Chandrasekhar's X- and Y-function explained

In atmospheric radiation, Chandrasekhar's X- and Y-function appears as the solutions of problems involving diffusive reflection and transmission, introduced by the Indian American astrophysicist Subrahmanyan Chandrasekhar.[1] [2] [3] [4] [5] The Chandrasekhar's X- and Y-function

X(\mu), Y(\mu)

defined in the interval

0\leq\mu\leq1

, satisfies the pair of nonlinear integral equations

\begin{align} X(\mu)&=1+\mu

1
\int
0
\Psi(\mu')
\mu+\mu'

[X(\mu)X(\mu')-Y(\mu)Y(\mu')]d\mu',\\[5pt] Y(\mu)&=

-\tau1/\mu
e

+\mu

1
\int
0
\Psi(\mu')
\mu-\mu'

[Y(\mu)X(\mu')-X(\mu)Y(\mu')]d\mu' \end{align}

where the characteristic function

\Psi(\mu)

is an even polynomial in

\mu

generally satisfying the condition
1\Psi(\mu)
\int
0

d\mu\leq

1
2

,

and

0<\tau1<infty

is the optical thickness of the atmosphere. If the equality is satisfied in the above condition, it is called conservative case, otherwise non-conservative. These functions are related to Chandrasekhar's H-function as

X(\mu)H(\mu),Y(\mu)0as\tau1 → infty

and also

X(\mu)1,Y(\mu)

-\tau1/\mu
e

as\tau1 → 0.

Approximation

The

X

and

Y

can be approximated up to nth order as

\begin{align} X(\mu)&=

(-1)n
\mu1 … \mun
1
2(0)]
[C1/2
1
1
W(\mu)

[P(-\mu)

-\tau1/\mu
C
0(-\mu)-e

P(\mu)C1(\mu)],\\[5pt] Y(\mu)&=

(-1)n
\mu1 … \mun
1
2(0)]
[C1/2
1
1
W(\mu)
-\tau1/\mu
[e

P(\mu)C0(\mu)-P(-\mu)C1(-\mu)] \end{align}

where

C0

and

C1

are two basic polynomials of order n (Refer Chandrasekhar chapter VIII equation (97)[6]),

P(\mu)=

n
\prod
i=1

(\mu-\mui)

where

\mui

are the zeros of Legendre polynomials and

W(\mu)=

n
\prod
\alpha=1
2\mu
(1-k
\alpha

2)

, where

k\alpha

are the positive, non vanishing roots of the associated characteristic equation

1=2

n
\sum
j=1
aj\Psi(\muj)
2
1-k
j

where

aj

are the quadrature weights given by

aj=

1
P2n'(\muj)
1
\int
-1
P2n(\muj)
\mu-\muj

d\muj

Properties

X(\mu,\tau1),Y(\mu,\tau1)

are the solutions for a particular value of

\tau1

, then solutions for other values of

\tau1

are obtained from the following integro-differential equations
\begin{align} \partialX(\mu,\tau1)
\partial\tau1

&=Y(\mu,\tau1)\int

1
0
d\mu'
\mu'

\Psi(\mu')

Y(\mu',\tau
1),\\ \partialY(\mu,\tau1)
\partial\tau1

+

Y(\mu,\tau1)
\mu

&=X(\mu,\tau1)\int

1
0
d\mu'
\mu'

\Psi(\mu')Y(\mu',\tau1) \end{align}

1
\int
0

X(\mu)\Psi(\mu)d\mu=1-

1
\left[1-2\int
0

\Psi(\mu)d\mu+

1
\left\{\int
0

Y(\mu)\Psi(\mu)d\mu\right\}2\right]1/2.

For conservative case, this integral property reduces to
1
\int
0

[X(\mu)+Y(\mu)]\Psi(\mu)d\mu=1.

xn=

1
\int
0

X(\mu)\Psi(\mu)\mund\mu,yn=

1
\int
0

Y(\mu)\Psi(\mu)\mund\mu,\alphan=

1
\int
0

X(\mu)\mund\mu,\betan=

1
\int
0

Y(\mu)\mund\mu

for brevity are introduced, then we have a relation stating

(1-x0)x2+y0y2+

1
2
2)
(x
1

=

1
\int
0

\Psi(\mu)\mu2d\mu.

In the conservative, this reduces to

y0(x2+y2)+

1
2
1
(x
0

\Psi(\mu)\mu2d\mu

\Psi(\mu)=a+b\mu2

, where

a,b

are two constants, then we have
\alpha
0=1+1
2
2)]
[a(\alpha
1
.

X(\mu),Y(\mu)

are solutions of the original equation, then so are these two functions

F(\mu)=X(\mu)+Q\mu[X(\mu)+Y(\mu)],G(\mu)=Y(\mu)+Q\mu[X(\mu)+Y(\mu)]

, where

Q

is an arbitrary constant.

See also

Notes and References

  1. Chandrasekhar, Subrahmanyan. Radiative transfer. Courier Corporation, 2013.
  2. Howell, John R., M. Pinar Menguc, and Robert Siegel. Thermal radiation heat transfer. CRC press, 2010.
  3. Modest, Michael F. Radiative heat transfer. Academic press, 2013.
  4. Hottel, Hoyt Clarke, and Adel F. Sarofim. Radiative transfer. McGraw-Hill, 1967.
  5. Sparrow, Ephraim M., and Robert D. Cess. "Radiation heat transfer." Series in Thermal and Fluids Engineering, New York: McGraw-Hill, 1978, Augmented ed. (1978).
  6. Chandrasekhar, Subrahmanyan. Radiative transfer. Courier Corporation, 2013.