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Transcript
Click here to begin
the activity.
Energy Basics
• Energy Is the Ability To Do Work
Energy is in everything. We use energy for everything we do, from
making a jump shot to baking cookies to sending astronauts into space.
Energy comes in different forms
•
•
•
•
•
•
•
Heat (thermal)
Light (radiant)
Mechanical (motion)
Electrical
Chemical
Nuclear energy
sound
Potential
• Mechanical (motion)
Electrical
• Chemical
• Nuclear energy
Kinetic
• Heat thermal
•Light (radiant)
•Mechanical (motion)
Electrical
Nuclear energy
•sound
There are two types of energy
• Stored (potential) energy
• Working (kinetic) energy
•
For example, the food you eat contains
chemical energy, and your body stores this
energy until you use it when you work or
play
Click your mouse
to begin.
•Decide whether each slide is an
example of potential or kinetic energy.
•Click on your answer to see if you are
correct.
Potential
Energy
Kinetic
Energy
Potential
Energy
Kinetic
Energy
Potential
Energy
Kinetic
Energy
Potential
Energy
Kinetic
Energy
Potential
Energy
Kinetic
Energy
Energy Sources
• Energy sources are
divided into two
groups — renewable
(an energy source that
can be easily
replenished) and
nonrenewable (an
energy source that we
are using up and
cannot recreate).
• Renewable and
nonrenewable energy
sources can be used to
produce secondary
energy sources
including electricity
and hydrogen
Renewable energy sources include:
• Solar energy from the sun,
which can be turned into
electricity and heat
• Wind
• Geothermal energy from heat
inside the Earth
• Biomass from plants, which
includes firewood from trees,
ethanol from corn, and
biodiesel from vegetable oil
• Hydropower from
hydroturbines at a dam
Alternative Energy Sources:
• These renewable energy sources are
sometimes called alternative energy sources
• Solar
• Water
• Wind
Nonrenewable Energy
• We get most of our energy
from nonrenewable energy
sources, which include the
fossil fuels — oil, natural
gas, and coal.
• They're called fossil fuels
because they were formed
over millions and millions
of years by the action of
heat from the Earth's core
and pressure from rock
and soil on the remains (or
"fossils") of dead plants