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Heat & By iTutor.com T- 1-855-694-8886 Email- [email protected] Thermodynamics

Heat & Thermodynamics

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Page 1: Heat & Thermodynamics

Heat &

By iTutor.com

T- 1-855-694-8886Email- [email protected]

Thermodynamics

Page 2: Heat & Thermodynamics

Energy that flows from something warm to

something cooler

A hotter substance gives KE to a cooler one

Heat is the transfer of energy between two

objects due to temperature differences

Heat is measured in Joules (J) because it is a form

of energy

Heat

Page 3: Heat & Thermodynamics

Heat

The name of the transfer process is heat. What gets transferred is energy.

Heat is NOT a substance although it is very convenient to think of it that way.

In fact, it used to be thought that heat was a substance.

There is a circular nature to the definitions used: (a) energy does work or produces heat, but(b) heat is a transfer of energy.

Page 4: Heat & Thermodynamics

Temperature

Temperature is the property which determines the direction heat will flow when two objects are brought into contact

Based on the motion of the particles in a substanceFast motion = high temperatureSlower motion = lower temperature

Relatively describes how the particles collide with the surface of the thermometer Collisions transfer energy

Page 5: Heat & Thermodynamics

Temperature Scales

FahrenheitCommon in the USFreezing point of water is 32ºFBoiling point of water is 212ºF

CelsiusCommon in the rest of the world (SI)Freezing point of water is 0ºCBoiling point of water is 100ºC

KelvinUsed for scienceFreezing point of water is 273KBoiling point of water is 373K

Page 6: Heat & Thermodynamics

Temperature and the Phases of Matter

In the Fahrenheit scale, water freezes at 32 degrees and boils at 212 degrees

The Celsius scale divides the difference between the freezing and boiling points of water into 100 degrees (instead of 180).

Page 7: Heat & Thermodynamics

Temperature and the Phases of Matter

All thermometers are based on some physical property (such as color or volume) that changes with temperature.

A thermometer is a device that changes its electrical resistance as the temperature changes.

A thermocouple is another electrical sensor that measures temperature.

Page 8: Heat & Thermodynamics

Heat and Thermal Energy

Temperature is NOT the same as thermal energy.

Thermal energy is energy stored in materials because of differences in temperature.

The thermal energy of an object is the total amount of random kinetic energy for all the atoms in the object.

Remember, temperature measures the random kinetic energy of each atom.

Page 9: Heat & Thermodynamics

Heat and Thermal Energy

Imagine heating a cup of coffee to a temperature of 100°C.

Next think about heating up 1,000 cups of coffee to 100°C.

The final temperature is the same in both cases but the amount of energy needed is very different.

Page 10: Heat & Thermodynamics

First Law of Thermodynamics

Energy loss is equal to energy gain.

Page 11: Heat & Thermodynamics

Second Law of Thermodynamics

Page 12: Heat & Thermodynamics

Energy and Heat flow

There Energy, in the process we call heat or heat flow, is constantly flowing into and out of all objects, including living objects.

 Heat flow moves energy from a higher temperature to a lower temperature.

The bigger the difference in temperature between two objects, the faster heat flows between them.   

When temperatures are the same there is no change in energy due to heat flow.

Radiation and Conduction are the two methods of heat transfer. Convection is a special type of conduction.

Heat has the units of energy; heat flow has the units of power.

Page 13: Heat & Thermodynamics

Heat flow is energy moving. It has the same units as power - energy per unit time .

It means that during the given amount of time, during which heat is flowing, a certain amount of energy is transferred or moved from one place to another place

Energy and Heat flow

Page 14: Heat & Thermodynamics

Three easy things to know about the way heat flows:1)  There has to be a temperature difference. Energy

only flows as heat if there is a temperature difference. 2)   Energy as heat flows from a higher temperature to a

lower temperature.3)   The greater or larger the difference in temperature,

the faster the energy flows.

Heat flow

Page 15: Heat & Thermodynamics

The science of how heat flows is called heat transfer.

There are three ways heat transfer works: conduction, convection, and radiation.

Heat flow depends on the temperature difference.

