1 00:00:00,750 --> 00:00:06,160 PROFESSOR: Today we want to discuss wave packets. 2 00:00:06,160 --> 00:00:10,550 We have studied already the motivations that 3 00:00:10,550 --> 00:00:13,100 led to the Schrodinger equation and we even 4 00:00:13,100 --> 00:00:16,660 included the potential that described 5 00:00:16,660 --> 00:00:19,790 very non-trivial dynamics. 6 00:00:19,790 --> 00:00:23,150 With that Schrodinger equation, you could jump and solve 7 00:00:23,150 --> 00:00:27,650 the hydrogen atom, you could go and do the harmonic oscillator 8 00:00:27,650 --> 00:00:30,890 and all kinds of things. 9 00:00:30,890 --> 00:00:35,000 But we might as well develop, still, 10 00:00:35,000 --> 00:00:38,840 our tools and intuition of what's going on. 11 00:00:38,840 --> 00:00:45,010 And quite a lot of intuition comes from the free particle. 12 00:00:45,010 --> 00:00:47,030 And the free particle is interesting 13 00:00:47,030 --> 00:00:53,050 because you can go beyond the de Broglie wavelengths and the de 14 00:00:53,050 --> 00:00:54,020 Broglie waves. 15 00:00:54,020 --> 00:00:58,520 You had a single plane wave representing a particle 16 00:00:58,520 --> 00:01:02,150 with momentum and with energy, but now you 17 00:01:02,150 --> 00:01:06,380 become more sophisticated and consider the superposition 18 00:01:06,380 --> 00:01:07,210 of those waves. 19 00:01:07,210 --> 00:01:20,820 So we'll begin by discussing the wave packets and uncertainty. 20 00:01:24,340 --> 00:01:29,590 So it's our first look into this Heisenberg uncertainty 21 00:01:29,590 --> 00:01:31,630 relationships. 22 00:01:31,630 --> 00:01:39,640 And to begin with, let's focus it as fixed time, t 23 00:01:39,640 --> 00:01:40,960 equals zero. 24 00:01:40,960 --> 00:01:45,340 So we'll work with packets at t equals zero. 25 00:01:45,340 --> 00:01:49,240 And I will write a particular wave function 26 00:01:49,240 --> 00:01:53,330 that you may have at t equals 0, and it's 27 00:01:53,330 --> 00:02:00,220 a superposition of plane waves. 28 00:02:00,220 --> 00:02:03,610 So it would be e to the ikx. 29 00:02:03,610 --> 00:02:09,949 You sum over many of them, so you're going to sum over k, 30 00:02:09,949 --> 00:02:17,590 but you're going to do it with a weight, and that's 5k. 31 00:02:17,590 --> 00:02:21,160 And there's a lot to learn about this, 32 00:02:21,160 --> 00:02:30,070 but the physics that is encoded here is that any wave at time 33 00:02:30,070 --> 00:02:34,300 equals 0, this psi of x at time equals 0, 34 00:02:34,300 --> 00:02:39,850 can be written as a superposition of states 35 00:02:39,850 --> 00:02:43,840 with momentum h bar k. 36 00:02:43,840 --> 00:02:49,840 You remember e to the ikx represents a particle or a wave 37 00:02:49,840 --> 00:02:53,830 that carries momentum h bar k. 38 00:02:53,830 --> 00:02:59,320 So this whole idea here of a general wave function 39 00:02:59,320 --> 00:03:03,340 being written in this way carries physical meaning 40 00:03:03,340 --> 00:03:06,270 for us. 41 00:03:06,270 --> 00:03:08,400 It's a quantum mechanical meaning, 42 00:03:08,400 --> 00:03:13,330 the fact that this kind of wave has momentum. 43 00:03:13,330 --> 00:03:21,510 But this phi of k, however, suppose 44 00:03:21,510 --> 00:03:25,250 you know this wave function at time equals 0. 45 00:03:25,250 --> 00:03:28,580 Phi of k is then calculable. 46 00:03:28,580 --> 00:03:31,320 Phi of k can be determined, and that's 47 00:03:31,320 --> 00:03:36,320 the foundation of what's called Fourier's theorem, that gives 48 00:03:36,320 --> 00:03:40,430 you a formula for phi of k. 49 00:03:40,430 --> 00:03:44,250 And it's a very similar formula. 50 00:03:44,250 --> 00:03:49,780 1 over 2 pi, this time an integral over x. 51 00:03:49,780 --> 00:03:55,410 So you take this of psi of x0 that you know 52 00:03:55,410 --> 00:04:00,390 and then multiply by e to the minus ikx. 53 00:04:00,390 --> 00:04:07,100 Integrate over x, and out comes this function of k. 54 00:04:07,100 --> 00:04:15,640 So if you know phi of x0, you know phi of k. 55 00:04:15,640 --> 00:04:20,769 You can calculate this interval and you can rewrite phi of x0 56 00:04:20,769 --> 00:04:24,310 as a superposition of plane waves. 