1 00:00:00,000 --> 00:00:00,500 2 00:00:00,500 --> 00:00:01,950 In the last video, we figured out 3 00:00:01,950 --> 00:00:05,590 how to construct a unit normal vector to a surface. 4 00:00:05,590 --> 00:00:08,800 And so now we can use that back in our original surface 5 00:00:08,800 --> 00:00:10,750 integral to try to simplify a little bit, 6 00:00:10,750 --> 00:00:13,320 or at least give us a clue how we can calculate these things. 7 00:00:13,320 --> 00:00:14,820 And also, think about different ways 8 00:00:14,820 --> 00:00:17,950 to represent this type of a surface integral. 9 00:00:17,950 --> 00:00:20,710 So if we just substitute what we came up as our normal vector, 10 00:00:20,710 --> 00:00:22,190 our unit normal vector right here, 11 00:00:22,190 --> 00:00:26,120 we will get-- so once again, it's 12 00:00:26,120 --> 00:00:31,540 the surface integral of F dot. 13 00:00:31,540 --> 00:00:33,499 And F dot all of this business right over here. 14 00:00:33,499 --> 00:00:35,123 And I'm going to write it all in white, 15 00:00:35,123 --> 00:00:36,900 just so it doesn't take me too much time. 16 00:00:36,900 --> 00:00:38,930 So the partial of r with respect to u 17 00:00:38,930 --> 00:00:41,940 crossed with the partial of r with respect 18 00:00:41,940 --> 00:00:46,280 to v over the magnitude of the same thing, partial 19 00:00:46,280 --> 00:00:49,560 of r with respect to u crossed with the partial of r 20 00:00:49,560 --> 00:00:51,770 with respect to v. 21 00:00:51,770 --> 00:00:53,709 And now, we've played with ds a lot. 22 00:00:53,709 --> 00:00:55,375 We know that the other way to write ds-- 23 00:00:55,375 --> 00:00:56,874 and I gave the intuition, hopefully, 24 00:00:56,874 --> 00:00:58,840 for that several videos ago when we first 25 00:00:58,840 --> 00:01:01,120 explored what a surface integral was all about. 26 00:01:01,120 --> 00:01:05,770 We know that ds is-- it can be represented 27 00:01:05,770 --> 00:01:08,420 as the magnitude of the partial of r with respect 28 00:01:08,420 --> 00:01:13,501 to u crossed with the partial of r with respect to v du dv. 29 00:01:13,501 --> 00:01:17,020 And Obviously, the du dv, it could be written as dv du. 30 00:01:17,020 --> 00:01:20,410 You could write it as da, a little chunk of area 31 00:01:20,410 --> 00:01:23,310 and the uv plane or in the uv domain. 32 00:01:23,310 --> 00:01:26,010 And actually, since now this integral's in terms of uv, 33 00:01:26,010 --> 00:01:27,760 we're no longer taking a surface integral. 34 00:01:27,760 --> 00:01:30,880 We're now taking a double integral over the uv domain. 35 00:01:30,880 --> 00:01:33,150 So you could say kind of a region in uv. 36 00:01:33,150 --> 00:01:38,100 So I'll say R to say that's it's a region in the uv plane 37 00:01:38,100 --> 00:01:39,550 that we're now thinking about. 38 00:01:39,550 --> 00:01:41,770 But there's probably a huge-- or there should be, 39 00:01:41,770 --> 00:01:43,720 or I'm guessing there's a huge simplification that's 40 00:01:43,720 --> 00:01:44,928 popping out at you right now. 41 00:01:44,928 --> 00:01:47,130 We're dividing by the magnitude of the cross product 42 00:01:47,130 --> 00:01:48,588 of these two vectors and then we're 43 00:01:48,588 --> 00:01:52,040 multiplying by the magnitude of the cross product of these two 44 00:01:52,040 --> 00:01:52,695 vectors. 