Chandrasekhar's H-function

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Chandrasekhar's H-function for different albedo

In atmospheric radiation, Chandrasekhar's H-function appears as the solutions of problems involving scattering, introduced by the Indian American astrophysicist Subrahmanyan Chandrasekhar.[1][2][3][4][5] The Chandrasekhar's H-function H(μ) defined in the interval 0μ1, satisfies the following nonlinear integral equation

H(μ)=1+μH(μ)01Ψ(μ)μ+μH(μ)dμ

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

01Ψ(μ)dμ12.

If the equality is satisfied in the above condition, it is called conservative case, otherwise non-conservative. Albedo is given by ωo=2Ψ(μ)=constant. An alternate form which would be more useful in calculating the H function numerically by iteration was derived by Chandrasekhar as,

1H(μ)=[1201Ψ(μ)dμ]1/2+01μΨ(μ)μ+μH(μ)dμ.

In conservative case, the above equation reduces to

1H(μ)=01μΨ(μ)μ+μH(μ)dμ.

Approximation

The H function can be approximated up to an order n as

H(μ)=1μ1μni=1n(μ+μi)α(1+kαμ)

where μi are the zeros of Legendre polynomials P2n and 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

Explicit solution in the complex plane

In complex variable z the H equation is

H(z)=101zz+μH(μ)Ψ(μ)dμ,01|Ψ(μ)|dμ12,0δ|Ψ(μ)|dμ0, δ0

then for (z)>0, a unique solution is given by

lnH(z)=12πii+ilnT(w)zw2z2dw

where the imaginary part of the function T(z) can vanish if z2 is real i.e., z2=u+iv=u (v=0). Then we have

T(z)=1201Ψ(μ)dμ201μ2Ψ(μ)uμ2dμ

The above solution is unique and bounded in the interval 0z1 for conservative cases. In non-conservative cases, if the equation T(z)=0 admits the roots ±1/k, then there is a further solution given by

H1(z)=H(z)1+kz1kz

Properties

  • 01H(μ)Ψ(μ)dμ=1[1201Ψ(μ)dμ]1/2. For conservative case, this reduces to 01Ψ(μ)dμ=12.
  • [1201Ψ(μ)dμ]1/201H(μ)Ψ(μ)μ2dμ+12[01H(μ)Ψ(μ)μdμ]2=01Ψ(μ)μ2dμ. For conservative case, this reduces to 01H(μ)Ψ(μ)μdμ=[201Ψ(μ)μ2dμ]1/2.
  • If the characteristic function is Ψ(μ)=a+bμ2, where a,b are two constants(have to satisfy a+b/31/2) and if αn=01H(μ)μndμ, n1 is the nth moment of the H function, then we have
α0=1+12(aα02+bα12)

and

(a+bμ2)01H(μ)μ+μdμ=H(μ)1μH(μ)b(α1μα0)

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).