SSC/Structure/BiPolytropes/51RenormaizePart2: Difference between revisions
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===Finite-Difference Representation of Equilibrium State=== | ===Finite-Difference Representation of Equilibrium State=== | ||
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<div align="center"><font color="red"><b>CAUTION!</b></font> Regarding Our Chosen Lagrangian Fluid Marker</div> | |||
If we were to use <math>\tilde{r}</math> as our primary Lagrangian fluid marker, we would be in a position to analytically specify the function, <math>\tilde{M}_r(\tilde{r})</math>. Here, however, we will call upon <math>\tilde{M}_r</math> rather than <math>\tilde{r}</math> to serve as the primary Lagrangian fluid marker because mass facilitates our efforts to highlight a variety of important physical properties of bipolytropic configurations. We will therefore need to specify the function, <math>\tilde{r}(\tilde{M}_r)</math> instead of <math>\tilde{M}_r(\tilde{r})</math>. | |||
For the core, this choice does not introduce any particularly difficult computational challenges because we can invert the <math>\tilde{M}_r(\tilde{r})</math> relationship analytically. This is not the case for the envelope, however; we will not be able to analytically specify <math>\tilde{r}(\tilde{M}_r)</math>. This is unfortunate, as a ''numerical'' (rather than analytic) specification will necessarily introduce additional errors into our solution of the displacement function — which already is a small and error-prone quantity. | |||
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<font color="red"><b>STEP1:</b></font> Divide the core into <math>(N_c+1)</math> grid lines — that is, into <math>N_c</math> radial zones — associating the first "grid line" with the center of the core and the last grid line with the radial location of the core/envelope interface. Choosing <math>0 \le \tilde{M}_r \le q</math> as the principal Lagrangian coordinate, and using the available analytic expressions, assign values to the following physical quantities at each grid line: | <font color="red"><b>STEP1:</b></font> Divide the core into <math>(N_c+1)</math> grid lines — that is, into <math>N_c</math> radial zones — associating the first "grid line" with the center of the core and the last grid line with the radial location of the core/envelope interface. Choosing <math>0 \le \tilde{M}_r \le q</math> as the principal Lagrangian coordinate, and using the available analytic expressions, assign values to the following physical quantities at each grid line: | ||
Revision as of 18:21, 20 August 2022
Radial Oscillations in (nc,ne) = (5,1) Bipolytropes
Logically, this chapter extends the discussion — specifically the subsection titled, Try Again — found in the "Ramblings" chapter in which we introduced a total-mass-based renormalization of models along sequences of bipolytropes.
Building Each Model
Basic Equilibrium Structure
Most of the details underpinning the following summary relations can be found here.
Note: For an n = 5 polytrope (like our bipolytrope's core), the units of the polytropic constant, , are .
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Note that, for a given specification of the molecular-weight ratio, , and the interface location, , in which case,
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Additional Relations
Core
The analytically prescribed radial pressure gradient in the core can be obtained as follows.
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Also,
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Hence,
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For comparison, in hydrostatic balance we expect …
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This matches our earlier expression, as it should.
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Takeaway Expression
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Envelope
Given that, for the envelope,
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and, |
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we deduce that,
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As a cross-check …
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and,
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That is,
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Correct!
Time-Dependent Euler Equation
We begin with the form of the,
Euler Equation
that is broadly relevant to studies of radial oscillations in spherically symmetric configurations. Recognizing from, for example, a related discussion that, , and that,
we obtain our
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Desired Form of the Euler Equation |
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Given as well that,
we see that,
Next, if as above, we multiply through by , we obtain the relevant,
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Normalized Euler Equation |
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where, as a reminder, the dimensionless time is,
Finite-Difference Representation of Equilibrium State
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CAUTION! Regarding Our Chosen Lagrangian Fluid Marker
If we were to use as our primary Lagrangian fluid marker, we would be in a position to analytically specify the function, . Here, however, we will call upon rather than to serve as the primary Lagrangian fluid marker because mass facilitates our efforts to highlight a variety of important physical properties of bipolytropic configurations. We will therefore need to specify the function, instead of . For the core, this choice does not introduce any particularly difficult computational challenges because we can invert the relationship analytically. This is not the case for the envelope, however; we will not be able to analytically specify . This is unfortunate, as a numerical (rather than analytic) specification will necessarily introduce additional errors into our solution of the displacement function — which already is a small and error-prone quantity. |
STEP1: Divide the core into grid lines — that is, into radial zones — associating the first "grid line" with the center of the core and the last grid line with the radial location of the core/envelope interface. Choosing as the principal Lagrangian coordinate, and using the available analytic expressions, assign values to the following physical quantities at each grid line:
- Mass: Set ; then, for , set
Example Models Along BiPolytrope Sequence 0.3100
For the case of and , we consider here the examination of models with three relatively significant values of the core/envelope interface:
- Model D : Approximate location along the sequence of the model with the maximum fractional core radius.
- Model C : Approximate location along the sequence of the onset of fundamental-mode instability.
- Model A : Exact location along the sequence of the model with the maximum fractional core mass.
Model C
Here we examine a discrete representation of a model along the sequence whose core/envelope interface is located a .
See Also
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Appendices: | VisTrailsEquations | VisTrailsVariables | References | Ramblings | VisTrailsImages | myphys.lsu | ADS | |