Gravity, Newton's laws and the orbits of the planets
This is a supporting page to the multimedia tutorial on gravitation in Physclips. In some parts, it gives a little more detail and discussion, and it has some derivations and appendices.
Gravity is a puny force. If you stand next to a tank containing many
tons of water, you don't even notice its gravitational force on you.
As we shall see, to produce substantial gravitational force, one of the objects has
to approach planetary size. Let's compare gravity with electricity: A hydrogen atom is an
electron and a proton. The electric attraction between them is larger
than the gravitational attraction by a factor of 5 x 1039.
The attractive force that holds the nucleus together -- aptly called
the strong force -- is stronger than the electric force over short range:
if the nucleus is small enough, the strong force 'wins' and the nucleus is stable. (However,
large nuclei are unstable: they divide by radioactive decay: elements with atomic number above about 90 are usually radioactive because the electrical repulsion among 90 protons tends to defeat the attraction of the strong force.) This appendix has a chart showing the known forces and some relations among them.
So why does gravity rule the universe?
Nuclear forces only have a finite range about the size of nucleus.
(This finite range is determined by Heisenberg's Uncertainty
Principle, using an argument that won a Nobel Prize for Hideki
Yukawa.) Electromagnetism and gravity both have very large, perhaps
infinite range.
Electric charge comes in positive and negative, which cancel. The
earth contains almost exactly the same number of protons and electrons, so
its electrical field is small. In contrast, mass is
always positive and, for gravity, every mass attracts every other mass.
So gravity runs the planets, the
stars, the galaxies, galactic clusters... Let's see how.
Before Galileo and
Newton, Aristotle's writings dominated European thought about physics.
Oversimplifying a little, it was thought that:
things on earth fall or rise because they find their 'natural' place
planets and other heavenly bodies move due to various, usually supernatural forces: in
ancient Greek metaphor, they are pushed by the sirens and fates. There was thought to be no connection between the two: in fact, natural and supernatural were
usually contrasted.
Newton's laws, however, apply to both, and the first and second laws (F= ma) state that:
Only acceleration requires force
Acceleration is the rate of change in
velocity. Imagine you're driving at a fixed speed: you push the accelerator,
and your speed increases: this is a positive forwards acceleration. But you
also need brakes to stop: a force is required to decelerate. Forces cause
accelerations, and also decelerations, which are just negative accelerations.
One of Galileo's and Newton's insights was that the 'natural' condition was
not zero speed but zero acceleration. If there are no forces -- no friction, no air resistance
etc -- then an object at rest remains at rest, and a moving object continues
moving at a constant speed in a straight line. This is Newton's first law of
motion.
A larger force is required to accelerate a massive truck than to
accelerate a bicycle. This is included in Newton's
laws of motion, which states that the total force F applied to a mass m produces an acceleration a where
F = ma.
Force and accleration are vectors,
meaning that they have direction, as well as magnitude. If the total force on
a body is in the North direction, then it will accelerate North. Force is
measured in newtons (abbreviation N). One newton is the force required to
accelerate one kg at one metre per second per second. A newton is about the
weight of a small apple.
Newton's law of motion says that a force is required to get an object
moving (an acceleration in the direction of its motion), or to stop it moving
(a negative acceleration in that direction). A force is also required to
change the direction of its motion because, as we shall see, that is also an
acceleration.
Note that mass is not the same as weight. If your mass is 70 kg,
then your weight on earth is 70 kg multiplied by the earth's gravitational
field, which is about 10 metres per second per second. So your weight is 700
newtons. Suppose you went to the moon, where the gravitational field is six
times smaller. Your mass would still be 70 kg -- you would still be made of
the same amount of material -- but your weight would be only 120 newtons. On
the moon, you would fall more slowly and it would take less force to hold
yourself upright, but it would still take the same force to accelerate you.
A change in motion requires a force
You're standing in the bus when it starts moving forwards (when it
accelerates forwards). You are holding onto the grab bar. The floor of
the bus pulls your feet forward, the grab bar pulls your arm and body
forward - you accelerate forward with the bus. Another passenger is not
holding the bar. His feet accelerate forward with the bus, but not his
body. The bus accelerates forwards, he falls backwards.
When the bus driver brakes, the reverse applies. The bus and the rail
apply a backwards force on you, and you decelerate (ie accelerate in the
negative or backwards direction). The body of other passenger, however,
continues forwards while the bus slows. The bus decelerates (ie
accelerates backwards), he falls forwards.
