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

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            <p type="main">
              <s id="s.002438">
                <expan abbr="tẽ-">
                  <pb pagenum="463" xlink:href="010/01/471.jpg"/>
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                  <lb/>
                pus</expan>
              T ad V, ita erit moles aquæ R ad S. </s>
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            <p type="margin">
              <s id="s.002439">
                <margin.target id="marg629"/>
              Ibidem.</s>
            </p>
            <p type="margin">
              <s id="s.002440">
                <margin.target id="marg630"/>
              Cap. 11. gra­
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              uia in fluido
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              velocitati­
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              bus inæqua­
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              libus ferri
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              debere.</s>
            </p>
            <p type="main">
              <s id="s.002441">
                <emph type="center"/>
              PROP. CCXXIII.
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              </s>
            </p>
            <p type="main">
              <s id="s.002442">
                <emph type="center"/>
                <emph type="italics"/>
              Si duæ fistulæ inæqualiter altæ habuerint orificia æqualia,
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              atque ex eis egrediantur moles aquæ æquales, tempora
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              effluxuum habebunt ſubduplicatam proportionem reci­
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              procam altitudinum fistularum.
                <emph.end type="italics"/>
                <emph.end type="center"/>
              </s>
            </p>
            <p type="main">
              <s id="s.002443">SIt altitudo fiſtulæ AB maior, quàm CD, & eorum
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              orificia B, D æqualia, & ex B egrediatur moles
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              aquæ R tempore T, ex D verò profluat moles aquæ
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              S æqualis ipſi R tempore V, & vt priùs, ſit BE media
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              proportionalis inter AB, &
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                <figure id="id.010.01.471.1.jpg" xlink:href="010/01/471/1.jpg"/>
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              CD; dico tempus V ad T
                <expan abbr="eã-dem">ean­
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                dem</expan>
              proportionem haberę,
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                <expan abbr="quã">quam</expan>
              EB ad CD, ſit moles aquæ
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              X illa, quæ defluit ab orificio
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              D eodem tempore T, igitur
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                <arrow.to.target n="marg631"/>
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              vt moles aquæ R ad X, ita erit
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              altitudo EB ad CD, poſteą
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              quia ab eodem oriſicio D fi­
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              ſtulæ CD exeunt duæ moles
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              aqueæ X, & S temporibus T,
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                <arrow.to.target n="marg632"/>
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              & V, igitur vt
                <expan abbr="tẽpus">tempus</expan>
              V ad T, ita ſe habet moles aquæ
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              S ad X: ſunt verò moles aquæ R, & S ex hypotheſi,
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              æquales, igitur ad eamdem molem X eamdem pro­
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              portionem habent; eſt verò EB ad CD vt R ad X;
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              atque V ad T vt S ad X; igitur altitudo EB ad CD
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                dem</expan>
              proportionem habebit, quam tempus V ad T. </s>
            </p>
            <p type="margin">
              <s id="s.002444">
                <margin.target id="marg631"/>
              Prop. 221.</s>
            </p>
            <p type="margin">
              <s id="s.002445">
                <margin.target id="marg632"/>
              Prop. 222.</s>
            </p>
            <p type="main">
              <s id="s.002446">
                <emph type="center"/>
              PROP. CCXXIV.
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              </s>
            </p>
            <p type="main">
              <s id="s.002447">
                <emph type="center"/>
                <emph type="italics"/>
              Duæ moles aquæ eodm tempore egredientes ex orificijs inæ-
                <emph.end type="italics"/>
                <emph.end type="center"/>
              </s>
            </p>
          </chap>
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