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Internal and External
Sources of Energy
by Emily Block and Lindsey LaBrie
Earth's Energy Sources
-Earth gets its energy in two ways:
-Internal (radioactive decay and gravitational
energy)
-External (the sun)
Earth's Early Internal Energy
-Far greater than what it is now due to 3
intense processes:
-Extraterrestrial Impacts (comets, meteors, etc)
-Gravity
-Radioactive Decay
Extraterrestrial Impacts
-Includes meteorites which contained iron and
stone, and comets
-When these things impacted the earth, they
added mass as well as size
-This increase in size lead to a greater
gravitational force
What it May Have Looked Like...
Gravity (Gravitational Energy)
-As the force of gravity
increased within the
earth, gravitational
energy made the
earth more
compact, which
turned into heat
energy
-Rocks are not good
conductors of heat,
and that is why the
core is much hotter
than the crust
-The heat that is present
in the core cannot
escape quickly
-Early earth had many more radioactive
elements than today, which means its core
used to be a lot hotter
-Radioactive elements break down over time
and release heat
-Some elements have a longer decay rate than
others, so they are still releasing heat energy
in the core
What Internal Energy Does
-Moves the continents around the globe
-Forms volcanoes and mountain ridges
-Causes earthquakes
Volcanoes
-Volcanoes are openings in Earth's crust that
release molten lava, ash, and gases.
-The molten rock is magma while under ground
and it is lava when it is above ground.
-Materials put off during a volcanic eruption:
-Lava, Water vapor, Hydrogen sulfide, Carbon dioxide,
volcanic bombs, lapilli (rock fragments), and ash.
4 Types of Usable Internal Energy
-Chemical
-Nuclear
-Geothermal
-Rotational (least usable)
Internal Energy
-Results from the breaking down of
radioisotopes over time
-Drives plate tectonics due to conduction
-Renews the surface of the Earth
External Energy
-The Earth gets its external energy from the
sun
-The sun radiates its energy in all directions so
only a small fraction of it reaches the Earth
-On a sunny day, the planet receives 1,350 Joules of
energy per second.
-Sun's radiation is sufficient enough to run
Earth's processes
Solar Radiation
-Only 51% of the solar radiation that reaches the Earth is
absorbed by the surface
-19% is absorbed by the
atmosphere
-16% by gases and dust
-3% by clouds
-30% is lost in space
-24% is reflected upward
-6% is scattered upward
Radiation
-The numbers on the chart are an average for
the Earth as a whole
-Different materials reflect things in different
ways
-Shiny and light-colored objects reflect more
radiation than dark-colored objects
Albedo
-An albedo is the amount of radiation an object
reflects
-Snow reflects 90% of the radiation that hits it, it
absorbs the rest. Therefore, snow has an
albedo of 0.9
-A dark forest reflects 5% of the radiation that
reaches it, so it has an albedo of 0.05
Runaway Albedo Effect
-If the entire Earth were to be covered in ice, it would take a
great amount of time for it to all melt away.
-If the Earth were a ball of ice, the volcanic systems would
continue to produce and give off carbon dioxide.
-The carbon dioxide would soon fill up our atmosphere and
make the snow and ice melt away.
-The process of filling the atmosphere with CO2 would take
millions of years.
Citations
-Earth's Energy Budget. N.d. Photograph. Docstock.com. Malj, 14 July 2011. Web. 29
Apr. 2013.
Global Sources of Energy. N.d. Photograph. etap.orgWeb. 30 Apr 2013.
-"Internal and External Energy; Energy Budget." Earth Science Lesson 4--Energy in
the Earth System. N.p., n.d. Web. 29 Apr. 2013.
-Schuller, Jason. "Rock Of Ages." Wreckroom. N.p., n.d. Web. 02 May 2013.
-Simmons, Marty. "External Sources of Energy of the Earth." EHow. Demand Media,
28 Mar. 2011. Web. 01 May 2013.
-Sun and Earth Images. 2013. Photograph. hdwallpaperspics.comWeb. 30 Apr 2013.
-Tariq, Malik. "Giant Sun Eruption Captured in NASA Video -- Science &
Technology -- Sott.net." SOTT.net. Space.com, 17 Nov. 2012. Web. 07 May 2013.
-"The Earth's Heat Furnace." How Volcanoes Work. N.p., n.d. Web. 30 Apr. 2013.
-The Rock Scientist. "Earth As A Snowball Part 3." Mind Blowing Science. N.p., 10
May 2012. Web. 08 May 2013
-"Unit 8: The Earth's Internal Energy." Unit 8: The Earth's Internal Energy.
Slideshare, n.d. Web. 07 May 2013.

