Introduction to Thermal Radiation

Similar documents
ME 476 Solar Energy UNIT TWO THERMAL RADIATION

Heat Transfer: Physical Origins and Rate Equations. Chapter One Sections 1.1 and 1.2

Thermal Radiation By: Prof. K M Joshi

Chapter 11 FUNDAMENTALS OF THERMAL RADIATION

INTRODUCTION Radiation differs from conduction and convection in that it does not require the presence of a material medium to take place.

Lecture # 04 January 27, 2010, Wednesday Energy & Radiation

Numerical Heat and Mass Transfer

21 1 INTRODUCTION. FIGURE 21 1 A hot object in a vacuum chamber loses heat by radiation only.

Chapter 1 INTRODUCTION AND BASIC CONCEPTS

Introduction to Electromagnetic Radiation and Radiative Transfer

Heat and Mass Transfer Unit-1 Conduction

Lecture 5: Greenhouse Effect

Lecture 22. Temperature and Heat

Lecture 5: Greenhouse Effect

Spectrum of Radiation. Importance of Radiation Transfer. Radiation Intensity and Wavelength. Lecture 3: Atmospheric Radiative Transfer and Climate

Lecture 3: Atmospheric Radiative Transfer and Climate

ATMOS 5140 Lecture 7 Chapter 6

Mechanical Engineering. Postal Correspondence Course HEAT TRANSFER. GATE, IES & PSUs

INFRAMET. 2.1 Basic laws

Electromagnetic Radiation. Physical Principles of Remote Sensing

Fundamental Concepts of Radiation -Basic Principles and Definitions- Chapter 12 Sections 12.1 through 12.3

Dr. Linlin Ge The University of New South Wales

AT622 Section 3 Basic Laws

Heriot-Watt University

1. The most important aspects of the quantum theory.

Chemistry 795T. Lecture 7. Electromagnetic Spectrum Black body Radiation. NC State University

Chemistry 795T. Black body Radiation. The wavelength and the frequency. The electromagnetic spectrum. Lecture 7

Chemistry 431. Lecture 1. Introduction Statistical Averaging Electromagnetic Spectrum Black body Radiation. NC State University

Paper No. : 04 Paper Title: Unit Operations in Food Processing Module-07: Heat Transfer 3: Heat Radiation

Law of Heat Transfer

Lecture Outline. Energy 9/25/12

Earth: A Dynamic Planet A. Solar and terrestrial radiation

Modeling of Environmental Systems

Thermal Systems. What and How? Physical Mechanisms and Rate Equations Conservation of Energy Requirement Control Volume Surface Energy Balance

Arctice Engineering Module 3a Page 1 of 32

Prof. Jeff Kenney Class 4 May 31, 2018

Lecture 4: Heat, and Radiation

Radiative heat transfer

THERMODYNAMICS METHODS OF HEAT TRANSFER RADIATION

Properties of Electromagnetic Radiation Chapter 5. What is light? What is a wave? Radiation carries information

Earth: the Goldilocks Planet

Thermodynamics and Energy. First Law of Thermodynamics and Energy Transfer Mechanisms. Applications of Thermodynamics

The Nature of Light I: Electromagnetic Waves Spectra Kirchoff s Laws Temperature Blackbody radiation

Chapter 3 Energy Balance and Temperature. Topics to be covered

ATMO/OPTI 656b Spring 2009

Modern Physics. Unit 1: Classical Models and the Birth of Modern Physics Lecture 1.4: Blackbody Radiation and Photoelectric Effect

Lecture 2 Blackbody radiation

What is it good for? RT is a key part of remote sensing and climate modeling.

