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Earth Science A — Earth in Space, Deep Time and a Restless Crust (California)

Curriculum

  • 4 Sections
  • 20 Lessons
  • Lifetime
Expand all sectionsCollapse all sections
  • Unit 1: The Sun, the Stars and the Universe
    5
    • 1.1
      Why the Sun Shines
      50 mins
    • 1.2
      Ellipses, Orbits and Kepler’s Laws
      100 mins
    • 1.3
      Arguing for the Big Bang
      50 mins
    • 1.4
      Stars as Element Factories
      100 mins
    • 1.5
      Performance Task — The Cosmic Biography of California Gold
      150 mins
  • Unit 2: Deep Time: Earth’s Formation and the Age of Rocks
    5
    • 2.1
      Reading Time in Rock Layers
      50 mins
    • 2.2
      Half-Life: The Clock Inside Rocks
      100 mins
    • 2.3
      How Old Is Earth? Weighing the Evidence
      50 mins
    • 2.4
      Earth and Life Changed Together
      100 mins
    • 2.5
      Performance Task — How Do We Know Earth’s Age?
      150 mins
  • Unit 3: Plate Tectonics and the San Andreas System
    5
    • 3.1
      Wallace Creek and the Moving Plates
      50 mins
    • 3.2
      Seismic Waves and Earth’s Layered Interior
      100 mins
    • 3.3
      How Fast Does the San Andreas Slip?
      100 mins
    • 3.4
      Building California at a Plate Boundary
      100 mins
    • 3.5
      Performance Task — Why California Has the San Andreas Fault
      150 mins
  • Unit 4: Rocks, Water and a Changing Surface
    5
    • 4.1
      Minerals, Rocks and the Rock Cycle
      100 mins
    • 4.2
      Running Water: A Stream-Table Investigation
      100 mins
    • 4.3
      Why Hillsides Fail: Water, Fire and Feedbacks
      100 mins
    • 4.4
      Water, the Rock Breaker: Ice, Solution and Heat
      100 mins
    • 4.5
      Performance Task — Reading a California Landscape
      150 mins

Why the Sun Shines

Unit 1  ·  Phenomenon Launch & Questioning  ·  Lesson 1 of 20

Why the Sun Shines

HS-ESS1-1EARTHA-CA
By the end of this lesson I can…

explain how nuclear fusion in the Sun’s core releases energy, use E = mc² to connect the Sun’s luminosity to its mass loss, and describe the Sun’s life span from its birth to a white dwarf.

Instruction

The phenomenon. On January 24, 1848, James Marshall saw flakes of gold in the tailrace of a sawmill at Coloma, on the American River. Geologists can show that every atom of that gold is older than the Sun. By the end of this unit you will be able to explain how that can be true. We start with the star we know best.

What the Sun does. The Sun gives off about 3.83 × 1026 watts, its luminosity. At Earth’s distance (1.496 × 1011 m) that power is spread over a sphere, so each square meter facing the Sun receives L / (4πd2) ≈ 1,361 W. This is the solar constant, and it drives weather, climate and life.

Where the energy comes from. Chemical burning cannot explain it: a Sun made of coal would burn out in a few thousand years. The answer is nuclear fusion. In the core, at about 15 million K, hydrogen nuclei (protons) move so fast that they overcome their electric repulsion and fuse. Through a chain of steps, four hydrogen nuclei become one helium-4 nucleus. Four hydrogen atoms have a mass of 4 × 1.007825 = 4.031300 u; one helium atom has 4.002603 u. About 0.7% of the mass is missing, and it leaves as energy, E = mc2.

Worked example: how much mass does the Sun lose? Divide the power by c2: 3.828 × 1026 W / (2.998 × 108 m/s)2 ≈ 4.26 × 109 kg every second, about 4.3 million metric tons. Since only 0.7% of the fused mass disappears, the Sun fuses about 4.26 × 109 / 0.0071 ≈ 6 × 1011 kg of hydrogen per second. That sounds enormous, but the Sun’s mass is 2 × 1030 kg, so it can keep this up for billions of years.

From core to Earth. Energy released in the core moves outward first by radiation, as photons are absorbed and re-emitted countless times, then by convection in the outer third of the Sun, where hot gas rises and cool gas sinks. The energy leaves the surface (about 5,800 K) as light and takes only about 8.3 minutes to cross the 150 million km to Earth, although it spent many thousands of years working its way out of the interior.

The Sun’s life span. The Sun is about 4.6 billion years old and is roughly halfway through its hydrogen-burning life of about 10 billion years. It is stable because outward gas pressure from fusion heat balances inward gravity. As helium builds up in the core, the core contracts and heats, and the Sun slowly brightens. In about 5 billion years it will swell into a red giant, fuse helium into carbon and oxygen, shed its outer layers as a planetary nebula, and leave a white dwarf about the size of Earth. It is not massive enough to explode.

Your questions. A good scientific question can be investigated. “Why is the Sun hot?” becomes “What reaction could release this much energy for 4.6 billion years?” Your question board should hold questions like that about the Sun, the stars and the gold.