What happens when the bus turns to the right, at constant speed?
According to Galileo and Newton, an unrestrained passenger would tend to
continue travelling in a straight line. For the passenger not holding
the grab bar, his feet turn the corner with the bus, but his body keeps
going forwards. The result is that he falls to the left. In this case,
the bus accelerates to the right, he falls to the left.
(When you try this experiment, make sure that the person sitting on
your left is simpatico.)
In
circular motion, we derive an expression for the centripital acceleration:
the acceleration towards the centre in circular motion. For an object
moving at speed v around a circle with radius r, the acceleration is
ac = v2/r.
The period T is the time taken
for one circle, so v = 2πr/T. So we can also write
ac = 4π2r/T2.
(Without maths,
we can still explain in an inexact way why it has this form: the bigger
v is, the larger the acceleration, because it goes from forwards at v to
backwards at v twice per cycle. But the cycle repeats at a rate
proportional to v/r, so it is proportional to both v and to v/r. For a
real explanation, you need the maths, which is given below.)
So an object travelling in a circle at constant speed is always
accelerating but, because the acceleration is towards the centre of the
circle (it's called a centripetal acceleration) it doesn't add to
or subtract from the speed. A force that causes a centripetal
acceleration is called a centripetal force. Let's now look at some
accelerations and forces.
Demonstrations of forces and acclerations
These film clips use a spring
to accelerate a bowling ball. You can tell whether the spring applies a force
from whether it is stretched or not, as in these photos.
In 1687, Isaac Newton wrote "I deduced that the forces which keep the
planets in their orbs must be reciprocally as the squares of their distances
from the centres about which they revolve; and thereby compared the force
requisite to keep the Moon in her orb with the force of gravity at the surface
of the Earth; and found them answer pretty nearly."
Here, \translated into modern units, is Newton's calculation of the centripital
acceleration of the moon due to its circular orbit around the earth. Its
direction is towards the earth. We can work out its magnitude from our
equation ac = 4π2r/T2, using the
distance from the earth to the moon (380,000 km) and its period of 27.3
days.
I don't know whether Newton ever
thought about falling apples, but if he did, he would have known that
(in today's units) they fall at 9.8 ms-2. So the ratio
of the accelerations is
Now we might expect that the effect
of the earth's gravity on the moon would be less, because it is further
away than the apple. For the apple, the distance from the earth's centre
is the earth's radius: Re = 6370 km. So the ratio of the
distances is
so
Hence Newton's
idea: what if the apple and the moon accelerate according to the same law?
What if every body in the universe attracts every other, via an inverse square
law? Note the contrast with the Aristotelean ideas mentioned above: for
Newton, the same laws govern the 'heavens' as govern familiar objects. (One
could see an extension of this idea as the ambit of contemporary physics: to
find a simple set of laws that explain everything, from the biggest to the
smallest, over the whole history of the universe.)
In modern notation, we write Newton's law thus: if two
bodies with masses m1 and m2 are separated by a distance
r, then the attraction between them is
There are several things to note:
The negative sign is used to mean an attraction. If m1,
m2 and the separation between them are positive (and they always
are -- there are no negative masses), then the gravitational force between
them is attractive. As we saw above, this is why gravity always wins on the
large scale.
The force is proportional to each of the masses. This is not surprising:
experimentally we find that two apples, side by side, fall with the same
acceleration as one apple, so the force on twice the mass is twice the force
on one.
There is a constant of proportionality, G, the universal constant of
gravitation, which we can measure – see below.
Gravitational forces, like all forces ever discovered, come in pairs
that are equal and opposite. If m1 attracts m2 with a
force F, then m2 attracts m1 with a
force -F. The observation that all forces come in such pairs
is Newton's third law of motion.
The r2 in the denominator means that the attraction gets
weaker in proportion as the square of the separation.
Why is gravity
inverse square? is an interesting question, and one explanation is geometrical. If we picture field lines radiating uniformly from a symmetrical mass distribution, the intensity of the field (the number of field lines per unit area) is the total number of field lines (say N) divided by the area of a sphere, which is 4πr2. So the field strength is N/4πr2.
This description is rarely used for gravity. In electricity, however, the analogous relation
between geometry and the strength of the field is standard and is called Gauss' Law. Magnetism is also an inverse square law, and one of Maxwell's equations is usually called Gauss' law for magnetism. If we were to use the same mathematical formulation for gravity as for electricity and magnetism, we should also have a factor 4π in the denominator. However, for gravity, the factor
(1/4π) is absorbed in the constant G.
