Archimedes, Natation of bodies, 1662

Page concordance

< >
Scan Original
61
62
63
64
65
66
67
68
< >
page |< < of 68 > >|
1
(d) By 5 of our ſe­
cond
of Conicks.
(e) By 29 of the
firſt
.
(f) By 39 of our
firſt
of Conicks.
It is to be demonſtrated in the ſame manner, that the Portion

that
hath the ſame proportion in Gravity to the Liquid, that the
Square
P F hath to the Square B D,
being
demitted into the Liquid, ſo,
65[Figure 65]
as
that its Baſe touch not the Li­
quid
, it ſhall ſtand inclined, ſo, as
that
its Baſe touch the Surface of the
Liquid
in one point only; and its Axis
ſhall
make therewith an angle equall
to
the Angle φ.] Let the Portion be to the
Liquid
in Gravity, as the Square P F to the
Square
B D: and being demitted into the
Liquid
, ſo inclined, as that its Baſe touch not
the
Liquid, let it be cut thorow the Axis by a
Plane
erect to the Surface of the Liquid, that
that
the Section may be A M O L, the Section
of
a Rightangled Cone; and, let the Section of the Liquids Surface be I O; and the Axit
of
the Portion and Diameter of the Section B D; which let be cut into the ſame parts as
we
ſaid before, and draw M N parallel to I O, that it may touch the Section in the Point
M
; and M T parallel to B D, and P M S perpe ndicular to the ſame.
It is to be demon­
strated
, that the Portion ſhall not reſt, but ſhall incline, ſo, as that it touch the Liquids
Surface
, in one Point of its Baſe only.
For,
66[Figure 66]
draw P C perpendicular to B D; and drawing
a
Line from A to F, prolong it till it meet with
the
Section in que and thorow P draw P φ pa­
rallel
to A Q: Now, by the things allready de­
monſtrated
by us, A F and F Q ſhall be equall
to
one another.
And being that the Portion hath
the
ſame proportion in Gravity unto the Liquid,
that
the Square P F hath to the Square B D; and
ſeeing
that the part ſubmerged, hath the ſame pro-

partion to the whole Portion; that is, the Squàre
M
T to the Square B D; (g) the Square M T
ſhall
be equall to the Square P F; and, by the
ſame
reaſon, the Line M T equall to the Line
P
F.
So that there being drawn in the equall & like
portions
A P Q Land A M O L, the Lines A Q and I O which cut off equall Portions, the
firſt
from the Extreme term of the Baſe, the laſt not from the Extremity; it followeth, that
A
Q drawn from the Extremity, containeth a leſſer Acute Angle with the Diameter of the
Portion
, than I O: But the Line P φ is parallel to the Line A Q, and M N to I O: There­
fore
, the Angle at φ ſhall be leſſer than the Angle at N; but the Line B C greater than B S;
and
S R, that is, M X, greater than C R, that is, than P Y: and, by the ſame reaſon, X T
leſſer
than Y F. And, ſince P Y is double to Y F, M X ſhall be greater than double to
Y
F, and much greater than double of X T.
Let M H be double to H T, and draw a
Line
from H to K, prolonging it.
Now, the Centre of Gravity of the whole Portion
ſhall
be the Point K; of the part within the Liquid H; and of the Remaining part above
the
Liquid in the Line H K produced, as ſuppoſe in ω It ſhall be demonſtrated in the ſame
manner
, as before, that both the Line K H and thoſe that are drawn thorow the Points H
and
ω parallel to the ſaid K H, are perpendicular to the Surface of the Liquid: The
Portion
therefore, ſhall not reſt; but when it ſhall be enclined ſo far as to touch the Sur­
face
of the Liquid in one Point and no more, then it ſhall ſtay.
For the Angle at N

Text layer

  • Dictionary
  • Places

Text normalization

  • Original
  • Regularized
  • Normalized

Search


  • Exact
  • All forms
  • Fulltext index
  • Morphological index