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==Principal Governing Equations== | ==Principal Governing Equations== | ||
According to the eloquent discussion of the broad subject of ''Fluid Mechanics'' presented by Landau and Lifshitz (1975), <FONT COLOR="#007700">the state of a moving fluid is determined by five quantities: the three components of the velocity</FONT> | According to the eloquent discussion of the broad subject of ''Fluid Mechanics'' presented by Landau and Lifshitz (1975), <FONT COLOR="#007700">the state of a moving fluid is determined by five quantities: the three components of the velocity</FONT> {{User:Tohline/Math/VAR_VelocityVector01}} <FONT COLOR="#007700">and, for example, the pressure</FONT> {{User:Tohline/Math/VAR_Pressure01}} <FONT COLOR="#007700">and the density</FONT> {{User:Tohline/Math/VAR_Density01}} <FONT COLOR="#007700">.</FONT> For our discussions of astrophysical fluid systems throughout this Hypertext Book [H_Book], we will add to this the gravitational potential {{User:Tohline/Math/VAR_NewtonianPotential01}}. <FONT COLOR="#007700">Accordingly, a complete system of equations of fluid dynamics should be</FONT> six <FONT COLOR="#007700">in number. For an ideal fluid these are:</FONT> | ||
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In this last expression, {{User:Tohline/Math/C_GravitationalConstant}} is the Newtonian gravitational constant. | |||
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Revision as of 00:32, 22 January 2010
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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>T \frac{ds}{dt} = \frac{d\epsilon}{dt} + P \frac{d}{dt} \biggl(\frac{1}{\rho}\biggr)</math> |
Poisson Equation
<math>\nabla^2 \Phi = 4\pi G \rho</math> |
In this last expression, <math>~G</math> is the Newtonian gravitational constant.
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