57 00:04:24,310 --> 00:04:28,360 So that's how you would do a Fourier representation. 58 00:04:28,360 --> 00:04:32,480 So somebody can give you an initial wave function, 59 00:04:32,480 --> 00:04:37,540 and maybe it's a sine function or a Gaussian or something, 60 00:04:37,540 --> 00:04:41,020 then what you would do if you wanted to rewrite it 61 00:04:41,020 --> 00:04:48,130 in this way, is calculate phi of k, because you know this psi, 62 00:04:48,130 --> 00:04:52,490 you can calculate this integral, at least with a computer. 63 00:04:52,490 --> 00:04:54,460 And once you know phi of k, you have 64 00:04:54,460 --> 00:05:00,580 a way of writing psi as a superposition of plane waves. 65 00:05:00,580 --> 00:05:04,600 So we've talked about this before, 66 00:05:04,600 --> 00:05:07,540 because we were doing wave packets before 67 00:05:07,540 --> 00:05:13,420 and we got some intuition about how you form a wave packet 68 00:05:13,420 --> 00:05:14,500 and how it moves. 69 00:05:14,500 --> 00:05:16,910 Now we didn't put the time dependence here, 70 00:05:16,910 --> 00:05:20,530 but that can wait. 71 00:05:20,530 --> 00:05:25,810 What I wish to explain now is how 72 00:05:25,810 --> 00:05:29,620 by looking at these expressions, you 73 00:05:29,620 --> 00:05:36,220 can understand the uncertainties that you find on the wave 74 00:05:36,220 --> 00:05:40,810 function, position, and momentum uncertainties, 75 00:05:40,810 --> 00:05:42,190 how they are related. 76 00:05:42,190 --> 00:05:46,960 So that is our real goal, understanding 77 00:05:46,960 --> 00:05:49,290 the role of uncertainties here. 78 00:05:49,290 --> 00:05:52,690 If phi of k has some uncertainty, 79 00:05:52,690 --> 00:05:57,820 how is the uncertainty in psi determined? 80 00:05:57,820 --> 00:06:01,850 So that's what we're looking for. 81 00:06:01,850 --> 00:06:04,180 So relationship of uncertainties. 82 00:06:06,820 --> 00:06:10,975 Now as before, we will take a phi of k, 83 00:06:10,975 --> 00:06:17,140 that we've usually be in writing, that depends on k 84 00:06:17,140 --> 00:06:22,906 and it's centered around some value k0. 85 00:06:22,906 --> 00:06:27,000 It's some sort of nice, centered function. 86 00:06:27,000 --> 00:06:33,300 And it has then, we say, some uncertainty 87 00:06:33,300 --> 00:06:36,030 in the value of the momentum. 88 00:06:36,030 --> 00:06:40,820 That is this signal, this phi of k 89 00:06:40,820 --> 00:06:45,336 that we're using to produce this packet. 90 00:06:45,336 --> 00:06:48,850 It has some uncertainty, it's not totally sharp, 91 00:06:48,850 --> 00:06:53,070 it's peaked around k0 but not fully sharp. 92 00:06:53,070 --> 00:06:56,630 So the uncertainty is called delta k 93 00:06:56,630 --> 00:07:01,360 and it's some typical width over here. 94 00:07:01,360 --> 00:07:05,600 Delta k is then uncertainty. 95 00:07:10,670 --> 00:07:13,040 Now it's not the purpose of today's lecture 96 00:07:13,040 --> 00:07:17,240 to make a precise definition of what the uncertainty is. 97 00:07:17,240 --> 00:07:19,610 This will come later. 98 00:07:19,610 --> 00:07:21,830 At this moment, you just want to get 99 00:07:21,830 --> 00:07:25,340 the picture and the intuition of what's going on. 100 00:07:25,340 --> 00:07:27,740 And there is some uncertainty here, 101 00:07:27,740 --> 00:07:31,130 perhaps you would say, look at those points 102 00:07:31,130 --> 00:07:36,650 where the wave goes from peak value to half value 103 00:07:36,650 --> 00:07:38,710 and see what is the width. 104 00:07:38,710 --> 00:07:41,490 That's a typical uncertainty. 105 00:07:41,490 --> 00:07:45,710 So all what we're going to do in these arguments 106 00:07:45,710 --> 00:07:47,880 is get for you the intuition. 107 00:07:47,880 --> 00:07:53,480 Therefore, the factors of 2 are not trustable. 108 00:07:53,480 --> 00:07:56,480 If you're trying to make a precise statement, 109 00:07:56,480 --> 00:07:59,450 you must do precise definitions. 