Borelli, Giovanni Alfonso, De motionibus naturalibus a gravitate pendentibus, 1670

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              Cap. 7. dę
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              natura flui­
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              ditatis.
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              <s id="s.001683">Prætereà quia experientia conſtat fluidi partes
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              glutine aliquo necti interſe debere, vt poſtea fusè
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              declarabitur, atque vis, & energia prædicti glutinis
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              ſit certi ac determinati gradus, huic verò contrapo­
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              nitur energia grauitatis, & velocitatis, quæ ſemper
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              magis, ac magis imminui poteſt, prout moles eius
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              ſubdiuiditur, hinc fit vt tandem ad eam exiguitatem
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              vis grauitatis, & impetus redigatur, vt æquari præ­
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              cisè poſſit energiæ glutinis ipſius fluidi, proindeque
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              vna alteri præualere nequeat, vnde æquatis viribus,
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              factoque æquilibrio neceſſariò particulæ illæ graues
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              in ipſo fluido innatantes in eodem ſitu quieſcere de­
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              bent. </s>
              <s id="s.001684">Hac ratione fieri poteſt, vt minimę ſalis parti­
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              culæ per aquam diſperſæ, & innatantes æquilibrari,
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              & quieſcere in ipſa aqua poſſint, proindeque aquą
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              ſemper ſalſedinem retinere valet. </s>
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              PROP. CLIII.
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              Vehementisſima aquæ ebullitio, quæ in diſſolutione calcis
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              apparet, pendet non ab inteſtino motu aquæ, ſed ab
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              eius grauitate diſſoluente, & exprimente igneas
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              particulas, quæ in calce contine­
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              bantur.
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            <p type="main">
              <s id="s.001687">IN calce poſtea intra
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              demerſa alia noua cau­
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              ſa feruoris oritur, quia in exiguis calcinati ſaxi
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              poroſitatibus, in eiuſque anfractibus includuntur in­
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              numeræ particulæ ignis ibidem inſinuatæ à
                <expan abbr="feruẽtiſ-ſimo">feruentiſ­
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                ſimo</expan>
              ardore fornacis, cùmque aqua ſuo pondere, & </s>
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