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183_notes:examples:earth_s_translational_angular_momentum [2014/11/16 20:48] – pwirving | 183_notes:examples:earth_s_translational_angular_momentum [2014/11/20 16:30] (current) – pwirving | ||
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=== Facts === | === Facts === | ||
+ | Mass of the Earth: 6 X 1024kg | ||
- | + | Distance from the Sun: 1.5 x 1011m | |
=== Lacking === | === Lacking === | ||
+ | The magnitude of the Earth' | ||
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=== Approximations & Assumptions === | === Approximations & Assumptions === | ||
+ | Assume Earth moves in a perfect circular orbit | ||
+ | Assume main interaction is with the sun | ||
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- | {{course_planning: | + | {{183_projects:mi3e_11-002.jpg?400}} |
+ | Circumference of a circle = 2πr | ||
+ | |||
+ | →p=m→v | ||
+ | |||
+ | v=s/t | ||
+ | |||
+ | |→Ltrans|=|→rA||→p|sinθ | ||
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=== Solution === | === Solution === | ||
- | The Earth makes one complete orbit of the Sun in 1 year, so its average speed is: | + | The Earth makes one complete orbit of the Sun in 1 year, so you need to break down 1 year into seconds and know that the distance the Earth travels in that time is 2πr in order to find its average speed is: |
v=2π(1.5×1011m)(365)(24)(60)(60)s=3.0×104m/s | v=2π(1.5×1011m)(365)(24)(60)(60)s=3.0×104m/s | ||
- | At location A | + | With this average velocity we can find the momentum of Earth at location A as we know the mass of the Earth and now know the velocity of the Earth. |
→p=⟨0,6×1024kg⋅3.0×104m/s,0⟩ | →p=⟨0,6×1024kg⋅3.0×104m/s,0⟩ | ||
+ | |||
+ | Computing for momentum we get: | ||
→p=⟨0,1.8×1029,0⟩kg⋅m/s | →p=⟨0,1.8×1029,0⟩kg⋅m/s | ||
∣→p∣=1.8×1029kg⋅m/s | ∣→p∣=1.8×1029kg⋅m/s | ||
+ | |||
+ | We know that the magnitude of the Earth' | ||
∣→Ltrans,Sun∣=(1.5×1011m)(1.8×1029kg⋅m/s)sin90∘ | ∣→Ltrans,Sun∣=(1.5×1011m)(1.8×1029kg⋅m/s)sin90∘ | ||
- | $\mid\vec{L}_{trans, | + | Compute for $\left|\vec{L}_{trans, |
- | At location B,∣→r∣,∣→p∣,andθ are the same as they were at location A, so ∣→Ltrans,Sun∣ | + | $\mid\vec{L}_{trans, |
+ | It turns out that at location B,∣→r∣,∣→p∣, |