183_notes:examples:earth_s_translational_angular_momentum

Calculate the magnitude of the Earth's translational (orbital) angular momentum relative to the Sun when the Earth is at location A and when the Earth is at location B as displayed in the representation of the situation in the representations. The mass of the Earth is 6 x 1024kg and its distance from the Sun is 1.5 x 1011m.

Facts

Mass of the Earth: 6 X 1024kg

Distance from the Sun: 1.5 x 1011m

Lacking

The magnitude of the Earth's translational (orbital) angular momentum relative to the Sun when the Earth is at location A on the representation and when it is at location B on the representation.

Approximations & Assumptions

Assume Earth moves in a perfect circular orbit

Assume main interaction is with the sun

Representations

mi3e_11-002.jpg

Circumference of a circle = 2πr

p=mv

v=s/t

|Ltrans|=|rA||p|sinθ

Solution

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

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=0,6×1024kg3.0×104m/s,0

Computing for momentum we get:

p=0,1.8×1029,0kgm/s

p∣=1.8×1029kgm/s

We know that the magnitude of the Earth's translational angular momentum relative to the sun is given by |Ltrans,Sun|=|rA||p|sinθ

Ltrans,Sun∣=(1.5×1011m)(1.8×1029kgm/s)sin90

Compute for |Ltrans,Sun| by inputting the known values for the variables.

Ltrans,Sun∣=2.7×1040kgm2/s

It turns out that at location B,r,p, and θ are the same as they were at location A, so Ltrans,Sun also has the same value it had at location A.

  • 183_notes/examples/earth_s_translational_angular_momentum.txt
  • Last modified: 2014/11/20 16:30
  • by pwirving