Abstract

It is well-known that equilibrium density profiles of gases and fluids in gravitational potentials have an r−1 dependence, where r is the radius. This is found in both astronomical observations and detailed simulations in spherically-symmetric geometries. It is also well-known that the standard equation for hydrostatic equilibrium does not produce such solutions. This paper utilizes a Lagrangian formulation that produces a closed-form r−1 solution and identifies the needed terms to be added to the standard equation for hydrostatic equilibrium to obtain such a solution. Variants of the r−1 solution avoid a density singularity at the origin and a total-enclosed mass singularity at infinity. The resulting solutions are shown to be in good agreement with well-established density profiles of ordinary matter in galaxies, dark matter haloes, and the atmosphere of earth. Comparisons are made to solutions based on the standard hydrostatic equation, including solutions based on the Lane-Emden equation. The origins of differences are explained.

Highlights

  • Numerical solutions for dark matter (DM) density profiles were found to have dependence inversely proportional to radius [1]

  • This paper utilizes a Lagrangian formulation that produces a closed-form r−1 solution and identifies the needed terms to be added to the standard equation for hydrostatic equilibrium to obtain such a solution

  • Comparisons are made to solutions based on the standard hydrostatic equation, including solutions based on the Lane-Emden equation

Read more

Summary

Introduction

Numerical solutions for dark matter (DM) density profiles were found to have dependence inversely proportional to radius [1]. Calculations using Equations (1) and (2) are inconsistent with an r−1 solution Such solutions have no cusp at the origin and are a poor match to the standard Sersic or Einasto profiles based on observations [1] [2] [3] [4] [6] [14] [15] [16]. This is found to be true for any polytropic exponent between about 1.1 and 2 in Section 4 below.

Derivation of a Generalized Equation for Hydrostatic Equilibrium
Generalized Equation for Earth’s Atmospheric Density Profile with Altitude
Solution near the Origin
Behavior of Solutions away from the Origin
Comparison to Einasto and De-Projected Sersic Profiles
Lane-Emden Solutions for Non-Relativistic Particles
Summary
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call