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 0≤μ≤1, satisfies the pair of nonlinear integral equations

X(μ)=1+μ∫01Ψ(μ′)μ+μ′[X(μ)X(μ′)−Y(μ)Y(μ′)]dμ′,Y(μ)=e−τ1/μ+μ∫01Ψ(μ′)μ−μ′[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)dμ≤12,

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)→e−τ1/μ as τ1→0.

Approximation

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

X(μ)=(−1)nμ1⋯μn1[C02(0)−C12(0)]1/21W(μ)[P(−μ)C0(−μ)−e−τ1/μP(μ)C1(μ)],Y(μ)=(−1)nμ1⋯μn1[C02(0)−C12(0)]1/21W(μ)[e−τ1/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(μ−μi) where μi are the zeros of Legendre polynomials and W(μ)=∏α=1n(1−kα2μ2), where kα are the positive, non vanishing roots of the associated characteristic equation

1=2∑j=1najΨ(μj)1−k2μj2

where aj are the quadrature weights given by

aj=1P2′n(μj)∫−11P2n(μj)μ−μjdμj

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)∫01dμ′μ′Ψ(μ′)Y(μ′,τ1),∂Y(μ,τ1)∂τ1+Y(μ,τ1)μ=X(μ,τ1)∫01dμ′μ′Ψ(μ′)Y(μ′,τ1)
  • ∫01X(μ)Ψ(μ)dμ=1−[1−2∫01Ψ(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 (1−x0)x2+y0y2+12(x12−y12)=∫01Ψ(μ)μ2dμ. In the conservative, this reduces to y0(x2+y2)+12(x12−y12)=∫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(α02−β02)+b(α12−β12)].
  • 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.