When the pressure on a sample of a dry gas is held constant, the
This directly proportional relationship can be written as: V ∝ T displaystyle Vpropto T or V T = k , displaystyle frac V T =k, where: V is the volume of the gas, T is the temperature of the gas (measured in kelvins), k is a constant. This law describes how a gas expands as the temperature increases; conversely, a decrease in temperature will lead to a decrease in volume. For comparing the same substance under two different sets of conditions, the law can be written as: V 1 T 1 = V 2 T 2 or V 2 V 1 = T 2 T 1 or V 1 T 2 = V 2 T 1 . displaystyle frac V_ 1 T_ 1 = frac V_ 2 T_ 2 qquad text or qquad frac V_ 2 V_ 1 = frac T_ 2 T_ 1 qquad text or qquad V_ 1 T_ 2 =V_ 2 T_ 1 . The equation shows that, as absolute temperature increases, the volume of the gas also increases in proportion. Contents 1 Discovery and naming of the law 2 Relation to absolute zero 3 Relation to kinetic theory 4 See also 5 References 6 Further reading 7 External links Discovery and naming of the law[edit]
The law was named after scientist Jacques Charles, who formulated the
original law in his unpublished work from the 1780s.
In two of a series of four essays presented between 2 and 30 October
1801,[2]
V 100 − V 0 = k V 0 displaystyle V_ 100 -V_ 0 =kV_ 0 , where V100 is the volume occupied by a given sample of gas at 100 °C; V0 is the volume occupied by the same sample of gas at 0 °C; and k is a constant which is the same for all gases at constant pressure. This equation does not contain the temperature and so has nothing to do with what became known as Charles' Law. Gay-Lussac's value for k (1⁄2.6666), was identical to Dalton's earlier value for vapours and remarkably close to the present-day value of 1⁄2.7315. Gay-Lussac gave credit for this equation to unpublished statements by his fellow Republican citizen J. Charles in 1787. In the absence of a firm record, the gas law relating volume to temperature cannot be named after Charles. Dalton's measurements had much more scope regarding temperature than Gay-Lussac, not only measuring the volume at the fixed points of water, but also at two intermediate points. Unaware of the inaccuracies of mercury thermometers at the time, which were divided into equal portions between the fixed points, Dalton, after concluding in Essay II that in the case of vapours, “any elastic fluid expands nearly in a uniform manner into 1370 or 1380 parts by 180 degrees (Fahrenheit) of heat”, was unable to confirm it for gases. Relation to absolute zero[edit] Charles' law appears to imply that the volume of a gas will descend to zero at a certain temperature (−266.66 °C according to Gay-Lussac's figures) or −273.15 °C. Gay-Lussac was clear in his description that the law was not applicable at low temperatures: but I may mention that this last conclusion cannot be true except so long as the compressed vapours remain entirely in the elastic state; and this requires that their temperature shall be sufficiently elevated to enable them to resist the pressure which tends to make them assume the liquid state.[3] At absolute zero temperature the gas possesses zero amount of energy and hence the molecules restrict motion. Gay-Lussac had no experience of liquid air (first prepared in 1877), although he appears to believe (as did Dalton) that the "permanent gases" such as air and hydrogen could be liquified. Gay-Lussac had also worked with the vapours of volatile liquids in demonstrating Charles' law, and was aware that the law does not apply just above the boiling point of the liquid: I may however remark that when the temperature of the ether is only a little above its boiling point, its condensation is a little more rapid than that of atmospheric air. This fact is related to a phenomenon which is exhibited by a great many bodies when passing from the liquid to the solid state, but which is no longer sensible at temperatures a few degrees above that at which the transition occurs.