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

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    <archimedes>
      <text>
        <body>
          <chap>
            <p type="main">
              <s id="s.001862">
                <pb pagenum="351" xlink:href="010/01/359.jpg"/>
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            <p type="margin">
              <s id="s.001863">
                <margin.target id="marg474"/>
              Cap. 8. cur
                <lb/>
              exiguæ aquæ
                <lb/>
              guttæ ſupra
                <lb/>
                <expan abbr="libellã">libellam</expan>
              aquæ
                <lb/>
              aſcendunt.</s>
            </p>
            <p type="main">
              <s id="s.001864">SI poſtea conſideremus
                <expan abbr="incongruẽtiam">incongruentiam</expan>
              pororum,
                <lb/>
              patet verum non eſſe aduerſariorum aſſertum
                <expan abbr="cũ">cum</expan>
                <lb/>
              aiunt, ideò ab aere impediri motiones partium aquę,
                <lb/>
              quia orificia pororum aeris ſtrictiora ſunt,
                <expan abbr="quã">quam</expan>
              vt per
                <lb/>
              ea aquæ particulæ ingredi, & fluere poſſint, nam hinc
                <lb/>
              inferre liceret neque aqueas particulas per
                <expan abbr="ipsãmet">ipsammet</expan>
                <lb/>
              aquam cieri, & excurrere poſſe; facilè enim percipi­
                <lb/>
              tur, quòd in aqua poroſitates non poſſunt eſſe adeò
                <lb/>
              amplæ, vt per eas intromitti poſſint particulæ eiuſ­
                <lb/>
              demmet aquæ, ſed debent eſſe multò minores, ſicuti
                <lb/>
              interſtitia, quæ in aceruo granorum tritici, vel milij
                <lb/>
              intercipiuntur, ſemper minora ſunt,
                <expan abbr="quã">quam</expan>
              grana eiuſ­
                <lb/>
              dem tritici, vel milij, aliàs facta acerui concuſſione
                <lb/>
              ſe mutuò magis conſtringerent amplexarentur quę
                <lb/>
              granula prædicta, intromiſſis nempè granulis in eiſ­
                <lb/>
              dem amplis interſtitijs. </s>
              <s id="s.001865">Hinc ſequitur vt æquè diffi­
                <lb/>
              cilè aquæ particulæ per ipſam aquam moueri, agita­
                <lb/>
              rique poſſint, quàm per aerem, quia nempè æquè in­
                <lb/>
              commodus eſt progreſſus aquæ per aquam, ac per ae­
                <lb/>
              rem; ſi verum eſt requiri poroſitates in fluido tantæ
                <lb/>
              amplitudinis vt capaces ſint particularum aquæ ad
                <lb/>
              hoc vt per prædictum fluidum moueri queant. </s>
              <s id="s.001866">cùm­
                <lb/>
              que aquæ anguſtæ poroſitates non impediant motum
                <lb/>
              particularum aquæ per ipſam aquam. </s>
              <s id="s.001867">ergò pariter
                <lb/>
              anguſtia pororum aeris non impediet motum
                <expan abbr="partiũ">partium</expan>
                <lb/>
              aquæ per aerem. </s>
            </p>
            <figure id="id.010.01.359.1.jpg" xlink:href="010/01/359/1.jpg" number="122"/>
          </chap>
        </body>
      </text>
    </archimedes>
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