Thursday, July 26, 2018

Chapter 3.4 - Instantaneous Velocity

In the previous section we saw average velocity and average speed. In this section we will see instantaneous velocity. We will write it in steps:
1. Fig.3.34 below shows a position-time graph of an object:
Fig.3.34
• In the above graph a point Q is marked. The following two items are clear:
(i) Q is at a distance of 5.12 m from the origin
(ii) The object passed Q when the stop watch showed 4 s
[Note: It is difficult to obtain the value 5.12 from the graph. So we can use the equation of the curve.
The equation is x = 0.08t3.
Substituting t = 4, we get:
s = 0.08 × (4)3= 0.08 × 64 = 5.12]  
2. Consider the instant at which the object passed Q
• We want to find the exact velocity at that instant
Let us try:
(i) The point of interest is Q. It is the position of the object when it travelled for 4 seconds
(ii) We need two neighbouring points of Q. 
• One before Q and 
• The other after Q
(iii) These new points should satisfy a condition:
• They must be at equal time intervals from Q
(iv)Let us choose a point P before Q such that:
    ♦ The object reached P, 1 s before Q. That is., when the stop watch showed 3 s  
• Let us choose a point R after Q such that:  
    ♦ The object reached R, 1 s after Q. That is., when the stop watch showed 5 s  
■ So the duration of travel from P to R = Δt = (t2 t1) = (5 - 3) = 2 s
This is shown in fig.3.35 below:
Fig.3.35
(v) In the above graph, the distances corresponding to t = 3 and t = 5 are calculated using the same procedure that we used for t = 4:
s(3) = 0.08 × (3)3= 0.08 × 27 = 2.16 m
s(5) = 0.08 × (5)3= 0.08 × 125 = 10 m
(vi) Now we join PR. This is shown in fig.3.36 below:

Fig.3.36
• Slope of PR can be calculated by completing the triangle PRR'
• We get: Slope of PR = altitudebase RR'PR' ΔxΔt = (10-2.16)(5-3) = 7.842 = 3.92 ms-1.
(vii) But we know that, this slope gives us only the 'average velocity' between P and R
• Though Q falls between P and R, 3.92 ms-1 is not the instantaneous velocity at Q
• The duration of travel from P to R is 2 s. This '2 s' is not an 'instant'
3. So let us reduce the time interval:
• We need two new neighbouring points of Q. One before Q and the other after Q
• Like before, these new points should also satisfy a condition:
They must be at equal time intervals from Q
(i) Let us choose a point P1 before Q such that:
    ♦ The object reached P1, 0.5 s before Q. That is., when the stop watch showed 3.5 s  
Let us choose a point R1 after Q such that:  
    ♦ The object reached R1, 0.5 s after Q. That is., when the stop watch showed 4.5 s  
■ So the duration of travel from P1 to R1 = Δt = (t2 t1) = (4.5 - 3.5) = 1 s
(ii) After marking P and R, we join them. This is shown in fig.3.37 below:

Fig.3.37
• In the above graph, the distances corresponding to t = 3.5 and t = 4.5 are calculated using the same procedure that we used for t = 4:
s(3) = 0.08 × (3.5)3= 0.08 × 27 = 3.43    
s(5) = 0.08 × (4.5)3= 0.08 × 125 = 7.29
(iii) Slope of P1R1 can be calculated by completing the triangle P1R1R1'
• To avoid congestion, we will zoom in on the required area. This is shown in fig.3.38 below:
Fig.3.38
• We get: Slope of DF = altitudebase R1R'P1R'1ΔxΔt = (7.29-3.43)(4.5-3.5) = 3.861 = 3.86 ms-1
(iv) But we know that, this slope gives us only the 'average velocity' between P1 and R1
• Though Q falls between P1 and R1, 3.86 ms-1 is not the instantaneous velocity at Q
• The duration of travel from P1 to R1 is 1 s. This '1 s' is not an 'instant'
4. So let us reduce the time interval:
• We need two new neighbouring points of Q. One before Q and the other after Q
• Like before, these new points should also satisfy a condition:
They must be at equal time intervals from Q
(i) Let us choose a point P2 before Q such that:
    ♦ The object reached P1, 0.25 s before Q. That is., when the stop watch showed 3.75 s  
Let us choose a point R2 after Q such that:  
    ♦ The object reached R2, 0.25 s after Q. That is., when the stop watch showed 4.25 s  
■ So the duration of travel from P2 to R2 = Δt = (t2 t1) = (4.25 - 3.75) = 0.5 s
(ii) After marking P2 and R2, we join them. This is shown in fig.3.39 below. The triangle is also shown:
Fig.3.39
• We get: Slope of DF = altitudebase R2R'P2R'2
ΔxΔt = (6.1413-4.2188)(4.25-3.75) = 1.92250.5 = 3.845 ms-1.
(iv) But we know that, this slope gives us only the 'average velocity' between P2 and R2
• Though Q falls between P2 and R2, 3.845 ms-1 is not the instantaneous velocity at Q
• The duration of travel from P2 to R2 is 0.5 s. This '0.5 s' is not an 'instant'