[3] The first mention of a temperature at which the volume of a gas might descend to zero was by William Thomson (later known as Lord Kelvin) in 1848:[7] This is what we might anticipate, when we reflect that infinite cold must correspond to a finite number of degrees of the air-thermometer below zero; since if we push the strict principle of graduation, stated above, sufficiently far, we should arrive at a point corresponding to the volume of air being reduced to nothing, which would be marked as −273° of the scale (−100/.366, if .366 be the coefficient of expansion); and therefore −273° of the air-thermometer is a point which cannot be reached at any finite temperature, however low. However, the "absolute zero" on the
The volume of a fixed mass of dry gas increases or decreases by 1⁄273 times the volume at 0 °C for every 1 °C rise or fall in temperature. Thus: V T = V 0 + ( 1 273 × V 0 ) × T displaystyle V_ T =V_ 0 +( tfrac 1 273 times V_ 0 )times T V T = V 0 ( 1 + T 273 ) displaystyle V_ T =V_ 0 (1+ tfrac T 273 ) where VT is the volume of gas at temperature T, V0 is the volume at 0 °C. Relation to kinetic theory[edit] The kinetic theory of gases relates the macroscopic properties of gases, such as pressure and volume, to the microscopic properties of the molecules which make up the gas, particularly the mass and speed of the molecules. In order to derive Charles' law from kinetic theory, it is necessary to have a microscopic definition of temperature: this can be conveniently taken as the temperature being proportional to the average kinetic energy of the gas molecules, Ek: T ∝ E k ¯ . displaystyle Tpropto bar E_ rm k ., Under this definition, the demonstration of Charles' law is almost trivial. The kinetic theory equivalent of the ideal gas law relates PV to the average kinetic energy: P V = 2 3 N E k ¯ displaystyle PV= frac 2 3 N bar E_ rm k , See also[edit] Boyle's law Combined gas law Gay-Lussac's law Avogadro's law Ideal gas law Hand boiler References[edit] ^ Fullick, P. (1994), Physics, Heinemann, pp. 141–42, ISBN 0-435-57078-1 . ^ J. Dalton (1802), "Essay II. On the force of steam or vapour from water and various other liquids, both in vacuum and in air" and Essay IV. "On the expansion of elastic fluids by heat," Memoirs of the Literary and Philosophical Society of Manchester, vol. 8, pt. 2, pages 550–574 and pages 595–602. ^ a b c Gay-Lussac, J. L. (1802), "Recherches sur la dilatation des gaz et des vapeurs" [Researches on the expansion of gases and vapors], Annales de chimie, 43: 137–175 . English translation (extract). On page 157, Gay-Lussac mentions the unpublished findings of Charles: "Avant d'aller plus loin, je dois prévenir que quoique j'eusse reconnu un grand nombre de fois que les gaz oxigène, azote, hydrogène et acide carbonique, et l'air atmosphérique se dilatent également depuis 0° jusqu'a 80°, le cit. Charles avait remarqué depuis 15 ans la même propriété dans ces gaz ; mais n'avant jamais publié ses résultats, c'est par le plus grand hasard que je les ai connus." (Before going further, I should inform [you] that although I had recognized many times that the gases oxygen, nitrogen, hydrogen, and carbonic acid [i.e., carbon dioxide], and atmospheric air also expand from 0° to 80°, citizen Charles had noticed 15 years ago the same property in these gases; but having never published his results, it is by the merest chance that I knew of them.) ^ See: Amontons, G. (presented 1699, published 1732) "Moyens de substituer commodément l'action du feu à la force des hommes et des chevaux pour mouvoir les machines" (Ways to conveniently substitute the action of fire for the force of men and horses in order to power machines), Mémoires de l’Académie des sciences de Paris (presented 1699, published 1732), 112–126; see especially pages 113–117. Amontons, G. (presented 1702, published 1743) "Discours sur quelques propriétés de l'Air, & le moyen d'en connoître la température dans tous les climats de la Terre" (Discourse on some properties of air and on the means of knowing the temperature in all climates of the Earth), Mémoires de l’Académie des sciences de Paris, 155–174. Review of Amontons' findings: "Sur une nouvelle proprieté de l'air, et une nouvelle construction de Thermométre" (On a new property of the air and a new construction of thermometer), Histoire de l'Academie royale des sciences, 1–8 (submitted: 1702 ; published: 1743). ^ Englishman
