Bernoulli, Daniel
,
Hydrodynamica, sive De viribus et motibus fluidorum commentarii
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SECTIO DUODECIMA.
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<
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<
s
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<
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">74.) </
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<
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">per cujus foramen o transfluere ponantur
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">Fig. 74.</
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aquæ velocitate uniformi & </
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<
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<
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">ducatur
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S N & </
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<
s
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">fingatur vas infinite amplum N M Q Paquis plenum usque in N P, ex
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quo canalis aquas ſuas perpetuo & </
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<
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">æquabiliter hauriat: </
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<
s
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">hæc ideo ſic fingo, ut
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cauſa adſit ſeu vis propellens uniformis, quæ aquas data velocitate propellat
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ſeu fluxum aquarum conſervet æquabilem: </
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<
s
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">Et ſine hac hypothef
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i problema
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noſtrum foret indeterminatum, quia velocitas eadem in eodem canali infini-
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tis modis ad temporis punctum generari poteſt & </
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<
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">propterea, ut habeatur
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menſura cauſæ aquas propellentis, fingenda eſt uniformitas in motu aquarum.</
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<
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<
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<
s
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">Fuerit nunc aquarum preſſio definienda in C F (aut c f): </
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<
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">huncque in
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finem putabimus rurſus abrumpi canalem in C E (aut c e) ſectione ad cana-
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lem perpendiculari examinaturi, quamnam accelerationem retardationemve
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guttula C E G F (vel c e g f) poſt primum rupturæ momentum receptura ſit:
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</
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<
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">quâ de cauſa generaliter motum momentaneum per vas decurtatum N M E C A
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Q P (vel N M c e A Q P) definiendum habemus. </
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<
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">Sitigitur velocitas guttulæ in-
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finite parvæ CEGF (ſeu c e g f) ipſo decurtationis puncto = v: </
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<
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= dx: </
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<
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">erit vis viva aquæ in vaſe decurtato motæ proportionalis quantitati
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v v, eamque proinde faciemus = α v v, intelligendo per litteram a quantita-
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tem quamcunque conſtantem, quæ pendet ab amplitudinibus canalis abrupti; </
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præciſa autem ejus determinatio hic non requiritur. </
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<
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in vaſe ficto N M QP negligi ob infinitam ejus amplitudinem: </
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<
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vel infinitæ non eſſet amplitudinis inde in calculo oritura fuiſſet variatio. </
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bemus jam incrementum vis vivæ aquæ in vaſe decurtato motæ = 2avdv, cui
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ſi addatur vis viva ſimul genita in guttula ejecta, oritur 2avdv + vvdx, quod
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eſt incrementum vis vivæ totale, debitum deſcenſui actuali guttulæ dx per alti-
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tudinem verticalem aquæ ſupra punctum C (vel c,) quam deſignabimus per a: </
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hinc igitur iſtud incrementum vis vivæ totale faciendum eſt æquale adx, ſic
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ut ſit
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2avdv + vvdx = adx vel
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{vdv/dx} = {a - vv/2a}.</
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<
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<
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quæ debeatur altitudini b, invenietur preſſionem aquæ in C F (aut cf) </
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