Borelli, Giovanni Alfonso
,
De motionibus naturalibus a gravitate pendentibus
,
1670
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Ibidem.</
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Cap. 10. de
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æquitempo
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ranea natu
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rali veloci
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tate
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grauiũ
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PROP. CCIII.
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Modò noua demonſtratione noſtra oſtendemus, quòd in duo
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bus medijs fluidis inæqualitèr denſis, & reſistentibus
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velocitates eiuſdem corporis grauis poſſunt habere maio
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rem, eamdem, & minorem proportionem reciprocam,
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quam habent crasſities eorumdem fluidorum, ſi tamen
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graue in vtroque fluido deſcendat.
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">IN vaſe CF ſit fluidum M, cuius
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dẽſitas
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, craſſities,
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vel reſiſtentia ad diſtractionem erit certæ, ac de
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terminatæ menſuræ, ſit illa S, atque in vaſe CG po
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natur aliud fluidum N, cuius craſſities, & reſiſtentia
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R ſit maior, quàm S. præterea
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idem mobile A, quod in vtro
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que fluido M, & N deſcende
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re valeat, eodem tempore T
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percurrat ſpatium CD fluidi
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M, ſpatium verò CE alterius
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fluidi N. & quia vis motiuą
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eiuſdem mobilis A vnica eſt,
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& certi, ac determinati gra
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dus, propterea impetus, & ve
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locitas naturalis eiuſdem gra
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uis A ſemper eſt
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eadẽ
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, & eiuſ
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dem gradus, ſi omninò remo
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ueri poſſent impedimenta, quæ à medij reſiſtentią
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afferuntur,
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nulla alia de cauſa alteretur, varietur
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que velocitas eiuſdem grauis A in diuerſis fluidis M, </
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