Difference between revisions of "User:Tohline/PGE"

From VistrailsWiki
Jump to navigation Jump to search
(Insert header template)
(Insert footer template)
Line 30: Line 30:
</div>
</div>


 
{{LSU_HBook_footer}}
----
 
<div align="center">
[http://www.vistrails.org/index.php/User:Tohline/H_Book Home] |
</div>

Revision as of 23:35, 18 January 2010

Whitworth's (1981) Isothermal Free-Energy Surface
|   Tiled Menu   |   Tables of Content   |  Banner Video   |  Tohline Home Page   |

Principal Governing Equations

According to the eloquent discussion of the broad subject of Fluid Mechanics presented by Landau and Lifshitz (1975), the state of a moving fluid is determined by five quantities: the three components of the velocity <math>\vec{v}</math> and, for example, the pressure <math>P</math> and the density <math> \rho </math> . For our discussions of astrophysical fluid systems throughout this Hypertext Book [H_Book], we will add to this the gravitational potential <math> \Phi </math>. Accordingly, a complete system of equations of fluid dynamics should be six in number. For an ideal fluid these are:

Euler's Equation
(Momentum Conservation)

<math>\frac{d\vec{v}}{dt} = - \frac{1}{\rho} \nabla P - \nabla \Phi</math>


Equation of Continuity
(Mass Conservation)

<math>\frac{d\rho}{dt} + \rho \nabla \cdot \vec{v} = 0</math>


Adiabatic Form of the
First Law of Thermodynamics

(Specific Entropy Conservation)

<math>\frac{d\epsilon}{dt} + P \frac{d}{dt} \biggl(\frac{1}{\rho}\biggr) = 0</math>


Poisson Equation

<math>\nabla^2 \Phi = 4\pi G \rho</math>

Whitworth's (1981) Isothermal Free-Energy Surface

© 2014 - 2021 by Joel E. Tohline
|   H_Book Home   |   YouTube   |
Appendices: | Equations | Variables | References | Ramblings | Images | myphys.lsu | ADS |
Recommended citation:   Tohline, Joel E. (2021), The Structure, Stability, & Dynamics of Self-Gravitating Fluids, a (MediaWiki-based) Vistrails.org publication, https://www.vistrails.org/index.php/User:Tohline/citation