Unit B-4: List of Subjects

Reading Problems , 15-33, 15-49, 15-50, 15-77, 15-79, 15-86, ,

Energy. Kinetic and Potential Energy. Kinetic Energy. Kinetic energy the energy of motion

Overview of fundamental atmospheric concepts

Chapter 3 Energy Balance and Temperature. Astro 9601

Mechanisms of heat transfer

K20: Temperature, Heat, and How Heat Moves

Temperature Scales

General Physics (PHY 2130)

Absorptivity, Reflectivity, and Transmissivity

Applied Thermodynamics HEAT TRANSFER. Introduction What and How?

Radiation Heat Transfer. Introduction. Blackbody Radiation. Definitions ,

MASSACHUSETTS INSTITUTE OF TECHNOLOGY Department of Physics Problem Solving 10: The Greenhouse Effect. Section Table and Group

THE EXOSPHERIC HEAT BUDGET

Chapter 13. Phys 322 Lecture 34. Modern optics

Modern Physics (Lec. 1)

TRANSMISSION OF HEAT

Take away concepts. What is Energy? Solar Radiation Emission and Absorption. Energy: The ability to do work

The Planck Distribution. The Planck law describes theoretical spectral distribution for the emissive power of a black body. It can be written as

Lecture 2 Global and Zonal-mean Energy Balance

Outline. Stock Flow and temperature. Earth as a black body. Equation models for earth s temperature. Balancing earth s energy flows.

Chapter 12. Temperature and Heat. continued

Blackbody radiation. Main Laws. Brightness temperature. 1. Concepts of a blackbody and thermodynamical equilibrium.

Atmospheric Radiation

Energy and Radiation. GEOG/ENST 2331 Lecture 3 Ahrens: Chapter 2

C ONTENTS CHAPTER TWO HEAT CONDUCTION EQUATION 61 CHAPTER ONE BASICS OF HEAT TRANSFER 1 CHAPTER THREE STEADY HEAT CONDUCTION 127

12.815/12.816: RADIATIVE TRANSFER PROBLEM SET #1 SOLUTIONS

G α Absorbed irradiation

2. Energy Balance. 1. All substances radiate unless their temperature is at absolute zero (0 K). Gases radiate at specific frequencies, while solids

The term "black body" was introduced by Gustav Kirchhoff in The light emitted by a black body is called black-body radiation.

Preface to the Second Edition. Preface to the First Edition

ElectroMagnetic Radiation (EMR) Lecture 2-3 August 29 and 31, 2005

Advanced Heat and Mass Transfer by Amir Faghri, Yuwen Zhang, and John R. Howell

1. Radiative Transfer. 2. Spectrum of Radiation. 3. Definitions

Sources of radiation

Physics 1501 Lecture 35

Lecture 2: principles of electromagnetic radiation

Section 7. Temperature Measurement

PROBLEM L. (3) Noting that since the aperture emits diffusely, I e = E/π (see Eq ), and hence

Lecture 4: Radiation Transfer

Lecture Notes Prepared by Mike Foster Spring 2007

Goal: The theory behind the electromagnetic radiation in remote sensing. 2.1 Maxwell Equations and Electromagnetic Waves

Lasers PH 645/ OSE 645/ EE 613 Summer 2010 Section 1: T/Th 2:45-4:45 PM Engineering Building 240

Fundamentals of Atmospheric Radiation and its Parameterization

Latest Heat Transfer

Lecture 3: Global Energy Cycle

Chapter 11. Energy in Thermal Processes

Understanding the Greenhouse Effect

Monday 9 September, :30-11:30 Class#03

HEAT TRANSFER 1 INTRODUCTION AND BASIC CONCEPTS 5 2 CONDUCTION

Radiation Conduction Convection

TOPIC # 6 The RADIATION LAWS

Transcription:

Introduction to Thermal Radiation Figures except for the McDonnell Douglas figures come from Incorpera & DeWitt, Introduction to Heat and Mass Transfer or Cengel, Heat Transfer: Practical pproach

