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Solar Neutrinos and the Decaying Neutrino Hypothesis

Jeffrey M. Berryman Northwestern University, Department of Physics & Astronomy, 2145 Sheridan Road, Evanston, IL 60208, USA    André de Gouvêa Northwestern University, Department of Physics & Astronomy, 2145 Sheridan Road, Evanston, IL 60208, USA    Daniel Hernández Northwestern University, Department of Physics & Astronomy, 2145 Sheridan Road, Evanston, IL 60208, USA
Abstract

We explore, mostly using data from solar neutrino experiments, the hypothesis that the neutrino mass eigenstates are unstable. We find that, by combining 8B solar neutrino data with those on 7Be and lower-energy solar neutrinos, one obtains a mostly model-independent bound on both the ν1\nu_{1} and ν2\nu_{2} lifetimes. We comment on whether a nonzero neutrino decay width can improve the compatibility of the solar neutrino data with the massive neutrino hypothesis.

preprint: NUHEP-TH/14-08

The discovery of distinct nonzero neutrino masses and nontrivial lepton mixing opened the door to several fundamental questions that revolve around the properties of the neutral leptons. Here we concentrate on what, experimentally and model-independently, is known about the neutrino lifetime.

In the absence of interactions and degrees of freedom beyond those of the Standard Model, the two heaviest neutrinos – ν2\nu_{2} and ν3\nu_{3} (ν1\nu_{1} and ν2\nu_{2}) in the case of the so-called normal (inverted) neutrino mass hierarchy Agashe:2014kda – are unstable, decaying into lighter neutrinos and photons (νiνjνkνl\nu_{i}\to\nu_{j}\nu_{k}\nu_{l} or νiνj+γ\nu_{i}\to\nu_{j}+\gamma, where i,j,k,l=1,2,3i,j,k,l=1,2,3). The associated lifetimes, given the tiny neutrino masses, are longer than 103710^{37} years – much longer than the age of the universe. The presence of new interactions, degrees of freedom, etc., can, of course, change the picture dramatically.

Experimental bounds on the lifetimes of the neutrinos are much shorter than those expected from the Standard Model minimally augmented to include nonzero neutrino masses. Consulting ‘The Review of Particle Physics’ Agashe:2014kda , one encounters different bounds that span almost twenty orders of magnitude. Bounds on the neutrino magnetic moment, for example, translate into bounds on radiative neutrino decays Broggini:2012df . Results from cosmic surveys sensitive to the expansion rate of the universe at different epochs are consistent with the existence of around three independent neutrino states, naively indicating that these do not decay within the span of billions of years. In order to translate measurements of the expansion rate of the universe into a bound on the neutrino lifetime, however, one must consider the nature of the neutrino decay process, since the daughters of the putative decay also contribute to the expansion rate of the universe and could, in principle, mimic the contributions of their parents Beacom:2004yd ; Hannestad:2005ex . The observation of the effects of nonzero neutrino masses in cosmic surveys might change the picture significantly Serpico:2007pt .

Model-independent bounds exist from experiments where the number of neutrinos produced in the source can be compared to the number of neutrinos detected some distance away. These include all neutrino oscillation experiments. Given a baseline LL and a “beam” energy EE, one expects to be sensitive to a neutrino decay width Γi\Gamma_{i} for νi\nu_{i} with mass mim_{i} such that

ΓimiLEdiLE=5.07(dieV2)(Lkm)(GeVE)1.\Gamma_{i}m_{i}\frac{L}{E}\equiv d_{i}\frac{L}{E}=5.07\left(\frac{d_{i}}{\rm eV^{2}}\right)\left(\frac{L}{\rm km}\right)\left(\frac{\rm GeV}{E}\right)\gtrsim 1. (1)

Here, for convenience, we define diΓimid_{i}\equiv\Gamma_{i}m_{i}, which has dimensions of energy-squared, for two reasons. On one hand, all bounds discussed here are sensitive to did_{i}: it is not possible to disentangle the neutrino mass from its decay width, both being unknown. On the other hand, did_{i}, measured in eV2, can be easily and directly compared to the neutrino mass-squared differences that are measured in neutrino oscillation experiments and “compete” with the decay effects. For conversion purposes, di=1011d_{i}=10^{-11} eV2 translates into a lifetime τi=70\tau_{i}=70 μ\mus for a neutrino with mass mi=1m_{i}=1 eV.

