Animated Solution for Physics - Oscillations: A highly rigid cubical block A of small mass M and side L is fixed rigidly on to another cubical block B of the same dimensions and of low modulus of rigidity η such that the lower face of A completely covers the upper face of B. The lower face of B is rigidly held on a horizontal surface. A small force F is applied perpendicular to one of the side faces of A. After the force is withdrawn, block A executes small oscillations, the time period of which is given by
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Visualized Solution
Understanding the Physical Setup
We have a highly rigid cubical block A of mass M and side L placed on top of another cubical block B of the same dimensions.
Block B has a low modulus of rigidity η and its lower face is fixed to a horizontal surface.
When a horizontal force F is applied to block A, it causes block B to undergo shear deformation by a small angle θ and horizontal displacement x.
Defining Modulus of Rigidity η
The modulus of rigidity η is defined as the ratio of shear stress to shear strain:
η=Shear StrainShear Stress=θF/A
where F is the restoring force, A is the area of the sheared surface, and θ is the shear angle.
Expressing Area A and Shear Angle θ
Since block B is a cube of side L, the area of its upper face is:
A=L2
For a small displacement x, the shear angle θ (in radians) is given by:
θ≈tanθ=Lx
Formulating the Restoring Force
Substituting A=L2 and θ=Lx into the modulus of rigidity equation:
η=x/LF/L2
Rearranging for the magnitude of the restoring force F:
F=η⋅L2⋅Lx=ηLx
Finding the Acceleration of Block A
The restoring force acts in the opposite direction of the displacement x:
Frestoring=−ηLx
Using Newton's second law, the acceleration a of block A of mass M is:
a=MFrestoring=−MηLx
Comparing with the Standard SHM Equation
The standard equation for simple harmonic motion is:
a=−ω2x
Comparing this with our acceleration equation:
ω2=MηL⟹ω=MηL
Calculating the Time Period T
The time period T of the oscillation is related to the angular frequency ω by:
T=ω2π
Substituting ω=MηL:
T=2πηLM
Thus, the correct option is (d).
Exploring Further: What if Block A is also Deformable?
If block A were also deformable with a modulus of rigidity ηA, the system would act as two shear springs in series.
The equivalent force constant would be:
keq1=kA1+kB1
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The Sigma Insight: Simple Harmonic Motion (SHM)
Solution Diagram
The Dance of Rigidity and Elasticity
Imagine a massive, highly rigid block sitting on top of a softer, jelly-like block. When you push the top block, it doesn't bend or warp; it simply slides as a single unit. But the block underneath—the elastic one—shears, stretching like a deck of cards being slid sideways. This beautiful interplay between rigid mass and elastic deformation is the heart of our problem.
In this classic JEE problem from 1992, we are asked to find the time period of small oscillations of a rigid block A resting on a deformable block B. This is not just a math exercise; it is a fundamental exploration of how elastic restoring forces drive simple harmonic motion (SHM).
Let's dive deep into the physics of shear deformation and discover how the geometry of the blocks dictates the rhythm of their oscillation.
Analyzing the Setup
Let's look at the two blocks. Block A has a mass M and side L. It is highly rigid, which means we can treat it as a point mass concentrated at its center of gravity when it comes to translation. It doesn't deform; it only moves.
Block B, however, is the elastic engine of this system. It has the same dimensions (side L) but a low modulus of rigidity η. Its bottom face is glued to a horizontal table, while its top face is glued to the bottom of block A.
When we apply a horizontal force F to block A, it shifts by a small distance x. Because block A is glued to block B, the top face of block B also shifts by x, while its bottom face remains fixed. This creates a shear strain in block B.
The Physics of Shear
Modulus of Rigidity
To understand how block B fights back against this displacement, we must look at the modulus of rigidityη. By definition, the modulus of rigidity is the ratio of shear stress to shear strain:
η=Shear StrainShear Stress
Shear stress is the restoring force F per unit area A of the face parallel to the force:
Shear Stress=AF
Since block B is a cube of side L, the area of its top face is:
A=L2
Shear strain is the angle of deformation θ. For a small horizontal displacement x and height L, we can use the small-angle approximation:
θ≈tanθ=Lx
Finding the Restoring Force
Now, let's substitute these geometric relations back into our definition of η:
η=x/LF/L2
Simplifying this fraction, we get:
η=LxF
Solving for the magnitude of the restoring force F, we find a remarkably simple relation:
F=ηLx
Notice how this force is directly proportional to the displacement x! This is exactly like Hooke's Law for a spring, where the effective spring constant is:
keff=ηL
This is a beautiful realization: a sheared elastic block behaves exactly like a horizontal spring with a stiffness proportional to its modulus of rigidity and its linear dimension!
The Equation of Motion and Time Period
Since the restoring force always acts in the direction opposite to the displacement, we can write the equation of motion using Newton's second law:
Frestoring=−ηLx
Ma=−ηLx
Dividing by the mass M, we get the acceleration a of block A:
a=−(MηL)x
This is the standard differential equation of simple harmonic motion, which has the form:
a=−ω2x
By comparing the two equations, we can immediately identify the angular frequency ω of the oscillation:
ω2=MηL⟹ω=MηL
The Final Rhythm
The time period T of the oscillation is the time taken for one complete cycle, given by:
T=ω2π
Substituting our value of ω:
T=2πηLM
This is our final elegant result, which corresponds perfectly to Option (d).
A Deeper Intuition
Let's look at the formula we derived: T=2πηLM. Does it make physical sense?
First, if the mass M of block A increases, the time period T increases. This is highly intuitive: a heavier block has more inertia, making it harder to accelerate, so it oscillates more slowly.
Second, if the modulus of rigidity η increases, the material becomes stiffer, the restoring force becomes stronger, and the time period T decreases. The block oscillates faster!
Third, if the side L increases, the time period T decreases. Why? Because a larger contact area A=L2 increases the restoring force faster than the increased height L reduces the shear strain. Thus, a larger block is stiffer in shear!
This problem is a masterclass in connecting the microscopic elastic properties of materials to macroscopic oscillatory motion. By mastering these connections, you unlock the true power of physics!