Strange-quark contribution to the ratio of neutral- to charged-current cross sections in neutrino-nucleus scattering

Physics – Nuclear Physics – Nuclear Theory

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

20 pages, 6 figures, Revtex, Submitted to Phys. Rev. C

Scientific paper

10.1103/PhysRevC.73.025501

A formalism based on a relativistic plane wave impulse approximation is developed to investigate the strange-quark content ($g_{A}^{s}$) of the axial-vector form factor of the nucleon via neutrino-nucleus scattering. Nuclear structure effects are incorporated via an accurately calibrated relativistic mean-field model. The ratio of neutral- to charged-current cross sections is used to examine the sensitivity of this observable to $g_{A}^{s}$. For values of the incident neutrino energy in the range proposed by the FINeSSE collaboration and by adopting a value of $g_{A}^{s}=-0.19$, a 30% enhancement in the ratio is observed relative to the $g_{A}^{s}=0$ result.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Strange-quark contribution to the ratio of neutral- to charged-current cross sections in neutrino-nucleus scattering does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Strange-quark contribution to the ratio of neutral- to charged-current cross sections in neutrino-nucleus scattering, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Strange-quark contribution to the ratio of neutral- to charged-current cross sections in neutrino-nucleus scattering will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-624484

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.