Heat Transfer. Conduction, Convection, and Radiation. Review: Temperature

Similar documents
There are four phases of matter: Phases of Matter

2,000-gram mass of water compared to a 1,000-gram mass.

heat By cillian bryan and scott doyle

Heat can be transferred by. and by radiation Conduction

Thermal Energy. Chapter 6 2 Transferring Thermal Energy

Conduction is the transfer of heat by the direct contact of particles of matter.

The Kinetic Theory of Matter. Temperature. Temperature. Temperature. Temperature. Chapter 6 HEAT

Exercises Conduction (pages ) 1. Define conduction. 2. What is a conductor?

Science 7 Unit C: Heat and Temperature. Topic 6. Transferring Energy. pp WORKBOOK. Name:

All matter is made of moving particles

Chapter 6. Heat is transferred from one place to another by three different processes

Conduction, Convection, and Radiation

Section 1: The Science of Energy¹

Demonstrate understanding of aspects of heat

Topic 6: Transferring Energy

Physics 111. Lecture 36 (Walker: ) Heat Capacity & Specific Heat Heat Transfer. May 1, Quiz (Chaps. 14 & 16) on Wed.

TEMPERATURE. 8. Temperature and Heat 1

L 18 Thermodynamics [3] Heat flow. Conduction. Convection. Thermal Conductivity. heat conduction. Heat transfer

Chapter 1 Heating Processes

Temperature, Heat, and Expansion

Energy Transfer Subtitle

Heat and Temperature

Heat and Temperature

Earth s Atmosphere. Energy Transfer in the Atmosphere. 3. All the energy from the Sun reaches Earth s surface.

* Defining Temperature * Temperature is proportional to the kinetic energy of atoms and molecules. * Temperature * Internal energy

Topic 2: Heat Affects Matter in Different Ways

THERMODYNAMICS METHODS OF HEAT TRANSFER RADIATION

What Is Air Temperature?

LECTURE NOTES. Heat Transfer. III B. Tech II Semester (JNTUA-R15) CHADALAWADA RAMANAMMA ENGINEERING COLLEGE (AUTONOMOUS)

Name Class Date. What are three kinds of energy transfer? What are conductors and insulators? What makes something a good conductor of heat?

Key Concept Heat in Earth s atmosphere is transferred by radiation, conduction, and convection.

What does temperature have to do with energy? What three temperature scales are commonly used? What makes things feel hot or cold?

High temperature He is hot

PHYSICS 220. Lecture 25. Textbook Sections Lecture 25 Purdue University, Physics 220 1

SPH3U1 Lesson 03 Energy

Introduction of Heat Transfer. Prepared by: Nimesh Gajjar GIT-MED

Chapter 11. Energy in Thermal Processes

Heat Transfer. Conduction Radiation Convection

JSUNIL TUTORIAL,SAMASTIPUR PH: CBSE Class-7 Science Heat and temperature solve questions and Notes

Energy Transfers. Heat Transfer. Internal Energy. Going With The Flow! 5/12/17. à Thermal Energy. Q = mcdt Q =DU. U = N(1/2mv 2 )

Topic 5 Practice Test

Table of Contents. Chapter: Atmosphere. Section 1: Earth's Atmosphere. Section 2: Energy Transfer in the Atmosphere. Section 3: Air Movement

Directed Reading. Section: Solar Energy and the Atmosphere RADIATION. identical point on the next wave. waves

Temperature and Heat 4.1. Temperature depends on particle movement Energy flows from warmer to cooler objects. 4.3

CPO Science Foundations of Physics. Unit 8, Chapter 26

Conduction, Convection, & Radiation

TRANSMISSION OF HEAT

Lecture 3: Light and Temperature

Assess why particular characteristics are necessary for effective conduction KEY POINTS

Chapter 14 Temperature and Heat

Conducting Energy and Heat. Energy Likes to Move. Radiating Energy

Energy is the ability to do work. Q: What is energy? Work is done when a force causes an object to move. Q: What is work? Q: Potential Energy

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

Chapter 11. Important to distinguish between them. They are not interchangeable. They mean very different things when used in physics Internal Energy

HEAT How is thermal energy transferred?

