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Neutrinos and neutrino mass from a supernovaIn
1987, a supernova exploded in the nearby Large Magellanic Cloud. Bahcall, Dar
and Piran were quick to point out in Nature that a neutrino burst from
the collapsing star should have reached Earth and that, if detected, it would
provide "a unique opportunity to test the theory of neutron star formation
in Type II supernova explosions". A note added in proof to their 'Scientific
Correspondence' confirmed that the Kamiokande neutrino detector in Japan had indeed
picked up a signal. The Kamiokande data also afforded the first opportunity to
determine the mass of the electron neutrino from astronomical data. A few weeks
later, in a letter to Nature, Bahcall and Glashow had set an upper limit
on the electron neutrino mass at 11 eV. Nature 326, 135136;
476477 (1987) | click
here for a PDF version (496 K) | | Neutrinos from
the recent LMC supernovaSirThe supernova explosion
that was observed recently1 in the nearby Large
Magellanic Cloud (LMC) provides a unique opportunity to test the theory of neutron
star formation in Type II supernova explosions. In particular, one can investigate
the prediction that almost all of the gravitational binding energy of the residue
neutron star (~3×1053 erg) was radiated within a few seconds
in the form of ~1058 neutrinos with average energy ~1015 Me V.
Here, we calculate the expected neutrino signals in terrestrial detectors which,
according to the standard supernova theory2–10,
should have been observed during a short period (~1 s) before the onset of the
optical supernova. (A measurement of the time delay between the first neutrino
and optical pulses would be of great importance for our understanding of supernovae.)
We also show how information on the fundamental properties of neutrinos (their
life-times, masses and mixings, and their magnetic moments) can be obtained from
neutrino observations of the LMC supernova. The number of neutrino-induced events
in a terrestrial detector due to differential fluxes df/dE
of neutrinos of types
is given by
where ni is the number of particles of type j
(atomic nuclei and electrons) in the target and s(j)
are their cross-sections for relevant reactions which depend on the neutrino type
and on the neutrino energy. Recently Wilson7
and Wilson et al.10 have calculated the
collapse of massive stars of 10, 15 and 25 M
and found that the predicted time-averaged neutrino signal does not vary greatly
from star to star. In Table 1 we list the neutrino fluxes at
the source as calculated by Wilson for a supernova explosion of a 25 M
star with a 1.6 M
iron core and the fluxes expected at a distance of 50 kpc from the supernova. We have calculated
the event rates in existing solar neutrino detectors using the spectra and fluxes
of Wilson7,10 and neutrino
cross-sections from Bahcall (ref. 11 and unpublished data).
Kamiokande II12, which contains 3 kt of water,
should experience about 50 events with a positron recoil energy in excess of 10
Me V. The events should all be concentrated within a few seconds at an epoch that
was a short time before the onset of the optical supernova on 24 February 1987.
The high time resolution of the detector and the bunching in time of the real
events should make the signal stand out above noise by a large factor. The 140-t
liquid-scintillator detectors of the University of Pennsylvania13
in the Homestake mine and the 90-t scintillator detector in the Mont Blanc Tunnel14
should have seen about 3 events each if the standard supernova theory is correct.
This signal is marginally detectable because of the high time resolution of the
experiments. A comparison of the arrival times for neutrino events seen in different
detectors will provide a crucial test of the physical reality of the observations;
the neutrinos should arrive essentially simultaneously at all terrestrial detectors.
For the 37Cl tank of Davis15, only
one additional 37Ar atom is expected to be produced, a signal which
would not be detectable. Standard supernova theory may be wrong.
It is more difficult to calculate how a star explodes than to estimate how the
Sun shines and we do have the solar neutrino problem. To show the power of observations
with existing neutrino detectors, we assume that 3×1053 ergs
are emitted as thermal neutrinos (temperature T) and that the energy is
distributed equally among all neutrino flavours. We find the following total number
of events for the three different classes of neutrino detector mentioned above:
(The
last relation overestimates the detection rate for temperatures above 5 Me V;
it is too large by a factor of about 2 at T = 10 Me V). A thermal spectrum
with a typical energy of T~1015 Me V would produce an event rate
for the 37Cl experiment that is an order of magnitude larger than the
standard supernova model. A number of authors, motivated by
the solar neutrino problem16, have suggested recently
that the neutrino has properties not included in the simplest electroweak model.