So the 1/r2 factor that it comes
from the three dimensional, approximately flat geometry of our universe. In a flat space, the interior angles of triangles add to 180°, the area of a sphere is 4πr2 and electromagnetic and gravitational force are proportional to 1/r2. If the angles of a triangle added to less than 180°, then these forces would decrease more strongly with r.
Another interesting question: the same quantity, mass, that appears in
Newton's equations of motion, also appears in Newton's (or Einstein's) law of gravitation. This is
not due to a lack of imagination on Newton's part: he thought carefully about
this coincidence. Why is the quantity (inertial mass mi) that determines inertia equal to (or at
least proportional to) the quantity (gravitational mass mg) that determines gravity? One reponse is that this it is not a
coincidence, and that the interactions among masses give rise to inertia. This is called Mach's
Principle. Another approach is mi and mg really are the same thing, which is a starting
point for Einstein's theory of General
Theory of Relativity. The proportionality of mi and mg has been and is still being tested in a number of several very sensitive experiments.
Newton showed that the gravitational effect of a spherically symmetric body is the same as it would be if all its mass were located at its centre (provided that you are outside the body). Planets and stars are nearly spherically symmetric, so one can calculate their gravitational effects using separations from their centres. To prove this requires some mathematics, which is given in this file.
This diagram shows, schematically, the technique used by Henry Cavendish in 1798 to obtain the first measurement of the mass of the earth, using equipment he inherited from John Mitchell. (From this one can readily obtain the value of G, but Cavendish did not do this, because the formulation of gravity in his day did not use the modern expression.)
Two large masses
are mounted on a rod, which is suspended by a thin wire. When the wire
is twisted, it tends to untwist itself (technically, it exerts a
restoring torque proportional to the angle of twist). This can be
calibrated: one can determine the forces required at each end of the rod
to twist the wire by a given angle (for instance, this can be determined
by rotating the rod, letting it go, and measuring the frequency of its
oscillation).
Once the system is stable, two large, known masses are positioned
near the masses on the rod. The tiny gravitational attraction between
the pairs of masses twists the wire slightly, and the force is
calculated from the new equilibrium position. In the diagram, the angle
has been exaggerated. In practice, the deflection may be very small, but
can be measured by mounting a mirror on the rod and measuring the
deflection of a beam of light projected onto a distant screen. Here is a
link to a Do it yourself
Cavendish experiment.
In modern notation, we should use Newton's equation for gravitational force:
From the deflection and the
calbration of wire, Cavendish calculated F. He already knew m1 and
m2, so he calculated the constants of proportionality for gravity. In modern versions of this experiment, we say that we measure G. Its value is G =
6.67 x 10-11 Nm2kg-2. In other words, two masses, each one kg and separated
by a metre attract each other with a force of 0.00000000007 newtons.
Cavendish used his measurements to determine the mass of the earth, Me. An
object of mass m at the earth's surface is Re from the
earth's centre. The magnitude of its weight is approximately* mg, where g is the
acceleration it has in free fall.
Cavendish's value for the mass of the earth was close to the currently accepted value of 5.97 x 1024 kg. Knowing the mass of the earth and its orbit
around the sun, one knows the centripital force exerted by the sun on the
earth, and so one can calculate the mass of the sun. (The orbits of moons
around most of the planets gives the masses of the planets.)
* "Approximately" is there because the earth rotates. This is explained below in Why g is not parallel to Fg
Gravity is a puny force
Although measurements of the constant of
gravitation are now much more accurate than those made by Cavendish, G is still
the least well known of the fundamental constants, simply because gravity is
so weak. Let's illustrate this with some values.
Oil tankers are among the largest objects we can easily move. Two
100,000 tonne tankers, anchored 100 m apart would exert a gravitational
attraction on each other of approximately
Gm1m2/r2 = 70 newtons. This force (roughly
the weight of a very small child) is tiny compared to the forces of
wind, waves and current. (Further it is equal to the gravitational
attraction of the volumes of water that they have displaced and so would be
harder to measure.)
What about the gravitational attraction between two 70 kg people sitting
0.4 m apart? Here, Gm1m2/r2 is 2
micronewtons, which is too small to feel, even with the tip of the
finger.