Let us write a summary of what we have done so far:
Step 1: We took points P and R which are centred at 4 s
• The duration of travel (Δt) from P to R was 2 s
• The average velocity with which the object travelled from P to R was 3.92 ms-1
• But the '2 s' is not an instant. So '3.92 ms-1' was discarded
Step 2: We took points P1 and R1 which are centred at 4 s
• The duration of travel (Δt) from P1 to R1 was 1 s
• The average velocity with which the object travelled from P1 to R1 was 3.86 ms-1
• But the '1 s' is not an instant. So '3.86 ms-1' was discarded
Step 3: We took points P2 and R2 which are centred at 4 s
• The duration of travel (Δt) from P2 to R2 was 0.5 s
• The average velocity with which the object travelled from P2 to R2 was 3.845 ms-1
• But the '0.5 s' is not an instant. So '3.845 ms-1' was discarded

• From the above 3 steps, it is clear that, with each step, the following two items are decreasing:
    ♦ Distance between P and R
    ♦ Time duration required for the travel between P and R
This can be shown as in fig.3.40 below:
Fig.3.40
• We can see that, the lines are becoming more and more aligned with the curve
• We must continue the steps until the time of travel between P and R is very small
• But it is not convenient to use graphs for further steps. because, the points will be very close to each other. We can use a table to do the calculations. It is shown below:

• The three steps that we already did are given in the first 3 rows of the table.
• Two more steps are done in the table. In the fifth step, Δt is very small. It is 0.01
■ But even this is not sufficient. Let us see the reason:
• Consider the ratio ΔxΔt . We know that this ratio gives the average velocity
• To get the instantaneous velocity, the denominator Δt must be very small (like 0.00000001 s)
• It must be very small. We call it: 'infinitesimal time' . The meaning of 'infinitesimal' can be seen here.
    ♦ And at the same time, it must not be equal to zero. Because, division by zero is undefined
• Mathematically, such a small denominator is indicated as: 'ΔxΔt when Δ 0'
    ♦ That is.,we need the ratio when 'Δt tends to zero'
• Such a ratio can be easily calculated using the principles of calculus which we will study in maths classes.
• The reader may try to write the answer after learning calculus. The answer will be obtained as 3.84 ms-1.
We know that, 'ΔxΔt' is a slope.

• When we use calculus, we get a value of ΔxΔt
    ♦ (The value of the ratio when the denominator Δt is very small)
• This value of the ratio, 'when Δt is very small', is also a slope
• It is the slope of the tangent to the curve at the point where we seek the instantaneous velocity
• The lines PR, P1R1P2Retc., touches the curve at two points
• But the tangent will touch the curve only at one point, which is Q

Another example:
In the above example, the equation of motion was x = 0.08t3. We used this equation to find the distances at various times. Now consider an object moving according to the equation: 
x = 8.5 + 2.5t2.
• What is the instantaneous velocity at t = 0 s ?
• What is the instantaneous velocity at t = 2 s ?
• What is the average velocity with which it travels between t = 2 and t = 4 s
Solution:
A. To find instantaneous velocities:
1. Based on the principles of calculus, the ratio 'ΔxΔt when Δ 0' is: 5t. 
2. So we get:
• At t = 0, the instantaneous velocity = 5 × 0 = 0 ms-1 
• At t = 2, the instantaneous velocity = 5 × 2 = 10 ms-1
B. To find average velocity:
1. Distance travelled when t = 2 s
= x(2) = (8.5 + 2.5×(2)2) = 18.5 m 
• Distance travelled when t = 4 s
= x(4) = (8.5 + 2.5×(4)2) = 48.5 m
2. So Δx = (48.5 - 18.5) = 30
• Δt = (t2 t1) = (4 - 2) = 2 s 
3. Average velocity = ΔxΔt 302 = 15 ms-1.