Explanations of the solar neutrino problem of this type include neutrino decay17,
resonant neutrino oscillations18 and a large neutrino
magnetic moment (L.B. Okun et al., preprint ITEP, 1986). The LMC supernova
can be used to test these suggestions. If the ~10 Me V 8B
solar neutrinos decay significantly during their flight from the Sun to Earth,
then essentially no neutrinos will survive the flight from the LMC supernova at
a distance of 50 kpc. Consequently, the neutrino decay hypothesis which may explain
the solar neutrino problem predicts no neutrino signals in underground neutrino
detectors from the recent LMC supernova. If neutrinos are detected, their life
times in the laboratory frame must exceed 105 years. Neutrino
oscillations increase the expected signals because the average energy of the nms
and nts is
about twice that of the nes (see Table
1). Electron neutrinos generate most of the signals and the interaction cross-sections
increase with incident neutrino energy. If the nms
and nts oscillate
into nes (and vice versa) after leaving
the neutron star (for example, through the MSW18
effect on positrons and electrons in the outer layers of the star) then the incident
nes will have higher energies and higher
cross-sections and consequently will have more events in terrestrial detectors.
Complete interchange between nes and nts
or nms will
increase the signals in water and liquid scintillators by about a factor of two
but will still produce only ~1 event in Davis's solar neutrino experiment. Dar19
has shown that if the neutrino magnetic moment is in the range 10−10
to 10−12 Bohr magnetons (which explains the solar neutrino problem
(L.B. Okun et al. preprint ITEP, 1986)), then relatively-high-energy neutrinos
with a thermal spectrum can escape from a supernova explosion as a result of magnetic
interactions with electrons. A conservative assumption, within this non-standard
picture, is that the ne neutrinos are emitted
with a temperature in excess of 10 Me V (and with about half the fluxes assumed
for the thermal case cited above) (see ref. 19). The event
rates for this model can be obtained from equation (2) by substituting the relevant
temperature and dividing by two (to correct for smaller fluxes). The
collapse event produces a fluence of ~3×1058 (mi/T)3/2e−m/T
of neutrinos of flavours i with mass mi. This flux contains
a significant amount of energy if the neutrino mass, mi, is
less than a few hundred MeV. If these massive neutrinos are unstable and decay
electromagnetically (see refs 20–22),
for example, via nH→ne+e++e−
or other electromagnetic decay modes, ~1053f(mi/T)3/2e−mi/T
ergs will be produced in electron–positron pairs and g-rays
between the Earth and the supernova (f = 1 if the neutrino life time, t,
is shorter than 5×1012s, the flight time from the supernova to
the Earth, and f = t/5×1012
otherwise). In order to observe an electromagnetic signal from this decay, it
must take place outside the collapsing star (t 103s).
If more than 10−12/[f(mi/T)3/2e−mi/T]
of this energy is converted to g-rays, within one
second (either by direct decay or by rapid electronpositron annihilation),
we should detect a g-ray burst coincident with the
n-signal. The absence of such a burst coincident with
the &n;-signal can be used to eliminate electromagnetic
decay modes of neutrinos with masses in the range of one to a few hundred Me V
and lifetimes larger than ~103s. Higher-energy neutrinos
will arrive at the Earth before lower-energy neutrinos if the neutrino has a finite
mass. However, this time delay, ~0.01(mn/1
eV)2(10 Me V/En)2s,
is too small to be observable for the LMC supernova. A yet unknown,
but potentially significant, fraction of the released energy might be emitted
as gravitational radiation. The gravitational wave emission depends strongly on
the asymmetry of the collapse and in particular on the amount of rotation of the
core. Even with the most optimistic assumptions about gravitational radiation
emission, Egr = 0.01 Mcore 0.016
M ,
and h = Dl/l 0.7×10−18,
the LMC supernova is just below the sensitivity of current detectors. However,
it is interesting to ask whether gravitational radiation would have been seen
by next generation detectors (such as the proposed Caltech/MIT interferometer)
with a sensitivity of 10−21. At low angular momentum, the gravitiational
radiation emissivity scales23 like J4.