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Chapter 14 Life Science Internal and External Sources of Energy

  • 1. Internal and External Sources of Energy by Emily Block and Lindsey LaBrie
  • 2. Earth's Energy Sources -Earth gets its energy in two ways: -Internal (radioactive decay and gravitational energy) -External (the sun)
  • 3. Earth's Early Internal Energy -Far greater than what it is now due to 3 intense processes: -Extraterrestrial Impacts (comets, meteors, etc) -Gravity -Radioactive Decay
  • 4. Extraterrestrial Impacts -Includes meteorites which contained iron and stone, and comets -When these things impacted the earth, they added mass as well as size -This increase in size lead to a greater gravitational force
  • 5. What it May Have Looked Like...
  • 6. Gravity (Gravitational Energy) -As the force of gravity increased within the earth, gravitational energy made the earth more compact, which turned into heat energy -Rocks are not good conductors of heat, and that is why the core is much hotter than the crust -The heat that is present in the core cannot escape quickly
  • 7. -Early earth had many more radioactive elements than today, which means its core used to be a lot hotter -Radioactive elements break down over time and release heat -Some elements have a longer decay rate than others, so they are still releasing heat energy in the core
  • 8. What Internal Energy Does -Moves the continents around the globe -Forms volcanoes and mountain ridges -Causes earthquakes
  • 9. Volcanoes -Volcanoes are openings in Earth's crust that release molten lava, ash, and gases. -The molten rock is magma while under ground and it is lava when it is above ground. -Materials put off during a volcanic eruption: -Lava, Water vapor, Hydrogen sulfide, Carbon dioxide, volcanic bombs, lapilli (rock fragments), and ash.
  • 10. 4 Types of Usable Internal Energy -Chemical -Nuclear -Geothermal -Rotational (least usable)
  • 11. Internal Energy -Results from the breaking down of radioisotopes over time -Drives plate tectonics due to conduction -Renews the surface of the Earth
  • 12. External Energy -The Earth gets its external energy from the sun -The sun radiates its energy in all directions so only a small fraction of it reaches the Earth -On a sunny day, the planet receives 1,350 Joules of energy per second. -Sun's radiation is sufficient enough to run Earth's processes
  • 13. Solar Radiation -Only 51% of the solar radiation that reaches the Earth is absorbed by the surface -19% is absorbed by the atmosphere -16% by gases and dust -3% by clouds -30% is lost in space -24% is reflected upward -6% is scattered upward
  • 14. Radiation -The numbers on the chart are an average for the Earth as a whole -Different materials reflect things in different ways -Shiny and light-colored objects reflect more radiation than dark-colored objects
  • 15. Albedo -An albedo is the amount of radiation an object reflects -Snow reflects 90% of the radiation that hits it, it absorbs the rest. Therefore, snow has an albedo of 0.9 -A dark forest reflects 5% of the radiation that reaches it, so it has an albedo of 0.05
  • 16. Runaway Albedo Effect -If the entire Earth were to be covered in ice, it would take a great amount of time for it to all melt away. -If the Earth were a ball of ice, the volcanic systems would continue to produce and give off carbon dioxide. -The carbon dioxide would soon fill up our atmosphere and make the snow and ice melt away. -The process of filling the atmosphere with CO2 would take millions of years.
  • 17. Citations -Earth's Energy Budget. N.d. Photograph. Docstock.com. Malj, 14 July 2011. Web. 29 Apr. 2013. Global Sources of Energy. N.d. Photograph. etap.orgWeb. 30 Apr 2013. -"Internal and External Energy; Energy Budget." Earth Science Lesson 4--Energy in the Earth System. N.p., n.d. Web. 29 Apr. 2013. -Schuller, Jason. "Rock Of Ages." Wreckroom. N.p., n.d. Web. 02 May 2013. -Simmons, Marty. "External Sources of Energy of the Earth." EHow. Demand Media, 28 Mar. 2011. Web. 01 May 2013. -Sun and Earth Images. 2013. Photograph. hdwallpaperspics.comWeb. 30 Apr 2013. -Tariq, Malik. "Giant Sun Eruption Captured in NASA Video -- Science & Technology -- Sott.net." SOTT.net. Space.com, 17 Nov. 2012. Web. 07 May 2013. -"The Earth's Heat Furnace." How Volcanoes Work. N.p., n.d. Web. 30 Apr. 2013. -The Rock Scientist. "Earth As A Snowball Part 3." Mind Blowing Science. N.p., 10 May 2012. Web. 08 May 2013 -"Unit 8: The Earth's Internal Energy." Unit 8: The Earth's Internal Energy. Slideshare, n.d. Web. 07 May 2013.