Two conclusions follow. One is that we can usually neglect
gravity unless at least one of the bodies approaches planetary size. The
second conclusion is a quotation attributed to Albert Einstein "Gravitation
cannot be held responsible for people falling in love".
However, as we mentioned above, the cancellation of positive and negative
electrical charge and the limited range of nuclear forces means that, on the
large scale, gravity wins. Which brings us to
and what has been known, after a metaphor used sometimes attributed to Pythagoras, as "the music of the
spheres". For two millenia or more, understanding the motion of the planets was one of the great goals of philosophers. This appendix may give some idea of the importance attached to this question.
As long ago as the fifth century BC, Leucippus and Democritus proposed a
heliocentric universe, i.e. one in which the planets orbit the sun. On the
mistaken assumption that the earth's motion ought to be noticeable, Hipparchus
(second century BC) and Ptolemy (second century AD) proposed a universe in
which the sun and planets executed complicated motions around the earth.
(Hipparchus, Ptolemy, Aristotle and many others were mistaken because they expected that one would sense velocity. In fact what we sense are forces – on our bodies, including parts of our inner ears – so our sense of motion comes from the forces required to produce the accelerations associated with the motion. As we show in the multimedia tutorial on Physclips, and also below the acceleration due to the rotation of the earth is only 0.034 m.s−2 at the equator and less at other latitudes. The force required to produce this acceleration is hundreds of times smaller than the usual forces required to support our weight. Further, it is very nearly constant: it changes its direction very slowly. So one cannot feel – nor even easily measure – the effects of the accelerations produced by the earth's rotation. For a demonstration, however, see the Foucault pendulum. Another criticism of the heliocentric model was the apparent absence of parallax in the positions of the stars. Before the development of good telescopes, this was difficult to observe, and Aristarchus proposed that they were infinitely distant.)
The Danish astronomer Tycho Brahe (1546-1601) made very many, very careful,
naked eye observations of the positions of the planets. He was joined by
Johannes Kepler, a tireless calculator. After a long time trying to fit
circular orbits and even musical harmonies to the data, Kepler eventually
discovered that the data were all well fitted by the following empirical laws.
Kepler's laws
1. All planets move in elliptical orbits, with the sun at one
focus.
The elliptical orbits of the planets are, however, not very far from being circles. (Mars was the most eccentric orbit that Kepler studied. The orbit of Pluto – unknown in Kepler's time – is much more eccentric.) The mass of the sun is so much greater
than that of the planets that the sun is very nearly the centre of mass of the solar
system.
(We return to this approximation below.)
2. A line joining the planet to the sun sweeps out equal areas in
equal time.
i.e. Planets move more slowly at apogee (distant), more
rapidly at perigee (close).
3. The square of the orbital period (i.e. the planet's 'year') is
proportional to the cube of the semi-major axis of its orbit.
Slow
orbits for distant planets, fast for close.
Why is it so? What
underlying reasons are there for Kepler's laws? It is difficult for a modern
person to have a feeling for the magnitude of this puzzle – hence this appendix. For two millenia,
this was the riddle of riddles. So Newton's demonstration that the three laws follow simply from his laws of mechanics was a major triumph and secured his fame. Proving the first law requires a reasonable amount of geometry, so we omit it here. In the multimedia tutorial on Physclips we derive the other two. To revise briefly here:
For
circular motion, with the sun at the centre (see below), the centripital acceleration is, as before
ac = rω2 = 4π2r/T2,
where r is the radius, ω the angular velocity and T the period. Now add a force whose
magnitude is GmM/r2 and set F = ma:
GmM/r2 = Fgravity = mac =
m4π2r/T2, so:
T2 = (4π2/MG)r3 (K2)
For circular orbits at least, we have derived Kepler's third
law in a few simple equations. The same force that makes the apple fall rules the heavens. The second law, which is animated below, follows just as simply from conservation of angular momentum. The proof, which is given in the multimedia section is repeated here:
For small angle δθ, the area subtended by δθ is that of a triangle with long side r:
δA = ½r.(rδθ).
The gravitational force acting towards the sun exerts no torque on the planet, so the angular momentum L about the focus of the orbit is conserved. If the momentum of the planet is p = mv,
|L| = |r X p| = |r X mr|
= mrvtangential
(You can revise vectors.) In terms of the angular velocity ω, this gives
|L| = mr.rω = mr2(δθ/δt) = m(r2δθ)/δt
and, using the expression for δA
|L| = 2mδA/δt
So, because |L| is constant, then in any given time δt, δA is constant.
