Observed solar neutrino fluxes are employed to constrain the interior
composition of the Sun. Including the effects of neutrino flavor mixing, the
results from Homestake, Sudbury, and Gallium experiments constrain the Mg, Si,
and Fe abundances in the solar interior to be within a factor 0.89 to 1.34 of
the surface values with 68% confidence. If the O and/or Ne abundances are
increased in the interior to resolve helioseismic discrepancies with recent
standard solar models, then the nominal interior Mg, Si, and Fe abundances are
constrained to a range of 0.83 to 1.24 relative to the surface. Additional
research is needed to determine whether the Sun's interior is metal poor
relative to its surface.Comment: accepted by MNRAS, 2 figure