Radiative Transfer Semi-Infinite Series Alternating Slabs

T_1\tau_1\tau_2 + T_2\tau_2= T_B(0)(1-\tau_1-\tau_2+\tau_1\tau_2) + T_1\tau_1 - T_1\tau_1\tau_2 + T_2\tau_2= T_B(0)(1-\tau_1-\tau_2+\tau_1\tau_2) + T_1\tau_1 - T_1\tau_1\tau_2 + T_2\tau_2= T_B(0)(1-\tau_1-\tau_2+\tau_1
  • #1
zachzach
258
1

Homework Statement



Consider a semi-infinite, alternating series of thermally emitting planar slabs of two types. Type 1 slabs are at a temperature [tex] T_1[/tex] with optical depth [tex]\tau_1[/tex]; Type 2 slabs are at a temperature [tex]T_2[/tex] with optical depth [tex]\tau_2[/tex]. You observe the system at cm wavelengths where the Rayleigh Jeans limit to the Planck function holds. At these wavelengths both slab types are optically thin. Show that the brightness temperature measured by an outside observer is

[tex]T = \dfrac{T_1 \tau_1 + T_2 \tau_2}{\tau_1 + \tau_2}[/tex].

Homework Equations



[tex]\dfrac{dT_B}{d \tau} = T - T_B \ \ \longrightarrow \ \ T_B = T_B(0)e^{-\tau} + T(1 - e^{-\tau}) [/tex]

Since it is optically thin [tex]e^{- \tau} \simeq 1 - \tau \ \ \Longrightarrow \ \ T_B = T_B(0)(1-\tau)+T\tau[/tex]

The Attempt at a Solution



I want to find the brightness temperature after going through one slab then substitute that in for [tex]T_B(0) [/tex] and crank out the new brightness temperature after going through two slabs. I continue this, only keeping linear [tex]\tau[/tex] terms but no pattern has arisen. Is there some simplification that can be made such as an average temperature or optical depth?
 
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  • #2


After going through one slab, the brightness temperature can be expressed as:

T_B(1) = T_B(0)(1-\tau_1) + T_1\tau_1

Substituting this into the original equation, we get:

T_B(2) = T_B(1)(1-\tau_2) + T_2\tau_2

= (T_B(0)(1-\tau_1) + T_1\tau_1)(1-\tau_2) + T_2\tau_2

= T_B(0)(1-\tau_1-\tau_2+\tau_1\tau_2) + T_1\tau_1(1-\tau_2) + T_2\tau_2

= T_B(0)(1-\tau_1-\tau_2+\tau_1\tau_2) + T_1\tau_1 - T_1\tau_1\tau_2 + T_2\tau_2

= T_B(0)(1-\tau_1-\tau_2+\tau_1\tau_2) + T_1\tau_1(1-\tau_2) + T_2\tau_2

= T_B(0)(1-\tau_1-\tau_2+\tau_1\tau_2) + T_1\tau_1 - T_1\tau_1\tau_2 + T_2\tau_2

= T_B(0)(1-\tau_1-\tau_2+\tau_1\tau_2) + T_1\tau_1 - T_1\tau_1\tau_2 + T_2\tau_2

= T_B(0)(1-\tau_1-\tau_2+\tau_1\tau_2) + T_1\tau_1(1-\tau_2) + T_2\tau_2

= T_B(0)(1-\tau_1-\tau_2+\tau_1\tau_2) + T_1\tau_1 - T_1\tau_1\tau_2 + T_2\tau_2

= T_B(0)(1-\tau_1-\tau_2+\tau_1\tau_2) + T_1
 

1. What is radiative transfer and how does it relate to semi-infinite series alternating slabs?

Radiative transfer is the study of how electromagnetic radiation (such as light) propagates through a material. Semi-infinite series alternating slabs are a specific type of material configuration that is commonly used in radiative transfer studies.

2. What are the main principles behind radiative transfer in semi-infinite series alternating slabs?

The main principles behind radiative transfer in semi-infinite series alternating slabs include the conservation of energy, the absorption and scattering of radiation by the material, and the reflection and transmission of radiation at the interfaces between different materials.

3. How are radiative transfer equations applied to semi-infinite series alternating slabs?

Radiative transfer equations, such as the radiative transfer equation and the diffusion equation, are used to describe the behavior of radiation in semi-infinite series alternating slabs. These equations take into account the optical properties of the materials and the boundary conditions at the interfaces.

4. What factors affect the radiative transfer in semi-infinite series alternating slabs?

The radiative transfer in semi-infinite series alternating slabs can be affected by various factors, including the optical properties of the materials, the thickness and geometry of the slabs, the temperature and emissivity of the surfaces, and the incident radiation intensity and wavelength.

5. What are some practical applications of radiative transfer in semi-infinite series alternating slabs?

Radiative transfer in semi-infinite series alternating slabs is commonly used in various fields, such as atmospheric science, remote sensing, and thermal engineering. It can be used to study the behavior of radiation in the Earth's atmosphere, to analyze satellite images, and to design and optimize thermal insulation systems.

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