Bernoulli, Daniel
,
Hydrodynamica, sive De viribus et motibus fluidorum commentarii
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mina in inſtrumentis hydraulicis raro occurrere ſolent, & </
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<
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">fingamus ſuperfi-
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ciem aquæ per centeſimam partem deſcendiſſe tantum totius altitudinis ini-
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tialis (deſcendiſſe autem aliquantulum aſſumo, quia à primo initio motus
<
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aquæ nullus ineſſe poteſt, nedum tantus, ut aqua effluens ad totam alti-
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tudinem aſcendere motu ſuo poſſit) hæ poſitiones faciunt m = 16n & </
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xml:space
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">mm =
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256nn, atque x = {99/100}a, unde prodit
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z = {128/127}({99/100} - ({99/100})
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)a = {92/100}a,
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quæ quidem aliquantulum differt à quantitate x, ſeu {99/100}a, ſed tamen non
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multum admodum, fitque differentia multo minor, cum minus eſt foramen,
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& </
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<
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xml:space
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">paullo magis deſcendit ſuperficies aquæ. </
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<
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">Igitur differt hæc Theoria à vul-
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gari potiſſimum circa fluxus initium, quo minor eſt motus, quam ſtatutum
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fuit: </
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<
s
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xml:space
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">è contrario circa fluxus finem majori velocitate aqua ejicitur, quam ſe-
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cundum principia ſolita deberet.</
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<
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">Hactenus conſideravimus motum aquæ à propria ſua gravitate
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ortum; </
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<
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">ponamus nunc vi aliena aquam ejectam fuiſſe præter vim gravitatis,
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talemque aquæ effluenti communicatam fuiſſe velocitatem, qua ad altitudi-
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nem multo majorem aſcendere poſſit, quam ſi ſola aquæ gravitas motum
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produxiſſet; </
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<
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">dein ſubito vim illam alienam evaneſcere, & </
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<
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qui; </
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">Id autem ſi fiat, experientia docet citiſſime aquæ velocitatem decreſce-
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re & </
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<
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">mox talem eſſe, ut notabililer non ſuperet velocitatem eam, quæ ex
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ſola aquæ gravitate oritura fuiſſet. </
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<
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xml:space
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">Ita videmus fieri aliquando in fontibus
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ſalientibus (de cujus rei cauſa vera atque menſura alibi dicam) ut aquæ ad
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triplam vel quadruplam majoremve altitudinem aſſiliat, quam eſt ordinaria;
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</
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<
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">quod cum ita contingit, ſaltus iſte protinus ceſſat ſolitamque altitudinem,
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quantum id ſenſibus percipi poteſt, non excedit: </
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<
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foraminibus non valde magnis perforatis; </
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<
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">nam cum foramen eſt ali-
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quanto majus, non ita cito decreſcit aquæ ſaltus. </
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<
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">Jam itaque examinabi-
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mus, quousque theoria cum iſtis phænomenis conveniat, accuratasque
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menſuras eorum, quales inde ſequuntur, ſubjungemus. </
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<
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xml:space
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">Ut vero rem ge-
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neraliter proſequamur, ponemus rurſus amplitudinem cylindri ad amplitu-
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dinem foraminis ut m ad n: </
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<
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xml:space
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">aquam ea explodi velocitate qua aſſurgere poſſit
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ad altitudinem a, eoque ipſo temporis puncto altitudinem aquæ ſupra </
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