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

List of thumbnails

< >
211
211
212
212
213
213
214
214
215
215
216
216
217
217
218
218
219
219
220
220
< >
page |< < of 579 > >|
    <archimedes>
      <text>
        <body>
          <chap>
            <p type="main">
              <s id="s.001077">
                <pb pagenum="207" xlink:href="010/01/215.jpg"/>
                <arrow.to.target n="marg277"/>
                <lb/>
              dente infrà ſupremam hy­
                <lb/>
                <figure id="id.010.01.215.1.jpg" xlink:href="010/01/215/1.jpg"/>
                <lb/>
              drargyri libellam DE, tunc
                <lb/>
              ſublato digito mercurius
                <lb/>
              profluet ab orificio C quo­
                <lb/>
              uſque altitudo FB extantis
                <lb/>
              hydrargyri ſupra libellam̨
                <lb/>
              DE ſit pedum duorum, &
                <lb/>
              quadrantis, vel vnius cubi­
                <lb/>
              ti, & quadrantis, nec vlte­
                <lb/>
              rius hydrargyrum grauiſſi­
                <lb/>
              mum deſcendit ſemperque
                <lb/>
              ad eamdem altitudinem̨
                <lb/>
              perſeuerat, licèt inclinetur
                <lb/>
              fiſtula, ſcilicèt ducta recta FG parallela horizonti
                <expan abbr="sẽ-per">sen­
                  <lb/>
                per</expan>
              ſummitas hydrargyri ad eamdem horizontalem
                <lb/>
              FG perueniet quomodocumque fiſtula inclinetur.
                <lb/>
              </s>
              <s id="s.001078">Ipſe Torricellius experimenti inuentor ſagaciſſimè
                <lb/>
              cauſam quoque huius effectus indagauit, animaduer­
                <lb/>
              tit enim nos in infima profunditate oceani aerei de­
                <lb/>
              merſos eſſe, & ſicuti maris aqua vndique fundum̨
                <lb/>
              comprimit per lineas horizonti perpendiculares, ſeù
                <lb/>
              directas verſus centrum telluris, ſic quoque in oceano
                <lb/>
              aereo niſus eius grauitatis exercetur perpendiculari­
                <lb/>
              tèr ſupra horizontis planum, vnde concipi debent cy­
                <lb/>
              lindri aerei perpendicularitèr ſuperficiem hydrargy­
                <lb/>
              ri DE ſupremam comprimentes; quia verò eadem̨
                <lb/>
              libella mercurij DE comprimitur quoque in ſitu B à
                <lb/>
              ſuperficie baſis B mercurialis cylindri FB efforma­
                <lb/>
              tur veluti libra, vel ſipho, quæ numquam quieſcit, ni-</s>
            </p>
          </chap>
        </body>
      </text>
    </archimedes>