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Stars as Laboratories for Fundamental Physics - MPP Theory Group

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388 Chapter 10<br />

of the Sun. 58 The simple estimate Eq. (10.26) remains approximately<br />

valid. A neutrino m<strong>as</strong>s-square difference m 2 2 −m 2 1 below about 10 −5 eV 2<br />

is required because of the small matter densities encountered in the convective<br />

layers.<br />

The bounds on neutrino dipole and transition moments discussed<br />

in Sect. 6.5.6 yield µ < ν ∼ 3×10 −12 µ B so that a magnetic-field strength<br />

B > ∼ 100 kG is required in the solar convection zone. Typical field<br />

strengths me<strong>as</strong>ured in sunspots where the flux breaks through the surface<br />

are of a few kG. While this may not be representative of the largescale<br />

toroidal field, several general arguments suggest that 10 kG is a<br />

generous upper limit (Shi et al. 1993). If there were much stronger<br />

fields they would have to be confined to flux ropes which would not<br />

be effective at inducing neutrino spin oscillations. There<strong>for</strong>e, the spin<br />

oscillation scenario would require anomalously large magnetic fields, in<br />

conflict with the arguments presented by Shi et al., or dipole moments<br />

in excess of what is allowed by the bounds of Sect. 6.5.6. Even smaller<br />

dipole moments than 3×10 −12 µ B require novel neutrino interactions.<br />

The solar magnetic field is believed to consist of two opposite flux<br />

tori, separated by the solar equatorial plane. In the course of a year the<br />

line of sight from Earth to the solar core varies between ±7 ◦ 15 ′ solar<br />

latitude and so the neutrinos me<strong>as</strong>ured here traverse a field configuration<br />

which varies in the course of a year. The predicted semiannual<br />

flux variation (Voloshin, Vysotskiĭ, and Okun 1986a), however, h<strong>as</strong> not<br />

been confirmed by any of the experiments.<br />

In the spin-flavor oscillation scenario involving Majorana neutrinos<br />

the Sun would be a source <strong>for</strong> antineutrinos, some of which could be<br />

ν e ’s by a combination of spin-flavor (ν e → ν µ ) and flavor (ν µ → ν e )<br />

oscillations. However, the Kamiokande data already yield restrictive<br />

limits on a solar ν e flux (Barbieri et al. 1991; see also Fig. 10.14).<br />

In summary, the magnetic spin oscillation scenario requires new neutrino<br />

interactions to generate large magnetic dipole moments, and new<br />

<strong>as</strong>trophysics to allow <strong>for</strong> sufficiently strong magnetic fields in the solar<br />

convection zone. Neither a semiannual variation of the flux nor ν e ’s<br />

have been observed; each would have been a smoking gun <strong>for</strong> the occurrence<br />

of this effect. There<strong>for</strong>e, one is led to disfavor the magnetic spin<br />

oscillation scenario. Then, of course, one is back to a statistical fluctuation<br />

<strong>as</strong> an explanation <strong>for</strong> the time structure of the Homestake data.<br />

58 Recent detailed investigations were per<strong>for</strong>med by Akhmedov, Lanza, and Petcov<br />

(1993, 1995), Kr<strong>as</strong>tev (1993), Nunokawa and Minakata (1993), Guzzo and Pulido<br />

(1993), and Pulido (1993, 1994). For a review of earlier works see Pulido 1992.

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