Time variation of the fine structure constant driven by quintessence
- 30 October 2003
- journal article
- research article
- Published by American Physical Society (APS) in Physical Review D
- Vol. 68 (8) , 083513
- https://doi.org/10.1103/physrevd.68.083513
Abstract
There are indications from the study of quasar absorption spectra that the fine structure constant may have been measurably smaller for redshifts Analyses of other data fission rate for the Oklo natural reactor, variation of -decay rate in meteorite studies, atomic clock measurements) which probe variations of in the more recent past imply much smaller deviations from its present value. In this work we tie the variation of to the evolution of the quintessence field proposed by Albrecht and Skordis, and show that agreement with all these data, as well as consistency with Wilkinson Microwave Anisotropy Probe observations, can be achieved for a range of parameters. Some definite predictions follow for upcoming space missions searching for violations of the equivalence principle.
Keywords
All Related Versions
This publication has 66 references indexed in Scilit:
- Methods for Constraining Fine Structure Constant Evolution with OH Microwave TransitionsPhysical Review Letters, 2003
- Does the fine structure constant vary? A detailed investigation into systematic effectsAstrophysics and Space Science, 2003
- Constraints on the variations of the fundamental couplingsPhysical Review D, 2002
- Further Evidence for Cosmological Evolution of the Fine Structure ConstantPhysical Review Letters, 2001
- The nuclear interaction at Oklo 2 billion years agoNuclear Physics B, 2000
- Search for Time Variation of the Fine Structure ConstantPhysical Review Letters, 1999
- The Oklo bound on the time variation of the fine-structure constant revisitedNuclear Physics B, 1996
- Re-Os Ages of Group IIA, IIIA, IVA, and IVB Iron MeteoritesScience, 1996
- Direct test of the constancy of fundamental nuclear constantsNature, 1976
- Cosmology and the Radioactive Decay Ages of Terrestrial Rocks and MeteoritesPhysical Review B, 1962