Therefore, the LMC supernova would have been detected even if the core was rotating
only at 1/30 of its breakup speed, which is as slow as the Crab pulsar today. Note
added in proof: Since this paper was received on 2 March the neutrino burst
was found by the Kamiokande experimental group, with properties generally consistent
with the calculated expectations. J.N. BAHCALL The
Institute for Advanced Study, Princeton, New Jersey 08540, USA A.
DAR* Department of Physics and Space, Technion,
Haifa, Israel T. PIRAN* Racah
Institute for Physics, Hebrew University, Jerusalem, Israel *Present
address: The Institute for Advanced Study, Princeton, New Jersey 08540, USA.
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Upper
limit on the mass of the electron neutrinoJ. N. Bahcall
& S. L. Glashow The Institute for Advanced Study, Princeton, New Jersey,
USA Harvard University, Cambridge, Masachusetts 02138, USA The historic
detection by the Kamiokande-II collaboration1
and the IMB collaboration2 of neutrinos from the
Large Magellanic Cloud (LMC) supernova provides the first opportunity to determine
the mass, ,
of the electron neutrino from astronomical observations. Here we show that ,
is less than 11 eV, provided only that propagation effects have not conspired
to sharpen, by more than a factor of two the narrow pulse-width of neutrinos,
observed by the Kamiokande-II collaboration from the LMC supernova. This result
improves on the laboratory limit on ,
and confirms the view that electron neutrinos do not constitute the major component
of the matter density of the Universe. Many authors have
discussed the fact that higher energy neutrinos from a distant supernova will
arrive at Earth before lower energy neutrinos if the neutrino has a finite mass3,4.
For the recently observed LMC supernova, the additional travel time, Dt,
that is required for a neutrino of energy E because it has a mass ,
where d is distance to the LMC:  For
any given neutrino mass, one can calculate from equation (1) the emission time
(offset by the light travel time) at the star for each neutrino that causes an
observable event. The data contain no further information. How does one decide
if the calculated departure times are 'acceptable'? Previous authors have not
discussed this question. Without some assumption about what
is physically or astronomically plausible, one cannot proceed further. We do not
have any a priori knowledge of the departure times of the neutrinos. Whatever
the neutrino mass, the complicated nuclear and hydrodynamic processes occurring
in the explosive formation of the neutron star might somehow yield a sequence
of emission times in just such a way as to produce the sharply peaked time structure
seen at Kamioka. Indeed, our analysis is based solely on the assumption that the
narrow (in time) observed pulse is not an accident resulting from propagation
effects. Before describing our method, we will summarize what
is known about the energies and arrival times of the observed Kamiokande-II events.
In both these water detectors, the dominant events are1,2,5
absorption by protons
and ne, scattering by electrons. The
first eight neutrino events arrived within less than 2 seconds, followed by a
period of 7 seconds in which no neutrinos were detected. There were then three
less certain neutrino events in the next 3 seconds. In the initial two-second
pulse, five of the eight events were observed in the first 0.5 s. The events corresponded
to measured positron (or electron) energies ranging from 7.5 MeV to 35 MeV, with
typical uncertainties of the order of 20%. (In deriving mass limits, we have converted
the observed (positron or electron) energies to neutrino energies by supposing
that each event was due to absorption on protons by antineutrinos. The IMB events
reported so far are all relatively high in energy ( 20
MeV) and are therefore less useful in setting limits on the neutrino mass. If
the observed pulse duration were caused solely by the mass of the neutrino, then
the higher energy events would have arrived first. This was not observed. The
time-ordered sequence of positron (or electron) energies was (all in MeV) 20,
13.5, 7.5, 9.2, 12.8, 35.4, 21.0, 19.8, 8.6, 13.0 and 8.9. Two of the lowest energy
events (7.5 MeV and 9.2 MeV) preceded by 1.2 s three higher energy events (35
MeV, 21 MeV and 19.8 MeV). We conclude that the duration of the pulse at the source
was at least 1.2 s and could have been (for zero neutrino mass) as long as the
entire observed pulse. The only assumption that we will make
is that propagation effects did not sharpen the pulse width of the observed neutrino
events by more than a factor of two. Thus the eight events which were detected
at Earth in the initial two seconds of the pulse are presumed not to have been
spread out at the source by more than four seconds. The choice of a factor of
two is arbitrary but we believe that it is conservative and, if the reader prefers
a different numerical factor, he can make the appropriate scaling using Table
1 (below). Stated differently, we assume that the effects of propagation on
the arrival times have not been such as to produce by accident a short pulse from
what was initially a much more diffuse signal.