110 00:07:59,450 --> 00:08:01,700 And that will come later, probably 111 00:08:01,700 --> 00:08:04,400 in about one or two lectures. 112 00:08:04,400 --> 00:08:08,510 So at this moment, that's the uncertainty, delta k. 113 00:08:08,510 --> 00:08:13,305 And let's assume that this phi of k is real. 114 00:08:21,180 --> 00:08:28,430 And its peaked around k0 uncertainty delta k. 115 00:08:28,430 --> 00:08:35,780 Now what happens with psi of x? 116 00:08:35,780 --> 00:08:41,480 Well, we had our statements about the stationary phase 117 00:08:41,480 --> 00:08:45,260 that you already are practicing with them for this homework. 118 00:08:47,870 --> 00:08:51,200 If you want to know where this function peaks, 119 00:08:51,200 --> 00:08:55,880 you must look where the phase, this phi-- 120 00:08:55,880 --> 00:08:59,390 we say it's real, so it doesn't contribute to the phase-- 121 00:08:59,390 --> 00:09:05,030 where the phase, which is here, is stationary, 122 00:09:05,030 --> 00:09:09,680 given the condition that it should happen at k0. 123 00:09:09,680 --> 00:09:11,870 The only contribution to the integral 124 00:09:11,870 --> 00:09:14,000 is basically around k0. 125 00:09:14,000 --> 00:09:16,130 So in order to get something, you 126 00:09:16,130 --> 00:09:19,520 must have a stationary phase, and the phase 127 00:09:19,520 --> 00:09:22,580 must be stationary as a function of k, 128 00:09:22,580 --> 00:09:25,240 because you're integrating over k. 129 00:09:25,240 --> 00:09:29,300 And the phase is kx, the derivative 130 00:09:29,300 --> 00:09:36,560 with respect to k of the face is just x, 131 00:09:36,560 --> 00:09:42,290 and that must vanish, therefore, so you expect this to be 132 00:09:42,290 --> 00:09:46,280 peaked around x equals zero. 133 00:09:46,280 --> 00:10:01,940 So the x situation, so psi of x0 peaks at x equals 0. 134 00:10:01,940 --> 00:10:06,340 And so you have a picture here. 135 00:10:06,340 --> 00:10:12,820 And if I have a picture, I would say, well it peaks around the x 136 00:10:12,820 --> 00:10:13,990 equals 0. 137 00:10:13,990 --> 00:10:17,560 So OK, it's like that. 138 00:10:17,560 --> 00:10:20,530 And here we're going to have some uncertainty. 139 00:10:20,530 --> 00:10:26,330 Here is psi of x and 0, and here is x. 140 00:10:29,330 --> 00:10:38,200 And let me mention, I've already become fairly imprecise here. 141 00:10:38,200 --> 00:10:41,620 If you were doing this, you probably 142 00:10:41,620 --> 00:10:43,310 would run into trouble. 143 00:10:43,310 --> 00:10:50,510 I've sort of glossed over a small complication here. 144 00:10:50,510 --> 00:10:54,600 The complication is that this, when 145 00:10:54,600 --> 00:10:58,040 I talk about the peaking of psi, and you probably 146 00:10:58,040 --> 00:11:05,240 have seen it already, you have to worry whether psi is real 147 00:11:05,240 --> 00:11:07,610 or psi is complex. 148 00:11:07,610 --> 00:11:11,120 So what is this psi here? 149 00:11:11,120 --> 00:11:12,560 Should it be real? 150 00:11:12,560 --> 00:11:14,490 Well actually, it's not real. 151 00:11:18,640 --> 00:11:21,190 You've done, perhaps, in the homework already 152 00:11:21,190 --> 00:11:26,220 these integrals, and you see that psi is not real. 153 00:11:26,220 --> 00:11:31,210 So when we say it peaks at x equals 0, 154 00:11:31,210 --> 00:11:33,460 how am I supposed to plot psi? 155 00:11:33,460 --> 00:11:36,640 Am I plotting the real part, the imaginary part, 156 00:11:36,640 --> 00:11:37,710 the absolute value? 157 00:11:37,710 --> 00:11:42,760 So it's reasonable to plot the absolute value 158 00:11:42,760 --> 00:11:49,360 and to say that psi absolute value peaks at x equals 0. 159 00:11:51,980 --> 00:12:02,340 And there will be some width again here, delta x, width. 160 00:12:02,340 --> 00:12:08,610 And that's the uncertainty in psi of x. 161 00:12:08,610 --> 00:12:13,490 So the whole point of our discussion for the next 10 162 00:12:13,490 --> 00:12:16,820 minutes is to just try to determine 163 00:12:16,820 --> 00:12:20,570 the relation between delta k and delta x 164 00:12:20,570 --> 00:12:24,030 and understand it intuitively.