In the multimedia section, we use the equation derived above, T2 = (4π2/MG)r3, to derive the period of orbits for earth's satellites, using G =
6.67 x 10-11 Nm2kg-2 and Me = 5.97 x 1024 kg. Many satellites, including the international space station, are in low earth orbit, meaning an orbit with a radius a little greater than that of the earth: say 6,500 km. Substitution in (K2) gives a period of about 90 minutes.
(So Puck, in Shakespeare's A Midsummer Night's Dream, seems to be out by a factor of two.)
Newton gave this nice idea to help explain orbits. First, consider a projectile (Newton imagined a cannonball) fired horizontally from the top of a mountain, over a distance small enough that the earth's surface can be considered flat. No matter what its horizontal speed, its vertical acceleration is g downwards.
If we fire it very fast, however, we can no longer neglect the curvature of the earth. At a particular value of the horizontal velocity (about 28,000 k.p.h.), the curvature of the path of the cannonball will match the curvature of the surface of the earth. The cannonball still accelerates downwards at g, but g is now the centripital acceleration of its circular motion, as shown below.
Another very important orbit is that of geosynchronous satellites, whose period of 23.9 hours keeps them above the same point on the earth's equator. Again, using equation
T2 = (4π2/MG)r3
and G =
6.67 x 10-11 Nm2kg-2 and Me = 5.97 x 1024 kg, we get an orbital radius of 42,000 km. In the animation, the size of the earth and the orbit (but not the satellite) are to scale. This orbit is very useful for communications satellites: if you point your dish towards the satellite, you don't have to move it.
(We note in passing that an object at rest on the earth's surface already has a speed of ωrecos (latitude), due to the rotation of the earth. This is over 1,000 k.p.h for tropical latitudes, which provides an incentive to locate space launch centres at low latitudes. This is probably one reason why NASA launches from Florida.)
In figure at right, a NASA airplane (nicknamed the 'vomit comet') cuts the power in its engines and, for about 25 seconds, travels in a trajectory that is nearly parabolic (none of the diagrams to scale, of course). Both the plane and its occupants accelerate towards the Earth at g: all are in free fall. Astronauts are thus exposed to free fall and obtain brief periods of experience in working in the condition of free fall and feeling "weightless".
There are some similiarities between the passenger (mass m) in the lift (let's put it at the equator) and an astronaut (mass m) in low Earth orbit. The weight of each is about mg. Both accelerate towards the centre of the Earth at approximately g. The difference is that the spacecraft makes a circle around the Earth in about 90 minutes, whereas the lift makes a circle around the Earth in about 24 hours. The acceleration g is just enough to keep an object in low Earth orbit with a period of roughly 90 minutes. This acceleration is far too great for the 'orbit' of the hapless passenger in the lift. If a satellite loses speed, it gradually spirals in towards the Earth. The horizontal speed of the passenger in the lift is so low that his 'spiral' towards the centre of the Earth is almost a straight line. (There have been a few 'approximately's and 'almost's in the above. If you are interested in the analysis of motion in the rotating frame of the Earth, have a look at the formal analysis of the motion of a pendulum at the Earth's surface.)
(What would it feel like if you really were weightless? Suppose you were in a spacecraft far from the sun, other stars, even other galaxies. Then you would be (nearly) weightless. How would it feel? If your spacecraft were not accelerating, then you would feel "weightless", just like someone in the space station. If you fired the engines of the spacecraft, however, you would feel as though you had weight. You could also produce the feeling of weight by spinning the space craft.)
(A further approximation: the gravitational force exerted on you by the earth is almost, but not quite, mg. For details, see Why g is not parallel to Fg.)
It is a common simplification to say that 'the moon's orbit is a circle about the earth': the gravitational attraction of the moon towards the earth provides the centripetal force for the moon's orbit. From Newton's third law, of course,
the moon attracts the earth with a force of equal magnitude, which accelerates the earth. So the earth and the moon each trace (almost perfectly) circular orbits about their common centre of mass. The sketched below illustrates this, but is not to scale.
Using subscripts m and e for the moon and earth, we can write
Magnitude of force on the moon due to earth: Fg = mmam = mmω2rm and
Magnitude of force on the earth due to moon: Fg = meae = meω2re.