Using Eq. (1), it is easy to naively estimate that long-baseline accelerator experiments like MINOS, T2K, and Noν\nuA, with L/E103L/E\sim 10^{3} km/GeV, are sensitive to di104d_{i}\gtrsim 10^{-4} eV2, atmospheric neutrino experiments like SuperKamiokande, with L/E105L/E\lesssim 10^{5} km/GeV, are sensitive to di106d_{i}\gtrsim 10^{-6} eV2, and the KamLAND reactor neutrino experiment, with L/E2×104L/E\lesssim 2\times 10^{4} km/GeV, is sensitive to di105d_{i}\gtrsim 10^{-5} eV2. Detailed analyses of atmospheric and MINOS data, for example, translate into d3105d_{3}\lesssim 10^{-5} eV2 GonzalezGarcia:2008ru and d3<1.2×104d_{3}<1.2\times 10^{-4} eV2 Gomes:2014yua , respectively, assuming d1,d2d3d_{1},d_{2}\ll d_{3}.

Astrophysical neutrinos, when directly observed in Earth-bound detectors, provide significantly more stringent bounds on some of the did_{i}. The observation of neutrinos from Supernova 1987A implies that at least one of the neutrino mass eigenstates made it from the explosion to the Earth and can be translated into di<1.2×1021d_{i}<1.2\times 10^{-21} eV2 for at least one i=1,2,3i=1,2,3 Frieman:1987as . A very strong bound on at least one of the did_{i} can also be derived Beacom:2002vi ; Meloni:2006gv ; Baerwald:2012kc ; Pakvasa:2012db ; Dorame:2013lka ; Fu:2014gja from the current and future observations of ultra-high-energy neutrinos using the IceCube detector Aartsen:2013bka .

Solar neutrinos have L/E1011L/E\sim 10^{11} km/GeV and hence are sensitive to di1012d_{i}\gtrsim 10^{-12} eV2. The authors of Beacom:2002cb were the first to point out that the 8B solar neutrino data translate into a very robust bound on d21011d_{2}\lesssim 10^{-11} eV2, mostly independent from d1d_{1} and d3d_{3}. In this letter, we revisit the impact of decaying neutrinos on solar neutrino data. Since the publication of Beacom:2002cb , our understanding of solar neutrinos and neutrino properties improved significantly. More and more precise KamLAND data not only confirmed the neutrino oscillation interpretation of solar neutrino data, but also provided a precision measurement of the “solar” mass-squared difference, Δm122m22m12\Delta m^{2}_{12}\equiv m_{2}^{2}-m_{1}^{2}, and a good independent measurement of the “solar” mixing angle θ12\theta_{12} Gando:2010aa . Borexino data allow a precision measurement of 7Be solar neutrinos, and a clean measurement of the pppp solar neutrinos Bellini:2011rx . Finally, recent reactor An:2013zwz ; Ahn:2012nd ; Abe:2012tg and accelerator data Abe:2013hdq have measured the “reactor angle” θ13\theta_{13}, revealing that it is nonzero but quite small, sin2θ130.02\sin^{2}\theta_{13}\sim 0.02. We will argue that all this information allows one to place, almost model-independently, bounds on both d1d_{1} and d2d_{2} from solar neutrino data. These results, when combined with results from atmospheric neutrinos, allow one to unambiguously place bounds on all three did_{i}, i=1,2,3i=1,2,3, which are robust, mostly model independent, and do not depend on the values of the neutrino masses or the neutrino mass hierarchy.

