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Gravitation
A
property of mutual attraction possessed by all bodies. The term
"gravity" is sometimes used synonymously. Gravitation is
one of four basic forces controlling the interactions of matter; the
others are the strong and weak nuclear forces and the
electromagnetic force. Attempts to unite these forces in one grand
unification theory have not yet been successful, nor have attempts
to detect the gravitational waves that relativity theory suggests
might be observed when the gravitational field of some very massive
object in the universe is perturbed.
The law of
gravitation, first formulated by Isaac Newton in 1684, states that
the gravitational attraction between two bodies is directly
proportional to the product of the masses of the two bodies and
inversely proportional to the square of the distance between them.
In algebraic form the law is stated
F=G
m1m2/r2
where
F is the gravitational force, m1 and m2 the masses of the two
bodies, d the distance between the bodies, and G the gravitational
constant. The value of this constant was first measured by the
British physicist Henry Cavendish in 1798 by means of the torsion
balance. The best modern value for this constant is 6.67 × 10-11 N
m2 kg-2. The force of gravitation between two spherical bodies, each
with a mass of 1 kilogram and with a distance of 1 metre between
their centres, is therefore 6.67 × 10-11 newtons. This is a very
small force; it is equal to the weight (at the Earth's surface) of
an object with a mass of about 0.007 micrograms (a microgram is one
millionth of a gram).
Effect of
Rotation
The
measured force of gravity on an object is not the same at all
locations on the surface of the Earth, principally because the Earth
is rotating. The measured, or apparent, weight of the object is the
force with which the object presses down on, for example, the pan of
a spring scale. This is equal to the reaction force with which the
pan presses upward on the object. Any object travelling at constant
speed in a circle is constantly accelerating towards the centre of
the circle. This centre-directed acceleration has to be sustained by
a centre-directed force, or centripetal force. In the case of the
object being weighed at the Earth's surface, the centripetal force
is the result of the fact that the upward supporting force from the
pan of the spring balance is slightly less than the object's weight.
Acceleration
Gravity is commonly measured in terms of the amount of
acceleration that the force gives to an object on the Earth. At the
equator the acceleration of gravity is 977.99 cm s-2 (centimetres
per second per second) (32 9/100 ft s-2 ) and at the poles it is
more than 983 cm s-2. The generally accepted international value for
the acceleration of gravity used in calculations is 980.665 cm s-2
(32 1/6 ft s-2). Thus, neglecting air resistance, any body falling
freely will increase its speed at the rate of 980.665 cm s-1 (32 1/6
ft s-1) during each second of its fall. The apparent absence of
gravitational attraction during spaceflight is known as zero gravity
or microgravity.
Gravitational
Forces
Because the moon has significantly less mass
than the earth, the weight of an object on its surface is only
one-sixth of its weight on the earth's surface. Since the earth and moon
pull in opposite directions, there is a point, 346,000 km (215,000
mi) from the earth, where the opposite gravitational forces cancel,
and the weight is zero.
Gravitational Lens
Astronomical phenomenon predicted by the
relativity theory of Albert Einstein. According to that theory,
objects in space that are sufficiently massive could act as a lens
for light coming from more distant objects in the same line of sight
with respect to observers on the Earth. If the configuration of
these objects was right, the lens effect could produce two or more
identical images of the more distant object. The first gravitational
lens was discovered in 1979 by a British astronomer, Dennis Walsh.
The lens is a giant elliptical galaxy, and it produces a double
image of a more distant quasar. A few other such phenomena have
since been observed, including the 1988 sighting of a possible
"Einstein ring" produced by a perfect alignment of nearer
and farther objects. Vast luminous arcs, or imperfect rings, have
also been observed.
Gravitational
Waves
Disturbances in space-time that are believed
to spread outwards at the speed of light from locations where masses
are being rapidly accelerated. Possible sources of such waves
include: violent supernova explosions, which are accompanied by the
collapse of stellar cores to form neutron stars or black holes;
interacting black holes; pulsars (rotating neutron stars); and
binary systems of neutron stars as their components coalesce and
die.
The
existence of gravitational waves is predicted by Albert Einstein's
general theory of relativity, but they have not yet been detected
directly. Indirect evidence for their existence has been found,
however. Gravitational waves would transport energy away from the
system in which the waves originate. Energy losses of the expected
order of magnitude have been observed in the "decay" of
the orbits of the two components of PSR 1913+16; this object
consists of two neutron stars that circle each other. Indeed, the
1993 Nobel Prize for Physics was awarded to Russell A. Hulse and
Joseph H. Taylor of Princeton University for this work and for the
discovery of binary pulsars.
More direct
observation of gravitational waves would give further and more
detailed confirmation of relativity and also lead to a new field of
astronomy in which new information may be gained about how stars
collapse, how black holes interact and how fast the universe is
expanding. But such detection is one of the most challenging
problems in present-day experimental physics. It depends on sensing
strains in space-extremely small changes in the distance between
distinct pieces of matter, caused by the waves. In most situations
the movements are larger if the overall distance is greater.
Theoretical analysis suggests that detectors need to be sensitive to
strains of the order of 10-21 to 10-22. This ratio is equivalent to
a change of approximately the diameter of an atom, or less, in the
distance of the Earth from the Sun. This change can occur over
timescales that range from milliseconds to hours, depending on the
type of source to be detected. The design of any detector depends on
the timescale of the signals it is to search for.
A number of
experiments for the detection of gravitational waves are being
developed. Some are based on sensing the oscillations induced by
gravitational waves in aluminium bars weighing several tonnes and
cooled to temperatures below 1 kelvin. This technique was pioneered
by Joseph Weber of the University of Maryland in the late 1960s.
However, the most promising ways to make very sensitive detectors
are to hang masses of a few tens of kilograms on pendulums several
kilometres apart on Earth and use laser interferometry to sense
their movements, or to make measurements between drag-free
artificial satellites separated by several million kilometres,
placed in orbits sufficiently high to be free of the effects of the
Earth's atmosphere. In these cases the two reference objects are
positioned to form two paths at an angle to each other and changes
in the relative lengths of the two arms are sensed.
In the United States
two detector systems, each with arms 4 km (2.5 mi) long, are being
built as part of the LIGO project; the first is in Washington state,
the second in Louisiana. In Europe the Italian/French VIRGO
interferometer, with arms 3 km (1.9 mi) long, is being built near
Pisa in northern Italy. GEO 600, a shorter interferometer with arms
of 600 m (about 2,000 ft) and of advanced technological design, is
being built near Hanover in north-western Germany by German and
British research groups in collaboration. A detector of somewhat
shorter arm length is being constructed in Japan. It is expected
that these detectors will be operational towards the end of the
century and that collaborative observations will allow the first
direct detection of gravitational waves to be made soon thereafter.
Plans are also being developed for long-baseline detectors in
Australia and Japan.
Because of
fluctuating local gravitational effects, Earth-based gravitational
wave detectors will be restricted to looking for signals above a few
hertz (1 hertz, or Hz, is one cycle per second). This allows
searches for stellar collapses, the coalescence of neutron stars in
binary systems, and signals from pulsars, either isolated or in
binary systems. However, there is a wealth of sources at much lower
frequency; these range from compact binary star systems to massive
black holes, interacting with each other or with ordinary matter,
and it is very important that the low-frequency regime should be
explored. In order to make this possible LISA, a space system using
satellites and a laser interferometer detector with arm lengths of 5
million km (3 million mi), is being considered by the European Space
Agency for launch around 2015. |