45 00:01:52,695 --> 00:01:54,070 Those are just scalar quantities. 46 00:01:54,070 --> 00:01:56,140 You divide by something and multiply by something. 47 00:01:56,140 --> 00:01:58,598 Well, that's just the same thing as multiplying or dividing 48 00:01:58,598 --> 00:01:59,390 by 1. 49 00:01:59,390 --> 00:02:01,420 So these two characters cancel out, 50 00:02:01,420 --> 00:02:05,930 and our integral simplifies to the double integral 51 00:02:05,930 --> 00:02:09,250 over that region, the corresponding region in the uv 52 00:02:09,250 --> 00:02:14,200 plane, of F-- of our vector field F 53 00:02:14,200 --> 00:02:16,880 dotted with this cross product. 54 00:02:16,880 --> 00:02:19,130 This is going to give us a vector right over here. 55 00:02:19,130 --> 00:02:20,740 That's going to give us a vector. 56 00:02:20,740 --> 00:02:22,282 It gives us actually a normal vector. 57 00:02:22,282 --> 00:02:24,031 And then when you divide by its magnitude, 58 00:02:24,031 --> 00:02:25,520 it gives you a unit normal vector. 59 00:02:25,520 --> 00:02:28,780 So this, you're going to take the dot product of F 60 00:02:28,780 --> 00:02:32,700 with r, the partial of r with respect 61 00:02:32,700 --> 00:02:41,170 to u crossed with the partial of r with respect to v du dv. 62 00:02:41,170 --> 00:02:45,550 Let me scroll over to the right a little bit, du dv. 63 00:02:45,550 --> 00:02:47,590 And we'll see in the few videos from now 64 00:02:47,590 --> 00:02:50,270 that this is essentially how we go about actually calculating 65 00:02:50,270 --> 00:02:50,860 these things. 66 00:02:50,860 --> 00:02:52,390 If you have a parameterization, you 67 00:02:52,390 --> 00:02:54,640 can then get everything in terms of a double integral, 68 00:02:54,640 --> 00:02:56,509 in terms of uv this way. 69 00:02:56,509 --> 00:02:58,800 Now, the last thing I want to do is explore another way 70 00:02:58,800 --> 00:03:01,050 that you'll see a surface integral like this written. 71 00:03:01,050 --> 00:03:03,379 It all comes from, really, writing this part 72 00:03:03,379 --> 00:03:04,170 in a different way. 73 00:03:04,170 --> 00:03:05,630 But it hopefully gives you a little bit more intuition 74 00:03:05,630 --> 00:03:07,700 of what this thing is even saying. 75 00:03:07,700 --> 00:03:09,240 So I'm just going to rewrite. 76 00:03:09,240 --> 00:03:12,570 I'm going to rewrite this chunk right over here. 77 00:03:12,570 --> 00:03:14,122 I'm just going to rewrite that chunk. 78 00:03:14,122 --> 00:03:16,580 And I'm going to use slightly different notation because it 79 00:03:16,580 --> 00:03:19,030 will hopefully help make a little bit more sense. 80 00:03:19,030 --> 00:03:21,100 So the partial of r with respect to u I 81 00:03:21,100 --> 00:03:25,930 can write as the partial of r with respect to u. 82 00:03:25,930 --> 00:03:27,600 And we're taking the cross product. 83 00:03:27,600 --> 00:03:30,300 Let me make my u's a little bit more u-like so we confuse them 84 00:03:30,300 --> 00:03:31,190 with v's. 85 00:03:31,190 --> 00:03:32,940 And we're taking the cross product of that 86 00:03:32,940 --> 00:03:36,400 with the partial of r with respect 87 00:03:36,400 --> 00:03:40,130 to v. So very small changes in our vector-- 88 00:03:40,130 --> 00:03:41,930 in our parameterization right here, 89 00:03:41,930 --> 00:03:44,100 our position vector given a small change in v. Very 90 00:03:44,100 --> 00:03:47,850 small changes in the vector given a small change in u. 91 00:03:47,850 --> 00:03:50,670 And then we're multiplying that times du dv. 92 00:03:50,670 --> 00:03:56,240 We're multiplying that times du dv. 93 00:03:56,240 --> 00:03:59,750 Now, du and dv are just scalar quantities. 