Setting these two expressions equal gives
rm/re = me/mm = (5.98 x 1024 kg)/(7.36 x 1022 kg) = 81.3 (i)
The distance between the centres of the earth and the moon gives a second equation:
re + r m = 3.85 x 108 m (ii)
Solving these gives rm = 3.80 x 108 m and re = 4.7 x 106 m
So the centre of both orbits, which is also the centre of mass, is 4700 km from the centre of the earth: it lies inside the earth. (In contrast, the analogous calculation shows that the centre of mass of the sun-Jupiter system lies outside of the sun.)
A puzzle
An interesting paradox: why doesn't the moon fall into the
sun? Calculate the point on a line between earth and sun at which the gravitational forces exerted on a mass m by the earth (Fe) and the sun (Fs) are equal and opposite.
Doing the calculation, we find that the point of equal attraction lies 260,000 km from the earth. But the moon is 380,000 km from the earth! At new moon, the point of equal attraction lies nearly on a line between the earth and the sun (during a solar eclipse, it lies exactly on this line). So, at new moon, will the moon fall into the sun? The problem and the calculation are described here. But I'm not giving answers: it's for you to solve!
When you lift something up, you expend energy -- you do work on it. This
energy is stored, in the sense that you can get it back again. It is called
gravitational potential energy. For instance, during periods of low
electricity demand, energy authorities in Australia use electrical energy from coal-fired
power stations to pump water up the Snowy Mountains into high dams. In periods
of high demand, they can then let it flow back downhill to get back the
gravitational potential energy of that water via the hydroelectric generators.
The gravitational potential energy U of two objects, masses M and m, at
separation r, is obtained from the definition of potential energy, −Ug = ∫ Fg.ds. (Revise potential energy.) Because gravity acts in the direction of −r, we can write Fg.ds as −Fgdr. Substituting from Newton's equation for Fg and integrating:
Again, we have a constant of integration to define, which means a zero of potential energy to choose. An astronomer would tell you that there is nothing special about the surface of the earth, so the zero of potential energy is taken by astronomical
convention at infinite separation, so set U = 0 at ri = ∞, which gives
A consequence of this general or astronomical convention is thatgravitational potential energy is always negative at finite
separation. This does not affect the main point that work must be done to lift
something: gravitational potential energy increases with separation. (If M is
the earth and m a small object, we speak of the U of m in the field of M.
However U is a property of the pair of objects and we could equally talk of
the potential energy of M in the field of m.)
The graph above shows two different expressions for gravitational potential energy of a mass m near the earth. For r > re, we use U = −GMem/r. Very close to the earth (in other words when (r − re) << re), we can use the approximation GMe/re ≅ g and the binomial expansion to write:
Escape "velocity" is minimum speed ve required to escape, i.e.
to get to a very large ('infinite') distance from a planet. An object launched
from earth with the earth's escape velocity would never return. To achieve
this, we need to give it an initial kinetic energy Ki =
½mvesc2 that is at least as great as the magnitude of U near the
earth. Rearranging yields
For the earth, vesc = 11 km.s−1 = 40,000 k.p.h. The animation below shows an object launched at this speed, i.e. with E = 0 , and so, at all times, K = −U.
From the equation above, we see that a very massive
(large M) and compact (small R) object has a very large escape velocity. If we
combine the laws of gravity and those of electromagnetism, we might ask how
small a given mass must be if its escape velocity equals the speed of light.
John Mitchell explained in 1783 that dark stars were possible: stars so dense
that no light escapes. We now call such objects black holes.
Setting vesc = c and rearranging the equation above gives
Rblack = 2GM/c2
the 'event horizon' of the black hole. If M lies inside Rblack, then no light escapes outside.
Having c2 in the denominator means
that this radius is small. For an object with the mass of the earth, it is = 9
mm. The earth is not going to contract to this size, so it won't become a
black hole.
For the sun, the value is 3 km. The sun is currently made of plasma, so one
might ask whether, when it cools and shrinks, it could become a black hole.
After all, it is electrically neutral, which reduces the possible repulsion
due to electric forces, and nuclear forces, though strong, have a small,
finite range.
The answer is no: for the sun, the repulsive forces among the atoms are
strong enough to prevent gravity from turning it into a black hole. For stars
somewhat bigger than the sun, however, these forces are not large enough, and
only repulsive nuclear forces are strong enough to resist gravity. Such stars
become neutron stars -- like a giant nucleus, in which gravity, intensified by
having a huge mass within a diameter of several km, is the main attractive
force.
