1 00:00:00,322 --> 00:00:01,780 PROFESSOR: What are we going to do? 2 00:00:01,780 --> 00:00:05,820 We're going to explore only the first Born approximation. 3 00:00:05,820 --> 00:00:09,090 And the first Born approximation corresponds 4 00:00:09,090 --> 00:00:12,105 to just taking this part. 5 00:00:16,640 --> 00:00:25,350 So this would be the first Born approximation. 6 00:00:29,700 --> 00:00:32,770 It corresponds to what we were doing here. 7 00:00:32,770 --> 00:00:35,040 What did we do here? 8 00:00:35,040 --> 00:00:41,040 Well, we're simplifying the second term, the integral term, 9 00:00:41,040 --> 00:00:43,980 by using what the Green's function looked like. 10 00:00:43,980 --> 00:00:46,260 We simplified this term. 11 00:00:46,260 --> 00:00:50,400 So all what we did here was valuable, 12 00:00:50,400 --> 00:00:52,980 except that there's one little difference. 13 00:00:52,980 --> 00:00:56,490 We-- in that Born approximation, we 14 00:00:56,490 --> 00:01:01,350 replaced the psi that appears inside the integral 15 00:01:01,350 --> 00:01:06,700 by the incident psi, which is the psi in here. 16 00:01:06,700 --> 00:01:11,260 So we will do that now to simplify 17 00:01:11,260 --> 00:01:16,640 this quantity in the so-called first Born approximation. 18 00:01:16,640 --> 00:01:18,060 When can we use it? 19 00:01:18,060 --> 00:01:21,140 So, very good. 20 00:01:21,140 --> 00:01:24,440 So when is the Born approximation 21 00:01:24,440 --> 00:01:28,260 a good approximation? 22 00:01:28,260 --> 00:01:33,980 Well, we are throwing away terms, in general. 23 00:01:33,980 --> 00:01:40,200 When we're putting an expansion of this form, we're saying, OK, 24 00:01:40,200 --> 00:01:44,690 we can set the wave function equal to the free part 25 00:01:44,690 --> 00:01:46,640 plus the interacting part. 26 00:01:46,640 --> 00:01:51,560 So we have the free part, and it gave us this quantity. 27 00:01:51,560 --> 00:01:55,410 And the interacting part gave us the second one. 28 00:01:55,410 --> 00:01:58,640 So the Born approximation is good 29 00:01:58,640 --> 00:02:01,940 when sort of the free Hamiltonian 30 00:02:01,940 --> 00:02:05,510 dominates over the perturbation. 31 00:02:05,510 --> 00:02:11,210 So if a scattering center has a finite-energy bump, 32 00:02:11,210 --> 00:02:14,620 and you're sending things with very high energy, 33 00:02:14,620 --> 00:02:17,390 the Born approximation should be very good. 34 00:02:17,390 --> 00:02:21,230 It's a high-energy approximation, 35 00:02:21,230 --> 00:02:24,830 in which you are basically saying 36 00:02:24,830 --> 00:02:29,120 that inside the integral, you can 37 00:02:29,120 --> 00:02:33,950 replace the plane-incident wave, because that dominates. 38 00:02:33,950 --> 00:02:35,540 That's not the whole solution. 39 00:02:35,540 --> 00:02:38,630 The whole solution then becomes the plane integral wave 40 00:02:38,630 --> 00:02:40,820 plus the scattered wave. 41 00:02:40,820 --> 00:02:45,080 But the plane wave dominates over the scattering process. 42 00:02:45,080 --> 00:02:49,160 So it should be valid in high energy. 43 00:02:49,160 --> 00:02:52,760 It's better and better in high-energy approximation. 44 00:02:57,740 --> 00:02:59,240 So we have it here. 45 00:02:59,240 --> 00:03:02,750 And let's, therefore, clean it up. 46 00:03:02,750 --> 00:03:07,670 So if we call this equation "equation A," we say, 47 00:03:07,670 --> 00:03:17,420 back to A. The first Born approximation, back to A. 48 00:03:17,420 --> 00:03:31,950 The first Born approximation gives us psi of r equals 49 00:03:31,950 --> 00:03:35,580 e to the i k i r. 50 00:03:35,580 --> 00:03:39,510 Now we put all the-- and this is all the arrows. 51 00:03:39,510 --> 00:03:47,790 And we have here minus 1 over 4 pi, integral d cubed r prime, 52 00:03:47,790 --> 00:03:55,720 e to the minus i k n dot r prime, u of r prime, 53 00:03:55,720 --> 00:04:02,790 and e to the i k i dot r prime. 54 00:04:02,790 --> 00:04:07,320 All this multiplied by e to the i k r over r. 55 00:04:11,980 --> 00:04:17,180 So let's put a few vectors here. 56 00:04:17,180 --> 00:04:19,459 That's it. 57 00:04:19,459 --> 00:04:20,070 OK. 58 00:04:20,070 --> 00:04:23,850 So it's basically this same thing here, 59 00:04:23,850 --> 00:04:27,120 but now replacing the incident wave here. 60 00:04:27,120 --> 00:04:30,840 That's the so-called first Born approximation. 