P2 Heat & Radiation Flashcards

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1
Q

Infrared radiation

A

Can transfer thermal energy without a medium

An electromagnetic wave

Invisible

All bodies emit radiation

Longer wavelength than visible light

Shorter wavelength than radio waves

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2
Q

How surfaces interact with infrared radiation

A

Can reflect, absorb, or emit infrared radiation

Good absorbers are usually bad reflectors

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3
Q

How shiny surfaces interact with infrared radiation

A

Compared to dull surfaces of the same colour, shiny surfaces are:

Poorer absorbers
Poorer emitters
Better reflectors

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4
Q

How perfect black bodies interact with infrared radiation

A

Absorbs all of the radiation that incidents on it

Doesn’t reflect or transmit radiation

As a good absorber is a good emitter, black body objects are the best possible emitters

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5
Q

How white surfaces interact with infrared radiation

A

Good reflectors

Poor emitters

Poor absorbers

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6
Q

How black surfaces interact with infrared radiation

A

Good emitters

Good absorbers

Poor reflectors

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7
Q

Factors affecting the amount of radiation emitted

A

Surface area
Surface temperature

The higher the surface area or temperature, the higher the rate of emission

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8
Q

Factors affecting temperature

A

Intensity of radiation emitted

Wavelength of radiation emitted

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9
Q

When is temperature constant

A

radiation absorbed = radiation emitted

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10
Q

When does the temperature change

A

radiation absorbed ≠ radiation emitted

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11
Q

Diffusion of heat

A

Heat will always transmit from a hotter to a cooler area

Rate of emission is higher if an object is hotter than its environment

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12
Q

Factors affecting absorption and emission

A

Internal temperature

Surface area

External temperature

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13
Q

The greenhouse effect process

A
  1. The sun emits short wavelength infrared radiation that enters the atmosphere and travels towards the Earth’s surface
  2. The Earth absorbs some of this radiation, but long wavelength radiation is reflected back into the atmosphere
  3. Greenhouse gases (e.g. carbon dioxide, methane, water vapour) can’t absorb the frequency of radiation emitted by the Sun. But they can absorb the longer wavelength reflected radiation
  4. The gases then re-radiate this energy in all directions, including back towards Earth
  5. This increases the temperature at the Earth’s surface
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14
Q

Emission to balance energy on Earth

A

Absorbed sunlight is balanced by heat radiated from the Earth’s surface and atmosphere

Most heat escapes from areas just north and south of the equator, where the surface is warm, but there are few clouds

Along the equator, persistent clouds prevent heat from escaping

The poles radiate little heat

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15
Q

Absorption to balance energy on Earth

A

340 Watts per square metre of solar energy falls on the Earth

29% is reflected back into space - primarily by clouds, but also by other bright surfaces and the atmosphere itself

~23% of incoming energy is absorbed in the atmosphere by atmospheric gases, dust, and other particles

The remaining 48% is absorbed at the surface

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16
Q

Thermal conductors

A

Materials which allows the conduction of thermal energy

17
Q

Thermal insulators

A

Materials which prevent or do not readily conduct thermal energy

18
Q

The greenhouse effect

A

The process of gases trapping heat to keep the Earth warm enough for life

The greenhouse effect can cause global warming if it becomes too strong

19
Q

Examples of thermal insulators

A

Polystyrene foam

Water

Mineral wool

Plastic

20
Q

Examples of thermal conductors

A

Copper

Aluminium

Brass

Silver

21
Q

Formula for specific heat capacity

A

specific heat capacity(J/Kg°C) = (change in energy(J)) / (mass(Kg) * change in temperature(°C))

22
Q

Conductivity of metals and non-metals

A

Metal are better conductors than non-metals

23
Q

Conductivity of copper and steel

A

Copper is a better conductor than steel

24
Q

Conductivity of glass and wood

A

Glass is a better conductor than wood

25
Q

Specific heat capacity

A

The amount of energy needed to increase a kilogram of a substance by 1°C

26
Q

Relationship between mass and change in temperature

A

Rate of energy transfer decreases as mass increases

27
Q

Thermal conductivity

A

The rate at which a material conducts thermal energy

28
Q

Factors affecting rate of energy transfer

A

Temperature difference across material

Thickness of material

Thermal conductivity of material

29
Q

Relationship between thickness and thermal conductivity

A

Thermal conductivity decreases as thickness increases

30
Q

Relationship between temperature and radiation emitted

A

Amount of radiation emitted increases as temperature increases

31
Q

Radiation emitted from an object with a constant temperature

A

An object at a constant temperature emits radiation at a continuous range of wavelength

32
Q

Relationship between heat and wavelength

A

Wavelength decreases as heat increases

33
Q

Factors affecting change in temperature

A

Amount of energy supplied

Mass

Type of substance

34
Q

Methods to reduce rate of emission from homes

A

Loft insulation

Cavity wall insulation

Double-glazed windows

Thick bricks (with low thermal conductivity)

Aluminium foil behind radiators

35
Q

Methods to heat homes

A

Electric/gas heater

Oil/gas central heating

Solid fuel stove/fireplace

36
Q

Cavity insulation

A

Insulation, with a lower thermal conductivity than air, between two layers of brick of an external wall