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

Table of figures

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(d) By 5 of our ſe­
cond of Conicks.
(e) By 29 of the
firſt.
(f) By 39 of our
firſt of Conicks.
Therefore, A Q and A M do make equall Acute Angles with

the Diameters of the Portions.] We demonſtrate this as in the Commentaries
upon the ſecond Concluſion.
E
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,
291[Figure 291]
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,
292[Figure 292]
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

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