Guillaume Amontons

Infobox Scientist
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birth_date = August 31, 1663
birth_place = Paris, France
death_date = October 11, 1705
death_place = Paris
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nationality = French
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field = physics
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known_for = tribology
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Guillaume Amontons (August 31, 1663 - October 11, 1705) was a French scientific instrument inventor and physicist. He was one of the pioneers in tribology, apart from Leonardo da Vinci, John Theophilius Desanguliers, Leonard Euler and Charles-Augustin de Coulomb.

Life

Guillaume was born in Paris, France. His father was a lawyer from Normandy who had moved to the French capital. While still young, Guillaume lost his hearing, which may have motivated him to focus entirely on science. He never attended a university, but was able to study mathematics, the physical sciences, and celestial mechanics. He also spent time studying the skills of drawing, surveying, and architecture.

He died in Paris, France.

Work

He was supported in his research career by the government, and was employed in various public works projects.

cientific instruments

Among his contributions to scientific instrumentation were improvements to the barometer (1695), hygrometer (1687), and thermometer (1695), particularly for use of these instruments at sea. He also demonstrated an optical telegraph and proposed the use of his clepsydra [Amontons, G. (1695) "Remarques et expériences physiques sur la construction d'une nouvelle clepsydre", Paris.] (water clock) for keeping time on a ship at sea.

Thermodynamics

Amontons investigated the relationship between pressure and temperature in gases though he lacked accurate and precise thermometers. Though his results were at best semi-quantitative, he established that the pressure of a gas increases by roughly one-third between the temperatures of "cold" and the boiling point of water [- (1699) "Method of substituting the force of fire for horse and man power to move machines", "Histoire et Mémoires de l'Académie Royale des Sciences", "p."112] . This was a substantial step towards the subsequent gas laws and, in particular, Charles's law.

His work led him to speculate that a sufficient reduction in temperature would lead to the disappearance of pressure. Thus, he is the first researcher to discuss the concept of an absolute zero of temperature, a concept later extended and rationalised by William Thomson, 1st Baron Kelvin.

Friction

In 1699, Amontons published his rediscovery of the laws of friction first put forward by Leonardo da Vinci [- (1699) "Histoire de l'Académie Royale des Sciences avec les Mémoires de Mathématique et de Physique", "p."206] . Though they were received with some scepticism, the laws were verified by Charles-Augustin de Coulomb in 1781 [Bowden, F.P. & Tabor, D. (1950) "The Friction and Lubrication of Solids" "pp"1, 87-89] .

Amontons' Laws of Friction

Leonardo da Vinci (1452-1519)) can be named as the father of modern tribology as he studied an incredible manifold of tribological subtopics such as: friction, wear, bearing materials, plain bearings, lubrication systems, gears, screw-jacks, and rolling-element bearings. 150 years before Amontons' Laws of Friction were introduced, he had already recorded them in his manuscripts. Hidden or lost for centuries, Leonardo da Vinci's manuscripts were read in Spain a quarter of a millennium later.

Amontons' Laws of Friction were first recorded in books during the late 17th century.

There 3 laws of friction are: [ [http://depts.washington.edu/nanolab/ChemE554/Summaries%20ChemE%20554/Introduction%20Tribology.htm | Introduction to Tribology - Friction] ]
*1. The force of friction is directly proportional to the applied load. (Amontons 1st Law)
*2. The force of friction is independent of the apparent area of contact. (Amontons 2nd Law)
*3. Kinetic friction is independent of the sliding velocity. (Coulomb's Law)

NOTE: These 3 laws only apply to dry friction, in which the addition of a lubricant modifies the tribological properties signifiantly.

Explaining Friction

By looking at any surface on the microscopic level, one would find that it is never perfectly flat. There would exist many tiny bumps and craters, due to imperfections on the surface and the alignment of molecules. (The skin does not feel the bumps and craters because they are too small to be detected.) Considering a smooth stone on a smooth flat road, the two surfaces would be still in contact, but only at a few points (the bumps do fot fit exactly into the craters). Due to electrostatic forces of repulsion between the atoms(nuclei and nuclei)Fact|date=February 2008 of the stone and the road, the road will exert a force on the stone, and the stone will exert a force on the road (normal contact forces). The NET force exerted on the stone would be the NORMAL contact force.

If net external forces cause the stone to move to the RIGHT, the forces that the road exert on the stone would be slightly skewed to the LEFT, thus the net force will be pointing UP but LEFTWARD (tilted contact force). As the vertical component of the net force is the normal contact force, the extra horizontal leftward component of the force would therefore be the FRICTIONAL force.(Note: friction OPPOSES motion)

Amontons First Law Explained*

Suppose the stone had a greater mass (hence greater weight as g=constant). The stone would then:
*exert a greater force on the road (the increased load causes the separation distance of the nuclei to decrease, force of repulsion becomes stronger(inverse-square law) ), AND
*more of the atoms of the road and the stone would be in contact. Hence, when the stone is moved, a greater frictional force would be produced (more areas of contact means that more forces can be skewed, producing more horizontal components of the contact forces).

Amontons law applies to any 2 surfaces, regardless of their orientation. (e.g. pressing a brick against the ceiling, etc.)

NOTE: Applied load means the normal contact force acting on the stone. That is, if the stone is being pushed down harder while it was trying to move, the force acting on the ground increases, and hence the force of the ground acting on the stone (normal contact) increases. This means that more force is required to move the stone across the ground. (frictional force increase)

Amontons Second Law Explained*

What this law means is that if two "equal masses" made of "similar material" are resting on the "same surface" with DIFFERENT SURFACES AREAS OF CONTACT, they would require the SAME AMOUNT of FORCE to start moving (overcome static friction) and to move at constant speed⁺.

To put it in another way: considering 2 equal masses, and the area in contact in situation A is greater than in situation B. This only means that in situation A, the load is distributed across a greater area then in situation B. However, the applied load is still the same! Thus to move both masses, we would require the same amount of applied force to overcome friction. (Amontons First Law)

⁺To maintain constant speed, net force has to be 0N. Assuming no drag forces,

In summary

Through studies and experimental observations on the properties of friction, a relationship between frictional force and normal contact force was established:

,

where μ is the coefficient of friction and N is the normal contact force.

This is as predicted by Amontons' two laws, where F_fric depends only on the normal contact force (reaction pair of the applied load), and is independent of the surface area in contact.

However, exceptions to Amontons' Law have been observed in various nanometric scenarios. For example, when two surfaces get close enough such that molecular interactions and atomic forces come into play, the two surfaces are attracted together and form what was known as 'negative load'. [ [http://everything2.com/index.pl?node_id=1210188| Everything2.com(source may not be reliable)] ]

*requires verification by specialist

Honours

*Member, Académie des Sciences, (1690)
*The Amontons crater on the Moon is named after him.

ee also

*Friction
*Coefficient of friction

Notes

Bibliography

*"Asimov's Biographical Encyclopedia of Science and Technology", Isaac Asimov, Doubleday & Co., Inc., 1972, ISBN 0-385-17771-2.
*cite book | author=Cardwell, D.S.L. | title=From Watt to Clausius: The Rise of Thermodynamics in the Early Industrial Age | publisher=Heinemann | year=1971 | id=ISBN 0-435-54150-1, "pp"18-19
*Amontons also published numerous papers.

External links

* [http://galileo.rice.edu/Catalog/NewFiles/amontons.html The Galileo Project entry] on which this biography is partly based.
* [http://www.nndb.com/people/573/000097282/ Short biography] , NNDB page