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Physics Letters B 555 (2003) 144-146
www. elsevier. com/locate/npe
KamLAND and solar neutrino data eliminate the LOW solution
V. Bargera, D. Marfatiab
a Department of Physics, University of Wisconsin, Madison, WI53706, USA b Department of Physics, Boston University, Boston, MA 02215, USA
Received 10 December 2002; accepted 13 January 2003
Editor: M. Cvetic
Abstract
The KamLAND reactor antineutrino experiment has detected a 3.4 a flux suppression relative to the expectation if no neutrino oscillations occur. We combine KamLAND data with solar neutrino data and show that the LMA solution is the only viable oscillation solution to the solar neutrino problem at the 4.4 a C.L. © 2003 Elsevier Science B.V. All rights reserved.
The neutral-current measurement at SNO convincingly demonstrated that electron neutrinos from the sun undergo a flavor transformation. Yet, the cause of this conversion was debatable. With the results from the KamLAND experiment [1], one can confidently state that the solar neutrino problem is solved. All explanations of the solar anomaly other than that neutrinos oscillate because they are massive are now either discarded or are sub-leading effects. From solar neutrino data alone, it has been deduced that the Large Mixing Angle (LMA) and LOW solutions are the most likely oscillation solutions [2]. Reactor antineutrino data from KamLAND prove that neutrinos oscillate with parameters confined to the large mixing angle (LMA) region at the 3.4a C.L. We assess how much more stronger this evidence becomes when KamLAND's data is combined with solar neutrino data.
E-mail address: marfatia@buphy.bu.edu (D. Marfatia).
Since solar neutrino experiments and the KamLAND experiment have different neutrino sources, their systematics are uncorrelated and their results independent. A statistical analysis involving a combination of these two types of experiments entails two distinct analyses, one of the solar data and one of KamLAND data. Subsequently the x2 contributions of the two are simply summed. For details and results of the solar analysis used in this Letter, we refer the reader to Ref. [2]. Here, we briefly describe our analysis of the KamLAND data only.
Electron antineutrinos from 20 nuclear reactors in Japan and South Korea are incident at the KamLAND detector. About 95% of the unoscillated flux originates with baselines between 80-344 km. We therefore evaluate the survival probability of the neutrinos in the vacuum limit of two-flavor oscillations; the transition probability of muon to electron neutrinos is known to be small at the atmospheric neutrino oscillation scale [3]. We use the spectra from the fission products of 235U, 239Pu, 238U and 241 Pu provided in Ref. [4]. We adopt the time-averaged relative fission yields
0370-2693/03/$ - see front matter © 2003 Elsevier Science B.V. All rights reserved. doi:10.1016/S0370-2693(03)00075-3
from the fuel components as provided by the KamLAND Collaboration [1]. This serves as a good representation of the averaging of time-evolution effects of the isotope evolution since all the reactors will not start and end their cycles at the same times. We assume that the fluctuations in the power output of each reactor arising from dead time for maintenance and seasonal variations of power requirements average so that the live times and efficiencies of all the reactors are the same. For the inverse neutron j -decay process via which antineutrinos are detected, we adopt the cross-section with nucleon recoil corrections. To determine the expected signal at KamLAND from each reactor, the fluxes are convoluted with the survival probability corresponding to the baseline of the reactor, the antineutrino cross-section and the detector response function (with energy resolution, 7.5%/s/E (MeV), and prompt energy threshold at 2.6 MeV [1]). Finally, the cumulative expected signal is obtained by summing over all the reactors.
To evaluate the statistical significance of an oscillation solution, we define x2 = xQ + xKamLAND, where Xq is defined by Eq. (9) of Ref. [2], and [5]
8 / N 6xp \
xLnLAND = E" AfP + Cln^h)
13 \ 2
+ J22aNlh+(1—^) . (1)
i=9 ^ '
Here, Nth and Nfxp are the theoretical and experimental numbers of events in the i th bin (each of width 0.425 MeV) and a = 6.42% is the uncertainty in the event rate calculation [1]. The normalization factor a is allowed to float so as to yield the smallest xKamLAND for a given set of oscillation parameters.
We first show the results of an analysis of KamLAND data alone to demonstrate that our assumption that the live times and efficiencies of all the reactors are the same does not affect the allowed regions. The 1a and 2a allowed regions are shown. The similarities between Fig. 1 and Fig. 6 of Ref. [1] are convincing after accounting for the fact that we have chosen tan2 0 as the abscissa. The best-fit solution is Am2 = 7.1 x 10-5 eV2 and tan2 0 = 0.64 with a = 1.008 and X2 = 5.57. In the LOW region we find x2 = 19.89 which is therefore acceptable only at the 3.4a C.L. (KamLAND quotes 99.95% C.L. [1] which is equiva-
_i_i_i_I_i_i_i_i_I_i_i_i_i_I_i_i_i_i_I_i_i_i_i_
0.2 0.4 0.0 0.8 1.0
Fig. 1. The 1a and 2a allowed regions from a fit to KamLAND data only. The best-fit point is at Am2 = 7.1 x 10-5 eV2 and tan2 0 = 0.64. The figure is symmetric under reflection about tan2 0 = 1.
0.2 0.4 0.6 0.8 1.0
tan2©
Fig. 2. The 2a and 3a allowed regions from a combined fit to KamLAND and solar neutrino data. The best-fit point is at Am2 = 7.1 x 10-5 eV2 and tan2 0 = 0.42. No region above Am2 = 10-4 eV2 is allowed at the 90% C.L.
lent to about 3.5 a). Note that with solar neutrino data alone, the LOW solution is allowed at the 99% C.L. or
about 2.6 a [2]. Thus, KamLAND data already constrains the LOW solution more than solar data.
In Fig. 2 we show the 2a and 3 a allowed regions from a combined analysis of KamLAND and solar neutrino data. The best-fit solution moves to Am2 = 7.1 x 10-5 eV2 and tan2 0 = 0.42 with a = 0.994 and X2 = 57.08. The best-fit point in the LOW region has X 2 = 79.78 thereby implying that the LOW solution is allowed only at 4.4 a.
We conclude that the LMA solution is unique at the 4.4 a C.L. A precise determination of the oscillation parameters is now only a matter of time [6].
Acknowledgements
This work was supported in part by the US Department of Energy under grant Nos. DE-FG02-91ER40676 and DE-FG02-95ER40896, and in part by the Wisconsin Alumni Research Foundation.
References
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