We will show, a posteriori, that decay effects are negligible for the L/EL/E values probed by the KamLAND experiment. This implies that the oscillation results obtained from KamLAND apply even if the neutrinos have a finite lifetime, including the fact that Δm122104\Delta m^{2}_{12}\sim 10^{-4} eV2 and sin22θ120.8\sin^{2}2\theta_{12}\sim 0.8. This in turn implies that neutrino oscillations from the core to the edge of the Sun, to a very good approximation, satisfy the adiabatic approximation. Ignoring the (very small) day–night effect but taking into account that the different neutrinos can decay into final states not accessible to the different solar neutrino detectors, the probability PeαP_{e\alpha} that a neutrino with energy EE born in the Sun as a νe\nu_{e} is detected as a να\nu_{\alpha}, α=e,μ,τ\alpha=e,\mu,\tau one astronomical unit LL_{\odot} away from the Sun is

Peα(E)i=1,2,3pei(E)|Uαi|2ediL/E,P_{e\alpha}(E)\simeq\sum_{i=1,2,3}p_{ei}(E)|U_{\alpha i}|^{2}e^{-d_{i}L_{\odot}/E}, (2)

where UαiU_{\alpha i}, i=1,2,3i=1,2,3, are the elements of the neutrino mixing matrix, while pei(E)p_{ei}(E) are the probabilities that the neutrino exits the Sun as νi\nu_{i} neutrino mass eigenstates. Strictly speaking, Eq. (2) is a good approximation when diR/E1d_{i}R_{\odot}/E\ll 1 where RR_{\odot} is the average solar radius. We will show that this is indeed the case for d1d_{1} and d2d_{2}, and we argue in the next paragraph that solar data are not sensitive to d3d_{3} effects.

Given that |Δm132|2×103|\Delta m^{2}_{13}|\sim 2\times 10^{-3} eV2 – even if one includes nonzero neutrino decay widths GonzalezGarcia:2008ru ; Gomes:2014yua pe3(E)|Ue3|2p_{e3}(E)\simeq|U_{e3}|^{2} for all relevant solar neutrino energies, E[100keV,20MeV]E\in[100~{\rm keV},20~{\rm MeV}]. Since |Ue3|2=sin2θ130.02|U_{e3}|^{2}=\sin^{2}\theta_{13}\simeq 0.02 is small, given the precision of the solar neutrino data, d3d_{3} related effects are irrelevant. In other words, the solar data are consistent with all d3d_{3} values. We anticipate that d30d_{3}\neq 0 effects impact only very modestly the constraints on the other oscillation and decay parameters. Henceforth, we ignore θ13\theta_{13} effects – we formally set it to zero – and treat solar neutrino oscillations as if there were only two neutrinos, νe\nu_{e} and νa\nu_{a} (aa for active).

At high solar neutrino energies, E5E\gtrsim 5 MeV, pe21p_{e2}\sim 1, pe10p_{e1}\sim 0, such that Peesin2θ12ed2L/EP_{ee}\sim\sin^{2}\theta_{12}e^{-d_{2}L_{\odot}/E} and Peacos2θ12ed2L/EP_{ea}\sim\cos^{2}\theta_{12}e^{-d_{2}L_{\odot}/E}. 8B solar neutrino data are hence very sensitive to d2d_{2} but have little sensitivity to d1d_{1} Beacom:2002cb . The most recent solar data from SNO Aharmim:2011vm indicate a PeeP_{ee} that decreases slowly as the neutrino energy decreases (as opposed to increasing, as predicted by the standard scenario, d1=d2=0d_{1}=d_{2}=0), a fact that is consistent with a judicious choice of d2d_{2}. For illustrative purposes, Fig. 1 depicts PeeP_{ee} and PeaP_{ea} as a function of EE, for sin2θ12=0.29\sin^{2}\theta_{12}=0.29, Δm122=7.5×105\Delta m^{2}_{12}=7.5\times 10^{-5} eV2, d1=0d_{1}=0, and d2=0d_{2}=0 or d2=2×1012d_{2}=2\times 10^{-12} eV2.

