1 00:00:00,000 --> 00:00:00,520 2 00:00:00,520 --> 00:00:03,242 In the last video, we began to explore Stokes' theorem. 3 00:00:03,242 --> 00:00:04,700 And what I want to do in this video 4 00:00:04,700 --> 00:00:07,060 is to see whether it's consistent with some 5 00:00:07,060 --> 00:00:09,050 of what we have already seen. 6 00:00:09,050 --> 00:00:12,190 And to do that, let's imagine-- so let me draw my axes. 7 00:00:12,190 --> 00:00:14,340 So that's my z-axis. 8 00:00:14,340 --> 00:00:16,680 That is my x-axis. 9 00:00:16,680 --> 00:00:19,610 And then that is my y-axis. 10 00:00:19,610 --> 00:00:23,430 And now let's imagine a region in the xy plane. 11 00:00:23,430 --> 00:00:25,770 So let me draw it like this. 12 00:00:25,770 --> 00:00:30,670 So let's say this is my region in the xy plane. 13 00:00:30,670 --> 00:00:34,850 I will call that region R. And I also 14 00:00:34,850 --> 00:00:36,580 have a boundary of that region. 15 00:00:36,580 --> 00:00:39,470 And let's say we care about the direction 16 00:00:39,470 --> 00:00:40,720 that we traverse the boundary. 17 00:00:40,720 --> 00:00:41,650 And let's say we're going to traverse it 18 00:00:41,650 --> 00:00:43,180 in a counterclockwise direction. 19 00:00:43,180 --> 00:00:47,150 So we have this path that goes around this region. 20 00:00:47,150 --> 00:00:49,890 We can call that c. 21 00:00:49,890 --> 00:00:51,950 So we'll call that c, and we're going 22 00:00:51,950 --> 00:00:57,010 to traverse it in the counterclockwise direction. 23 00:00:57,010 --> 00:01:02,310 And let's say that we also have a vector field f. 24 00:01:02,310 --> 00:01:05,360 That essentially its i component is just 25 00:01:05,360 --> 00:01:08,030 going to be a function of x and y. 26 00:01:08,030 --> 00:01:10,310 And its j component is only going 27 00:01:10,310 --> 00:01:12,530 to be a function of x and y. 28 00:01:12,530 --> 00:01:14,780 And let's say it has no k component. 29 00:01:14,780 --> 00:01:17,230 So the vector field on this region, 30 00:01:17,230 --> 00:01:18,750 it might look something like this. 31 00:01:18,750 --> 00:01:20,422 I'm just drawing random things. 32 00:01:20,422 --> 00:01:21,880 And then if you go off that region, 33 00:01:21,880 --> 00:01:23,350 if you go in the z direction, it's 34 00:01:23,350 --> 00:01:25,700 just going to look the same as you go higher and higher. 35 00:01:25,700 --> 00:01:27,930 So that vector, it wouldn't change 36 00:01:27,930 --> 00:01:29,660 as you change your z component. 37 00:01:29,660 --> 00:01:31,450 And all of the vectors would essentially 38 00:01:31,450 --> 00:01:35,790 be parallel to, or if z is 0, actually 39 00:01:35,790 --> 00:01:39,100 sitting on the xy plane. 40 00:01:39,100 --> 00:01:41,480 Now given this, let's think about what 41 00:01:41,480 --> 00:01:46,010 Stokes' theorem would tell us about the value of the line 42 00:01:46,010 --> 00:01:48,980 integral over the contour-- let me 43 00:01:48,980 --> 00:01:51,470 draw that a little bit neater-- the line 44 00:01:51,470 --> 00:02:00,960 integral over the contour c of f dot 45 00:02:00,960 --> 00:02:05,960 dr, f dot lowercase dr, Where dr is obviously 46 00:02:05,960 --> 00:02:08,280 going along the contour. 47 00:02:08,280 --> 00:02:11,470 So if we take Stokes' theorem, then this quantity 48 00:02:11,470 --> 00:02:13,850 right over here should be equal to this quantity 49 00:02:13,850 --> 00:02:14,610 right over here. 50 00:02:14,610 --> 00:02:18,850 It should be equal to the double integral over the surface. 51 00:02:18,850 --> 00:02:21,270 Well this region is really just a surface 52 00:02:21,270 --> 00:02:23,450 that's sitting in the xy plane. 