Lagrange points and tides Flashcards
what’s a hill sphere
the range from a planet at which its gravity dominates the orbital motion of nearby objects
what’s a Lagrange point?
positions at which a third body can co-rotate with two larger masses (orbit the same centre of mass with the same period)
Lagrange period formula
T² = 4π²/G(M₁+M₂) * a³
M₁: mass of sun
M₂: mass of planet
a: distance between M₁ and M₂
T: orbital period of third body
how many Lagrange points are there and where are they
5 total
L₁ : between planet and sun (very close to the planet)
L₂: opposite side of the planet to L₁ (still very close to the planet)
L₃: 180° further ahead in the orbit of the planet
L₄: 60° further ahead of the planet’s orbit (for M₁»_space;M₂)
L₅: 60° further behind the planet’s orbit (for M₁»_space;M₂)
whats special about Lagrange points 4 and 5
they are stable equilibria. If a satellite in those orbits was perturbed then the Coriolis force would move them back
Since points 1, 2, and 3 are unstable equilibria, satellites must actively orbit these points.
what causes tides
the gradient of the gravitational force across a body.
whats the difference in gravitational force from the moon and sun and which has a larger effect on tides
sun is 178x greater gravitational force
moon is 2.2x greater effect on the tides
what are the consequences on the tides of the moon orbiting the earth
the earth’s rotation slows due to the rotational energy dissipating as a result of the friction between the ocean and the earth’s body.
one of the bulges in the ocean (high tide) is ahead of the line joining the earth-moon. this leading bulge pulls on the moon, increasing its orbital energy and moving it outwards
in terms of angular momentum, why does earths spin slow down
there’s a net torque on the ocean bulges from the moon. this torque causes the angular momentum of earth to decrease. To conserve angular momentum this leads to an increase in the orbital angular momentum of the earth-moon system
what’s the Roche limit
the minimum orbital radius of a satellite before it would break apart.
why is the tidal bulge no aligned with the moon
draw earth (2D) rotating anti-clockwise. draw the moon somewhere and the first tidal bulge is slightly further anti-clockwise than the line joining the earth and moon. the gap is called tidal lag. its caused by the ocean being dragged along by the earth’s rotation
whats spring tide and neap tide
spring tide: tides with the largest range between high and low tide
neap tide: tides with the smallest range between high and low tide
how do you approximate the distance from a planet to L₂
find dϕ/dx and put it =0 (=0 at the lagrange points)
ϕ = U/m is the effective potential per unit mass
a: distance between planet and sun
d: distance from planet to Lagrange point
U/m = -G[ M₁/(x-x₁) + M₂/(x₂-x) ] - ½x²ω²
where M₂ is the planet’s mass.
dϕ/dx = G[M₁/(x-x₁)² + M₂/(x-x₂)² ] - xω² = 0
since M₁»_space; M₂: x₁ –> 0, x₂ –> a, x= a+d
G[M₁/(a+d)² + M₂/d² ] - (a+d)ω² = 0
sub in ω = 2π/T = (GM₁/a³)^½
M₁/(a+d)² + M₂/d² = (a+d)M₁/a³
M₁/a²(1+d/a)² + M₂/d² = (a+d)/a * M₁/a²
M₁/a² * (1 -2d/a) + M₂/d² = (1+d/a) * M₁/a²
M₂/d² = 3M₁* d/a³
M₂/3M₁ = d³/a³
d = a (M₂/3M₁)^1/3