Casati, Paolo, Terra machinis mota : dissertationes geometricae, mechanicae physicae hydrostaticae

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            <p type="main">
              <s>
                <pb xlink:href="018/01/163.jpg" pagenum="149"/>
              cut ſi aqua implens vas A R attenuaretur ſe­
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              cundùm aliquam partem in aërem, & reli­
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              qua eiiceretur, iterum autem ad naturalem
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              denſitatem rediens eiectam aquam exſuge­
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              ret, differentia ponderis vaſis non ſoli aquæ
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              eiectæ tribuenda eſſet, ſed toti aquæ vas im­
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              plenti. </s>
              <s>Hinc eſt quod, cum aqua in Æoli­
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              pilam admiſſa non ſit ſecundùm molem̨
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              æqualis toti aëri, qui eam implebat, ac pro­
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              inde non ſit æqualis moli, quæ habet pon­
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              dus gran. 4, non habetur præcisè Ratio gra­
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              uitatum ſecundùm ſpeciem. </s>
            </p>
            <p type="margin">
              <s>
                <margin.target id="note71"/>
                <emph type="italics"/>
              LXXI
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              Experimen­
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              tum Aeoli­
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              pilæ ad ſum­
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              mum osten­
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              dit grauita­
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              tem aëris
                <expan abbr="cõ-munis">con­
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                munis</expan>
              iņ
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              aëre ignito,
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              non autem
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              abſolutè: nec
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              ex eo habe­
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              tur quæſita
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              proportio
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              grauitatum
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              aquæ & aë­
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              ris.
                <emph.end type="italics"/>
              </s>
            </p>
            <p type="main">
              <s>
                <emph type="italics"/>
              Merſ.
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              </s>
              <s> Id meæ ſententiæ vlteriùs fauet: ſi
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              enim aquæ moles, quam ſuxit Æolipila,
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              minor eſt mole aëris, qui numerat in pon­
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              dere grana 4, plus aliquid aquæ addendum
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              erit, vt moles æquales ſint; atque adeò mul­
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              tò maior erit Ratio grauitatis aquæ ad gra­
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              uitatem aëris, quam ſit deprehenſa Ratio
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              1356 ad 1. </s>
            </p>
            <p type="main">
              <s>
                <emph type="italics"/>
              Guld.
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              </s>
              <s> Non hæc eo conſilio afferebam, vt
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              irem contrà; ſed tantùm vt rem paulò ob­
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              ſcuriorem mihi ipſe enucleatiùs explicarem,
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              & te audirem, ſi quid ſortè à veritate aut à
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              tuâ mente alienum intelligerem. </s>
              <s>Cæterùm
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              non nego maiorem eſſe Rationem grauitatis
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              aquæ æolipilam implentis ad grauitatem aë­
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              ris eam pariter implentis, ac ſit Ratio gra­</s>
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          </chap>
        </body>
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