Borelli, Giovanni Alfonso, De motionibus naturalibus a gravitate pendentibus, 1670
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              fluxibilitate particulas calcis
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              vinculaque
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                <expan abbr="relaxãdo">relaxando</expan>
              , apertis oſtiolis egreſſus concedatur igneis
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              illis corpuſculis, quæ poſtea expreſſa ab excedenti
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              aquæ pondere velociori motu ſursùm per
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                dunt</expan>
              , proindeque in tranſitu bullularum ignearum̨
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              aquæ partes laterales celeriùs, & vehementiùs agi­
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              tantur. </s>
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              Cap, 7. de
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              natura flui­
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              ditatis.
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              PROP. CLIV.
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              Idipſum verificatur in diſſolutione metallorum
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              ab aqua forti.
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              <s id="s.001692">IDipſum eadem ferè ratione producit aqua fortis,
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              vel regia in metallis, dum enim intra illius poro­
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              ſitates vi ponderis eius inſinuatur, ſalibus quibus a­
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              qua fortis referta eſt, veluti talis, ac ſcalpris abradit
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              ſolidas aliquas metalli particulas, ſimulque relaxat
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              oſtiola, egreſſumque concedit materiæ igneæ ibidem
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                <expan abbr="contẽtæ">contentæ</expan>
              , quæ expreſſa ab inſigni grauitate aquæ for­
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              tis velociſſimo motu per eamdem
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              ſursùm
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                dit</expan>
              incluſa in ampullis exiguis, & copioſiſſimis, quæ
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              ebullitionem feruentem producunt, vnà cum ingenti
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              aquæ agitatione; quæ omnia immeritò ab inteſtiną
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              partium aquæ fortis agitatione quiſquam effici cen­
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              ſeret, cùm adſit neceſſaria, & euidentiſſima cauſą
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              nempè ſimplex grauitas aquæ fortis, quæ eſt impoſ­
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              ſibile vt intra poroſitates inanes, aut à leuiori cor­
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              pore oppletas, non inſinuetur, & proinde in eius
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              motu impetum non concipiat, cuius virtute exiguæ </s>
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