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.

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