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(ta initials) first name (print) last name (print) brock id (ab17cd) (lab date) Experiment 2 Harmonic motion Prelab preparation Print a copy of this experiment to bring to your scheduled lab session. The data, observations and notes entered on these pages will be needed when you write your lab report. Compile these printouts to create a lab book for the course. Perform the following tasks as indicated. Then answer the following questions and submit them in your Harmonic Motion pre-lab assignment, due at Turnitin the day before you perform your experiment in the lab. Turnitin will not accept submissions after the due date. Unsubmitted pre-lab assignments are assigned a grade of zero. The Harmonic Motion pre-lab template is found at the Lab Documents page at the course web site: http://www.physics.brocku.ca/courses/1p91_dagostino/lab-manual/ 1. Video Introduction Watch the video introduction. 2. Review If needed, review exponential and logarithmic functions by completing the module FLAP MATH 1-5, Exponential and logarithmic functions, found at http://www.physics.brocku.ca/pplato Begin by trying the fast-track quiz to gauge your understanding of the topic and if necessary review the module in depth, then try the exit test. 3. Review If needed, review trigonometric functions by completing the FLAP module FLAP MATH 1-6: Trigonometric functions, found at http://www.physics.brocku.ca/pplato Begin by trying the fast-track quiz to gauge your understanding of the topic and if necessary review the module in depth, then try the exit test. 4. Think about a back-and-forth motion that you remember seeing or experiencing. Briefly describe the motion. In particular, what happened to the amplitude of the motion as time passed? 5. Sketch a rough position-time graph of the motion that you thought about in the previous question. It s not necessary to label the axes with numbers; what we are most interested in is that you can approximately represent the long-term behaviour of a realistic back-and-forth motion. 9

10 EXPERIMENT 2. HARMONIC MOTION 6. Guess what kind of function might accurately model the graph that you roughly sketched in the previous question. For instance, is it a linear function? Is it a quadratic function? Is it some combination of functions? 7. Play with the simulation found here: https://phet.colorado.edu/en/simulation/pendulum-lab Experiment by varying the amount of friction in each run. After you have explored a few runs of the simulation, briefly describe any additional understanding that you have gained beyond what you wrote in Question 4. Also briefly describe how increasing the friction changes the motion. If any new understanding that you have gained from the simulation causes you to revise your approximate graph of such a motion, sketch the new graph. If any new understanding that you have gained from the simulation causes you to revise your guess about what kind of function models this kind of motion, revise your guess here. 8. Briefly summarize what you have learned about this kind of motion from doing the prelab exercises. 9. Refresh your memory by reviewing the Error1 and Error2 WeBWorK homework assignments. 10. Refresh your memory by reviewing the Physicalab videos.! Important! Be sure to have every page of this printout signed by a TA before you leave at the end of the lab session. All your work needs to be kept for review by the instructor, if so requested. CONGRATULATIONS! YOU ARE NOW READY TO PROCEED WITH THE EXPERIMENT! The simple harmonic oscillator A simple harmonic oscillator (SHO) is a model system that is used to describe numerous real physical systems. The reason for this is profound: the same fundamental equations that describe the motion of a mass-on-a-spring also describe, to a very good approximation, the inter-atomic forces that hold all matter together. At least in a first approximation, we can fairly accurately pretend that every solid object we touch is held together by springs connecting pairs of atoms. The details of these interactions are studied in advanced courses in condensed matter physics and quantum mechanics, but two masses connected by a coiled elastic spring represent an excellent model system, from which much can be learned. With no external forces applied to a solid material, the inter-atomic springs are at their equilibrium lengths, neither stretched nor compressed. The application of an external stretching force to the material will cause these springs to extend, thereby increasing the bulk length of the material. When the applied external force is removed, the springs return to their equilibrium lengths, restoring the material to its original dimensions. Such restoring forces may be overcome by a large enough applied external force that will cause the object to deform permanently or to break. The maximum force applicable without permanent distortion is called the elastic limit of the material. Hooke s law states that the stretch or compression x of a material is directly proportional to the applied force F. The proportionality constant, called the spring constant k, has the units of Newtons per metre (N/m) and is a measure of the stiffness of the material being considered. This proportionality between force and elongation has been found to be an excellent approximation for any body as long as the elastic limit of the material is not exceeded. For an object attached to a spring, Hooke s law is F s = kx, (2.1)

