Philosophical transactions, Vol. L. Part II. For the year 1758.: Giving some account of the present undertakings, studies, and labours, of the ingenious, in many considerable parts of the world.Various
History
Philosophical transactions, Vol. L. Part II. For the year 1758.: Giving some account of the present undertakings, studies, and labours, of the ingenious, in many considerable parts of the world.
Various
Science -- Periodicals
But the heights in both sections being equal, the sections are
directly as the breadths;
Consequently the velocities are reciprocally as the breadths.
VI. _In a running stream, the water above any obstacles put therein
will rise to such a height, that by its fall the stream may be
discharged as fast as it comes._
For the same body of water, which flowed in the open chanel, must
pass thro’ the passages made by the obstacles:
And the narrower the passages, the swifter will be the velocity of
the water:
But the swifter the velocity of the water, the greater is the height,
from whence it has descended:
Consequently the obstacles, which contract the chanel, cause the
water to rise against them.
But the rise will cease, when the water can run off as fast as it
comes:
And this must happen, when, by the fall between the obstacles, the
water will acquire a velocity in a reciprocal proportion to that in
the open chanel as the breadth of the open chanel is to the breadth
of the narrow passages.
VII. _The quantity of the fall caused by an obstacle in a running
stream is measured by the difference between the heights fallen from
to acquire the velocities in the narrow passages and open chanel._
For just above the fall, the velocity of the stream is such, as would
be acquired by a body falling from a height higher than the surface
of the water:
And at the fall, the velocity of the stream is such, as would be
acquired by the fall of a body from a height more elevated than the
top of the falling stream; and consequently the real fall is less
than this height.
Now as the stream comes to the fall with a velocity belonging to a
fall above its surface;
Consequently the height belonging to the velocity at the fall must be
diminished by the height belonging to the velocity, with which the
stream arrives at the fall.
PROBLEM.
_In a chanel of running water, whose breadth is contracted by one or
more obstacles; the breadth of the chanel, the mean velocity of the
whole stream, and the breadth of the water-way between the obstacles
being given; To find the quantity of the fall occasioned by those
obstacles._
Let _b_ = breadth of the chanel in feet.
_v_ = mean velocity of the water in feet per sec.
_c_ = breadth of the water-way between the obstacles.
Now 25: 21∷ _c_: 21 ⁄ 25 _c_ the water-way contracted. _Principle III._
And 21 ⁄ 25 _c_: _b_∷ _v_: 25_b_ ⁄ 21_c_ _v_ the veloc. _per_ sec. in
the water-way between the obstacles. _Princip. V._
Also (2_a_)²: _vv_∷ _a_: _vv_ ⁄ 4_a_ the height fallen to acquire the
vel. v. I. & II.
And (2_a_)²: (25_b_ ⁄ 21_c_)² × _vv_∷ _a_: (25_b_ ⁄ 21_c_)² × _vv_ ⁄
4_a_ the height fallen to acquire the vel. 25_b_ ⁄ 21_c_ _v_. I. & II.
Then (25_b_ ⁄ 21_c_)² x (_vv_ ⁄ 4_a_) - (_vv_ ⁄ 4_a_) is the measure of
the fall required. VII.
Or ((25_b_ ⁄ 21_c_)² - 1) × _vv_ ⁄ 4_a_ is a rule, by which the fall
may be readily computed.
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