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Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

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Page 1: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

Page 2: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

4. How Orbits Work

Astronomy 1001, Sept 2007 – Prof. K. Davidson

Page 3: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

KEPLER’S LAWS (c. 1610)

Page 4: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

1. Each planet follows an elliptical orbit,

with

the Sun at one focus*

2. Equal areas in equal times

3. Period squared = radius cubed

* (Note: the orbits aren’t aligned)

Page 5: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

KEPLER’S FIRST LAW (except that planets’ orbits are usually more circular than this)

Page 6: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

KEPLER’S SECOND LAW:“EQUAL AREAS IN EQUAL TIMES”

Page 7: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

KEPLER’S THIRD LAW relates the speeds of different planets; those farther out move slower.

If a = average distance from the Sun* and P = orbital period, then

P 2 = (constant) x a 3 .

* (Distance is reckoned from the center of the Sun.)

Page 8: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

Kepler’s third law -- the numbers

a (AU) P (yr) a 3 P 2

MERCURY 0.387 0.241 0.058

0.058

VENUS 0.723 0.615 0.378

0.378

EARTH 1.000 1.000 1.00

1.00

MARS 1.524 1.881 3.54 3.54

JUPITER 5.203 11.86 141 141

SATURN 9.54 29.46 868 868

Page 9: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

Isaac Newton (1642 – 1727)

Page 10: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

Newton’s theory of dynamics, also called mechanics

Motions of objects impelled by forces

Page 11: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

Brief digression ...

A VECTOR IS A QUANTITY THAT HAS A DIRECTION IN SPACE.

examples: ** POSITION ** ** VELOCITY ** ** ACCELERATION **

Page 12: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

“vector addition”

Page 13: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

VELOCITY tells us how POSITION changes with time (in all directions);

Page 14: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

VELOCITY tells us how POSITION changes with time (in all directions);

ACCELERATION tells us how VELOCITY changes with time (in all directions).

Page 15: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

VELOCITY tells us how POSITION changes with time (in all directions);

ACCELERATION tells us how VELOCITY changes with time (in all directions).

So: If we know an object’s three-dimensional acceleration at all times, then we can predict its motion.

Page 16: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

“If we know an object’s acceleration at all times, then we can predict its motion.”

( Newton invented a new kind of math specifically for this purpose: “differential calculus”, which concerns rates of change. )

Page 17: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

Newton also invented the concept of force in the modern sense.

FORCE = MASS x ACCELERATION, or

F = m a , or

a = F / m .

( F and a are vectors; they have directions.)

Page 18: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

Newton’s

crucial

“thought experiment”

(1665)

Page 19: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

Page 20: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

Page 21: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

The Moon’s orbit around Earth

r = 384000 km = about 60 x (radius of Earth),

v = 3700 km/hr = 1.02 km/s.

So the required acceleration toward earth is

a = v 2 / r = 0.27 cm / s / s.

Page 22: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

Moon’s acceleration toward Earth isabout 0.27 cm / s / s.

So what? -- Our acceleration towardEarth is g = 980 cm / s / s. Newtonnoticed that these have the ratio3600.

60 x farther makes gravity weaker by a factor of 3600 x.

This is obviously 60 x 60 = 60 2 !

Page 23: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

Newton’s law of gravity:

( attractive force between M and m )

= G x M x m / (distance) 2 .

For instance, 3 x farther makes it 9 x

weaker;

10 x farther makes it 100 x weaker.

Page 24: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

THE “INVERSE SQUARE LAW” OF GRAVITY WAS ENOUGH TO EXPLAIN KEPLER’S LAWS!

1. Orbits are ellipses, Sun at one focus

2. Equal areas in equal times

3. Period squared = orbit radius cubed

Page 25: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

NEWTON’S REVOLUTION WAS AS IMPORTANT AS COPERNICUS’.

There are “laws of physics” that apply

everywhere, from this room to the

edge

of the universe. In 1680 this was a

breathtaking new idea!

It led to modern physical science.

Page 26: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

Newton’s influence on the following century -- “the age of reason”, at least for philosophers.

His historical importance was recognized in his own time -- arguably “the most important man in the world”, outranking even Louis XIV.

Page 27: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

ORBIT SHAPES: ELLIPSE, PARABOLA, HYPERBOLA

Page 28: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

“CONIC SECTIONS”:

CIRCLE

ELLIPSE

PARABOLA

HYPERBOLA

Page 29: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

ENERGY IN ORBITS

-- KINETIC ENERGY -- POTENTIAL ENERGY

K.E. + P.E. = constant

The Roller Coaster analogy

Page 30: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)

CELESTIAL MECHANICS

(ORBITAL DYNAMICS)

Kepler’s laws are not exactly true ...

Page 31: Ast 1001 lecture 4 -- 2007 Sept 13 (kd). 4. How Orbits Work Astronomy 1001, Sept 2007 – Prof. K. Davidson

Ast 1001 lecture 4 -- 2007 Sept 13 (kd)