Thermal Radiation Occurs in solids, liquids, and gases Occurs at the speed of light Has no attenuation in a vacuum Can occur between two bodies with a colder medium in between pplications: satellite temperature management, taking accurate temperature measurements, designing heaters for manufacturing, estimating heat gains through windows, infrared cameras, metal cooling during manufacturing, Greenhouse effect, lasers, insulating cryogenic tanks, thermos design, ice skating rink ceiling design

Background Electromagnetic radiation energy emitted due to changes in electronic configurations of atoms or molecules where l=wavelength (usually in mm), n=frequency In a vacuum c=c o =2.998x10 8 m/s Other media: c=c o /n lwhere cn=index n of refraction

Background, cont. Radiation photons or waves? Max Planck (1900): each photon has an energy of h=planck s constant=6.625 x 10-34 Js Shorter wavelengths have higher energy e hn hc l

Radiation Spectrum

Types of Radiation Two categories Volumetric phenomenon radiation emitted or absorbed throughout gases, transparent solids, some fluids Surface phenomenon radiation to/from solid or liquid surface Thermal radiation emitted by all substances above absolute zero Includes visible & infrared radiation & some UV radiation.

Radiation Properties Magnitude of radiation varies with wavelength it s spectral. The wavelength of the radiation is a major factor in what its effects will be. Earth/sun example Radiation is made up of a continuous, nonuniform distribution of monochromatic (single-wavelength) components. Magnitude & spectral distribution (how the radiation varies with wavelength) vary with temp & type of emitting surface.

Emission Variation with Wavelength

Blackbody Radiation Blackbody a perfect emitter & absorber of radiation; it absorbs all incident radiation, and no surface can emit more for a given temperature and wavelength Emits radiation uniformly in all directions no directional distribution it s diffuse Example of a blackbody: large cavity with a small hole Joseph Stefan (1879) total radiation emission per unit time 4& area over 2 all wavelengths Eand b in st all directions: W m

Planck s Distribution Law Sometimes we care about the radiation in a certain wavelength interval For a surface in a vacuum or gas C 1 2 Ebl T W m μm 5 l exp C lt 1 where C C k 1 2 2hc hc o 2 o k 13805. x10 1. 439x10-23 2 3. 742x10 J/K 8 4 W μm μm K 4 m Boltzmann's constant 2 Integrating this function over all l gives us E b st 4

Radiation Distribution Radiation is a continuous function of wavelength Magnitude increases with temp. t higher temps, more radiation is at shorter wavelengths. Solar radiation peak is in the visible range.

Wien s Displacement Law Wavelength of radiation with the largest magnitude can be found for different temps using Wien s Displacement Law: Note that color is a function of absorption & reflection, not emission lt max 2897.8 mmk power

Blackbody Radiation Function We often are interested in radiation energy emitted over a certain wavelength interval. This is a tough integral to do!

Blackbody Radiation Function Use blackbody radiation function, F l (often called the fractional function) F l T l 0 E bl st T If we want radiation between l 1 & l 2, F l 4 dl T F T F T 1l2 l2 l1

More Radiation Properties Directional distribution a surface doesn t emit the same in all directions. Hemispherical refers to all directions

ngle definitions zenith angle q up and down) azimuthal angle f side to side)

Solid ngle differential solid angle dwd n /r 2 = d 1 cosq/r 2 =sinq dq df solid angle is for a sphere what an angle is for a circle Units: steradians (sr); For a sphere w=4 sr

Solid ngle, cont.

Spectral Intensity I l,e : rate at which radiant energy is emitted at the wavelength l in the (q,f) direction, per unit area of the emitting surface normal to this direction, per unit solid angle about this direction, and per unit wavelength interval dl about l Translation: rate of emission at a given wavelength, in a given direction, per unit area, solid angle, and wavelength interval Units: W/(m 2 sr mm)

Spectral Intensity I l l q f,,, e n dq d d d l d d n 1 cos q

To solve for dq dq I d d d l, e l, q, f 1cosq l Sometimes we know the intensity I e rather than the spectral intensity (i.e., the rate of emission in a given direction, per unit area and solid angle). This is I l,e integrated over all wavelengths. Then dq I q, f d cosq d e 1

Total heat flux To find the total heat flux, we must integrate over both angles and wavelength. OR,, 0 2 2 q l I l q f cosq sinq dq df l 0 0 q q l dl l 2 2 0 0 0 l, e q I cos sin d d d total heat flux l, e l, q, f q q q f l spectral heat flux total heat flux

Emissive Power E: amount of radiation emitted per unit area Spectral hemispherical emissive power E l (often leave out the word hemispherical ) W/m 2 l Rate of emission per unit area of radiation of a given wavelength l in all directions per unit wavelength interval Total (hemisperical) emissive power E (W/m 2 ) q emitted Rate of emission per unit area of radiation of all wavelengths and in all directions; this is

Diffuse emitters Diffuse emitter: intensity is the same in all directions; integration is easy! E l I l and E I l l, e 0 where Ie Il, edl e

Irradiation, G Irradiation: radiation incident on (hitting) a surface per unit area Use subscript i Same equations as E except replace E with G and I l,e with I l,i (intensity of incident radiation)

Radiosity, J Radiosity: all radiation leaving a surface per unit area, both emitted and reflected Use subscript e+r Same equations as E except replace E with J and I l,e with I l,e+r (intensity of emitted+reflected radiation)

Example 1 small surface of area 1 =3 cm 2 diffusely emits radiation with an emissive power of 7350 W/m 2. Part of the radiation strikes another small surface of area 2 =5 cm 2 oriented as shown on the board. a) Find the intensity of the emitted radiation. b) Find the solid angle subtended by 2 when viewed from 1. c) Find the rate of radiation emitted by 1 that strikes 2.

3 Introduction to Mass Transfer

Overview Thermodynamics heat and mass transfer chemical reaction rate theory(chemical kinetics)

Rudiments of Mass Transfer Open a bottle of perfume in the center of a room---mass transfer Molecular processes(e.g., collisions in an ideal gas) turbulent processes.

Mass Transfer Rate Laws Fick s law of Diffusion one dimension: m Y ( m m ) B D B dy dx Mass flow of species per unit area Mass flow of species associated with bulk flow per unit area Mass flow of species associated with molecular diffusion per unit area

The mass flux is defined as the mass flowrate of species per unit area perpendicular to the flow: m m / The units are kg/s-m 2 D B is a property of the mixture and has units of m 2 /s, the binary diffusivity.

It means that species is transported by two means: the first term on the right-hand-side representing the transported of resulting from the bulk motion of the fluid, and the second term representing the diffusion of superimposed on the bulk flow.

In the abseence of diffusion, we obtain the obvious result that where is the mixture mass flux. The diffusion flux adds an additional component to the flux of : m Y ( m m ) Y m m B Bulk flux of species D B dy dx Diffusiona l flux of species,m,diff.

n analogy between the diffusion of mass and the diffusion of heat (conduction) can be drawn by comparing Fourier s law of conduction: Q k x dt dx

The more general expression m Y ( m m B D B Y where the bold symbols represent vector quantities. In many instants, the molar form of the above equation is useful: ) N x ( N N B ) D B x

Where is the molar flux(kmol/s-m 2 ) of species, x is the N mole fraction, and c is the mixture molar concentration(kmol mix /m 3 ) The meanings of bulk flow and diffusion flux become clearer if we express the total mass flux for a binary mixture as the sum of the mass flux of species and the mass flux of species B:

m m m B Mixture mass flux Speies mass flux Species B mass flux

For one dimension: or m Y m D B dy dx Y B m D B dy dx B m ( Y Y ) m B dy DB dx D B dy dx B

For a binary mixture, Y +Y B =1, thus, D B dy dx D B dy B dx 0 Diffusional flux of species Diffusional flux of species B

In general, overall mass conservation required that: m 0 i,diff

This is called ordinary diffusion. Not binary mixture; thermal diffusion pressure diffusion.

