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Transcript
“EARTH’S ENERGY“
1
5.1) Electromagnetic Energy.
energy
is the ability to do work.
Everything that is done in the universe
involves the use or transfer of energy.
2
There are two sources for Earth’s
heat energy.
1) Internal source
 heat from earth’s interior.
Comes from;
1 - remnant heat
2 - radioactive decay.
3
2) External source
Comes from;
Insolation – energy from the sun.
(In/sol/ation) incoming solar
radiation.
This drives most Earth surface
processes.
4
Electromagnetic Energy.
energy that is radiated (given off) by all
matter that is not at absolute zero.
absolute zero = the lowest possible
temperature.
0 Kelvin or -273oC.(-459.67F)
the higher the temperature, the greater the
amount of energy that is given off.
5
Characteristics and Types of
Electromagnetic Energy.
• different types of electromagnetic energy
are distinguished by their wavelength.
• wavelength - the distance from one crest of
a wave to the next crest.
6
diagram;
crest
one wavelength
|
|
trough
crest
|
|
one wavelength
trough
7
Electromagnetic Spectrum
See ESRT p. 14
Short Wave Energy
High energy
Long Wave Energy
Low energy
8
The electromagnetic spectrum
a model that shows all the types of
electromagnetic energy.
Visible light is the only portion of the
spectrum that we can see with our eyes.
9
1) Which type of electromagnetic radiation
has the longest wavelength?
(1) ultraviolet
(2) gamma rays
(3) visible light
(4) radio waves
10
2) Which graph best represents the relative
wavelengths of the different forms of
electromagnetic energy?
11
3) Which color of the visible spectrum has
the shortest wavelength?
(1) violet
(2) blue
(3) yellow
(4) red
12
4) In which list are the forms of
electromagnetic energy arranged in order
from longest to shortest wavelengths?
(1) gamma rays, x rays, ultraviolet rays,
visible light
(2) radio waves, infrared rays, visible light,
ultraviolet rays
(3) x rays, infrared rays, blue light, gamma
rays
(4) infrared rays, radio waves, blue light,
red light
13
5) What is the basic difference between
ultraviolet, visible, and infrared radiation?
(1) half-life
(2) temperature
(3) wavelength
(4) wave velocity
14
DATE
Main Ideas and Supporting Details
15
There are three types of
spectrum.
1) continuous
 a continuous band of colors, with one color
blending into the next, the “real” rainbow.
 Produced by a glowing solid or liquid, or by a
highly compressed glowing gas.
16
2) bright line (emission)
dark background with a series of thin
brightly colored lines.
Produced from a non-compressed gas.
17
3) dark line (absorption)
a continuous spectrum with thin black
lines.
Produced from the sun’s light, where light
passes through a cooler gas.
18
19
Interactions between
Electromagnetic Energy and an
Environment.
When electromagnetic waves strike an
object they may be….
20
1) refracted
 bent.
21
2) reflected
bounced off.
22
3) scattered
refracted and/or reflected in various
directions.
23
4) transmitted
passed through the material.
24
5) absorbed
taken into the material.
25
Surface Properties and
Absorption.
The characteristics of the surface of a
material will determine the amount of
electromagnetic energy that can be
absorbed.
26
Characteristics
1) Color
dark color – absorbs well.
light color – absorbs poorly. (it
reflects energy)
2) Texture
rough surface – absorbs well.
smooth surface – absorbs poorly. (it
reflects energy)
27
A material that absorbs
electromagnetic energy well will..
heat up quickly.
28
A material that heats up quickly
will also..
radiate (gives off) energy well.
It will cool quickly
29
5-2)
Transfer of Energy
Energy moves from a …
region of high concentration
(a source)
to a …
region of low concentration
(a sink).
SOURCE
SINK
(high)
(low)
30
heat energy –
energy that is transferred from a
region of high temperature to a
region of lower temperature.
31
Achieving Dynamic
Equilibrium
Heat will move from a ..
source to a sink until their energies
are equal.
Dynamic Equilibrium is achieved
when..
the amount of energy being gained is
equal to the amount of energy being
lost.
32
3 Methods of Energy
Transfer
33
1 - CONDUCTION
Heat energy is transferred from
atom to atom, when vibrating atoms
collide.
Conduction is most effective in
solids.
diagram:
34
35
HOT
36
DATE
Main Ideas and Supporting Details
37
2 - CONVECTION
caused by differences in density.
warmer portions have a lower density
and rise.
cooler portions have a greater density
and sink.
only occurs in fluids;
gases.
liquids and
convection currents occur in;
– atmosphere, the hydrosphere, & below
the lithosphere.