^ Gay-Lussac (1802), from page 166: "Si l'on divise l'augmentation totale de volume par le nombre de degrés qui l'ont produite ou par 80, on trouvera, en faisant le volume à la température 0 égal à l'unité, que l'augmentation de volume pour chaque degré est de 1 / 223.33 ou bien de 1 / 266.66 pour chaque degré du thermomètre centrigrade." If one divides the total increase in volume by the number of degrees that produce it or by 80, one will find, by making the volume at the temperature 0 equal to unity (1), that the increase in volume for each degree is 1 / 223.33 or 1 / 266.66 for each degree of the centigrade thermometer. From page 174: " … elle nous porte, par conséquent, à conclure que tous les gaz et toutes les vapeurs se dilatent également par les mêmes degrés de chaleur." … it leads us, consequently, to conclude that all gases and all vapors expand equally [when subjected to] the same degrees of heat. ^ Thomson, William (1848), "On an Absolute Thermometric Scale founded on Carnot's Theory of the Motive Power of Heat, and calculated from Regnault's Observations", Philosophical Magazine: 100–6 . ^ Thomson, William (1852), "On the Dynamical Theory of Heat, with numerical results deduced from Mr Joule's equivalent of a Thermal Unit, and M. Regnault's Observations on Steam", Philosophical Magazine, 4 . Extract. Further reading[edit] Krönig, A. (1856), "Grundzüge einer Theorie der Gase", Annalen der
Physik, 99: 315–22, Bibcode:1856AnP...175..315K,
doi:10.1002/andp.18561751008 . Facsimile at the Bibliothèque
nationale de
External links[edit] The Wikibook School Science has a page on the topic of: Making Charles' law tubes
v t e Diving medicine, physiology, physics and environment Diving medicine Injuries and disorders Pressure Oxygen Freediving blackout Hyperoxia Hypoxia (medical) Oxygen toxicity Inert gases Atrial septal defect Avascular necrosis Decompression sickness Dysbaric osteonecrosis High-pressure nervous syndrome Hydrogen narcosis Isobaric counterdiffusion Nitrogen narcosis Taravana Uncontrolled decompression Carbon dioxide Hypercapnia Hypocapnia Aerosinusitis Air embolism Alternobaric vertigo Barodontalgia Barostriction Barotrauma Compression arthralgia Decompression illness Dental barotrauma Dysbarism Ear clearing Frenzel maneuver Valsalva maneuver Immersion Asphyxia Drowning Hypothermia Immersion diuresis Instinctive drowning response Laryngospasm Salt water aspiration syndrome Swimming-induced pulmonary edema List of signs and symptoms of diving disorders Cramps Diving disorders Motion sickness Surfer's ear Treatments Diving chamber Diving medicine Hyperbaric medicine Hyperbaric treatment schedules In-water recompression Oxygen therapy Fitness to dive Diving physiology Artificial gills (human)
Blood–air barrier
Blood shift
Breathing
Circulatory system
CO₂ retention
Cold shock response
Dead space (physiology)
Decompression (diving)
Decompression theory
Diving reflex
Diving physics Ambient pressure
Amontons' law
Anti-fog
Archimedes' principle
Atmospheric pressure
Boyle's law
Diving environment Algal bloom Breaking wave Ocean current Current (stream) Ekman transport Halocline List of diving hazards and precautions Longshore drift Rip current Stratification Surf Surge (wave action) Thermocline Tides Turbidity Undertow (water waves) Upwelling Researchers in diving medicine and physiology Arthur J. Bachrach Albert R. Behnke Paul Bert George F. Bond Robert Boyle Albert A. Bühlmann John R Clarke William Paul Fife John Scott Haldane Robert William Hamilton Jr. Leonard Erskine Hill Brian Andrew Hills Felix Hoppe-Seyler Christian J. Lambertsen Simon Mitchell Charles Momsen John Rawlins R.N. Charles Wesley Shilling Edward D. Thalmann Jules Triger Diving medical research organisations Aerospace Medical Association
Categories: Diving medicine Underwater diving physiology Underwater diving physics Physical oceanography |