplest way to verify oscillations experimentally is to prove the
absence of a particular type of neutrinos at a certain distance from a source,
which emits just that type of neutrinos. However, the experiment can only be
successful if the distance between the source and the detector matches the
frequency of the oscillations. For maximum success there is an optimal minimum
distance.
The first proof of the neutrino oscillations, and hence that of the
existence of the neutrino mass, came from the Super-Kamiokande experiment in
central Honshu in Japan (see the map below, Fig. 1). One proved the
oscillations between muon- and tau-neutrinos, by measuring atmospheric
neutrinos, which are given rise by cosmic radiation. With the help of direction
sensitive detection methods, one performed measurements partly on neutrinos
generated above the detection site, i.e. close to the detectors, and partly on
neutrinos which were generated on the diagonally opposite side of the Earth. The
distance, i.e. the diameter of the Earth, was perfect for confirming the
existence of oscillations through the difference in the detection intensity
between the two detectors. This is one of the two measurements for which the Nobel prize in
physics was awarded in 2015.
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Figure 1. The site of the Kamioka and Super-Kamiokande
experiment i Honshu, Japan, with the site of several
nuclear reactors indicated by a grey ring around the
detector facility
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However, for completeness and certainty, the other two types of neutrino
oscillations, both related to electron neutrinos, had also to be shown. These
were much harder to achieve, since there was no suitable source with a suitable
distance to a detector in such a natural way as for the muon-tau-neutrino
oscillations. It is at this point that nuclear reactors came in to the picture.
Nuclear reactors are very intensive sources of electron-neutrinos (actually, antineutrinos, but this is an unimportant detail in the context), hence
they are very suitable for measuring both
electron-muonneutrino as well as electron-tauneutrino-oscillations. It
was even suggested that the operation of nuclear reactors can be monitored from
a distance by measuring the neutrino flux.
It turned out that the site of the Super-Kamiokande-experiment was very
fortunate in this respect. Namely, there are a number of nuclear reactors in
form of a ring around the detector facility, at a distance of between 140 to
180 km (see Fig. 1 above). (These measurements were performed about 8 years
before the Fukushima accident, hence all reactors were in operation then). The
detector was re-built for the purpose of this experiment, and was re-named KamLAND.
It was in this experiment that the oscillations between electron- and muon-neutrinos
were verified. A paper on these experiments, published in the Physical Review
Letters by the research group led by Professor Atsuto Suzuki at Tohoku
University, Sendai, became the most frequently cited paper during a period in 2003.
The use of nuclear reactors is mentioned even in the title of the paper: ”First
results from KamLAND: Evidence for reactor antineutrino disappearance” (Fig. 2).
Now there was only the third type of oscillations to be found, namely
that between the electron- and tau-neutrinos.
And even here the experiment had to be based on reactor neutrinos, but the
reactors around KamLAND were not at a suitable distance. It was clear that the
source should lie much closer to the detectors. At that point, the neutrino
physicists asked for help from reactor physicists, and this is how I came into
the picture.
Figure 2. Photo of the author and data of the
pioneering publication on the detection of reactor neutrino oscillations. From
a slide, courtesy of Prof. A. Suzuki.
It was on one of my numerous visits to Japan,
in 2005, when I was about to meet my colleagues at Tohoku University in Sendai.
I got a message from my first host and long-standing friend, Prof. Kojiro
Nishina of Nagoya University, that the Vice President of Tohoku University, Prof.
A. Suzuki, who found the second type of oscillations, wanted to meet me. He was
trying to find a strong, movable neutrino source. During our meeting he asked me
if it was possible to construct a movable nuclear reactor for neutrino
experiments, in the race for finding the third type of neutrino oscillations.
His idea was to move the reactor under the ground,
presumably vertically, since it is not easy to move a nuclear reactor on the
surface in densely populated areas. That was no easy question. The idea of SMRs (compact small- and medium size
reactors), which exist now at least on the drawing board, did not exist then
yet. I recommended to use an accelerator driven subcritical system, which has
good safety margins and can be shut down and start up again between the moves.
Nuclear vessels, such as submarines, icebreakers or aircraft carriers, could
not come into the question, since the distance to the closes coastline was too
long.
The KamLAND project with a movable nuclear
reactor has not come about, the technical, safety and financial problems were
simply prohibitively large. The third types of oscillations were instead
verified not by putting a source to a suitable distance to an existing
detector, rather by building a detector facility close to a large nuclear
reactor site with several reactors. These experiments were performed first in
China in 2012, then even in France and later on in South Korea. In all three measurements,
neutrinos from nuclear power plants were used. The first, decisive experiments
were made in China, around the six reactors of the Daya Bay site, with six
antineutrino detectors. The distance between the detectors and the reactors
varied between 0.5 and 1.5 kms. The movable reactor which Prof. Suzuki was
thinking of, would not need to travel a long distance.
Personally, I was glad to hear about the
experiments in KamLAND in Japan and Daya Bay in China, for the double reason
that partly now I am a reactor physicist, but partly because I have some past
in theoretical physics. I studied particle physics at the Lorand Eötvös
University in Budapest and had strong interaction as the special field. My
master thesis had the title ”Dual resonance model with SU(6)-symmetry for meson
scattering”. Neutrinos interact through the weak forces, so my area was at a
completely different area. Despite of this and that I have left the area of
theoretical physics long ago, I am naturally delighted that my present field of
work could contribute to fundamental science, and also that the question of
neutrino oscillations and neutrino mass is now finally settled :) .