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

Table of figures

< >
[Figure 151]
[Figure 152]
[Figure 153]
[Figure 154]
[Figure 155]
[Figure 156]
[Figure 157]
[Figure 158]
[Figure 159]
[Figure 160]
[Figure 161]
[Figure 162]
[Figure 163]
[Figure 164]
[Figure 165]
[Figure 166]
[Figure 167]
[Figure 168]
[Figure 169]
[Figure 170]
[Figure 171]
[Figure 172]
[Figure 173]
[Figure 174]
[Figure 175]
[Figure 176]
[Figure 177]
[Figure 178]
[Figure 179]
[Figure 180]
< >
page |< < of 579 > >|
1
pus
T ad V, ita erit moles aquæ R ad S.
Ibidem.
Cap. 11. gra­
uia in fluido
velocitati­
bus inæqua­
libus ferri
debere.
PROP. CCXXIII.
Si duæ fistulæ inæqualiter altæ habuerint orificia æqualia,
atque ex eis egrediantur moles aquæ æquales, tempora
effluxuum habebunt ſubduplicatam proportionem reci­
procam altitudinum fistularum.
SIt altitudo fiſtulæ AB maior, quàm CD, & eorum
orificia B, D æqualia, & ex B egrediatur moles
aquæ R tempore T, ex D verò profluat moles aquæ
S æqualis ipſi R tempore V, & vt priùs, ſit BE media
proportionalis inter AB, &
161[Figure 161]
CD; dico tempus V ad T ean­
dem
proportionem haberę,
quam EB ad CD, ſit moles aquæ
X illa, quæ defluit ab orificio
D eodem tempore T, igitur

vt moles aquæ R ad X, ita erit
altitudo EB ad CD, poſteą
quia ab eodem oriſicio D fi­
ſtulæ CD exeunt duæ moles
aqueæ X, & S temporibus T,

& V, igitur vt tempus V ad T, ita ſe habet moles aquæ
S ad X: ſunt verò moles aquæ R, & S ex hypotheſi,
æquales, igitur ad eamdem molem X eamdem pro­
portionem habent; eſt verò EB ad CD vt R ad X;
atque V ad T vt S ad X; igitur altitudo EB ad CD ean­
dem
proportionem habebit, quam tempus V ad T.
Prop. 221.
Prop. 222.
PROP. CCXXIV.
Duæ moles aquæ eodm tempore egredientes ex orificijs inæ-

Text layer

  • Dictionary
  • Places

Text normalization

  • Original

Search


  • Exact
  • All forms
  • Fulltext index
  • Morphological index