In the next section, we will see acceleration.

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Friday, July 20, 2018

Chapter 3.3 - Average velocity and Average speed

In the previous section we saw some applications of the position-time graph. In this section we will see average speed and average velocity.

• In the previous section we saw an object moving with a uniform velocity. 
• But in day to day life, we often see objects moving with non-uniform velocity.
■ Consider the object that we saw in the previous section. 
• We turned the stop watch on only when the object reached P. 
    ♦ From P onwards, it travelled with a uniform velocity of 12 ms-1
• But the object started it's journey from O. It started from rest at O.
■ If started from rest at O, how did it attain a velocity of 12 ms-1?
We can put this question in another way using the following 4 statements:
(i) At the instant when the object started from rest, the velocity will be zero
(ii) When it is at P, the velocity is 12 ms-1
(iii) So the velocity increased from zero to 12 ms-1
(iv) How did this increase happen?
• To find the answer, we will do another experiment. This time, we observe the motion of a car
• Also this time, will turn on the stop watch at the very instant when the car starts it's motion from O
• We will need the help of the odometer or trip meter of the car
(Trip meter is more preferable because, it can be reset to zero)  
Let us begin:
(i) At the instant when the car begins it's motion, t = 0, x = 0
(ii) When t = 1 s, the trip meter reading is 1.8 m
• That means, in the first second, the car moved 1.8 m. 
• Let this new position be A. 
    ♦ Then OA = 1.8 m
This is shown in fig.3.29 below:
 
Fig.3.29
(iii) When t = 2 s, the trip meter reading is 7.2 m
• That means, in the second second, the car moved (7.2 - 1.8) = 5.4 m. 
• Let this new position be B. Then: 
    ♦ AB = 5.4 m 
    ♦ OB = 7.2 m
This is shown in fig.3.23 above
(iv) When t = 3 s, the trip meter reading is 16.2 m
• That means, in the third second, the car moved (16.2 - 7.2) = 9 m. 
• Let this new position be C. Then: 
    ♦ BC = 9 m 
    ♦ OC = 16.2 m
This is shown in fig.3.23 above
(v) When t = 4 s, the trip meter reading is 28.8 m
• That means, in the fourth second, the car moved (28.8 - 16.2) = 12.6 m. 
• Let this new position be D. Then: 
    ♦ CD = 12.6 m
    ♦ OD = 28.8 m
This is shown in fig.3.23 above
(vi) When t = 5 s, the trip meter reading is 45 m
• That means, in the fifth second, the car moved (45 - 28.8) = 16.2 m. 
• Let this new position be E. Then: 
    ♦ DE = 16.2 m 
    ♦ OE = 45 m
This is shown in fig.3.23 above
(vii) When t = 6 s, the trip meter reading is 64.8 m
• That means, in the sixth second, the car moved (64.8 - 45) = 19.8 m. 
• Let this new position be E. Then: 
    ♦ EF = 19.8 m 
    ♦ OF = 64.8 m
This is shown in fig.3.23 above
(viii) When t = 7 s, the odometer reading is 88.2 m
• That means, in the seventh second, the car moved (45 - 28.8) = 23.4 m. 
• Let this new position be E. Then: 
    ♦ EG = 23.4 m 
    ♦ OG = 88.2 m

From the above values, the following two points become very clear: 
(i) In the previous experiment, 
    ♦ The time durations are all same: 1 s
    ♦ The distance travelled in each of these durations are the same: 12 m
• That means the object travelled with a uniform velocity
(ii) In the present experiment 
    ♦ The time durations are all same: 1 s
    ♦ But the distance travelled in each of these durations are not the same
• That means, the object travelled with non-uniform velocity
Let us plot the position-time graph. It is shown in fig.3.30 below:
Fig.3.30
• To avoid congestion, coordinates of only alternate points are written.
■ We see that, the graph is a curve

