Decoding the Velocity Graph
Imagine you are tracking the motion of a bicycle. You are given a graph that plots its velocity v against its displacement x. Your mission is to translate this information into an acceleration-displacement (a−x) graph.
Looking closely at the given v−x graph, we can clearly see that the motion is divided into two distinct phases. The first phase is a steady climb from x=0 to x=200 m, where the velocity increases linearly. The second phase, from x=200 m to x=400 m, shows the bicycle cruising at a constant velocity. To find the acceleration, we must analyze these two phases separately.
The Master Equation of Kinematics
When dealing with velocity as a function of time, acceleration is simply the slope of the graph, a=dtdv. However, our graph plots velocity against displacement. We cannot just take the slope!
Instead, we must use the chain rule to link acceleration, velocity, and displacement. This gives us our master equation:
This equation tells us that the acceleration at any point is the product of the velocity itself and the slope of the v−x graph at that point.
Analyzing the First Phase (0≤x≤200)
In this region, the v−x graph is a perfect straight line. Let's find its mathematical equation using the standard slope-intercept form, v=mx+c.
The line starts at a velocity of 10 m/s, so our y-intercept c is 10.
To find the slope m, we calculate the 'rise over run':
So, the equation for velocity is:
Now, let's plug this into our master equation. We need the derivative of velocity with respect to displacement, dxdv, which is simply the slope we just calculated: 51.
Substituting these into a=vdxdv:
Look at this beautiful result! The acceleration a is a linear function of x. This means the a−x graph for this phase will also be a straight line.
Let's check the boundary values to see where this line starts and ends:
- At x=0, a=250+2=2 m/s2.
- At x=200, a=25200+2=8+2=10 m/s2.
So, the acceleration increases linearly from 2 to 10.
Analyzing the Second Phase (x>200)
Beyond 200 m, the bicycle stops speeding up and maintains a constant velocity of 50 m/s.
Because the velocity is constant, its rate of change with respect to displacement is zero:
Plugging this into our master equation:
The acceleration instantly drops to zero and stays there for the remainder of the journey.
The Final Picture
Combining our findings, the true a−x graph must show a straight line rising from 2 to 10 between x=0 and x=200, followed by an abrupt drop to 0 for the rest of the motion.
Comparing this with our options, Option (a) perfectly captures this dynamic reality!