Finally, for yet larger stars, even nuclear forces do not provide strong
enough force to resist gravity. The result is a black hole, from which light
cannot escape. Although it is black -- emitting no light -- radiation can be
produced near the black hole. However, this is not how we can find them. The
only way we can find them is from the effect of their gravitational field on
other stars (as shown in the multimedia tutorial on Physclips) or on light (the effect is like that shown at right).
So far, we have only mentioned Newton's theory of gravitation. Although it
is an excellent theory, it does not agree with experiment if one investigates
extremely large fields, or moderately large fields with very high precision.
In other words, it is wrong. However, it is such an excellent approximation
that Newtonian gravity is what we use to calculate in almost all
circumstances, while recognising that it is just a very convenient
approximation to more exact theories.
To be accepted, any new theory of gravity must give virtually the same
answer as Newton's in all of the many cases where Newton's theory works, but
must also give the right answer for the cases where we know that Newton's
theory fails, such as the slight deflection of starlight passing very close to
the sun (observable during a solar eclipse) and certain aspects of the orbit
of Mercury that cannot be accounted for by considering the effects of the
other planets.
Several other
theories do this, of which one of the simplest and by far the most widely
used is Einstein's General
Theory of Relativity. Philosophically, General Relativity is very
different from Newtonian gravity, in that it doesn't use forces. Rather, the
effect of large masses is to curve space, and the curvature of space
determines the motion of objects. It is often summarised thus: "matter tells
space how to curve, and space tells matter how to move".
So, if there are several competing theories that all do better than
Newton's, what theory of gravitation should we use? The mission of Gravity Probe B was to conduct experiments to distinguish among some current theories of
gravitation, but it had limited results.
However, both Einstein's and Newton's theories of gravity have a problem
when they encounter quantum mechanics, and that problem involves the very
nature of space and time. We explain this further on Gravity,
relativity and quantum mechanics.
Fortunately, the scale of the problem is that of the Planck length, which
is 1.6 x 10-35 metres. This is immeasurably small, and it is
perhaps not too surprising that our ideas about space would need to be revised
on this scale.
(Yes, small: the Planck
length is 0.000000000000000000000000000000000016 metres. Let's
compare it with the size of an atom, which is already about 100,000 times
smaller than anything you can see with your unaided eye. Suppose that you
measured the diameter of an atom in Planck lengths, and that you counted off
one Planck length each second. To measure the atomic diameter in Planck
lengths would take you 10,000,000 times the current age of the
universe.)
While we're on the subject, let's be quantitative about these limits, and let's look at Newtonian mechanics from other perspectives.
Newtonian gravity is accurate if the gravitational potential energy Ugravis much less than the proper energy mc2. At the earth's surface, Ugrav/mc2 ≅ 7 x 10−10. So, unless you are looking for very high precision, Newtonian gravity is an excellent approximation. However, time is often measured very precisely, and such precision is used in navigation systems. So general relativistic corrections cannot be neglected in such applications.
Newtonian mechanics is accurate if relative velocities are small compared with that of light. For a jet airliner, v/c < 10−6. Macroscopic objects travel much more slowly than c, but atomic particles and especially electrons are regularly accelerated to high speeds. Again, timing and navigation systems sometimes require the precision that obliges relativistic calculations.
Newtonian mechanics is also limited by scale. It is accurate if the product of momentum and a typical length is much greater than Planck's constant, h. For a small molecule at room temperature,
(momentum*size)/h ~ 10. For a molecule in a gas, the typical size of the container is large compared to the molecule, so classical mechanics is fine, unless the temperature (and therefore the molecular speeds) is very low. On the molecular scale, however, Quantum Mechanics begins to be important. For low mass objects, such as electrons, and especially at lower temperatures, momentum*size may be much less than one, and quantum effects may dominate.
To an excellent approximation, the gravitational force on a mass m at the earth's surface is Fg ≅ mg. An excellent approximation, but not exact (except at the poles), because of the earth's rotation: the earth's surface is not an inertial frame. A point on the earth's surface is accelerating with centripital acceleration whose magnitude is
acentrip = rω2 = re(cos θ) ω2
where re(cos θ) is the radius of the earth, ω is its angular velocity about its axis and θ is the latitude. When we measure the weight mg of a mass m, we typically do this by putting it on a balance and measuring the normal force N required to keep it stationary with respect to the earth – i.e. to keep it accelerating with acentrip. So
macentrip = N + Fg or
−N = Fg − macentrip.
