Borelli, Giovanni Alfonso
,
De motionibus naturalibus a gravitate pendentibus
,
1670
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s.001970
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372
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ctu excurrent versùs parietem, cui ſuis villis adhæ
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rebunt, ex qua adhæſione momentum eius grauitatis
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denuò imminuetur, & ideò renouabitur cauſa vlte
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rioris eius eleuationis à compreſſione laterali aquæ
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ſuo momento non imminuto comprimentis, & hinc
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ſequitur continuatio prædicti aſcenſus rotando, &
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adhærendo parieti, quouſque efficiatur æquilibrium
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cum prædicta aqua collaterali liberè premente. </
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s.001971
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Cap. 8. cur
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exiguæ aquę
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guttæ ſupra
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libellã
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aquæ
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aſcendunt.</
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">Et hìc notandum eſt, quòd vis prædictæ adhæſio
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nis aquæ non eſt æqualis in omnibus partibus prædi
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ctæ montuoſitatis, ſed omnium maxima eſt illa, quæ
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retinet mini nas aquæ particulas immediatè
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abbr
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parietẽ
">parietem</
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tangentes, quæ non ſecùs, ac ſi eſſent claui, vel vn
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cini tenaci nexu ibidem inſinuantur, & minima erit
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vis illa, quæ retinet remotiſſimas, & poſtremas par
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ticulas dictæ montuoſitatis aquæ, aliarum verò par
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tium illæ, quæ parieti viciniores ſunt, maiori tena
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citate ſuſpendentur, quam aliæ partes aquæ a præ
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dicto pariete magis remotæ. </
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<
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id
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s.001973
">Et hinc oritur decliuitas
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illa montis aquæ pendentis. </
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Declinitas
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prædicti a
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quei montis
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pendet ex in
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æqualitate
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virtutis mon
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tium.</
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s.001975
">Hic iam reſoluere poſſumus aliud problema val
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dè agitatum, vnde nimirùm proueniat, quòd aquą
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in fiſtulis tenuiſſimis vtrinque apertis ſursùm aſcen
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dat. </
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<
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id
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s.001976
">Et primo loco phænomena, quæ in hac opera
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tione obſeruantur, recenſeri debent. </
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Proponun
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tur obſerua
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tiones
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aſcẽ-ſus
">aſcen
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ſus</
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aquæ in
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fiſula gra
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ciliſſimis.</
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<
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id
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">Poſtquam graciliſſima fiſtula EH contingit aquæ
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ſuperficiẽ
">ſuperficiem</
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RV in H videmus, quòd ſubito aqua ſen
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ſim aſcendere incipit ad notabilem altitudinem HK
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eiuſdem cauitatis ſupra aquæ ſubiectæ libellam RV. </
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