Heat flow

Page 16: Heat & Thermodynamics

Heat flow

Page 17: Heat & Thermodynamics

Heat Conduction

Conduction occurs when two object at different temperatures are in contact with each other.

Heat flows from the warmer to the cooler object until they are both at the same temperature.

Conduction is the movement of heat through a substance by the collision of molecules. At the place where the two object touch, the faster-moving molecules of the warmer object collide with the slower moving molecules of the cooler object.

Page 18: Heat & Thermodynamics

Heat Conduction

Conduction is the transfer of heat through materials by the direct contact of matter.

Dense metals like copper and aluminum are very good thermal conductors.

A thermal insulator is a material that conducts heat poorly.

Page 19: Heat & Thermodynamics

Thermal Conductivity

The thermal conductivity of a material describes how well the material conducts heat.

Page 20: Heat & Thermodynamics

Heat Conduction Equation

PH = k A (T2 -T1) L

Area of cross section (m2)

Length (m)

Thermal conductivity(watts/moC)

Heat flow (watts)

Temperaturedifference (oC)

Page 21: Heat & Thermodynamics

Convection

Convection is the transfer of heat by the motion of liquids and gases.– Convection in a gas occurs

because gas expands when heated.

– Convection occurs because currents flow when hot gas rises and cool gas sink.

– Convection in liquids also occurs because of differences in density.

Page 22: Heat & Thermodynamics

Convection

When the flow of gas or liquid comes from differences in density and temperature, it is called free convection.

When the flow of gas or liquid is circulated by pumps or fans it is called forced convection.

Page 23: Heat & Thermodynamics

Convection

Both free and forced convection help to heat houses and cool car engines.

Page 24: Heat & Thermodynamics

Convection

Convection depends on speed and surface area. Motion increases heat transfer by convection in all

fluids. If the surface contacting the fluid is increased, the

rate of heat transfer also increases.

Page 25: Heat & Thermodynamics

Convection and Sea Breezes

On a smaller scale near coastlines, convection is responsible for sea breezes.

During the daytime, land is much hotter than the ocean.

A sea breeze is created when hot air over the land rises due to convection and is replaced by cooler air from the ocean.

At night the temperature reverses so a land breeze occurs.

Page 26: Heat & Thermodynamics

Heat Convection Equation

PH = h A (T2 -T1)

Area contacting fluids (m2)

Heat transfer coefficient(watts/m2oC)

Heat flow (watts)

Temperaturedifference (oC)

Page 27: Heat & Thermodynamics

Radiation

Radiation is heat transfer by electromagnetic waves.

Thermal radiation is electromagnetic waves (including light) produced by objects because of their temperature.

The higher the temperature of an object, the more thermal radiation it gives off.

Page 28: Heat & Thermodynamics

• Radiation

Radiation

Heat from the sun is the best example of radiation.

The sun is rays reach the earth without having any material medium in between the earth and the sun.

The electromagnetic rays carry energy from the sun is surface to the earth and heat up the earth and its atmosphere.

Page 29: Heat & Thermodynamics

Radiant Heat

We do not see the thermal radiation because it occurs at infrared wavelengths invisible to the human eye.

Objects glow different colors at different temperatures.

Page 30: Heat & Thermodynamics

The graph of power versus wavelength for a perfect blackbody is called the blackbody spectrum.

Radiant Heat

A perfect blackbody is a surface that reflects nothing and emits pure thermal radiation.

Page 31: Heat & Thermodynamics

Radiant Heat

The total power emitted as thermal radiation by a blackbody depends on temperature (T) and surface area (A).

Real surfaces usually emit less than the blackbody power, typically between 10 and 90 percent.

The Kelvin temperature scale is used in the Stefan-Boltzmann formula because thermal radiation depends on the temperature above absolute zero.

Page 32: Heat & Thermodynamics

Stefan-Boltzmann formula

P = s AT4

Surface area (m2)

Stefan-Boltzmann constant5.67 x 10-8 watts/m2K4)

Power (watts)

Absolute temperature (K)

Page 33: Heat & Thermodynamics

The End

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