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Absorption of Radiation01:05

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The rate of heat transfer by emitted radiation is described by the Stefan-Boltzmann law of radiation:
Conduction, Convection and Radiation: Problem Solving01:20

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There are three methods by which heat transfer can take place: conduction, convection, and radiation. Each method has unique and interesting characteristics, but all three have two things in common: they transfer heat solely because of a temperature difference; and the greater the temperature difference, the faster the heat transfer.
In order to solve a problem related to heat transfer, first of all, the situation needs to be examined to determine the type of heat transfer involved. This could...
Plane Electromagnetic Waves I01:30

Plane Electromagnetic Waves I

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Radiation: Applications01:17

Radiation: Applications

The average temperature of Earth is the subject of much current discussion. Earth is in radiative contact with both the Sun and dark space; it receives almost all its energy from the radiation of the Sun and reflects some of it into outer space. Dark space is very cold, about 3 K, so Earth radiates energy into it. For instance, heat transfer occurs from soil and grasses, the rate of which can be so rapid that frost can occur on clear summer evenings, even in warm latitudes.
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Linear Approximations01:23

Linear Approximations

For a differentiable function of two variables, linear approximation estimates values near a known point by replacing the curved surface with its tangent plane. Consider the function\begin{equation*}f(x,y)=x^2+3y^2\end{equation*}near the point (2, 1). The exact value at this point is f(2, 1) = 22 + 3(1)2 = 4 + 3 = 7.The linear approximation of f(x, y)) near (a, b) is\begin{equation*}L(x,y)=f(a,b)+f_x(a,b)(x-a)+f_y(a,b)(y-b)\end{equation*}First, compute the partial derivatives: fx(x, y) = 2x and...
Radiation Pressure: Problem Solving01:09

Radiation Pressure: Problem Solving

The radiation pressure applied by an electromagnetic wave on a perfectly absorbing surface equals the energy density of the wave. The wave's momentum also gets transferred to the surface when an electromagnetic wave is entirely absorbed by it. The rate at which momentum is transmitted to an absorbing surface perpendicular to the propagation direction equals the force on the surface.
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Related Experiment Video

Updated: Jun 16, 2026

Scattering And Absorption of Light in Planetary Regoliths
11:34

Scattering And Absorption of Light in Planetary Regoliths

Published on: July 1, 2019

Approximate method for radiative transfer in scattering absorbing plane-parallel media.

Y S Chou

    Applied Optics
    |February 23, 2010
    PubMed
    Summary
    This summary is machine-generated.

    This study introduces an approximate method for calculating radiation transfer in scattering and absorbing media. The approach simplifies complex equations, offering accurate solutions for engineering applications.

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    Area of Science:

    • Radiative Transfer Theory
    • Computational Physics
    • Optical Engineering

    Background:

    • Calculating radiation transfer in scattering and absorbing media is crucial for various engineering applications.
    • Existing methods for solving the radiative transfer equation can be computationally intensive.

    Purpose of the Study:

    • To develop an approximate method for calculating specific intensities in plane-parallel media.
    • To simplify the integral-differential transfer equation into a system of ordinary differential equations.

    Main Methods:

    • Representing the phase function using a Legendre series.
    • Expressing scattered intensity as a series of scattering orders.
    • Reducing the transfer equation to ordinary differential equations.
    • Employing simple numerical integration in optical depth.

    Main Results:

    • The method successfully reduces the integral-differential transfer equation.
    • Closed-form solutions are obtained for isotropic scattering.
    • Approximate solutions show 10-25% agreement with exact numerical solutions for both isotropic and anisotropic cases.

    Conclusions:

    • The developed approximate method provides accurate and efficient solutions for radiative transfer problems.
    • This method is suitable for most engineering applications requiring specific intensity calculations.