Borelli, Giovanni Alfonso
,
De motionibus naturalibus a gravitate pendentibus
,
1670
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Cap. 8. cur
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exiguæ aquæ
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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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<
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">SI poſtea conſideremus
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abbr
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incongruẽtiam
">incongruentiam</
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pororum,
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lb
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patet verum non eſſe aduerſariorum aſſertum
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abbr
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cũ
">cum</
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aiunt, ideò ab aere impediri motiones partium aquę,
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quia orificia pororum aeris ſtrictiora ſunt,
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expan
abbr
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quã
">quam</
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vt per
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ea aquæ particulæ ingredi, & fluere poſſint, nam hinc
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inferre liceret neque aqueas particulas per
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abbr
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ipsãmet
">ipsammet</
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aquam cieri, & excurrere poſſe; facilè enim percipi
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tur, quòd in aqua poroſitates non poſſunt eſſe adeò
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amplæ, vt per eas intromitti poſſint particulæ eiuſ
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demmet aquæ, ſed debent eſſe multò minores, ſicuti
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interſtitia, quæ in aceruo granorum tritici, vel milij
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intercipiuntur, ſemper minora ſunt,
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quã
">quam</
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grana eiuſ
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dem tritici, vel milij, aliàs facta acerui concuſſione
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ſe mutuò magis conſtringerent amplexarentur quę
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granula prædicta, intromiſſis nempè granulis in eiſ
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dem amplis interſtitijs. </
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<
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">Hinc ſequitur vt æquè diffi
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cilè aquæ particulæ per ipſam aquam moueri, agita
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rique poſſint, quàm per aerem, quia nempè æquè in
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commodus eſt progreſſus aquæ per aquam, ac per ae
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rem; ſi verum eſt requiri poroſitates in fluido tantæ
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amplitudinis vt capaces ſint particularum aquæ ad
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hoc vt per prædictum fluidum moueri queant. </
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<
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s.001866
">cùm
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que aquæ anguſtæ poroſitates non impediant motum
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particularum aquæ per ipſam aquam. </
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<
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s.001867
">ergò pariter
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anguſtia pororum aeris non impediet motum
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partiũ
">partium</
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aquæ per aerem. </
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