Molecular basis of Diffusion Kinetic theory of gases: Consider a stationary (no bulk flow) plane layer of a binary gas mixture consisting of rigid, nonattracting molecules in which the molecular mass of each species and B is essential equal. concentration(mass-fraction) gradient exists in the gas layer in the x-direction and is sufficiently small that the mass-fraction distribution can be considered linear over a distance of a few molecular mean free paths,, as illustrated in Fig 3.1

verage molecular properties derived from kinetic theory: v Z a mean speed of species molecules 8kBT ( ) m Wall collision frequency of molecules per unit area 1/ 2 n ( V 1 Mean free path ntot 2 2 ( ) V vearage perpendicular distance from plane of last collision toplane where next collision occurs 1 4 ) v 2 3

Where k B is Boltzmann s constant; m the mass of a single molecular, n /V is the number of molecular per unit volume, n tot /V is the total number of molecules per unit volume is the diameter of both and B molecules.

ssuming no bulk flow for simplicity, the net flux of molecules at the x-plane is the difference between the flux of molecules in the positive x-direction and the flux of molecules in the negative x-direction: which, when expressed in terms of the collision frequency, becomes m m m, ( ) xdir,( ) xdir

m Net mass flux of species Number of moleculescrossing plane at x originating fromplane at x - a ( Z ) xa m ( Z ) xa m per unit time and area Mass single molecule Number of moleculescrossing plane at x originating fromplane at x a per unit time and area Mass single molecule

We can use the definition of density (m tot /V tot ) to relate Z to the mass fraction of molecules: Z m 1 4 n m m tot v 1 4 Y v

Substituting the above Equation into the early one, and treating the mixture density and mean molecular speeds as constants yields m 1 4 v( Y Y, xa, xa )

With our assumption of a linear concentration distribution Solving the above equation for the concentration difference and substituting into equation 3.14, we obtain our final result: / 3 4 2,,,, a x a x a x a x Y Y a Y Y dx dy

m v dy 3 dx Comparing the above equation with the first equation, we define the binary diffusivity D B as D B v 3

Using the definitions of the mean molecular speed and mean free path, together with the ideal-gas equation of state PV=nk B T, the temperature and pressure dependence of D B can easily be determined or D 2 k T m T P 3 B B 1/ 2 ( ) 3 3 2 D B T 3/ 2 1 P

Thus, we see that the diffusivity depends strongly on temperature( to the 3/2 power) and inversely with pressure. The mass flux of species, however, depends on the product D B,which has a square-root temperature dependence and is independent of pressure: In many simplified analyses of combustion processes, the weak temperature dependence is neglected and D is treated as a constant. 1/ 2 0 1/ 2 D B T P T

Comparison with Heat Conduction To see clearly the relationship between mass and heat transfer, we now apply kinetic theory to the transport of energy. We assume a homogeneous gas consisting of rigid nonattracting molecules in which a temperature gradient exists. gain, the gradient is sufficiently small that the temperature distribution is essentially linear over several mean free paths, as illustrated in Fig. 3.2.

The mean molecular speed and mean free path have the same definitions as given in Eqns. 3.10a and 3.10c, respectively; however, the molecular collision frequency of interest is now based on the total number density of molecules, n tot /V, i.e., Z verage wall collision frequency per unit area 1 4 n tot v V

In our no-interaction-at-a-distance hard-sphere model of the gas, the only energy storage mode is molesular translational, i.e., kinetic, energy. We write an energy balance at the x- direction is the difference between the kinetic energy flux associated with molecules traveling from x-a to x and those traveling form x+a to x Q Z ( ke) Z ( ke) x xa xa

Since the mean kinetic energy of a molecule is given by the heat flux can be related to the temperature as ke 1 mv 2 2 3 2 k B T Q 3 2 k B Z ( T xa T xa )