Refer to caption
Figure 1: PeeP_{ee} (black) and PeaP_{ea} (red) as a function of the solar neutrino energy, for sin2θ12=0.29\sin^{2}\theta_{12}=0.29, Δm122=7.5×105\Delta m^{2}_{12}=7.5\times 10^{-5} eV2, d1=0d_{1}=0 and d2=0d_{2}=0 (solid) or d2=2×1012d_{2}=2\times 10^{-12} eV2 (dashed). Also depicted are the data points used to estimate the allowed values of d1d_{1} and d2d_{2}, including one sigma error bars. See text for details.

At low solar neutrino energies, E1E\lesssim 1 MeV, solar neutrino oscillations are well approximated by simple, averaged-out vacuum oscillations such that pe1cos2θ12p_{e1}\sim\cos^{2}\theta_{12}, pe2sin2θ12p_{e2}\sim\sin^{2}\theta_{12}, and Peecos4θ12ed1L/E+sin4θ12ed2L/EP_{ee}\sim\cos^{4}\theta_{12}e^{-d_{1}L_{\odot}/E}+\sin^{4}\theta_{12}e^{-d_{2}L_{\odot}/E} and Peasin2θ12cos2θ12(ed2L/E+ed1L/E)P_{ea}\sim\sin^{2}\theta_{12}\cos^{2}\theta_{12}(e^{-d_{2}L_{\odot}/E}+e^{-d_{1}L_{\odot}/E}). 7Be and pppp solar neutrino measurements are hence sensitive to both d1d_{1} and d2d_{2}. In isolation, the low-energy solar neutrino data can be used to place a bound on either d1d_{1} or d2d_{2}, but not both. This is easy to see: the data are consistent with ed1L/E0e^{-d_{1}L_{\odot}/E}\to 0 or ed2L/E0e^{-d_{2}L_{\odot}/E}\to 0 as long as one judiciously chooses sin2θ12\sin^{2}\theta_{12}. For example, in the limit, say, ed1L/E0e^{-d_{1}L_{\odot}/E}\to 0, Peesin4θ12P_{ee}\sim\sin^{4}\theta_{12} and Peasin2θ12cos2θ12P_{ea}\simeq\sin^{2}\theta_{12}\cos^{2}\theta_{12} can be made to fit the data, roughly, Pee0.55P_{ee}\sim 0.55 Bellini:2011rx , by choosing sin2θ12=0.75\sin^{2}\theta_{12}=0.75 (in the “dark side” de Gouvea:2000cq ), which is consistent with data from KamLAND Gando:2010aa . This possibility, however, is ruled out by 8B data, which “require” sin2θ120.3\sin^{2}\theta_{12}\sim 0.3.

In summary, combined low and high energy solar neutrino data allow one to place nontrivial bounds on both d1d_{1} and d2d_{2}, i.e., the possibility that either ed1L/E0e^{-d_{1}L_{\odot}/E}\to 0 or ed2L/E0e^{-d_{2}L_{\odot}/E}\to 0 is ruled out. d2d_{2} is mostly constrained by the 8B data, while d1d_{1} is mostly constrained by the 7Be and pppp data. Given the order-of-magnitude difference between the neutrino energies, we anticipate the d1d_{1} bound to be, roughly, an order of magnitude stronger than the d2d_{2} bound.

