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

Table of figures

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              <s id="s.002485">
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                <lb/>
              hoc in ſequentibus quoque ſupponatur) ſi ſpatia æ­
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              qualia X, & Z ſursùm aſcendendo percurrerint AC
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              quidem tempore T, & DF tempore V; dico tempus
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              V ad T eſſe vt AB ad GB; quia per æqualia ſpatia X,
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              & Z in aqua eleuantur ſolida AC, & DF, ergo ſuis æ­
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              qualibus baſibus expellunt è locis ſupremis æquales
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              cylindros aqueos, & hæ æquales aquæ moles deor­
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              sùm
                <expan abbr="fluũt">fluunt</expan>
              per ſiphones tubicos excauatos æquè craſ­
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              ſos, ſcilicèt æqualium baſium, propterea quod baſes
                <lb/>
              BC, & EF æquales ſunt inter ſe, igitur ex ſiphonibus
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              tubicis inæqualium
                <expan abbr="altitudinũ">altitudinum</expan>
              ha­
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                <figure id="id.010.01.479.1.jpg" xlink:href="010/01/479/1.jpg"/>
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              bentibus orificia, ſeu baſes æqua­
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              les defluunt duæ aquæ moles inter
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              ſe æquales, ſed natura
                <expan abbr="prædictorũ">prædictorum</expan>
                <lb/>
                <arrow.to.target n="marg643"/>
                <lb/>
              ſiphonum exigit, vt tempus V, quo
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              data moles aquæ profluit ab orifi­
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              cio infimo ſiphonis ambientis cy­
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              lindrum DF ad tempus T, quo mo­
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              les aquæ illi æqualis defluit ex æ­
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              quali orificio ſiphonis ambientis
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              cylindrum AC, eamdem proportionem habeat, quam
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              altitudo GB ad DE, & in prædictis temporibus tan­
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              tumdem eleuantur cylindri, quantæ ſunt moles aquæ
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              ex vtriſque ſiphonibus effluxæ: igitur tempus V, quo
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              ſolidum DF eleuatur ad tempus T ſublimationis ſo­
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              lidi AC eamdem
                <expan abbr="proportionẽ">proportionem</expan>
              habebit, quam altitu­
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              do GC ad altitudinem DE. </s>
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            <p type="margin">
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              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="margin">
              <s id="s.002487">
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              Pr. 223.</s>
            </p>
            <p type="main">
              <s id="s.002488">Secundò ſint ijdem cylindri aqua grauiores; ſimi­
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              liter æquales aquæ moles ſursùm fluunt per ſiphones </s>
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