53 00:02:23,450 --> 00:02:26,077 So it should really just be the double integral-- 54 00:02:26,077 --> 00:02:27,660 let me write that in that same-- it'll 55 00:02:27,660 --> 00:02:31,310 be the double integral over our region, which is really 56 00:02:31,310 --> 00:02:35,110 just the same thing as our surface, 57 00:02:35,110 --> 00:02:37,840 of the curl of f dot n. 58 00:02:37,840 --> 00:02:40,437 So let's just think about what the curl of f dot n is. 59 00:02:40,437 --> 00:02:42,270 And then d of s would just be a little chunk 60 00:02:42,270 --> 00:02:45,510 of our region, a little chunk of our flattened surface 61 00:02:45,510 --> 00:02:46,220 right over there. 62 00:02:46,220 --> 00:02:50,180 So instead of ds, I'll just write da. 63 00:02:50,180 --> 00:02:54,000 But let's think of what curl of f dot n would actually be. 64 00:02:54,000 --> 00:02:56,060 So let's work on curl of f first. 65 00:02:56,060 --> 00:02:58,910 So the curl of f-- and the way I always 66 00:02:58,910 --> 00:03:00,810 remember it is we're going to take 67 00:03:00,810 --> 00:03:06,850 the determinant of this ijk partial 68 00:03:06,850 --> 00:03:10,820 with respect to x, partial with respect to y, 69 00:03:10,820 --> 00:03:12,330 partial with respect to z. 70 00:03:12,330 --> 00:03:14,450 This is just the definition of taking the curl. 71 00:03:14,450 --> 00:03:16,820 We're figuring out how much this vector field 72 00:03:16,820 --> 00:03:18,910 would cause something to spin. 73 00:03:18,910 --> 00:03:20,980 And then we want the i component, which 74 00:03:20,980 --> 00:03:24,416 is our function p, which is just a function of x and y, 75 00:03:24,416 --> 00:03:26,990 j component, which is just the function q. 76 00:03:26,990 --> 00:03:30,720 And there was no z component over here, so 0. 77 00:03:30,720 --> 00:03:32,892 And so this is going to be equal to-- well 78 00:03:32,892 --> 00:03:34,350 if we look at the i component, it's 79 00:03:34,350 --> 00:03:35,960 going to be the partial of y of 0. 80 00:03:35,960 --> 00:03:42,570 That's just going to be 0, minus the partial of q with respect 81 00:03:42,570 --> 00:03:43,450 to z. 82 00:03:43,450 --> 00:03:46,000 Well what's the partial of q with respect to z? 83 00:03:46,000 --> 00:03:48,190 Well q isn't a function of z at all. 84 00:03:48,190 --> 00:03:50,470 So that's also going to be 0-- let me write this out 85 00:03:50,470 --> 00:03:52,330 just so it's not too confusing. 86 00:03:52,330 --> 00:03:56,180 So our i component, it's going to be partial of 0 87 00:03:56,180 --> 00:03:57,130 with respect to y. 88 00:03:57,130 --> 00:04:01,000 Well that's just going to be 0 minus the partial of q 89 00:04:01,000 --> 00:04:02,290 with respect to z. 90 00:04:02,290 --> 00:04:04,340 Well the partial of q with respect to z 91 00:04:04,340 --> 00:04:05,700 is just going to be 0. 92 00:04:05,700 --> 00:04:07,500 So we have a 0 i component. 93 00:04:07,500 --> 00:04:10,260 And then we want to subtract the j component. 94 00:04:10,260 --> 00:04:16,700 And then the j component partial of 0 with respect to x is 0. 95 00:04:16,700 --> 00:04:20,079 And then from that you're going to subtract the partial of p 96 00:04:20,079 --> 00:04:22,180 with respect to z. 97 00:04:22,180 --> 00:04:25,590 Well once again, p is not a function of z at all. 98 00:04:25,590 --> 00:04:28,160 So that's going to be 0 again. 99 00:04:28,160 --> 00:04:33,911 And then you have plus k times the partial of q with respect 100 00:04:33,911 --> 00:04:34,410 to x. 101 00:04:34,410 --> 00:04:36,320 Remember this is just the partial derivative operator. 