61 00:04:30,840 --> 00:04:34,380 But now this is really good. 62 00:04:34,380 --> 00:04:42,405 We can compare this with what we usually called f theta of phi. 63 00:04:45,860 --> 00:04:51,740 The expression of our brackets is the scattering amplitude 64 00:04:51,740 --> 00:04:53,990 f theta phi. 65 00:04:53,990 --> 00:04:56,390 So here we have an answer. 66 00:04:56,390 --> 00:05:04,860 f at wave number k of theta and phi is equal to this integral. 67 00:05:04,860 --> 00:05:06,090 Let's write it out. 68 00:05:06,090 --> 00:05:13,340 Minus 1 over 4 pi, integral d cubed r prime. 69 00:05:13,340 --> 00:05:17,100 And now we will combine the exponentials. 70 00:05:17,100 --> 00:05:21,940 Happily, the two exponentials depend on r prime. 71 00:05:21,940 --> 00:05:25,470 So it's a difference of exponents, 72 00:05:25,470 --> 00:05:30,930 and we will call it e to the minus i, 73 00:05:30,930 --> 00:05:44,410 capital-K vector dot r prime, u of r prime, 74 00:05:44,410 --> 00:05:55,340 where this capital-K vector is equal-- 75 00:05:55,340 --> 00:05:56,480 I kept the sign-- 76 00:05:56,480 --> 00:06:05,430 k n minus-- this time we'll enter with a minus in that k-- 77 00:06:05,430 --> 00:06:16,440 k i or k s, the scattering k, minus the incident i vector. 78 00:06:16,440 --> 00:06:20,970 Remember, we defined there, on that blackboard, 79 00:06:20,970 --> 00:06:26,420 the scattered momentum as k times the direction 80 00:06:26,420 --> 00:06:30,420 of observation, that unit vector. 81 00:06:30,420 --> 00:06:39,190 So in combining these two exponentials into a single one, 82 00:06:39,190 --> 00:06:42,960 we have this capital-K vector that 83 00:06:42,960 --> 00:06:44,660 is a pretty important vector. 84 00:06:44,660 --> 00:06:48,520 And now, this is a nice formula. 85 00:06:48,520 --> 00:06:54,400 It kind of tells you story that there are not many ways 86 00:06:54,400 --> 00:06:57,460 to generate things that are interesting. 87 00:07:00,400 --> 00:07:05,170 Here it says that f k, the scattering amplitude, 88 00:07:05,170 --> 00:07:10,480 as a function of theta and phi, is nothing else than a Fourier 89 00:07:10,480 --> 00:07:17,130 transform of the potential evaluated at what we would 90 00:07:17,130 --> 00:07:21,150 call the transfer momentum. 91 00:07:21,150 --> 00:07:26,960 So the scattering and bridges are doing Fourier transforms 92 00:07:26,960 --> 00:07:29,390 of the potential. 93 00:07:29,390 --> 00:07:30,470 Pretty nice. 94 00:07:30,470 --> 00:07:34,070 Pretty pictorial way of thinking about it. 95 00:07:34,070 --> 00:07:37,190 Fourier transforms are functions of-- 96 00:07:37,190 --> 00:07:40,910 I think when people look at this formula, 97 00:07:40,910 --> 00:07:44,060 there's a little uneasiness, because the angles don't 98 00:07:44,060 --> 00:07:46,900 show up on the right side. 99 00:07:46,900 --> 00:07:49,350 You have theta and phi on the left, 100 00:07:49,350 --> 00:07:53,690 but I don't see a theta, nor a phi, on the right. 101 00:07:53,690 --> 00:07:57,492 So I think that has to be always clarified. 102 00:08:00,560 --> 00:08:04,285 So for that, if you want to use, really, theta and phi, 103 00:08:04,285 --> 00:08:08,675 I think most people will assume that k incident is indeed 104 00:08:08,675 --> 00:08:11,460 in the z-direction. 105 00:08:11,460 --> 00:08:12,360 z-direction. 106 00:08:12,360 --> 00:08:13,905 So here is k incident. 107 00:08:17,720 --> 00:08:20,640 And it has some length. 108 00:08:20,640 --> 00:08:23,810 k scattered has the same length. 109 00:08:23,810 --> 00:08:28,290 It's made by the same wave number k without any index, 110 00:08:28,290 --> 00:08:32,590 but multiplied by the unit vector n. 111 00:08:32,590 --> 00:08:36,390 As opposed to k incident, that is the same k multiplied 112 00:08:36,390 --> 00:08:38,650 by the unit z vector. 113 00:08:38,650 --> 00:08:43,770 So the scattered vector is the vector in the direction 114 00:08:43,770 --> 00:08:45,520 that you're looking at. 115 00:08:45,520 --> 00:08:48,370 So this is k s. 116 00:08:48,370 --> 00:08:49,900 It's over here. 117 00:08:49,900 --> 00:09:00,870 And therefore this vector is the one that has the phi and theta 118 00:09:00,870 --> 00:09:03,120 directions. 