Lecture 5-6

25
Astronautics 309 Lecture 5-6

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Transcript of Lecture 5-6

Page 1: Lecture 5-6

Astronautics 309 Lecture 5-6

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Outline

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The Two-Body Problem

Position as a function of

Time

What other forces?

Circular orbit

Elliptical orbit Parabolic arc

Hyperbolic arc

The EoM

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The Orbit Formula (true anomaly)

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The position as a function of true anomaly

v? =h

rRate of change of true anomaly

Removing position from the equation:

tp = 0

✓p = 0

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Circular Orbit

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When (e=0) the integral is simple:

relation between true anomaly and time:

as a fraction of one period:

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Elliptical Orbit

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From the integration:

The mean anomaly:

in elliptic orbit:

The mean motion:

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Elliptical Orbit

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Kepler’s transformation:uniform circular motion for an ellipse

Eccentric anomaly

the relation between two geometries:

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Kepler’s Equation

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Relation between true anomaly and eccentric anomaly:

Kepler’s equation

mean anomaly eccentric anomaly

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Example

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Example

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Parabolic Trajectory

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when (e=1), the integration is simple:

mean anomaly:

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Example

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Hyperbolic Trajectory

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for e>1, well!

defining the mean anomaly:

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Hyperbolic Trajectory

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to simplify the integration:

cosh

2 F � sinh

2 F = 1defining an auxiliary angle F:

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simplifies:

Hyperbolic Trajectory

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cosh

2 F � sinh

2 F = 1

hyperbola equation

when:

hyperbolic mean anomaly hyperbolic eccentric anomalyrelation between true anomaly and

hyperbolic eccentric anomaly

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Summary

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similarity between ellipse an hyperbola

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Force Model

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Newtonian motion:

r = F(t, r, r)/m

Two-Body Gravitational Force:

r = � µ

r3r

Other forces on a satellite in the Earth’s atmosphere:

• Geopotential (the effect of non-spheric body on the gravity) • Solar Radiation Pressure (SRP) • Atmospheric Drag

Mathematically modeling the acting forces on all the particles of a dynamical system.

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Geopotential

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Using potential to derive equations of motion:

r = �rU

U = �µ

r

Gravitational Potential:

For a small element:

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Geopotential

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We can use an polynomial expansion to write:

Using spherical coordinate:

where Legendre Polynomial

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Geopotential

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Legendre Polynomial

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Geopotential

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Using normalized coefficient:

Then, the force can be written as:

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Geopotential

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The Earth:

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Geopotential

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The Earth:

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Solar Radiation Pressure (SRP)

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The pressure by absorbed and reflected photons

Using solar flux � =1

A

dE

dt

momentum by a single photon : ⌫ p⌫ =E⌫

c

dp =dE

c=

cAdtchange of the momentum for a small element:

F =dp

dt=

cAForce: Pressure: P =

c

� = 1367 Wm�2

P� = 4.56⇥ 10�6Nm�2At 1AU:

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Solar Radiation Pressure (SRP)

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Absorption Reflection

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Atmospheric Drag

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Depends on relative velocity

Assume that atmosphere rotates with the Earth

Drag force model: