Borelli, Giovanni Alfonso
,
De motionibus naturalibus a gravitate pendentibus
,
1670
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augmentum molis glaciei non efficitur ab aſperſione,
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& miſtione corpuſculorum, & ſalium
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,
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ſed ab alia longè diuerſa cauſa phænomenon hoc de
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pendet. </
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Cap. 13. cau
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ſa rarefacti
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onis glaciei
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affertur.</
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<
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">Hoc Gaſſendus indicaſſe videtur, cùm ait, in glacie
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non paucas aeris particulas commiſceri, proptereą
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quòd videmus congelationem aquæ initium habere
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in eius ſummitate, quæ aerem contingit, & hinc po
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ſtea inferiùs propagari versùs fundum; & hinc ait
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pẽ-dere
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dere</
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, quòd glacies ſuper aquam innatat, cùm ſit aere
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impręgnata; à quo poſtea veriſimile eſt perſuaſum̨
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fuiſſe ampliari poſſe molem aquæ glaciatæ, & hoc
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conijcitur ex eius verbis, dum ait,
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cùm verum ſit
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aquã
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calefactam refrigeſcendo citiùs fortiuſque conglaciare,
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frigidam, ecquam aliam putemus cauſam, quàm quia facta
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maiore
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quadã
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partium aquæ laxitate, ipſe aer faciliùs ſub
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ingreditur, & vehementiùs ſtringit particulas aquæ, qui
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bus commiſcetur?
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<
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">Ex quibus Gaſſendi verbis elicitur, quòd ab aere
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deforis adueniente in actu congelationis aqua infle
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tur, & rarefiat. </
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PROP. CCLXXIII.
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Nec paritér augetur aquæ moles ànouo aere de foris adueni
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ente in actu congelationis eius, neque à directione, &
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tẽ-ſione
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ſione</
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anguillularum aquæ.
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<
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">SI hoc verum eſſet, cùm omninò prohibetur aeris
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ingreſſus intra aquam, non deberet in actu con
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gelationis rarefieri, & ampliari eius moles, vtcùm̨
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vas plumbeum, vel aureum aqua plenum, &
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