The temperature difference in Eqn 3.22 relates to the temperature gradient following the same form as Eqn. 3.15 i.e., dt dx T T 2a Substituting difference in Eqn. 3.22 employing the definition xa xa of Z and a, we obtain our final result for the heat flux: Q x 1 2 k B n ( V dt ) v dx

Comparing the above with Fourier s law of heat conduction(eqn. 3.4), we can identify the thermal conductivity k as 1 n k k ( ) v B 2 V Expressed in terms of T and molecular mass and size, the thermal conductivity is k 3 kb 3 m 4 1/ 2 T 1/ 2

The thermal conductivity is thus proportional to the squareroot of temperature, as is the D B product. For real gases, the true temperature dependence is greater. 1/ 2 k T

Species Conservation Consider the one-dimensional control volume of Fig. 3.3, a plane layer x thick.

The net rate of increase in the mass of within the control volume relates to the mass fluxes and reatction rate as follows: dm dt, cv [ m ] x [ m ] xx m V Rates of increase of mass of within control volume Mass flow of into the control volume Mass flow of out of the control volume Mass prodution rate of species by chemical reaction

is the mass production rate of species per unit volume(kg /m 3 -s). In Chapter 5, we specifically deal with how m to determine. Recognizing that the mass of within the control volume is m,cv =Y a m cv =Y V cv and that the volume V cv =x, Eqn. 3.28 can be written: m

Dividing through by x and taking the limit as x0, Eqn. 3.29 becomes x m x Y D m Y x Y D m Y t Y x x x B x B ] [ ] [ ) ( B m x Y D m Y x t Y ] [ ) (

Or, for the case of steady flow where ( Y ) / t m d 0 dy [ Y m D ] Equation 3.31 is the steady-flow, Bone-dimensional form of dx dx species conservation for a binary gas mixture, assuming species diffusion occurs only as a result of concentration gradients; i.e., only ordinary diffusion is considered. For the multidimensional case, Eqn. 3.31 can be generalized as 0

m m 0 Net rate of production of species by chemical reaction, per unit volume Net flow of species out of control volume, per unit volume

Some application The stefan Problem: Consider liquid, maintained at a fixed height in a glass cylinder as illustrated in Fig. 3.4.

Mathematically, the overall conservation of mass for this system can be expressed as Since =0, then m ( x) constant m m B m B m m ( x) costant

Equation 3.1 now becomes: m Y m D Rearranging and separating variables, we obtain B dy dx m dx dy D B 1 Y

ssuming the product D B to be constant, Eqn. 3.36 can be integrated to yield m where C is the constant of xintegration. ln[1 With the Y boundary ] C condition: DB Y, ( x 0) Y i

We eliminate C and obtain the following mass-fraction distribution after removing the logarithm by exponentiation: Y ( x) 1 (1 Y, i )exp[ m x D B ]

The mass flux of, Eqn. 3.39. Thus,, can be found by letting Y (x=l)=y, in m m D L B 1Y ln[ 1Y,, i ]

From the above equation, we see that the mass flux is directly proportional to the product of the density and the mass diffusivity and inversely proportional to the length, L. Larger diffusivities thus produce larger mass fluxes. To see the effects of the concentrations at the interface and at the top of the varying Y,i, the interface mass fraction, from zero to unity.

Physically, this could correspond to an experiment in which dry nitrogen is blown across the tube outlet and the interface mass fraction is controlled by the partial pressure of the liquid, which, in turn, is varied by changing the temperature. Table 3.1 shows that at small values of Y,i, the dimensionless mass flux is essentially proportional to Y,i, For Y,I greater than about 0.5, the mass flux increases very rapidly.

Table 3.1 Effect of interface mass fraction on mass flux Y,i m /( D / L) 0 0 0.05 0.0513 0.10 0.1054 0.20 0.2231 0.50 0.6931 0.90 2.303 0.99 6.908 B

Liquid-Vapor Interface Boundary Conditions