1 00:00:00,510 --> 00:00:03,630 PROFESSOR: Next is this phenomenon that when 2 00:00:03,630 --> 00:00:08,760 you have a wave packet and it moves 3 00:00:08,760 --> 00:00:13,390 it can change shape and get distorted. 4 00:00:13,390 --> 00:00:17,700 And that is a very nice phenomenon 5 00:00:17,700 --> 00:00:22,680 that takes place in general and causes 6 00:00:22,680 --> 00:00:25,410 technological complications. 7 00:00:25,410 --> 00:00:28,440 And it's conceptually interesting. 8 00:00:28,440 --> 00:00:32,729 So let's discuss it. 9 00:00:32,729 --> 00:00:35,340 So it's still wave packets. 10 00:00:35,340 --> 00:00:44,680 But now we have to go back and add some time to it. 11 00:00:44,680 --> 00:00:49,380 So shape changes. 12 00:00:53,360 --> 00:00:58,490 So we had a psi of x and t is equal to 1 13 00:00:58,490 --> 00:01:06,480 over square root of 2 pi phi of k e to the ikx 14 00:01:06,480 --> 00:01:09,230 e to the minus i omega of kt. 15 00:01:12,020 --> 00:01:16,340 And what did we do with this to analyze how it propagates? 16 00:01:16,340 --> 00:01:23,960 We expanded omega of k as omega of k0, 17 00:01:23,960 --> 00:01:29,750 which, again, this quantity is centered and peaks around k0, 18 00:01:29,750 --> 00:01:39,800 plus k minus k0 times d omega dk at k0 19 00:01:39,800 --> 00:01:51,740 plus 1/2 k minus k0 squared, the second omega, dk squared at k0. 20 00:01:51,740 --> 00:01:54,610 And it might seem that this goes on forever. 21 00:01:57,170 --> 00:01:58,850 And what did we do before? 22 00:01:58,850 --> 00:02:03,350 We looked at this thing and we did the integral with this term 23 00:02:03,350 --> 00:02:07,090 and ignored the next. 24 00:02:07,090 --> 00:02:10,009 And with this term, we discovered 25 00:02:10,009 --> 00:02:17,780 that the profile moves with this velocity, the group velocity. 26 00:02:17,780 --> 00:02:21,970 Now we want to go back and at least get 27 00:02:21,970 --> 00:02:26,210 an idea of how this term could change the result. 28 00:02:26,210 --> 00:02:30,020 And it would change the result by deforming 29 00:02:30,020 --> 00:02:32,360 the shape of the packet. 30 00:02:32,360 --> 00:02:37,400 So it is of interest to know, for example, how long you have 31 00:02:37,400 --> 00:02:40,970 to wait before your packet gets totally deformed, 32 00:02:40,970 --> 00:02:44,370 or how do you evolve a packet. 33 00:02:44,370 --> 00:02:50,120 So we need to recall these derivatives. 34 00:02:50,120 --> 00:03:00,880 So the omega vk is the same as de dp by multiplying by h bar. 35 00:03:00,880 --> 00:03:04,100 And this you'll remember, was p over m. 36 00:03:07,190 --> 00:03:14,030 The edp is p over m and is equal to h bar k over m. 37 00:03:18,160 --> 00:03:25,330 So the second omega, dk squared. 38 00:03:25,330 --> 00:03:29,590 I must differentiate the first derivative with respect to k. 39 00:03:29,590 --> 00:03:32,440 So I differentiate the first derivative with respect k. 40 00:03:32,440 --> 00:03:37,420 And now I get just h bar over m, which is quite nice. 41 00:03:37,420 --> 00:03:44,950 And the third derivative, the 3 omega, dk cubed, is 0. 42 00:03:44,950 --> 00:03:49,000 And therefore, I didn't have to worry about these terms. 43 00:03:49,000 --> 00:03:51,820 The series terminates. 44 00:03:51,820 --> 00:03:55,390 The Taylor series terminates for this stuff. 45 00:03:55,390 --> 00:03:56,305 Yes? 46 00:03:56,305 --> 00:03:57,679 AUDIENCE: The reason this happens 47 00:03:57,679 --> 00:03:59,040 is because we're [INAUDIBLE]. 