Electric energy Radiant energy Nuclear energy

Chapter 11. Energy in Thermal Processes

Chapter 16 Temperature and Heat

,Solar Energy, Greenhouse effect, Convection.notebook October 31, 2016

K20: Temperature, Heat, and How Heat Moves

Energy: Conservation and Transfer

The inputs and outputs of energy within the earth-atmosphere system that determines the net energy available for surface processes is the Energy

HEATING THE ATMOSPHERE

Energy, Temperature, & Heat. Energy, Temperature, & Heat. Temperature Scales 1/17/11

Chapter Introduction Lesson 1 Forms of Energy Lesson 2 Energy Transformations Lesson 3 Thermal Energy on the Move Chapter Wrap-Up

Thermal Energy. Thermal Energy Transfers

Chapter Introduction Lesson 1 Forms of Energy Lesson 2 Energy Transformations Lesson 3 Thermal Energy on the Move Chapter Wrap-Up

8.5 - Energy. Energy The property of an object or system that enables it to do work. Energy is measured in Joules (J).

Heat Transfer. Phys101 Lectures 33, 34. Key points: Heat as Energy Transfer Specific Heat Heat Transfer: Conduction, Convection, Radiation.

Question. Woodstoves. Thermal Energy. Heat. Burning Wood. Chemical Forces. Which is more effective at heating a room:

Most of the energy from the light sources was transferred to the sand by the process of A) conduction B) convection C) radiation D) transpiration

Chapter 14 Heat. Lecture PowerPoints. Chapter 14 Physics: Principles with Applications, 7 th edition Giancoli

Black Body Radiation and Planck's Quantum Hypothesis

Temperature, Thermal Energy, and Heat

WEATHER. Review Note Cards

Broughton High School. Thermal Energy. Physical Science Workbook Chapter 6 Thermal Energy 2016 Mr. Davis

Thermal Energy and Heat Notes. Ch. 14

Physics Mechanics

HEAT HISTORY. D. Whitehall

Chapter 2: The global ledger of radiation and heat

Temperature of body can be increased by doing work on it. Here W = E mgh = E internal

Bernoulli s Principle. Application: Lift. Bernoulli s Principle. Main Points 3/13/15. Demo: Blowing on a sheet of paper

P5 Heat and Particles Revision Kinetic Model of Matter: States of matter

Ready for some more SCIENCE Homer?

Thermodynamics - Heat Transfer June 04, 2013

Earth Science Unit 5- Weather Knowledge Packet

Introduction to Electromagnetic Radiation and Radiative Transfer

General Physics (PHY 2130)

The Atmosphere. Composition of the Atmosphere. Section 2

Atoms and molecules are in motion and have energy

Temperature. Temperature Scales. Temperature (cont d) CHAPTER 14 Heat and Temperature

Physics 101: Lecture 26 Conduction, Convection, Radiation

Science 1206 Chapter 1 - Inquiring about Weather

PHYSICS 289 Experiment 3 Fall Heat transfer and the Greenhouse Effect

Temperature and Heat. Chapter 10. Table of Contents. Chapter 10. Chapter 10. Bellringer. Objectives. Chapter 10. Chapter 10

10.1 TEMPERATURE, THERMAL ENERGY AND HEAT Name: Date: Block: (Reference: pp of BC Science 10)

The Atmosphere and Atmospheric Energy Chapter 3 and 4

Ready for some more SCIENCE Homer? ( Homer gives his brain a pep talk )

PHYS:1200 LECTURE 18 THERMODYNAMICS (3)

Table of Contents. Chapter: Atmosphere. Section 1: Earth's Atmosphere. Section 2: Energy Transfer in the Atmosphere. Section 3: Air Movement

Transcription:

Heat Transfer Conduction, Convection, and Radiation Review: Temperature! Temperature is:! The quantity that tells how hot or cold something is compared with a standard! A measure of the average kinetic energy of the molecules of a substance! Temperature IS NOT energy! If something has a higher temperature, its molecules have more energy, but temperature is not the same thing as energy

Review: Thermal Energy! Thermal Energy is:! The total energy (kinetic plus potential) of the particles that make up a substance.! A.K.A.: Internal Energy! Heat is: Review: Heat! The thermal energy that flows from an object at higher temperature to one at lower temperature, commonly measured in calories or Joules.! Heat is exchanged until thermal equilibrium is reached

A Comparison Temperature Thermal Energy Heat Measures average kinetic energy. The sum of all the kinetic energies. The flow of thermal Energy. Question 1:! If a hot object is placed next to a cold object:! Is heat exchanged?! If heat is exchanged, in what direction does heat travel?