11 where F s is the force exerted by the spring on the object and x is the displacement of the object from its equilibrium position. The negative sign expresses the fact that the force exerted by the spring on the object is in the direction opposite to the object s displacement. For this reason, it is often described as a restoring force, because it tends to restore equilibrium. That is, when the object is not at its equilibrium position, the force that the spring exerts on the object is directed towards the equilibrium position. If the spring force and gravity are the only forces acting on the object, the system is called a simple harmonic oscillator, and the object undergoes simple harmonic motion sinusoidal oscillations about the equilibrium point, with a constant amplitude, and a constant frequency that does not depend on the amplitude. Simple harmonic motion is equivalent to an object moving around the circumference of a circle at constant speed, in the sense that the same formulas describe each kind of motion. In the absence of friction, the oscillations will continue forever. Friction robs the oscillator of its mechanical energy, transferring it to thermal energy, and so the oscillations decay, and eventually stop altogether. This process is called damping, and so in the presence of friction, this kind of motion is called damped harmonic oscillation. Frequently this frictional force can be approximated as proportional to the velocity of the moving mass (think of air resistance), F d = Rv. Depending on the strength of the friction coefficient R, a damped harmonic oscillator can either oscillate with a frequency slightly smaller than in the non-damped case, and with an amplitude decreasing with time (underdamped oscillator), or decay exponentially to the equilibrium position, without oscillations (overdamped oscillator). Mass on a vertical spring When an object of mass m is attached to a hanging spring, the object experiences a gravitational force F g = mg and a force due to the additional stretch of the spring. The latter force is described by Hooke s law, F s = ky 0, where y 0 is the magnitude of the additional stretch of the spring. By drawing a free-body diagram for the hanging object, and doing a bit of algebraic manipulation, you can arrive at the following conclusions: F g = F s mg = ky 0 m = k g y 0. (2.2) If the mass is displaced from its new equilibrium position and released, it will begin to oscillate according to y = A 0 cos(ω 0 t + φ), ω 0 = k/m = 2πf 0 = 2π (2.3) T 0 where A 0 and φ are the initial amplitude and phase angle of the oscillation, T 0 is the period in seconds, and ω 0 is the angular speed in radians/second. If a damping force F d is present, the oscillation decays exponentially at a rate determined by the damping coefficient γ: y = A 0 e ( γt) cos(ω d t + φ), γ = R 2m, ω d = ω 2 0 γ2 (2.4) Note two interesting details; first, the damped frequency of oscillations, ω d, is smaller than ω 0 because of the subtraction of γ 2 under the square root. However, if R is not very large, this reduction is not all that noticeable, even though the decrease in the amplitude due to the e γt term may be readily observed. Second, in the case of air resistance, F d = Rv is an approximate relation, valid only for slow speeds. As the speed increases, the turbulent air flow exerts resistance that is proportional to the square of the velocity, F d = Cv 2. Here C is the so-called drag coefficient. Unfortunately, this expression cannot be solved analytically and one has to use numerical methods (computer) to determine approximate solutions. Note also that the hanging spring is stretched by its own weight and may exhibit twisting as well as lateral oscillations when stretching, factors that are neglected in our analysis. One other simplifying assumption: this experiment assumes an ideal massless spring connected to a point mass m. Even with all these approximations, Equation 2.4 lends itself very nicely to an experimental investigation.

