Salusbury, Thomas, Mathematical collections and translations (Tome I), 1667

Table of figures

< >
[Figure 31]
[Figure 32]
[Figure 33]
[Figure 34]
[Figure 35]
[Figure 36]
[Figure 37]
[Figure 38]
[Figure 39]
[Figure 40]
[Figure 41]
[Figure 42]
[Figure 43]
[Figure 44]
[Figure 45]
[Figure 46]
[Figure 47]
[Figure 48]
[Figure 49]
[Figure 50]
[Figure 51]
[Figure 52]
[Figure 53]
[Figure 54]
[Figure 55]
[Figure 56]
[Figure 57]
[Figure 58]
[Figure 59]
[Figure 60]
< >
page |< < of 701 > >|
1neſe territories, and many other places, where very great ſuits
and differences ariſe, which not being to be determined with in­
telligible reaſons, come oftentimes to be decided, by force of
armes; and inſtead of flowing their Grounds with Waters, they
cruelly flow them with the ſhedding of humane blood, impiouſly
inverting the courſe of Peace and Juſtice, ſowing ſuch diſorders
and feuds, as that they are ſometimes accompanied with the ru­
ine of whole Cities, or elſe unprofitably charge them with vain,
and ſometimes prejudicial expences.
PROPOS. IV. THEOR. II.
If a River increaſe in quick height, the quantitie of
Water which the River diſchargeth after the in­
creaſe, hath the Proportion compounded of the
Proportions of the Quick height to the Quick
height, and of the velocity to the velocity.
Let there be a River, which whilſt it is low, runneth thorow
the Regulator D F, with the Quick height A B, and after­
wards let a Flood come; and then let it run with the height
D B, I ſay, that the quantity of the Water that is diſcharged
through D F, to that which diſchargeth through A F, hath the
proportion compounded of the proportions of the velocity
through D F to the velocity through A F, and of the height
D B to the height A B.
As the velocity through D F is to the
velocity through A F, ſo let the line R be to the line S; and as
the height D B is to the height A B; ſo let the line S be to the
47[Figure 47]
line T.
And let a Section be ſuppoſed L M N equal to the
Section D F in height and length, but let it be in velocity equal
to the Section AF.
Therefore the quantity of the Water that run­
neth through D F to that which runneth through L N, ſhall be

Text layer

  • Dictionary
  • Places

Text normalization

  • Original
  • Regularized
  • Normalized

Search


  • Exact
  • All forms
  • Fulltext index
  • Morphological index