Now re(cos θ) ω2 is 0.034 m.s−2 at the equator, less at other latitudes and zero at the poles. Usually, we then make the approximation that re(cos θ) ω2 << g = 9.8 m.s−2, so N ≅ Fg.
The diagram above may seem odd, because the vertical of the string is not at right angles to the horizontal. That's because, in that diagram, we exaggerated the angles of the forces, but didn't consider the effects of rotation on the shape of the earth. So, let's hang the mass on a string and leave it at rest, with respect to the earth. As shown, the tension in the string will be almost the same as mg, but not quite. The string hangs vertically, by definition of vertical. However, this direction is not quite parallel to Fg and it does not point exactly at the centre of the earth. A similar argument determines the shape of the earth. The surface of a bowl of water is horizontal, by definition. Here, the normal force and the gravitational force acting on a mass at the surface of the water must also add to give acentrip,, otherwise the water would flow out of the bowl. So the surface of the water – horizontal – is at right angles to the string in our example.
The earth's shape is determined by the the forces on it and, on a large scale, it is very close to that of a drop of spinning fluid so, the earth's (large scale average) surface is also, roughly, at right angles to the string.
In the animation below, the rate of rotation is exaggerated so that the difference in angle and the tiny eccentricity of the earth's shape – both very tiny in practice – can be seen.
What happens if you spin so fast that the string points away from the axis of the earth? The next animation shows this unhappy (but unlikely) result.
Appendix: Film clips illustrating Newton's second law
The film clips below use a spring to accelerate a bowling ball. You can
tell whether the spring applies a force from whether it is stretched or not,
as in these photos. Use the step frame button on the film clips.
Space travel has made us blasé about motion in the skies. This may give us some flavour of the Mediaeval view: Christopher Marlowe (a contemporary and rival of Shakespeare) created Doctor Faustus
(perhaps based on the historical character Paracelsus) -- a
philosopher/scientist who sells his soul for knowledge. Here is an extract
from the play, in Act VI:
Faustus: I am resolv'd: Faustus shall
ne'er repent.
Come, Mephistophiles, let us dispute
again,
And argue of divine
astrology.
Tell me, are there many heavens above the
moon?
Are all celestial bodies but one
globe,
As is the substance of this centric
earth? Mephistopheles: As are
the elements, such are the spheres
Mutually folded in
each other's orb,
And,
Faustus,
All jointly move upon one
axletree
Whose terminine is termed the world's wide
pole;
Nor are the names of Saturn, Mars, or
Jupiter
Feign'd but are erring
stars. Faustus: But tell me, have they all one
motion, both situ et
tempore? Mephistopheles: All jointly
move from East to West in twenty-four hours upon the poles of the world;
but differ in their motion upon the poles of the
zodiac. Faustus:
Tush!
These slender trifles Wagner can
decide;
Hath Mephistophiles no greater
skill?
Who knows not the double motion of the
planets?
The first is finish'd in a natural
day;
The second thus: as Saturn in thirty years;
Jupiter in twelve; Mars in four; the Sun, Venus, and Mercury in a year;
the moon in twenty-eight days. Tush, these are freshmen's suppositions.
But tell me, hath every sphere a dominion or
intelligentia? Mephistopheles: Ay. Faustus:
How many heavens, or spheres, are
there? Mephistopheles: Nine:
the seven planets, the firmament, and the empyreal
heaven. Faustus: Well, resolve me in this
question: Why have we not conjunctions, oppositions, aspects, eclipses,
all at one time, but in some years we have more, in some
less? Mephistopheles: Per
inæqualem motum respectu totius*.
*On
account of their unequal motion in relation to the
whole Faustus: Well, I am answered.
Tell me who made the
world. Mephistopheles: I will
not.
Are we ready now for the Age of Enlightenment?
I cannot resist making the following observation. Someone who lived in Elizabethan England could have attended premières of three plays in which three of the greatest playwrights of the language each make a hero or anti-hero of the scholar/ philosopher/ magus: Marlowe's The Tragickal History of Doctor Faustus, Shakespeare's The Tempest and Jonson's The Alchemist.
Very different views, but with interesting common perspectives. And each with insights that have some direct relevance to our 'brave new world'.
Not to mention fabulous writing – the extract above doesn't doesn't do them justice.
Happy birthday,
theory of relativity!
As of June 2005,
relativity is 100 years old. Our contribution was Einstein Light:
relativity in brief... or in detail. It explains the key ideas in a
short multimedia presentation, which is supported by links to broader and
deeper explanations.