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Jepler°s second observation was that the planets do not go around the sun at |
a uniform speed, but move faster when they are nearer the sun and more sÌowly |
when they are farther from the sun, in precisely this way: Suppose a planet |
--- Trang 141 --- |
Z7 |
2 Z7 |
Fig. 7-2. Kepler's law of areas. |
1s observed at any two successive times, let us say a week apart, and that the |
radius vector* is drawn to the planet for each observed position. The orbital are |
traversed by the planet during the week, and the two radius vectors, bound a |
certain plane area, the shaded area shown in Fig. 7-2. If two similar observations |
are made a week apart, at a part of the orbit farther from the sun (where the |
planet moves more slowly), the similarly bounded area is exactly the same as in |
the first case. So, in accordance with the second law, the orbital speed of each |
planet is such that the radius “sweeps out” equal areas in equal times. |
tPinally, a third law was discovered by Kepler much later; this law is of a |
diferent category from the other two, because it deals not with only a single |
planet, but relates one planet to another. 'This law says that when the orbital |
period and orbit size of any two planets are compared, the periods are proportional |
to the 3/2 power of the orbit sỉze. In this statement the period is the tỉme interval |
1t takes a planet to go completely around ïits orbit, and the size is measured by |
the length of the greatest diameter of the elliptical orbit, technically known as |
the major axis. More simply, If the planets went in circles, as they nearly do, the |
time required to go around the circle would be proportional to the 3/2 power of |
the diameter (or radius). Thus Kepler”s three laws are: |
I. Each planet moves around the sun in an ellipse, with the sun at one focus. |
TL. The radius vector from the sun to the planet sweeps out equal areas in |
equal intervals of time. |
TH. The squares of the periods of any two planets are proportional to the ceubes |
of the semimajor axes of their respective orbits: 7' œ a3⁄2. |
—* A radius vector is a line drawn from the sun to any point in a planet”s orbit. |
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7-3 Development of dynamics |
While Kepler was discovering these laws, Galileo was studying the laws of |
motion. The problem was, what makes the planets go around? (In those days, |
one of the theories proposed was that the planets went around because behind |
them were invisible angels, beating their wings and driving the planets forward. |
You will see that this theory is now modifiedL It turns out that in order to keep the |
planets going around, the invisible angels must fly in a diÑerent direction and they |
have no wings. Otherwise, it is a somewhat similar theoryl) Galileo discovered a |
very remarkable fact about motion, which was essential for understanding these |
laws. That is the principle oŸ 7nmerf2a—lŸ something is moving, with nothing |
touching it and completely undisturbed, it will go on forever, coasting at a |
uniform speed in a straight line. (W2, does i% keep on coasting? We do not |
know, but that is the way it is.) |
Newton modifed this idea, saying that the only way to change the motion |
of a body is to use ƒorce. lf the body speeds up, a force has been applied #n |
the direction oƒ motion. On the other hang, 1f its motion is changed to a new |
đircction, a force has been applied s7deuazs. Newton thus added the idea that |
a Íforce is needed to change the speed ør ¿he direcfion of motion of a body. For |
example, IŸ a stone is attached to a string and is whirling around in a circle, i% |
takes a force to keep 1È in the circle. We have to pull on the string. In fact, the |
law is that the acceleration produced by the force is inversely proportional to the |
mass, or the force is proportional to the mass times the acceleration. The more |
massive a thing is, the stronger the force required to produce a given acceleration. |
(The mass can be measured by putting other stones on the end of the same string |
and making them go around the same circle at the same speed. In this way 1 |
1s found that more or less force is required, the more massive object requiring |
more force.) The brilliant idea resulting from these considerations is that no |
tangeniial force is needed to keep a planet in its orbit (the angels do not have to |
ñy tangentially) because the planet would coast in that direction anyway. lÝ there |
were nothing at all to disturb it, the planet would go of in a sứraight line. But |
the actual motion deviates from the line on which the body would have gone if |
there were no force, the deviation beiïng essentially at right angles to the motion, |
not in the direction of the motion. In other words, because of the principle of |
inertia, the force needed to control the motion of a planet arownd the sun is not |
a force around the sun but #øouard the sun. (TỶ there is a force toward the sun, |
the sun might be the angel, oŸ coursel) |
--- Trang 143 --- |
7-4 Newton?s law of gravitation |
tFrom his better understanding of the theory of motion, Newton appreciated |
that the sun could be the seat or organization of forces that govern the motion of |
the planets. NÑewton proved to himself (and perhaps we shall be able to prove it |
soon) that the very fact that equal areas are swept out in equal times is a precise |
sign post of the proposition that all deviations are precisely rœd¿al—that the law |
Of areas 1s a direct consequence of the idea that all of the forces are directed |
exactly £ouard the sun. |
Next, by analyzing Kepler's third law it is possible to show that the farther |
away the planet, the weaker the forces. If two planets at diferent distances |
from the sun are compared, the analysis shows that the forces are inversely |
proportional to the squares of the respective distances. With the combination |
of the two laws, Newton concluded that there must be a force, inversely as the |
square of the distance, directed in a line between the two obJects. |
Being a man of considerable feeling for generalities, NÑewton supposed, of |
course, that this relationship applied more generally than just to the sun holding |
the planets. It was already known, for example, that the planet Jupiter had |
moons going around it as the moon of the earth goes around the earth, and |
Newton felt certain that each planet held its moons with a force. He already knew |
of the force holding us on the earth, so he proposed that this was a unớuersal |
ƒorce—that cuerWthing pulls cueruthing cls. |
The next problem was whether the pull of the earth on its people was the |
“same” as its pull on the moon, 1.e., inversely as the square of the distance. If |
an objJect on the surface of the earth falls 16 feet in the first second after it 1s |
released from rest, how far does the moon fall in the same time? We might say |
that the moon does not fall at all. But if there were no force on the moon, 1§ |
would go of in a straight line, whereas it goes in a circle instead, so it really |
ƒalls ín Írom where i% would have been ïf there were no force at all. We can |
calculate from the radius of the moon's orbit (which is about 240,000 miles) and |
how long it takes to go around the earth (approximately 29 days), how far the |
mmoon moves in its orbit in 1 second, and can then calculate how far it falls in |
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