12 EXPERIMENT 2. HARMONIC MOTION Procedure and analysis The experimental setup consists of a vertical stand from which hangs a spring. A platform attached to the bottom of the spring accepts various mass loads. The spring-mass system is free to move in the vertical direction. When the platform is static, its height above the table can be measured with a ruler. When the system is in motion, Physicalab can be used to record the time-dependent change in distance from a rangefinder to the bottom of the platform. The rangefinder measures distance by emitting an ultrasonic pulse and timing the delay for the echo to return. Part 1: Static properties of springs In the following exercises you will determine the force constants of two different springs, distinguished as #1 and #2. You can then verify that their combined force constant satisfies the equation derived in the review section of the experiment. Note: Use positive k values in all the following steps. Equation 2.2 represents a straight line with slope k/g = m/ y so that k = m/ y g. By varying m, measuring y 0 and fitting the resulting data to the equation of a straight line, the force constant k for the spring can be determined. Note that the absolute distance y 0 does not matter, however the change in distance y with mass m is critical. Suspend spring #1, labelled [ ], from the holder and load it with the 50 g platform. Use a ruler to carefully measure the distance y from the top of the table to the bottom of the platform to a precision of 1 mm. Record your result in Table 2.1. Determine the mass required to bring the platform near the top of the table and record this new distance, then select several intermediate masses and fill in Table 2.1.? Why do you want to determine a mass that brings the platform near to the table? Enter the data pairs (y,m) in the Physicalab data window. Select scatter plot and click Draw to generate a graph of your data. mass (kg) y (m) Table 2.1: Data for determining the spring force constant k 1 of spring #1, labelled [ ]? Did you choose to include the mass of the platform (50g) as part of the stretching mass m in Table 2.1? How would the graph and the resulting value for the spring constant k be affected by your choice? Select fit to: y= and enter A+B*x in the fitting equation box. Click Draw to perform a linear fit on your data, then evaluate k 1 and the associated error σ(k 1 ). Click Send to: to email yourself a copy of the graph for later inclusion in your lab report. B =... ±... A =... ±... k 1 =... =... =...

13 k 1 =... =... =... k 1 =... ±... Repeat the above procedure using spring #2, labelled [ ], recording your results in Table 2.2, then determine the spring constant k 2 for the spring. mass (kg) y (m) Table 2.2: Data for determining the spring force constant k 2 of spring #2, labelled [ ] B =... ±... A =... ±... k 2 =... =... =... k 2 =... =... =... k 2 =... ±... Connect together springs #1 and #2, and repeat the procedure, entering your data in Table 2.3, to determine the experimental effective spring constant k e of the two springs: mass (kg) y (m) Table 2.3: Data for determining the effective spring force constant k e of springs #1 and #2 B =... ±... A =... ±... k e =... =... =... k e =... =... =... k e =... ±... Calculate the theoretical effective spring constant k e and k e for the two springs #1 and #2:

14 EXPERIMENT 2. HARMONIC MOTION k 1 =... ±... k 2 =... ±... k e = k 1 k 2 =... =... k 1 + k 2 k e = k 2 e ( k1 ) 2 ( ) 2 k2 + =... =... k1 2 k2 2 Part 2: Damped harmonic oscillator k e =... ±... You will now explore the behaviour in time of an oscillating mass with the aid of a computer-controlled rangefinder. This device sends out an ultrasonic pulse that reflects from an object in the path of the conical beam and returns to the rangefinder as an echo. The rangefinder measures the elapsed time to determine the distance to the object, using the speed of sound at sea level as reference. By accumulating a series of coordinate points (ω,m) and fitting your data to Equation 2.4, you can use several methods to determine the spring constant for the oscillating mass system. Select one of the two springs to use: will use spring labelled [ ]. With each of the masses used previously with this spring, raise the platform a small distance, then release it to start the mass swinging vertically. Wait until the spring/mass system no longer exhibits any erratic oscillations. Login to the Physicalab software. Check the Dig1 box and choose to collect 200 points at 0.05 s/point. Click Get data to acquire a data set. Select scatter plot, then Click Draw. Your points should display a smooth slowly decaying sine wave, without peaks, stray points, or flat spots. If any of these are noted, adjust the position of the rangefinder and acquire a new data set. Select fit to: y= and enter A*cos(B*x+C)*exp(-D*x)+E in the fitting equation box. Click Draw. If you get an error message the initial guesses for the fitting parameters may be too distant from the required values for the fitting program to properly converge. Look at your graph and enter some reasonable initial values for the amplitude A of the wave and the average (equilibrium) distance E of the wave from the detector. C corresponds to the initial phase angle of the sine wave at x=0. The angular speed B (in radians/s) is given by B= 2π/T. Estimate the time x= T between two adjacent minima of the sine wave then estimate and enter an initial guess for B. The damping coefficient D determines the exponential decay rate of the wave amplitude to the equilibrium distance E. When D = 1/x, the envelope will have decreased from A 0 to A 0 e 1 = A 0 /e = A 0 /2.718 A 0 /3. Make an initial guess for D by estimating the time t=x required for the envelope to decrease by 2/3. Check that the fitted waveform overlaps well your data points, then label the axes and include as part of the title the value of mass m used. Email yourself a copy of all graphs as part of your lab data set. Record the results of the fit in Table 2.4, then complete the table as before.

15 mass (kg) y 0 (m) ω 0 (rad/s) γ (s 1 ) Table 2.4: Experimental results for damped harmonic oscillator The spring constant k can be determined as before from the slope of a line fitted through the (y 0,m) data in Table 2.4. Generate and save the graph, then record the result below: k(y 0 ) =... ±... The spring constant k can also be determined fron the period of oscillation of the mass. Rearranging the terms in Equation 2.3 yields m = k/ω0 2. Enter the coordinate pairs from Table 2.4 in the form (ω 0,m) and view the scatter plot of your data. Select fit to: y= and enter A+B/x**2 in the fitting equation box. This is more convenient than squaring all the ω 0 values and fitting to A+B/x. Click Draw to perform a quadratic fit on your data. Print the graph, then enter below the value for the spring constant: k(ω 0 ) =... ±... The damped harmonic oscillator equation 2.4 predicts that the frequency of oscillation depends on the damping coefficient γ so that your experiment actually yields values for ω d rather than ω 0. Calculate ω 0 from ω d using an average value for γ.? Which ω d value should be used? Why? ω 0 =... =... =...? Is the difference between ω d and ω 0 significant? Explain. Calibration of rangefinder It was assumed that the rangefinder is properly calibrated and measuring the correct distance. It is always a good practice to check the calibration of instrument scales against a known good reference, in this case the ruler scale. Calibration errors are systematic errors and can be corrected. Once the amount of mis-calibration is determined, the mis-calibrated data can be adjusted to represent correct values. Check the calibration of your rangefinder against the ruler. Compare the distance results for two points from the (y 0,m) data in Part 1 (ruler) and Part 2 (rangefinder). The mass difference between the points must be the same for both parts. If the rangefinder is calibrated, the distance differences should also be the same (within measurement error).? How do you choose the two calibration points that give the least relative error?

16 EXPERIMENT 2. HARMONIC MOTION Part 1: y 1 =... y 2 =... y 2 y 1 =... ±... Part 2: y 1 =... y 2 =... y 2 y 1 =... ±...? Why are two calibration points sufficient? IMPORTANT: BEFORE LEAVING THE LAB, HAVE A T.A. INITIAL YOUR WORKBOOK! Lab report Go to our web page http://www.physics.brocku.ca/courses/1p91_dagostino/lab-manual/ to access the online lab report template for this experiment. Complete the template as instructed and submit it to Turnitin before the lab report submission deadline, late in the evening six days following your scheduled lab session. Turnitin will not accept submissions after the due date. Unsubmitted lab reports are assigned a grade of zero. Notes:...............