Diagram:
38
39
40
3 - RADIATION.
caused by electromagnetic waves.
no medium is needed to transfer
electromagnetic waves.
examples; sunlight warming the earth
or heating the inside of a car.
diagram;
41
Diagram 1; Earth
42
Energy travels
through space
43
Diagram 2; Inside car
The inside is hotter
than the
temperature outside.
44
5-3) Transformation of
Energy
changing one type of energy into
another.
45
Examples;
1) friction –
 kinetic energy is transformed into
heat energy.
 glacier flowing down a valley.
2) waves
 Wind blowing on the ocean.
 energy from atmosphere to
hydrosphere.
46
Transformations of
Mechanical Energy
mechanical energy –
potential + kinetic energy.
the energy of an object that is not
related to the motion of atoms.
47
kinetic energy energy of motion.
the faster an object moves, the
greater its kinetic energy.
48
potential energy energy of position, or phase. (“stored
energy”)
 the higher an object is above the
center of the earth, the greater its
potential energy.
49
Example;
Waterfall
50
Water at the top of
a waterfall has
potential energy.
as the water falls,
some of its
potential energy
becomes kinetic
energy.
diagram
51
52
Capture this energy…
(Build your own waterfall)
Hydroelectric
Height 726
River view of the eventual
site of Hoover Dam, circa
1904
53
54
55
Transformation of
Electromagnetic Energy
Electromagnetic energy absorbed by
an object is reradiated at a longer
wavelength.
high temp. emits short wavelength.
lower temp emits longer wavelength.
56
Earth example;
Short wavelength radiation from the
sun (insolation) is absorbed and …
….reradiated as longer wavelength
radiation (infrared) from the earth.
diagram
57
Long wave from Earth
Short wave from sun.
58
Temperature
59
temperature
is a measure of the average kinetic
energy of the particles of a body of
matter.
One molecule
Atoms in a gas
60
The instrument that is
used to measure
temperature is a ….
thermometer
Mercury thermometer
Galileo thermometer
digital
IR thermometer
61
There are three different
temperature scales…




Fahrenheit
Celsius
Kelvin – do not use degree sign;
absolute zero is 0K
use ESRT to do conversions
62
63
200 oF
=
93
140 oF =
60oC
46 oF
=
8
5 oF
=
-15
-13 oF
=
-25 oC
o
C =
oC
oC
367 K
=
333
=
280 K
=
258
=
248 K
K
K
64
Heat and Thermal Energy
FYI
Heat – is the transfer or
flow of energy from a
Hot object to one that is
cooler.
Thermal energy – When
you feel a warm object
You are actually feeling
thermal energy – the
movement of molecules
that make up the object.
65
Heat energy is measured in
a unit called a joule.
4.184 joules = 1 calorie
1 calorie
• heat needed to raise one gram of
liquid water by one degree Celsius.
66
Different materials heat up at
different rates.
Specific Heat
• heat needed to raise one gram of any
substance one degree Celsius.
• or…specific heat can be defined as
–the resistance a material presents
to heating up or cooling off.
67
68
Liquid water has the highest specific
heat of all naturally occurring
substances. see Earth Science Reference Tables.
For a 1 gram sample..
4.18 J raises temp 1oC
4.18 J raises temp 6932oC
Heat Energy and Changes of
State
70
Melting
Solid to liquid.
(ice cubes melting)
71
melting titanium
Solidification (freezing)
Liquid to solid (water freezing)
Toronto
72
Evaporation (vaporization)
Liquid to gas (boiling water)
73
Condensation
Gas to liquid
(rain, mirror in bathroom)
dew
74
Sublimation
Solid to gas
dry ice
(decrease in snowpack)
75
Changes of State (phase)
solid
liquid
gas
76
Changes of State (phase)
HEAT IS RELEASED
precipitation
solidification
condensation
solid
334 J/g
melting
liquid
2260 J/g
gas
vaporization
sublimation
HEAT IS ABSORBED
77
Stored Heat and Changes of
States
During a change of state,
heat added does not change the
temperature.
The added heat energy is
being converted to a kind of
potential energy, or stored heat.
78
Draw and label diagram;
Heating of Water
gas
evaporation
condensation
100oC
temperature
liquid
melting
0oC
freezing
solid
-100oC
time
79
Earth's Energy Supply
80
1 - Solar Energy
Of all the types of electromagnetic
radiation from the sun, the one with
the greatest intensity is …
visible light.
Solar energy is produced by …
nuclear fusion.
81
2 - Earth's own Energy
1 - heat that remains from when the
Earth formed.
2 - nuclear decay of radioactive
materials.
82