Bernoulli, Daniel, Hydrodynamica, sive De viribus et motibus fluidorum commentarii

Page concordance

< >
Scan Original
51 37
52 38
53 39
54 40
55 41
56 42
57 43
58 44
59 45
60 46
61 47
62 48
63 49
64 50
65 51
66 52
67 53
68 54
69 55
70 56
71 57
72 58
73 59
74 60
75
76 62
77 63
78 64
79 65
80 66
< >
page |< < (43) of 361 > >|
    <echo version="1.0RC">
      <text xml:lang="la" type="free">
        <div xml:id="echoid-div55" type="section" level="1" n="40">
          <p>
            <s xml:id="echoid-s1130" xml:space="preserve">
              <pb o="43" file="0057" n="57" rhead="SECTIO TERTIA."/>
            (1 - {mm/nn})vdξ + ξdv = - xdξ
              <lb/>
            cujus integralis, quod patet multiplicatis terminis per ξ - {mm/nn} hæc eſt
              <lb/>
            v = ξ
              <emph style="super">{mm/nn} - 1</emph>
            ſ - xξ
              <emph style="super">- {mm/nn}</emph>
            dξ.
              <lb/>
            </s>
            <s xml:id="echoid-s1131" xml:space="preserve">Fuerit v. </s>
            <s xml:id="echoid-s1132" xml:space="preserve">gr. </s>
            <s xml:id="echoid-s1133" xml:space="preserve">canalis rectus & </s>
            <s xml:id="echoid-s1134" xml:space="preserve">ita inclinatus verſus horizontem, ut ſinus anguli
              <lb/>
            intercepti inter utrumque ſit ad ſinum totum ut 1 ad g, erit ξ = gx; </s>
            <s xml:id="echoid-s1135" xml:space="preserve">unde
              <lb/>
            v = {nna/2nn - mm} (({a/x})
              <emph style="super">{nn - mm/nn}</emph>
            - {x/a})
              <lb/>
            quæ æquatio cum non differat ab æquatione §. </s>
            <s xml:id="echoid-s1136" xml:space="preserve">13. </s>
            <s xml:id="echoid-s1137" xml:space="preserve">pro Cylindris verticalibus
              <lb/>
            data, ſequitur in utroque caſu velocitates aquæ easdem eſſe, poſtquam deſ-
              <lb/>
            cenſus verticales ſuperficiei aquæ iidem ſunt: </s>
            <s xml:id="echoid-s1138" xml:space="preserve">Igitur accelerationes in locis
              <lb/>
            homologis utrobique ſimiles ſunt ratione altitudinum verticalium, & </s>
            <s xml:id="echoid-s1139" xml:space="preserve">hoc tan-
              <lb/>
            tum diſcriminis intercedit, quod in canali inclinato lentius fiant, idque in
              <lb/>
            ratione ut 1 ad g: </s>
            <s xml:id="echoid-s1140" xml:space="preserve">facile igitur ſenſibus percipi poterunt hæ accelerationes in
              <lb/>
            canalibus valde inclinatis, quæ in verticalibus ob nimiam mutationum celeri-
              <lb/>
            tatem non poſſunt. </s>
            <s xml:id="echoid-s1141" xml:space="preserve">Cœterum patet per ſe ex eo, quod frictiones à longitu-
              <lb/>
            dine tubi augeantur, non poſſe non velocitates inde diminui, ad quod ani-
              <lb/>
            mum advertent ii, quibus experimenta hâc de re inſtituere animus erit.</s>
            <s xml:id="echoid-s1142" xml:space="preserve"/>
          </p>
        </div>
      </text>
    </echo>