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According to the law of universal gravitation, the attractive force between two bodies is proportional to the product of their masses and inversely proportional to the square of the distance between them.

The constant of proportionality is called , the gravitational constant, the universal gravitational constant, or Newton's constant. The gravitational constant is a fundamental physical constant which appears in Newton's law of universal gravitation and in Einstein's theory of general relativity.

In SI units, the 2002 CODATA recommended value of the gravitational constant is

= (6.6742 ± 0.0010) × 10−11 N m2 kg-2 = (6.6742 ± 0.0010) × 10−11 m3 kg-1 s-2

Another authoritative estimate is given by the International Astronomical Union (see Standish, 1995).

The gravitational force is relatively weak. As an example, two SUVs, each with a mass of 3000 kilograms and placed with their centers of gravity 3 metreFor other uses of "metre" and "meter", see Metre (disambiguation). The metre is the basic unit of length in the International System of Units (SI: Systeme International d'Unites). It is defined as the length of the path travelled by light in absolute vacus apart, will attract each other with a force of about 67 micronewtons. This force is approximately equal to the weightFor the 1994 album by the group Rollins Band, see Weight (album). Weight is the force exerted upon an object by virtue of its position in a gravitational field. In a constant gravitational field, such as the Earth's, this force is proportional to the obje of a large grain of sand.

1 Measurement of the gravitational constant

was first implicitly measured by Henry CavendishHenry Cavendish ( October 10, 1731 February 24, 1810) was a British scientist. The grandson of the Second Duke of Devonshire, he attended Cambridge from 1749 to 1753 but left without taking a degree. He inherited a large fortune which enabled him to pursu (Philosophical Transactions 1798Events February- October Irish Rebellion of 1798 April 7 The Mississippi Territory is organized from territory ceded by Georgia and South Carolina and is later twice expanded to include disputed territory claimed by both the U. and Spain April 26 France a). He used a horizontal torsion beam with lead balls whose inertia (in relation to the torsion constant) he could tell by timing the beam's oscillation. Their faint attraction to other balls placed alongside the beam was detectable by the deflection it caused. However, it is worth mentioning that the aim of Cavendish was not to measure the gravitational constant but rather to measure the mass of the Earth through the precise knowledge of the gravitational interaction.

The accuracy of the measured value of has increased only modestly since the original experiment of Cavendish.

is quite difficult to measure, as gravity is much weaker than other fundamental forces, and an experimental apparatus cannot be separated from the gravitational influence of other bodies. Furthermore, gravity has no established relation to other fundamental forces, so it does not appear possible to measure it indirectly. A recent review (Gillies, 1997) shows that published values of have varied rather broadly, and some recent measurements of high precision are, in fact, mutually exclusive.

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