In order to estimate the upper bounds on d1d_{1} and d2d_{2}, we perform a simple χ2\chi^{2} fit to sin2θ12,d1,d2\sin^{2}\theta_{12},d_{1},d_{2}, fixing Δm122=7.5×105\Delta m^{2}_{12}=7.5\times 10^{-5} eV2, the best fit from KamLAND, and setting sin2θ13=0\sin^{2}\theta_{13}=0, as discussed earlier. Given that KamLAND provides the dominant contribution to the measurement of Δm122\Delta m^{2}_{12}, this is a very reasonable approximation. Since in the decaying-neutrinos scenario Pee+Pea1P_{ee}+P_{ea}\leq 1, we need to consider separately the information on the electron and the “active” neutrino components of the solar neutrino flux. In detail, we include the following experimental information, depicted in Fig. 1:

  • Pee=0.56±0.06P_{ee}=0.56\pm 0.06 for E=380E=380 keV, as extracted from a combined fit to Borexino and low-energy neutrino data Bellini:2011rx . This analysis is performed, effectively, by using Borexino data in order to establish the oscillated 7Be neutrino flux and hence extract the pppp neutrino flux from other data. This procedure depends only weakly on the hypothesis that Pee+Pea=1P_{ee}+P_{ea}=1. This result is consistent with Borexino’s recent independent measurement of the low energy solar neutrino flux Bellini:2014uqa .

  • s=Pee+rPea=0.62±0.05s=P_{ee}+rP_{ea}=0.62\pm 0.05 for E=862E=862 keV from the Borexino data Bellini:2011rx . r=0.22r=0.22 is the ratio of the νe+e\nu_{e}+e to the νa+e\nu_{a}+e elastic scattering cross-sections at 7Be neutrino energies.

  • SNO performed a detailed measurement of PeeP_{ee} as a function of energy Aharmim:2011vm . We choose PeeP_{ee} values at E=4MeVE=4~{\rm MeV} and E=10MeVE=10~{\rm MeV}, Pee=0.26±0.12P_{ee}=0.26\pm 0.12 and Pee=0.32±0.02P_{ee}=0.32\pm 0.02, respectively, as representatives of the SNO data. These points are chosen in order to both capture the statistical power of the SNO experiment and to include some of the shape information. A proper treatment of the SNO data, including all different observables, correlations, etc., can only be handled by the Collaboration itself. We verify that, in the case d1=d2=0d_{1}=d_{2}=0, our extracted best fit value for sin2θ12\sin^{2}\theta_{12} and the associated one sigma error bar are in good agreement with the most recent global analyses of neutrino data Gonzalez-Garcia:2014bfa .

  • The SNO experiment is also sensitive to the presence of a νa\nu_{a} flux from the Sun thanks to its neutral current and ν+e\nu+e elastic scattering measurements. It is, therefore, possible to measure PeeP_{ee} and PeaP_{ea} as a function of energy with SNO data (see, for example, Ahmad:2002jz ). Ref. Aharmim:2011vm , however, does not discuss the independent extraction of PeaP_{ea} from the data, replacing it instead by 1Pee1-P_{ee}. Here we estimate the extracted value of PeaP_{ea} from SNO data as follows. We define the central value using Pea=1PeeP_{ea}=1-P_{ee} while fixing the one-sigma error bar on PeaP_{ea} as that on PeeP_{ee}, multiplied by 5\sqrt{5}. The factor of 55 is very close to the ratio of the elastic νe+e\nu_{e}+e cross-section to that for νa+e\nu_{a}+e at 8B neutrino energies and agrees with the relative uncertainties for the electron and active neutrino fluxes measured by SNO in Ahmad:2002jz .

We note that SuperKamiokande also measures the neutrino flux using elastic neutrino–electron scattering (see, e.g., Abe:2010hy ). We do not include data from SuperKamiokande in our simplified fit as they mostly contributes to the measurement of PeaP_{ea} – which we can only estimate here – and have a higher energy threshold than SNO data.

