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

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    <archimedes>
      <text>
        <body>
          <chap>
            <p type="main">
              <s id="s.000801">
                <pb pagenum="159" xlink:href="010/01/167.jpg"/>
                <arrow.to.target n="marg202"/>
                <lb/>
              VG multò magis aqua inſinuabitur infra aerem dila­
                <lb/>
              tando ſinum ampliorem ODAIR, & multò magis­
                <lb/>
              incuruabitur aeris ſuperficies EBD, tum à vi qua flui­
                <lb/>
              da ſe ſe connectunt conglobanturque, quotieſcum­
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              que in fluido ipſis hetherogeneo
                <expan abbr="collocãtur">collocantur</expan>
              , cùm ab
                <lb/>
              acceſſu noui aeris expulſi à cauitate infima DAIRO.
                <lb/>
              </s>
              <s id="s.000802">Poftquàm verò magis fiſtula deprimitur in ſitu val­
                <lb/>
              dè inclinato VH eadem ratione profluet aqua versùs
                <lb/>
              partem infimam, & omninò aerem ſeparabit, diuel­
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              letque à fundo vaſis, & proindè ſubintrabit ad oc­
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              cupandum ſpatium ODAICHR. </s>
              <s id="s.000803">Poſtremò perdu­
                <lb/>
              cta fiſtula ad inclinationem omnium maximam iņ
                <lb/>
              ſitu VK perpendiculari ad
                <expan abbr="horizontẽ">horizontem</expan>
              aqua, quæ iam
                <lb/>
              inſinuata fuerat circa, & infra aerem tumefactum, &
                <lb/>
              contornatum EBDC,
                <expan abbr="tãdèm">tandèm</expan>
              omninò aerem à fundo,
                <lb/>
              & lateribus vaſis diuellet, & proindè multò magis
                <lb/>
              deſcenſus, & compreſſio aquæ ambientis per latera
                <lb/>
              vaſis, & aeris continuari poteſt; & vniuerſa hæc o­
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              peratio pendet, vt dictum eſt, non ab aere ſpontę
                <lb/>
              aſcendente, neque ab eius leuitate, ſed ab exceſſu
                <lb/>
              grauitatis fluidæ aquæ ambientis, quæ in vertigine
                <lb/>
              fiſtulæ neceſſariò ſeparat, atque diuellit aerem à la­
                <lb/>
              teribus, & fundo vaſis, & ſic via ſternitur commodiſ­
                <lb/>
              ſima, vt continuari, & proſequi preſſio aquæ poſſit,
                <lb/>
              vnde aer ſursùm expulſus continuare poteſt eius cur­
                <lb/>
              ſum, ſi, inquam, hoc obſeruatum, & adnotatum fuiſ­
                <lb/>
              ſet, proculdubiò ex mutatione figuræ planæ in tumi­
                <lb/>
              dam in aere aſcendente per aquam non deduxiſſet
                <lb/>
              prædictus author aeris leuitatem poſitiuam. </s>
            </p>
          </chap>
        </body>
      </text>
    </archimedes>
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