• We have seen that, slope of the position-time graph will give the velocity
• If the object moves with uniform velocity, the position-time graph will be a straight line
• Then we can easily calculate the slope. That slope will be same at all points
• But here, the graph is a curve. The slope will be different at different points.
• That means, the velocity is different at different points
• In such a situation, we use average velocity.
We can explain this using an example:
1. Consider the points D and F
• The car passed through both D and F 
2. Suppose someone wants to know the 'velocity with which the car travelled between D and F'
• We cannot give a definite answer. Because the velocity continuously changed
3. In such a situation we take the ratio: Displacement from D to FTime required for the travel from D to F
• We know that:
    ♦ Displacement from D to F = Δx = (x2-x1) = (y coordinate of F - y coordinate of D) 
    ♦ = (64.8 - 28.8) = 36
Time required to travel from D to F = Δt (t2-t1(x coordinate of F - x coordinate of D) 
    ♦ = (6 - 4) = 2
• So the ratio is 36= 18 ms-1.
4. This velocity of 18 ms-1 is the average velocity with which the object travelled from D to F. 
We can write the definition:
■ Average velocity is defined as the displacement (Δx) divided by the time duration (Δt) in which the displacement occurs
• The formula is:

    ♦ The bar over v is a standard notation used to indicate average quantities
5. We can check whether this formula is dimensionally correct:
• On the left side we have velocity [LT-1]
• On the right side, 
    ♦ in numerator we have distance [L]
    ♦ in denominator we have distance [T]
• Thus we get [LT-1] on both sides


We have seen that, if the velocity is uniform, we can easily calculate the velocity as the slope
■ Can we relate average velocity to slope?
Let us try:
• The portion between D and F is enlarged and shown in fig.3.31 below:
Fig.3.31
• We know that DF is a curve. But now, a straight line is draw between them in cyan colour
• Also a triangle DFF' is formed
• Now take the ratio: altitudebase
• We get: altitudebase FF'DF' = (64.8-28.8)(6-4) = 362 = 18 ms-1
So we can write:
■ Average velocity is the slope of the line joining the initial and final positions of the object in the position-time graph

• We have seen the details about average velocity. 
• Average speed can also be calculated in a similar way. 
• But in the numerator, instead of 'displacement', we use 'path length'. Thus we write:
Average speed =
Total path length between two pointsTime required for the travel between the two points

■ Average velocity is a vector quantity. It has both magnitude and direction 
■ Average speed is a scalar quantity. It has magnitude but no direction 
The difference between the two can be understood using an example. We will write it in steps:
1. Fig.3.32 below shows the positions of an object at various times shown by a stop watch
Fig.3.32
From the fig., the following information can be obtained:
(i) The object moves along the x axis
(ii) It started it's journey from the origin
    ♦ At that instant the stop watch was turned on
(iii) It travelled in the +x direction
(iv) After 18 seconds it reached P
    ♦ P is 360 m away from O
(v) Then it began to travel in the -x direction
(vi) After 6 more seconds, it reached Q
    ♦ Q is 240 m away from O
2. We are asked to find the following two items:
(i) The average velocity with which the object travelled from O to Q
(ii) The average speed with which the object travelled from O to Q 
Solution:
Part 1: To find average velocity: 
1. To get a better understanding of the problem, we will see the position-time graph of the motion of an object: 
Fig.3.32
• The graphs are curves. So it is clear that, the object travelled with non-uniform velocity
• But that does not affect this problem because we are asked to find average velocity and speed
2. Average velocity depends only on initial and final positions and also the time. 
• It does not matter whether it is uniform or non-uniform velocity
• We have:

x2 = position of the final point Q = 240 
x1 = position of the initial point O = 0 
• So displacement = Δx = (x2-x1) = (240-0) = 240
t2 = time at which the final point Q is reached = 24 s 
t1 = time at which the object is at the initial position = 0 s 
• So duration required for the displacement = Δt = (t2-t1) = (24-0) = 24 s
3. Thus average velocity = 24024 = 10 ms-1
Another method:
1. We have seen that, average velocity is the slope of the line joining initial and final points. 
• This line is shown in fig.3.33 below:
Fig.3.33
2. Clearly, altitude = QQ' = 240
• Base = OQ' = 24
• Thus we get: Slope = altitudebase QQ'OQ' = 24024 = 10 ms-1
Part 2:
To find average speed:
1. For this, we have to take the total path length
• Total path length = (Distance from O to P + Distance from P to Q) = (360+120) = 480
2. Total time - 24 s
3. We have: Average speed =
Total path length between two pointsTime required for the travel between the two points 48024 = 20 ms-1s
■ So we find that average velocity and average speed need not be the same


Now we will see a solved example. The link is given below:
Solved example 3.1

In the next section, we will see instantaneous velocity.

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