CSIR-NET
2012 (June) 104
:
(A). If
ω and ω0 represent the seismic signal frequencies and resonant frequencies,
respectively, of a seismometer, in which of the following case, it
would behave as a displacement meter.
A)
ω0 >>ω B) ω0 << ω
C) ω0 =ω D) ω0 =1/ω
Answer:
B
Explanation:
1.
A long period seismometer is an instrument in which the resonant
frequency (ω0) is very low. The lag between the
seismometer and the ground motion becomes zero and the amplitude of
the seismometer displacement becomes equal to the amplified ground
displacement. It is sometimes called a displacement meter.
2.
It is usually designed to record seismic signals with frequencies in
the range 0.01 Hz to 0.1 Hz which is ‘periods’ of 100 seconds
down to 10 seconds.
3.
Long-period seismometer also called displacement meter, therefore
resonant frequency(ω0) is very low compared to seismic signal frequency(ω).
Extra information:
Displacement meter:
$u=\frac{A\omega^2}{\omega_0^2 +\omega^2} \cos(\omega t-\triangle)---(1)$
Here $ \omega_0^2 << \omega^2$
$u=Acos\omega t=q$
Accelerometer:
$u=\frac{A\omega^2}{\omega_0^2 +\omega^2} \cos(\omega t-\triangle)---(1)$
Here $ \omega_0^2 >> \omega^2$
$u=\frac{1}{\omega_0^2}Acos\omega t=q$
$\frac{\partial u}{\partial t}=-\frac{1}{\omega_0^2}A \omega sin\omega t$
$\frac{\partial u^2}{\partial^2 t}=-\frac{1}{\omega_0^2}A \omega^2 cos\omega t$
we know that
$u=Acos\omega t=q$
$\frac{\partial u}{\partial t}=-A \omega sin\omega t=\dot{q}$
$\frac{\partial u^2}{\partial^2 t}=-A \omega^2 cos\omega t =\ddot{q}$
Therefore,
$\frac{\partial u^2}{\partial^2 t}=-\frac{1}{\omega_0^2} \ddot{q}$
Reference: Fundamentals of Geophysics, William Lowrie.
(C).
The velocity of tsunami wave traveling through an open ocean of depth
5km is about
A)
220 m/s B) 20 m/s C) 2 m/s
D) 800 m/s
Solution:
The velocity of the tsunami wave (V)= √(g*d)
g=
acceleration due to gravity = 9.8 m/s
d=
depth = 5km
= 5000m
V=
√ (9.8 * 5000)
=
√(49,000)
=221.359
m/s
Therefore
the velocity of tsunami wave (V) = 220 m/s
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