Question 2:! Do warmer objects always have more thermal energy (internal energy) than cooler objects? Conduction

Conduction: How does this method work?! Conduction takes place within materials and between different materials that are in direct contact. Conduction: How does this method work?! Conduction is explained by collisions between atoms or molecules! Warmer atoms move more violently (they have more energy). These warmer atoms bump into nearby atoms and transfer energy, resulting in an increase in the motion of the nearby atoms.

Conduction: How does this method work?! Free electrons that drift through the metal jostle and transfer energy by colliding with atoms and other free electrons Conduction: What moves?! Conduction involves the transfer of energy from molecule to molecule; energy moves from one place to another but molecules do not.

Conduction: Heat Conductors! Materials that conduct heat well are known as heat conductors.! Metals are the best heat conductors since metals have loose outer electrons! If you touch a piece of metal that is at room temperature it often "feels cold." This is because metal is a good conductor of heat. It quickly conducts heat away from your body. Conduction: Heat Insulators! Poor conductors of heat, such as styrofoam and air, are called good insulators.! Liquids and gases are in general good insulators. Porous materials with lots of small spaces are good insulators.! A blanket on your bed does not provide your body with heat. It just slows the conduction of your body heat to the colder air.! Insulation delays heat transfer, it can not prevent it!

Convection Convection: How does this method work?! Convection occurs when a fluid is heated.! Fluids are both liquids and gases.

Convection: How does this method work?! When a fluid is heated, it expands and becomes less dense; since it is less dense, it rises.! Warmer fluid floats on top of cooler fluid.! Cooler fluid then moves to the bottom and the process continues.! Convection currents keep a fluid stirred as it is heated. Convection: What Moves! Convection involves the movement of a fluid; if there is not a fluid, convection cannot occur.

Convection: Example! Convection currents stir the atmosphere and produce winds.! Convection currents are produced by uneven heating of the air near the surface of the earth. Convection: Example! Land warms and cools more quickly than water. Thus convection currents are often evident at the shore in sea breezes and lands breezes.

Radiation Radiation: How does this method work?! Radiation is heat transfer through electromagnetic waves.! Any object that has temperature radiates heat.! Radiation is the only form of heat transfer that can occur in a vacuum.! Heat transfer by radiation takes place from everything to everything, even in empty space.

Radiation: What Moves! With radiation, only energy moves from the warmer object to the cooler object. Radiation: Examples! We receive lots of warmth from the sun as radiation. Go outside on a sunny day and the warmth you feel of the sun on your face is radiation.! Most of the heat we feel when near a fire is radiation.

Radiation: Good Absorbers are Good Emitters! Good absorbers of radiant energy are also good emitters (and poor absorbers are poor emitters.) For example, a radio antenna that is constructed to be a good emitter of radio waves will also be a good receiver of radio waves.! A black mug will allow warm liquids to cool really quickly but it will also allow cool liquids to warm really quickly. On a sunny day Earth's surface is a net absorber. At night it is a net emitter. Radiation: Wavelengths Emitted! All objects continually emit radiant energy in a mixture of wavelengths. Objects at lower temperatures emit longer waves and objects at higher temperature emit waves of shorter wavelength. Objects of everyday temperatures emit waves mostly in the longer wavelength end of the infrared region.

Radiation: Wavelengths Emitted! Shorter wavelength infrared waves absorbed by our skin produce the sensation of heat.! If an object is hot enough, some of the radiant energy it emits is in the form of visible light. At a temperature of about 500 C an object begins to emit the longest wavelengths we can see, red light. At about 1200 C all the different waves to which the eye is sensitive are emitted and we see an object as white hot. Radiation: Absorption and Reflection are Opposite Processes! A good absorber of radiant energy reflects very little radiant energy and appears dark. A perfect absorber reflects no radiant energy and appears perfectly black.! Good reflectors of radiant energy are poor absorbers. Light colored objects reflect more light and heat than darker colored objects. This is why wear lighter colored clothing in summer to stay cool.

Heat Transfer for a Mouse