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Simple Nature - Light and Matter

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around until I got this result, since a decrease of exactly 10% iseasy to discuss. Notice how the amplitude after two cycles is about0.81 m, i.e., 1 m times 0.9 2 : the amplitude has again dropped byexactly 10%. This pattern continues for as long as the simulationruns, e.g., for the last two cycles, we have 0.34818/0.38694=0.89982,or almost exactly 0.9 again. It might have seemed capricious when Ichose to use the unrealistic equation F = −bv, but this is the payoff.Only with −bv friction do we get this kind of mathematically simpleexponential decay.Because the decay is exponential, it never dies out completely;this is different from the behavior we would have had with Coulombfriction, which does make objects grind completely to a stop at somepoint. With friction that acts like F = −bv, v gets smaller as theoscillations get smaller. The smaller <strong>and</strong> smaller force then causesthem to die out at a rate that is slower <strong>and</strong> slower.Analytic treatmentTaking advantage of this unexpectedly simple result, let’s findan analytic solution for the motion. The numerical output suggeststhat we assume a solution of the forme / A damped sine wave, ofthe form x = Ae −ct sin(ω f t + δ).f / Self-check G.x = Ae −ct sin(ω f t + δ) ,where the unknown constants ω f <strong>and</strong> c will presumably be related tom, b, <strong>and</strong> k. The constant c indicates how quickly the oscillations dieout. The constant ω f is, as before, defined as 2π times the frequency,with the subscript f to indicate a free (undriven) solution. Allour equations will come out much simpler if we use ωs everywhereinstead of fs from now on, <strong>and</strong>, as physicists often do, I’ll generallyuse the word “frequency” to refer to ω when the context makes itclear what I’m talking about. The phase angle δ has no real physicalsignificance, since we can define t = 0 to be any moment in time welike.self-check GIn figure f, which graph has the greater value of c? ⊲ Answer, p. 923The factor A for the initial amplitude can also be omitted withoutloss of generality, since the equation we’re trying to solve, ma +bv + kx = 0, is linear. That is, v <strong>and</strong> a are the first <strong>and</strong> secondderivatives of x, <strong>and</strong> the derivative of Ax is simply A times thederivative of x. Thus, if x(t) is a solution of the equation, thenmultiplying it by a constant gives an equally valid solution. This isanother place where we see that a damping force proportional to v isthe easiest to h<strong>and</strong>le mathematically. For a damping force proportionalto v 2 , for example, we would have had to solve the equationma + bv 2 + kx = 0, which is nonlinear.For the purpose of determining ω f <strong>and</strong> c, the most general formwe need to consider is therefore x = e −ct sin ω f t , whose first <strong>and</strong>174 Chapter 3 Conservation of Momentum

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