Vocabulary in context

  • nuclear fusion — The joining of light atomic nuclei into a heavier nucleus, releasing energy because the product has slightly less mass than the reactants.
  • luminosity — The total power a star emits, in watts.
  • solar constant — The solar power received per square meter at Earth’s average distance, facing the Sun: about 1,361 W/m².
  • red giant — A late stage of a star like the Sun, when the core has run out of hydrogen and the outer layers swell and cool.
  • white dwarf — The hot, dense, Earth-sized core left after a Sun-like star sheds its outer layers.

Formative check

Work through these before moving on. They are not graded — they tell you, and your teacher, whether the standard below has landed yet.

Make a prediction

Suppose the Sun were a giant ball of coal burning in oxygen. About how long could it shine at its present brightness?

Only a few thousand years. Chemical reactions release far too little energy per kilogram. The Sun’s 4.6-billion-year age (from meteorites and Moon rocks) demands nuclear fusion, which converts about 0.7% of the fused mass into energy.
+50 XP

Four hydrogen nuclei fuse into one helium nucleus. What happens to the 0.7% of mass that is ‘missing’?

Mass and energy are conserved together: the missing mass leaves as energy, carried away by photons and neutrinos.
Fill in the blank

The Sun converts about million metric tons of mass into energy every second, and its light takes about minutes to reach Earth.

Draw and label a model of the Sun that shows the core, the radiative zone, the convective zone and the surface, with arrows for how energy moves in each. Add two balanced arrows for gravity and gas pressure. Then write two investigable questions about the Sun or the Coloma gold for the class question board.

0 words
Quick self-check

How confident are you that you can explain how fusion powers the Sun and describe the stages of its life?

Not yetVery confident

Practice

Work these on paper or in your notebook, then open Check your answer. Aim for all of Fluency and Application; try at least one Challenge.

Printable version: this unit’s practice workbook (PDF)

Fluency

Build speed and accuracy with the core skill.

  1. Convert 1250 km/h to m/s.
    Check your answer
    Answer: 347.22 m/s
  2. Convert 1250 kPa to atm.
    Check your answer
    Answer: 12.34 atm
  3. Four hydrogen-1 atoms (1.007825 u each) fuse into one helium-4 atom (4.002603 u). What mass is ‘missing’, and what percentage of the starting mass is it?
    Check your answer
    Answer: 0.028697 u, about 0.71%
    4 × 1.007825 = 4.031300 u; 4.031300 − 4.002603 = 0.028697 u; 0.028697 / 4.031300 = 0.0071.
  4. How much energy is released if 1.0 kg of mass is converted completely to energy? (c = 2.998 × 108 m/s)
    Check your answer
    Answer: 8.988 × 1016 J
    E = mc2 = 1.0 × (2.998 × 108)2.
  5. Light travels 1.496 × 1011 m from the Sun to Earth at 2.998 × 108 m/s. How long does the trip take, in seconds and minutes?
    Check your answer
    Answer: about 499 s, or 8.3 minutes
    t = d / v.

Application

Use the skill in context. Show your reasoning.

  1. The Sun’s luminosity is 3.828 × 1026 W. How much mass does it convert to energy each second, and each year (1 year = 3.156 × 107 s)?
    Check your answer
    Answer: about 4.26 × 109 kg/s; about 1.34 × 1017 kg per year
    m = L / c2; multiply by the seconds in a year.
  2. At that rate for 10 billion years, what fraction of the Sun’s mass (1.989 × 1030 kg) is converted to energy? Does this threaten the Sun’s stability?
    Check your answer
    Answer: about 0.07% of its mass; no, the Sun ends its main-sequence life because its core runs low on hydrogen, not because it runs out of mass
    4.259e+09 × 3.156 × 1017 s / 1.989 × 1030 = 6.76e-04.
  3. The solar constant at Earth (1.000 AU) is 1,361 W/m2. Sunlight spreads as 1/d2. What is it at Mars (1.524 AU) and at Jupiter (5.203 AU)?
    Check your answer
    Answer: Mars about 586 W/m2; Jupiter about 50 W/m2
    Divide 1,361 by the distance in AU squared.

Challenge

Stretch problems. Expect to think before you write.

  1. Use the solar constant (1,361 W/m2) and Earth’s distance (1.496 × 1011 m) to calculate the Sun’s luminosity. Explain the geometry.
    Check your answer
    Answer: about 3.83 × 1026 W
    The Sun’s power spreads over a sphere of radius d, area 4πd2; L = 1,361 × 4π(1.496 × 1011)2.

Review

Keep earlier skills sharp.

  1. What volume does 4.6 g of ice (density 0.917 g/cm3) occupy?
    Check your answer
    Answer: 5.0 cm3
    Volume = mass / density.
  2. Convert 60 km/h to m/s.
    Check your answer
    Answer: 16.67 m/s

CA NGSS and CCSS literacy standards addressed: HS-ESS1-1, SEP.1, SEP.2, CCC.5, RST.9-10.4, MP.2

UC A-G Area D pillar: Nuclear fusion and the life span of the Sun

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