Table
1 The width of the neutrino pulse at the neutron star
mve, (eV) | D8
(seconds) | D11 (seconds) |
0.0 | 1.9 | 12.4 |
5.0 | 2.3 | 12.4 | 9.0 | 3.8 | 12.8 |
10.0 | 4.4 | 13.0 | 15.0 | 8.3 | 14.8 |
20.0 | 13.8 | 18.4 | 26.6 | 23.6 | 24.9 |
The maximum difference in departure times
of the first eight events is D8 and of
the entire eleven events is D11. |
Table 1 shows as
a function of assumed neutrino mass the computed duration, at the neutron star,
of both the first eight events (D8) and
all the reported events (D11). For
= 0, these quantities are equal to the observed values of 2 s and 13 s. The inferred
durations at the star increase monotonically with assumed mass because the observed
events do not have the relation between energy and arrival time that is implied
by equation (1). Using the best estimates given by the Kamiokande collaboration
for all of the energies we find that if
exceeds 9.0 eV, then the 2 s initial pulse that is observed on Earth would have
been longer than 4 s at the neutron star. We have also recalculated the upper
limit by varying the nominal energies within their quoted errors. In all cases,
the pulse width at the source is at least twice the value measured at Earth if
 11
eV. We conclude therefore that
The strength of this limit derives from the lower energy events (7.5
MeV, 9.2 MeV and 12.8 MeV), all of which are observed to move at large angles
with respect to the direction of the LMC (108, 70 and 135 degrees respectively).
The measured directions show that these three events are not due to electron-neutrino
scattering, which is strongly forward peaked. A neutrino mass
of 27 eV is required, according to Table 1, to make the entire
set of eleven observed events twice as long (25 s) at the source than is observed
at Earth. We reject this possibility as physically implausible because it implies
that the initial pulse (observed to be 1.9 s in duration at the Earth, and surely
a physically significant phenomenon) was compressed in time by more than an order
of magnitude (from 22.4 s at the star). There are other ways,
most of them more complicated, of analysing the Kamiokande-II data. One can, of
course, obtain more stringent limits provided one is willing to introduce stronger
assumptions regarding what is astronomically or physically plausible. For example,
if one could justify the claim that the five events observed in the first 0.5
seconds had a distinct astrophysical origin, one could lower the upper limit to
7.5 eV including the measurement errors. Conservatively, we
conclude that the mass of the electron neutrino must be less than or equal to
11 eV. This limit is stronger than has been achieved by 50 years of measurements
on terrestrial systems. Larger detectors sensitive to lower
energy neutrinos should be able to observe, with much higher event rates, subsequent
supernovae explosions in the Galaxy. Supernovae in the Galaxy could be as frequent
as one a decade6 if they occur in obscured regions
and are therefore not associated with observable optical supernovae. The next
observation of neutrinos from a supernova explosion will provide an independent
measurement of the neutrino mass and will exclude the extremely unlikely possibility
that the LMC distance, the detected neutrino energies and the departure times
all conspired to sharpen greatly the neutrino signal from the collapse. With larger
detectors, it should be possible to set even better limits on (or measure) the
mass of the electron neutrino. The higher event rates will permit experimentalists
to determine characteristics of the ambient material at the time the neutron star
is being formed. In the extended periods between observable explosions, the detectors
can be used to measure accurately the arrival times, energies and directions of
solar neutrinos. We thank the Kamiokande-II collaboration and
the IMB collaboration for sharing with us their epochal data. This work was supported
in part by the NSF. Received Friday 13 March; accepted 23 March 1987.
- Hirata, K. et al. Phys. Rev. Lett. (submitted).
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R. M. Phys. Rev. Lett. (submitted).
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N. Proc. Int. Meet. Astrophysics and Elementary Particles, Common Problems
Rome, Italy (eds Cabibbo. N., Dallaporta, N., Gratton, L., Pacini, F. & Salvini,
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T. Phys. Lett. B102, 299302 (1981).
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J. N. & Piran, T. Astrophys. J. 167, L77L81 (1983).
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