48 00:03:59,040 --> 00:04:00,040 PROFESSOR: That's right. 49 00:04:02,950 --> 00:04:07,670 So of what is it that we get? 50 00:04:07,670 --> 00:04:20,140 Well, this term is roughly then 1/2 k minus k0 squared 51 00:04:20,140 --> 00:04:22,210 times h bar over m. 52 00:04:25,730 --> 00:04:37,500 And we can go back to the integral 53 00:04:37,500 --> 00:04:38,870 that we're trying to do. 54 00:04:38,870 --> 00:04:43,790 We don't do it again or not by any means. 55 00:04:43,790 --> 00:04:46,310 But just observe what's going on there. 56 00:04:50,010 --> 00:04:56,460 And we have an e to the minus i omega of kt 57 00:04:56,460 --> 00:04:58,910 that we did take into account. 58 00:04:58,910 --> 00:05:02,310 But the term that we're dropping now 59 00:05:02,310 --> 00:05:07,740 is a term that is minus i omega of k, 60 00:05:07,740 --> 00:05:13,380 well, whatever we have here, 1/2 k minus k0 61 00:05:13,380 --> 00:05:16,280 squared h bar over mt. 62 00:05:19,660 --> 00:05:24,050 That's the phase that we ignored before. 63 00:05:32,250 --> 00:05:41,140 But now we'll just say, that we expect, therefore, 64 00:05:41,140 --> 00:05:44,770 that the shape doesn't change as long as we 65 00:05:44,770 --> 00:05:47,530 can ignore this phase. 66 00:05:47,530 --> 00:05:52,015 And this phase would start changing shape of the object. 67 00:05:54,800 --> 00:06:06,370 So our statement is going to be that we have no shapes. 68 00:06:06,370 --> 00:06:09,000 So let's imagine you started with a packet 69 00:06:09,000 --> 00:06:11,610 that sometime t equals 0. 70 00:06:11,610 --> 00:06:14,710 And then you let time go by. 71 00:06:14,710 --> 00:06:18,370 Well, there's some numbers here and time is increasing. 72 00:06:18,370 --> 00:06:22,740 At some point, this phase is going to become unignorable. 73 00:06:22,740 --> 00:06:25,420 And it's going to start affecting everything. 74 00:06:25,420 --> 00:06:34,550 But we have no shape change, or no appreciable shape change, 75 00:06:34,550 --> 00:06:42,650 as long as this quantity is much less than 1. 76 00:06:42,650 --> 00:06:48,500 So as long as say, k minus k0 squared 77 00:06:48,500 --> 00:06:56,570 h bar over m absolute value of t is much less than 1, 78 00:06:56,570 --> 00:06:57,690 no shape change. 79 00:07:02,590 --> 00:07:08,110 Now it's convenient to write it in terms of things 80 00:07:08,110 --> 00:07:10,520 that are more familiar. 81 00:07:10,520 --> 00:07:17,990 So we should estimate this thing. 82 00:07:17,990 --> 00:07:25,850 Now we're doing estimates in a very direct and rough way here. 83 00:07:25,850 --> 00:07:32,220 But look, your integrals are around k0. 84 00:07:32,220 --> 00:07:35,450 And as you remember, they just extend a little bit 85 00:07:35,450 --> 00:07:37,190 because it has some width. 86 00:07:37,190 --> 00:07:43,770 So k minus k0, as you do the integral over k, 87 00:07:43,770 --> 00:07:46,760 you're basically saying this thing 88 00:07:46,760 --> 00:07:50,660 is about the size of the uncertainty in k. 89 00:07:50,660 --> 00:07:53,825 So I'll put here delta k squared. 90 00:07:57,020 --> 00:08:05,880 Then you'll have h bar t over m much less than 1. 91 00:08:05,880 --> 00:08:10,790 Now h bar times delta k is delta p. 92 00:08:10,790 --> 00:08:20,570 So this equation is also of the form delta p squared t 93 00:08:20,570 --> 00:08:28,020 over h bar m much less than 1. 