Chandrasekhar's X- and Y-function

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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(μ), Y(μ) defined in the interval 0μ1, satisfies the pair of nonlinear integral equations

X(μ)=1+μ01Ψ(μ)μ+μ[X(μ)X(μ)Y(μ)Y(μ)]dμ,Y(μ)=eτ1/μ+μ01Ψ(μ)μμ[Y(μ)X(μ)X(μ)Y(μ)]dμ

where the characteristic function Ψ(μ) is an even polynomial in μ generally satisfying the condition

01Ψ(μ)dμ12,

and 0<τ1< 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(μ)H(μ),Y(μ)0 as τ1

and also

X(μ)1,Y(μ)eτ1/μ as τ10.

Approximation

The X and Y can be approximated up to nth order as

X(μ)=(1)nμ1μn1[C02(0)C12(0)]1/21W(μ)[P(μ)C0(μ)eτ1/μP(μ)C1(μ)],Y(μ)=(1)nμ1μn1[C02(0)C12(0)]1/21W(μ)[eτ1/μP(μ)C0(μ)P(μ)C1(μ)]

where C0 and C1 are two basic polynomials of order n (Refer Chandrasekhar chapter VIII equation (97)[6]), P(μ)=i=1n(μμi) where μi are the zeros of Legendre polynomials and W(μ)=α=1n(1kα2μ2), where kα are the positive, non vanishing roots of the associated characteristic equation

1=2j=1najΨ(μj)1k2μj2

where aj are the quadrature weights given by

aj=1P2n(μj)11P2n(μj)μμjdμj

Properties

  • If X(μ,τ1), Y(μ,τ1) are the solutions for a particular value of τ1, then solutions for other values of τ1 are obtained from the following integro-differential equations
X(μ,τ1)τ1=Y(μ,τ1)01dμμΨ(μ)Y(μ,τ1),Y(μ,τ1)τ1+Y(μ,τ1)μ=X(μ,τ1)01dμμΨ(μ)Y(μ,τ1)
  • 01X(μ)Ψ(μ)dμ=1[1201Ψ(μ)dμ+{01Y(μ)Ψ(μ)dμ}2]1/2. For conservative case, this integral property reduces to 01[X(μ)+Y(μ)]Ψ(μ)dμ=1.
  • If the abbreviations xn=01X(μ)Ψ(μ)μndμ, yn=01Y(μ)Ψ(μ)μndμ, αn=01X(μ)μndμ, βn=01Y(μ)μndμ for brevity are introduced, then we have a relation stating (1x0)x2+y0y2+12(x12y12)=01Ψ(μ)μ2dμ. In the conservative, this reduces to y0(x2+y2)+12(x12y12)=01Ψ(μ)μ2dμ
  • If the characteristic function is Ψ(μ)=a+bμ2, where a,b are two constants, then we have α0=1+12[a(α02β02)+b(α12β12)].
  • For conservative case, the solutions are not unique. If X(μ), Y(μ) are solutions of the original equation, then so are these two functions F(μ)=X(μ)+Qμ[X(μ)+Y(μ)], G(μ)=Y(μ)+Qμ[X(μ)+Y(μ)], where Q is an arbitrary constant.

See also

References

Template:Reflist

  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.