An difríocht idir athruithe ar: "Dlí Boyle"

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''Italic text''[[Íomhá:Boyles Law animated.gif|thumb|Beochan ag taispeáint na hidirghaolmhaireachta idir brú (''p'') agus toirt (V) nuair atá mais agus teocht seasmhach.]] Tá '''Dlí Boyle''' nó '''Dlí Mariotte''', dá ngairtear '''Dlí Boyle-Mariott''' go minic, a ainmníodh i ndiaidh an fealsamh nádúrtha agus scríbhneoir diagachta Angla-Éireannach, [[Robert Boyle]] agus an luibheolaí agus fisiceoir Francach [[Edme Mariotte]], ar cheann de na dlíthe teirmidinimice arb é dlí an gháis idéalaigh iad. Baineann sé brú agus toirt an gháis idéalach ag teocht tairiseach. Tugann an Dlí seo le fios an méid seo a leanas; "Tá toirt maise gháis i gcomhreir inbhéartach leis an mbrú ar an ngás ag teocht sheasmhach."
 
Is éard is '''Dlí Boyle''' ann, ar a dtugtar '''Dlí Mariotte''' freisin, ná an gaol maidir le comhbhrú agus leathnú [[Gás|gáis]] ag teocht sheasmhach. Deirtear sa ghaol eimpíreach seo, a bheartaigh an fealsamh nádúrtha Angla-Éireannach agus scríbhneoir diagachta, [[Robert Boyle]] sa bhliain 1662, go n-athraíonn [[brú]] (''p'') cainníocht áirithe gáis go inbhéartach leis an [[toirt]] (V) ag teocht sheasmhach; i bhfocail eile, i bhfoirm chothromóide
Nuair a mhéadaítear an brú laghdaítear an toirt, i bhfocail eile, i bhfoirm chothromóide
{|
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| style="padding: 0.2em 0.4em;" | <math>p \propto \frac{1}{V}</math>
| style="padding: 0.2em 0.4em;" | Ta an brú i gcomhréir inbhéirteach leis an toirt
|-
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==Stair==
 
[[File:Boyles Law.svg|thumb|Graf de bhunsonraí Boyle]]
Thug [[Richard Towneley]] agus [[Henry Power]] an gaol seo idir brú agus toirt faoi deara den chéad uair sa 17ú haois.<ref>See:
* Henry Power, ''Experimental Philosophy, in Three Books'' … (London: Printed by T. Roycroft for John Martin and James Allestry, 1663), pp. 126–130. Available on-line at: [https://quod.lib.umich.edu/e/eebo/a55584.0001.001/155?page=root;size=125;view=text Early English Books Online]. On page 130, Power presents (not very clearly) the relation between the pressure and the volume of a given quantity of air: "That the measure of the Mercurial Standard, and Mercurial Complement, are measured onely by their perpendicular heights, over the Surface of the restagnant Quicksilver in the Vessel: But Ayr, the Ayr's Dilatation, and Ayr Dilated, by the Spaces they fill. So that here is now four Proportionals, and by any three given, you may strike out the fourth, by Conversion, Transposition, and Division of them. So that by these Analogies you may prognosticate the effects, which follow in all Mercurial Experiments, and predemonstrate them, by calculation, before the senses give an Experimental [eviction] thereof." In other words, if one knows the volume V<sub>1</sub> ("Ayr") of a given quantity of air at the pressure p<sub>1</sub> ("Mercurial standard", i.e., atmospheric pressure at a low altitude), then one can predict the volume V<sub>2</sub> ("Ayr dilated") of the same quantity of air at the pressure p<sub>2</sub> ("Mercurial complement", i.e., atmospheric pressure at a higher altitude) by means of a proportion (because p<sub>1</sub> V<sub>1</sub> = p<sub>2</sub> V<sub>2</sub>).