102 00:04:36,320 --> 00:04:38,180 So the partial of q with respect to x. 103 00:04:38,180 --> 00:04:41,160 104 00:04:41,160 --> 00:04:43,450 And from that we're going to subtract the partial of p 105 00:04:43,450 --> 00:04:44,570 with respect to y. 106 00:04:44,570 --> 00:04:49,690 107 00:04:49,690 --> 00:04:56,150 So the curl of f just simplifies to this right over here. 108 00:04:56,150 --> 00:04:58,880 Now what is n? 109 00:04:58,880 --> 00:05:02,250 What is the unit normal vector. 110 00:05:02,250 --> 00:05:04,300 Well we're in the xy plane. 111 00:05:04,300 --> 00:05:05,930 So the unit normal vector is just 112 00:05:05,930 --> 00:05:07,940 going to be straight up in the z direction. 113 00:05:07,940 --> 00:05:10,390 It's going to have a magnitude of 1. 114 00:05:10,390 --> 00:05:12,450 So in this case, our unit normal vector 115 00:05:12,450 --> 00:05:14,660 is just going to be the k vector. 116 00:05:14,660 --> 00:05:18,490 So we're essentially just going to take-- so curl of f is this. 117 00:05:18,490 --> 00:05:21,880 And our unit normal vector is just 118 00:05:21,880 --> 00:05:24,510 going to be equal to the k. 119 00:05:24,510 --> 00:05:26,920 It's just going to be the k unit vector. 120 00:05:26,920 --> 00:05:28,230 It's going to go straight up. 121 00:05:28,230 --> 00:05:31,160 So what happens if we take the curl of f dot k? 122 00:05:31,160 --> 00:05:34,030 If we just dot this with k. 123 00:05:34,030 --> 00:05:36,080 We're just dotting this with this. 124 00:05:36,080 --> 00:05:39,730 Well, we're just going to end up with this part right over here. 125 00:05:39,730 --> 00:05:43,930 So curl of f dot the unit normal vector is just 126 00:05:43,930 --> 00:05:45,400 going to be equal to this business. 127 00:05:45,400 --> 00:05:49,260 It's just going to be equal to the partial of q with respect 128 00:05:49,260 --> 00:05:54,980 to x minus the partial of p with respect to y. 129 00:05:54,980 --> 00:05:57,944 And this is neat because using Stokes' theorem 130 00:05:57,944 --> 00:05:59,610 in the special case, where we're dealing 131 00:05:59,610 --> 00:06:03,030 with a flattened-out surface in the xy plane, 132 00:06:03,030 --> 00:06:07,960 in this situation, this just boiled down to Green's theorem. 133 00:06:07,960 --> 00:06:12,030 This thing right over here just boiled down to Green's theorem. 134 00:06:12,030 --> 00:06:15,920 So we see that Green's theorem is really just a special case-- 135 00:06:15,920 --> 00:06:17,840 let me write theorem a little bit neater. 136 00:06:17,840 --> 00:06:20,390 We see that Green's theorem is really 137 00:06:20,390 --> 00:06:22,800 just a special case of Stokes' theorem, 138 00:06:22,800 --> 00:06:27,360 where our surface is flattened out, and it's in the xy plane. 139 00:06:27,360 --> 00:06:30,140 So that should make us feel pretty good, although we still 140 00:06:30,140 --> 00:06:32,240 have not proven Stokes' theorem. 141 00:06:32,240 --> 00:06:34,530 But the one thing that I do like about this is seeing 142 00:06:34,530 --> 00:06:36,780 that Green's theorem and Stokes' theorem is consistent 143 00:06:36,780 --> 00:06:39,430 is now it starts to make sense of this right over here. 144 00:06:39,430 --> 00:06:40,810 When we first learned Green's theorem, we were like, 145 00:06:40,810 --> 00:06:41,380 what is this? 146 00:06:41,380 --> 00:06:42,565 what's going on over here? 147 00:06:42,565 --> 00:06:44,190 But now this is telling us this is just 148 00:06:44,190 --> 00:06:47,920 taking the curl in this region along this surface. 149 00:06:47,920 --> 00:06:50,840 And now starts to make a lot of sense based on the intuition 150 00:06:50,840 --> 00:06:54,090 that we saw in the last video.