Borelli, Giovanni Alfonso
,
De motionibus naturalibus a gravitate pendentibus
,
1670
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bere deſcenſum, vel aſcenſum in aqua, ſed ſolum
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modò tarditatem afferret, non autem quietem abſo
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lutam, vt fatentur Ghetaldus, Steuinus, & alij. </
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<
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minutiſſima grana terrea, ſalium, metallorum, & non
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minùs particulæ minimæ corporum leuiorum ligni,
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aeris, &c. </
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perficiem reſpectu puſillæ grauitatis eorum non ta
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men poſſent omninò quieſcere in medio aquæ, ſed
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tiſſimo</
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motu aſcenderent, vel deſcenderent, vt exigit
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exceſſus, vel defectus grauitatis ſpecificæ corpuſcu
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lorum demerſorum à grauitate fluidi aquei; ſed hoc
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eſt falſum, metalla enim, ſales, & aer in minutiſſimą
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granula redacta immobilitèr in medio aquę
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,
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& ibidem perſeuerant, igitur falfum eſt aquam gluti
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ne omnino priuari, & nil prorsùs penetrationi reſiſte
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re; erit igitur aliquantiſper aqua glutinoſa,
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ſaltem aliquam puſillam; & ſuperficialem viſcoſita
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tem. </
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æquilibratæ atque ſuſtineantur exiguam compreſſio
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nem creant, & proindè machinulæ ſuperficiales par
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ticularum aquæ ſubiectæ non poſſunt valde diſtrahi,
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vel conſtringi, & ſic minimam vim reſilientem exer
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cere poſſunt. </
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Cap. 7. dę
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natura flui
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ditatis.</
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ambiuntur, ergo aqua non minùs quàm aer condenſa
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ri deberet quod repugnat experientiæ. </
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<
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quòd prædicta lanugo valdè exigua eſt reſpectu in
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ternæ ſoliditatis cuiuſlibet globuli aquei, & ſic noņ
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negatur quòd aliquantiſper aqua condenſari, conſti-</
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