Fig. 2 depicts the result of our fit in the d1×d2d_{1}\times d_{2}-plane, obtained after marginalizing over sin2θ12\sin^{2}\theta_{12}. The best fit point is d1=3.4×1019eV2,d2=1.6×1013d_{1}=3.4\times 10^{-19}~{\rm eV}^{2},d_{2}=1.6\times 10^{-13} eV2 and the hypothesis d1=d2=0d_{1}=d_{2}=0 fits the data quite well. At the two-sigma confidence level, d1<1.6×1013d_{1}<1.6\times 10^{-13} eV2 and d2<9.3×1013d_{2}<9.3\times 10^{-13} eV2, in agreement with the naive estimates discussed above. The constraints above justify the approximations that led to Eq. (2), especially d1,2R/E1d_{1,2}R_{\odot}/E\ll 1 for all solar neutrino energies. Our result indicates that the neutrino decay hypothesis does not allow for a fit to the solar data that is significantly better than the standard “large mixing angle solution,” mostly due to the low energy 7Be and pppp neutrino measurements. We emphasize, however, that a detailed analysis of all solar neutrino data including the neutrino decay hypothesis is best left to the experimental collaborations, and that a reanalysis of the SNO data – one that treats both Pee(E)P_{ee}(E) and Pea(E)P_{ea}(E) as independent functions – as a function of energy is required. We hope our results encourage the pursuit of such an analysis.

Refer to caption
Figure 2: Allowed values of d1d_{1} and d2d_{2} at the one, two and three sigma. The best fit point d1=3.4×1019eV2,d2=1.6×1013d_{1}=3.4\times 10^{-19}~{\rm eV}^{2},d_{2}=1.6\times 10^{-13} eV2 is indicated by a dot.

In summary, we have argued that the solar neutrino data, combined with reactor data, allow one to place mostly model-independent bounds on the lifetimes of ν1\nu_{1} and ν2\nu_{2}. Using a subset of the solar neutrino data and the data from KamLAND, we estimate that d1<1.6×1013d_{1}<1.6\times 10^{-13} eV2 and d2<9.3×1013d_{2}<9.3\times 10^{-13} eV2 at the two-sigma confidence level. A complete analysis would reveal exactly where these bounds lie. As a “by-product” of our analysis, the atmospheric neutrino bound discussed in GonzalezGarcia:2008ru applies, robustly, to ν3\nu_{3}: d3105d_{3}\lesssim 10^{-5} eV2. Along with solar and atmospheric neutrino data, the only other robust bound comes from SN1987A which translates, as discussed earlier, into di<1.2×1021d_{i}<1.2\times 10^{-21} for one of the three mass-eigenstates, most likely ν1\nu_{1} or ν2\nu_{2}.

The bounds are ‘mostly model-independent’ in the following sense. They are independent from the values of the neutrino masses themselves, and apply for both mass hierarchies. No assumption is made regarding the nature of the neutrino – Majorana or Dirac – or of the daughter particles into which the neutrinos would be decaying. We are assuming, however, that if the decay-daughters were to consist of lighter active neutrinos, these would not leave a significant imprint in the detectors under consideration, i.e., they don’t “look” like the parent neutrinos. This is a modest assumption. Daughter neutrinos from neutrino decay have, necessarily, less energy than their parents, and only those that decay along the flight-path of the parent make it to the detector. We also do not allow for the possibility, recently discussed in a more generic context Berryman:2014yoa , that the neutrino decay hypothesis translates into more mixing parameters, i.e., that the neutrino mass and decay eigenstates are not the same.

Acknowledgements

We thank Roberto Oliveira for useful discussions and collaboration during the early stages of this work. DH and AdG thank the Kavli Institute for Theoretical Physics in Santa Barbara, where part of this work was completed, for its hospitality. DH benefitted from fruitful discussions with Hisakazu Minakata, Sandip Pakvasa, Tom Weiler, and Walter Winter. The work of AdG and DH was supported in part by the National Science Foundation under Grant No. NSF PHY11-25915. This work is sponsored in part by the DOE grant #DE-FG02-91ER40684.

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