119 00:09:03,120 --> 00:09:05,280 That is that vector. 120 00:09:05,280 --> 00:09:10,900 And the vector k is k scattered minus k initial. 121 00:09:10,900 --> 00:09:17,260 So the vector k is the transfer vector-- 122 00:09:17,260 --> 00:09:22,680 is the vector that takes you from k initial to k 123 00:09:22,680 --> 00:09:27,510 s, is the vector that must be added to k initial 124 00:09:27,510 --> 00:09:31,060 to give you the scattered vector. 125 00:09:31,060 --> 00:09:34,100 So this vector, capital vector K-- 126 00:09:34,100 --> 00:09:36,260 it's a little cluttered here. 127 00:09:36,260 --> 00:09:37,860 Let me put the z in here. 128 00:09:41,070 --> 00:09:46,970 That vector is over there, and that vector 129 00:09:46,970 --> 00:09:53,575 is a complicated vector, not so easy to express in terms of k i 130 00:09:53,575 --> 00:09:57,270 and k s, because it has a component down. 131 00:09:57,270 --> 00:10:01,560 But it has an angle phi as well. 132 00:10:05,250 --> 00:10:09,250 But one thing you can say about this vector is its magnitude 133 00:10:09,250 --> 00:10:14,060 is easily calculable, because there is a triangle here 134 00:10:14,060 --> 00:10:21,530 that we drew that has k incident and k s. 135 00:10:21,530 --> 00:10:22,530 And here is k. 136 00:10:22,530 --> 00:10:26,640 So this has length k, this has length k, 137 00:10:26,640 --> 00:10:34,260 and this has length capital K. The triangle with angle theta. 138 00:10:34,260 --> 00:10:38,300 So if you drop a vertical line, you 139 00:10:38,300 --> 00:10:44,500 see that k is twice this little piece, which 140 00:10:44,500 --> 00:10:49,820 is little k sine theta over 2. 141 00:10:54,530 --> 00:10:59,240 So that's one way that formula on the right-hand side 142 00:10:59,240 --> 00:11:02,030 has the information of theta. 143 00:11:02,030 --> 00:11:04,370 It also has the information of phi, 144 00:11:04,370 --> 00:11:10,760 because you also need phi to determine the vector k. 145 00:11:10,760 --> 00:11:13,880 So this is an approximation, but look 146 00:11:13,880 --> 00:11:19,040 how powerful approximations are, in general, in physics. 147 00:11:19,040 --> 00:11:21,920 This approximation is an approximation 148 00:11:21,920 --> 00:11:25,540 for the scattering amplitude. 149 00:11:25,540 --> 00:11:29,720 It-- first, it's a very nice physical interpretation, 150 00:11:29,720 --> 00:11:33,560 in terms of a Fourier transform of potential. 151 00:11:33,560 --> 00:11:36,910 Second, it gives you answers even 152 00:11:36,910 --> 00:11:41,570 in the case where the potential is not spherically symmetric. 153 00:11:41,570 --> 00:11:44,890 You remember, when potentials were spherically symmetric, 154 00:11:44,890 --> 00:11:48,430 the scattering amplitude didn't depend on phi, 155 00:11:48,430 --> 00:11:50,770 and we could use partial waves. 156 00:11:50,770 --> 00:11:53,350 And that's a nice way of solving things. 157 00:11:53,350 --> 00:11:59,290 But here, at the expense of not being exact, 158 00:11:59,290 --> 00:12:03,730 we have been able to calculate a scattering amplitude 159 00:12:03,730 --> 00:12:08,620 when the potential is not spherically symmetric. 160 00:12:08,620 --> 00:12:13,660 So you manage to go very far with approximations. 161 00:12:13,660 --> 00:12:17,170 You don't get the exact things, but you 162 00:12:17,170 --> 00:12:23,480 can go into results that are a lot more powerful. 163 00:12:23,480 --> 00:12:30,170 So this is an explanation of this formula. 164 00:12:30,170 --> 00:12:31,620 And we can use this formula. 165 00:12:31,620 --> 00:12:33,410 In fact, we'll do a little example. 166 00:12:33,410 --> 00:12:36,560 And these are the things that you still 167 00:12:36,560 --> 00:12:39,390 have to do a bit in the homework as well. 168 00:12:39,390 --> 00:12:41,630 Many of them are in Griffiths. 169 00:12:41,630 --> 00:12:45,590 And indeed, technically speaking, 170 00:12:45,590 --> 00:12:49,870 what you need to finish for tomorrow hinges a bit 171 00:12:49,870 --> 00:12:50,990 in what I'm saying. 172 00:12:50,990 --> 00:12:55,220 But the final formulas are well written in Griffiths 173 00:12:55,220 --> 00:12:59,330 explicitly, and in fact, half of the problems are solved there. 174 00:12:59,330 --> 00:13:03,190 So it shouldn't be so difficult.