94 00:08:28,020 --> 00:08:31,720 There's several forms of this equation that is nice. 95 00:08:31,720 --> 00:08:35,210 So this is a particularly nice form. 96 00:08:37,929 --> 00:08:43,929 So if you know the uncertainty and momentum of your packet, 97 00:08:43,929 --> 00:08:49,360 or wave packet, up to what time, you can wait 98 00:08:49,360 --> 00:08:54,390 and there's no big deformation of this wave packet. 99 00:08:54,390 --> 00:08:57,940 Another thing you can do is involve the uncertainty in x. 100 00:09:01,210 --> 00:09:06,640 Because, well, delta p delta x is equal to h bar. 101 00:09:06,640 --> 00:09:08,220 So we can do that. 102 00:09:19,250 --> 00:09:33,270 And so with delta p times delta x equal to about h bar, 103 00:09:33,270 --> 00:09:45,420 you can write t less than h bar over m 104 00:09:45,420 --> 00:09:48,280 over a delta p squared, which would 105 00:09:48,280 --> 00:09:53,200 be h squared delta x squared. 106 00:09:53,200 --> 00:09:55,830 I think I'm getting it right. 107 00:09:55,830 --> 00:10:07,440 Yep, so t much less than m over h bar delta x squared. 108 00:10:07,440 --> 00:10:10,430 That's another way you could write this inequality. 109 00:10:14,490 --> 00:10:17,460 There is one way to write the inequality 110 00:10:17,460 --> 00:10:20,940 that you can intuitively feel you 111 00:10:20,940 --> 00:10:23,700 understand what's happening. 112 00:10:23,700 --> 00:10:31,460 And take this form a from a. 113 00:10:36,040 --> 00:10:49,320 Write it as delta p t over m is less than h bar over delta p. 114 00:10:55,550 --> 00:10:59,960 And h bar over delta p is delta x. 115 00:10:59,960 --> 00:11:17,810 So you go delta p over mt much less than delta x. 116 00:11:23,820 --> 00:11:26,570 I think this is understandable. 117 00:11:30,450 --> 00:11:35,920 Why does the packet change shape? 118 00:11:35,920 --> 00:11:39,690 The reason it changes shape is because the group velocity 119 00:11:39,690 --> 00:11:42,960 is not the same for all the frequencies. 120 00:11:42,960 --> 00:11:47,550 The packet mostly moves with k0. 121 00:11:47,550 --> 00:11:51,690 And we haven't rated the group velocity in k0. 122 00:11:51,690 --> 00:11:56,820 But if it would have a definite velocity, 123 00:11:56,820 --> 00:11:59,130 we would have a definite momentum. 124 00:11:59,130 --> 00:12:00,930 But that's not possible. 125 00:12:00,930 --> 00:12:04,260 These things have uncertainty in momentum. 126 00:12:04,260 --> 00:12:10,180 And they have uncertainty in k that we use it to write it. 127 00:12:10,180 --> 00:12:15,900 So different parts of the wave can 128 00:12:15,900 --> 00:12:19,890 move with different velocities, different group velocities. 129 00:12:19,890 --> 00:12:24,470 The group velocity you evaluated at k0. 130 00:12:24,470 --> 00:12:28,440 But some part of the packet is propagating 131 00:12:28,440 --> 00:12:34,380 with group velocities that are near k0 but not exactly there. 132 00:12:34,380 --> 00:12:38,190 So you have a dispersion in the velocity, which 133 00:12:38,190 --> 00:12:41,670 is an uncertainty in the velocity 134 00:12:41,670 --> 00:12:43,750 or an uncertainty in the momentum. 135 00:12:43,750 --> 00:12:47,680 Think, the momentum divided by mass is velocity. 136 00:12:47,680 --> 00:12:52,510 So here it is, an uncertainty in the velocity. 