Earthquakes and other earth movements — John Shaqi
Earthquakes and other earth movementsMilne, John
Science
Earthquakes and other earth movements
Milne, John
Earthquakes
If a column, A B C D, receive a shock or be suddenly moved in the
direction of the arrow, the centre of gravity, G, of this column will
revolve round the edge, and tend to describe the path G O. If it passes
O, the column will fall. The work done in such a case as this is equal
to lifting the column through the height _o_ _h_.
If G A = _a_, the angle G A _h_ = φ, and the weight of the body = W,
then the above work equals
W_a_ (1 - cos φ).
This must equal the work acquired—that is to say, the kinetic energy of
rotation of the body, or
W _w_^2 K^2
W_a_ (1 - cos φ) = ———————————.
2 _g_
Where _w_ is the angular velocity of the body at starting, K the radius
of gyration round A, and _g_ the velocity acquired by a falling body in
one second. Whence
_w_^2 K^2 = 2 _ga_ (1 - cos φ),
but _w_, the angular velocity, is equal to the statical couple applied,
divided by the moment of inertia, or,
V_a_ cos φ
_w_ = ——————————,
K^2
squaring and substituting
K^2 1 - cos φ
V^2 = 2_g_ × ——— × —————————,
_a_ cos^2 φ
K^2
and since the length of the corresponding pendulum is _l_ = ———,
_a_
1 - cos φ
V^2 = 2_gl_ × —————————.
cos^2 φ
To apply this to any given case we must find the value of _l_ or of
K^2
———.
_a_
Mallet finds these values for the cube, solid and hollow rectangular
parallelopipeds, solid and hollow cylinders, &c. In these formulæ we
have a direct connection between the dimensions and form of a body and
the velocity with which the ground must move beneath it to cause its
overthrow.
[Illustration: FIG. 15.]
Not only is the case discussed for horizontal forces, but also for
forces acting obliquely. Similar reasonings are applied to the
productions of fractures in walls, but as there is uncertainty in our
knowledge of the co-efficient of force necessary to produce fracture
_through joints across_ beds of masonry, the deductions ought not to
be applied as the measures of velocity. Where the fractures occur at
the base or in horizontal planes, or in those of the continuous beds of
the masonry, or through homogeneous bodies, the uncertainty is not so
great, and for cases like these Mallet gives several illustrations. The
distance to which bodies had been projected, as, for example, ornaments
from the tops of pedestals, coping-stones from the edges of roofs, were
also used as means of determining the angle at which the shock had
emerged, or, if this be known, for determining the velocity.
Public-domain text, read in full here on John Shaqi.
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