Deep-MOND polytropes
arXiv:2012.11412 · doi:10.1103/PhysRevD.103.044043
Abstract
Working within the deep-MOND limit (DML), I describe spherical, self-gravitating systems governed by a polytropic equation of state, . As self-consistent structures, such systems can serve as heuristic models for DML, astronomical systems, such as dwarf spheroidal galaxies, low-surface-density elliptical galaxies and star clusters, and diffuse galaxy groups. They can also serve as testing ground for various theoretical MOND inferences. In dimensionless form, the equation satisfied by the radial density profile is (for ) . Or, , where , and . I discuss properties of the solutions, contrasting them with those of their Newtonian analogues -- the Lane-Emden polytropes. Due to the stronger MOND gravity, all DML polytropes have a finite mass, and for () all have a finite radius. (Lane-Emden spheres have a finite mass only for .) I use the DML polytropes to study DML scaling relations. For example, they satisfy a universal relation (for all and ) between the total mass, , and the mass-average velocity dispersion : . However, the relation between and other measures of the velocity dispersion, such as the central, projected one, , does depend on (but not ), defining a `fundamental surface' in the space. I also describe the generalization to anisotropic polytropes, which also all have a finite radius (for ), and all satisfy the above universal relation. This more extended class of models exhibits the central-surface-densities relation: a tight relation between the baryonic and the dynamical central surface densities predicted by MOND.
13 pages, 16 Figures. Minor changes to match published version
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- The distribution and morphologies of Fornax Cluster dwarf galaxies suggest they lack dark matter
- Aether scalar tensor theory confronted with weak lensing data at small accelerations
- Central-surface-densities correlation in general MOND theories
- Structure of the equivalent Newtonian systems in MOND N-body simulations. Density profiles and the core-cusp problem