137 00:12:52,510 --> 00:12:55,095 And if you multiply the uncertainty 138 00:12:55,095 --> 00:12:59,720 in the velocity times this time that you can wait, 139 00:12:59,720 --> 00:13:04,280 then the change in shape is not much 140 00:13:04,280 --> 00:13:08,060 if this product, which is the difference of how 141 00:13:08,060 --> 00:13:12,080 one part moves with respect to the other, the difference 142 00:13:12,080 --> 00:13:14,540 of relative term, is still smaller 143 00:13:14,540 --> 00:13:17,690 than the uncertainty that controls 144 00:13:17,690 --> 00:13:19,980 the shape of the packet. 145 00:13:19,980 --> 00:13:22,070 So the packet has a delta x. 146 00:13:28,060 --> 00:13:31,840 And as long as this part, the left part of the packet, then 147 00:13:31,840 --> 00:13:36,880 the top of the packet, the difference of velocities 148 00:13:36,880 --> 00:13:42,070 times the time, it just still compared to delta x is small, 149 00:13:42,070 --> 00:13:44,770 then the thing doesn't change much. 150 00:13:44,770 --> 00:13:51,490 So I think this is one neat way of seeing 151 00:13:51,490 --> 00:13:54,460 what an equation that you sometimes 152 00:13:54,460 --> 00:13:58,140 use in this form, sometimes use in in this form-- 153 00:13:58,140 --> 00:14:03,700 it's just things that you can use in different ways. 154 00:14:03,700 --> 00:14:11,100 So for example, I can do this a little exercise. 155 00:14:14,090 --> 00:14:20,700 If you have delta x equals 10 to the minus 10 meters, that's 156 00:14:20,700 --> 00:14:23,440 atomic size for an electron. 157 00:14:31,210 --> 00:14:38,940 How long does it remain localized? 158 00:14:46,310 --> 00:14:49,250 So you have an electron. 159 00:14:49,250 --> 00:14:50,550 And you produce a packet. 160 00:14:50,550 --> 00:14:54,650 You localize it to the size of an atom. 161 00:14:54,650 --> 00:14:58,160 How long can you wait before this electron is just 162 00:14:58,160 --> 00:14:59,460 all over the room? 163 00:14:59,460 --> 00:15:05,300 Well, when we say this t, and we say this time, 164 00:15:05,300 --> 00:15:08,600 we're basically saying that it's roughly still there. 165 00:15:08,600 --> 00:15:11,810 Maybe it grew 20%, 30%. 166 00:15:11,810 --> 00:15:13,490 But what's the rough time that you 167 00:15:13,490 --> 00:15:16,230 can expect that it stays there? 168 00:15:16,230 --> 00:15:20,720 So in this case, we can use just this formula. 169 00:15:20,720 --> 00:15:28,820 And we say the time could be approximately 170 00:15:28,820 --> 00:15:34,490 m over h bar delta x squared. 171 00:15:34,490 --> 00:15:35,990 It's fun to see the numbers. 172 00:15:39,500 --> 00:15:44,870 You would calculate it with mc squared over h bar 173 00:15:44,870 --> 00:15:50,590 c times delta x over c, this squared. 174 00:15:54,760 --> 00:16:01,485 The answer is about 10 to the minus 16 seconds, not much. 175 00:16:07,140 --> 00:16:14,320 This is a practical issue in accelerators as well. 176 00:16:14,320 --> 00:16:16,780 Particle physics accelerators, they 177 00:16:16,780 --> 00:16:22,540 concern bunches, a little bunch of protons in the LHC. 178 00:16:22,540 --> 00:16:26,530 It's a little cylinder in which the wave functions 179 00:16:26,530 --> 00:16:31,190 of the protons are all collimated very thin, short, 180 00:16:31,190 --> 00:16:33,880 a couple of centimeters short. 181 00:16:33,880 --> 00:16:40,420 And after going around many times around the accelerator, 182 00:16:40,420 --> 00:16:44,440 they always have to be compressed and kept back, 183 00:16:44,440 --> 00:16:45,850 sent back to shape. 184 00:16:45,850 --> 00:16:51,190 Because just of diffusion, these things just propagate. 185 00:16:51,190 --> 00:16:56,430 And so it's a rather important thing.