94 00:03:59,750 --> 00:04:01,290 They're infinitesimally small. 95 00:04:01,290 --> 00:04:03,084 But for the sake of this argument, 96 00:04:03,084 --> 00:04:04,750 you can just view-- they're not vectors, 97 00:04:04,750 --> 00:04:06,500 they're just scalar quantities. 98 00:04:06,500 --> 00:04:09,730 And so you can essentially include them-- 99 00:04:09,730 --> 00:04:11,530 if you have the cross product. 100 00:04:11,530 --> 00:04:18,470 If you have a cross b times some scalar value-- I don't know, x, 101 00:04:18,470 --> 00:04:23,610 you could rewrite this as x times a cross b, 102 00:04:23,610 --> 00:04:28,530 or you could write this as a cross x times 103 00:04:28,530 --> 00:04:30,700 b, because x is just a scalar value. 104 00:04:30,700 --> 00:04:31,540 It's just a number. 105 00:04:31,540 --> 00:04:33,206 So we could do the same thing over here. 106 00:04:33,206 --> 00:04:35,650 We can rewrite all of this business as-- 107 00:04:35,650 --> 00:04:39,630 and I'm going to group the du where we have the partial-- 108 00:04:39,630 --> 00:04:41,300 or with respect to u in the denominator. 109 00:04:41,300 --> 00:04:42,966 And I'll do the same thing with the v's. 110 00:04:42,966 --> 00:04:48,430 And so you will get the partial of r with respect 111 00:04:48,430 --> 00:04:52,440 to u times du, times that scalar. 112 00:04:52,440 --> 00:04:54,240 So that'll give us a vector. 113 00:04:54,240 --> 00:04:55,750 And we're going to cross that. 114 00:04:55,750 --> 00:04:58,530 We're going to cross that with the partial of r with respect 115 00:04:58,530 --> 00:05:06,650 to v dv. 116 00:05:06,650 --> 00:05:08,814 Now, these might look notationally 117 00:05:08,814 --> 00:05:10,480 like two different things, but that just 118 00:05:10,480 --> 00:05:12,470 comes from the necessity of when we 119 00:05:12,470 --> 00:05:16,780 take partial derivatives to say, oh, no, this vector function 120 00:05:16,780 --> 00:05:18,887 is defined-- it's a function of multiple variables 121 00:05:18,887 --> 00:05:20,720 and this is taking a derivative with respect 122 00:05:20,720 --> 00:05:22,010 to only one of them. 123 00:05:22,010 --> 00:05:23,510 So this is, how much does our vector 124 00:05:23,510 --> 00:05:26,330 change when you have a very small change in u? 125 00:05:26,330 --> 00:05:28,880 But this is also an infinitesimally small change 126 00:05:28,880 --> 00:05:31,950 in u over here, we're just using slightly different notation. 127 00:05:31,950 --> 00:05:33,280 So for the sake of-- and this is a little bit 128 00:05:33,280 --> 00:05:35,280 loosey-goosey mathematics, but it will hopefully 129 00:05:35,280 --> 00:05:37,860 give you the intuition for why this thing could 130 00:05:37,860 --> 00:05:39,790 be written in a different way. 131 00:05:39,790 --> 00:05:42,290 These are essentially the same quantity. 132 00:05:42,290 --> 00:05:44,770 So if you divide by something and multiply by something, 133 00:05:44,770 --> 00:05:46,072 you can cancel them out. 134 00:05:46,072 --> 00:05:48,280 If you divide by something and multiply by something, 135 00:05:48,280 --> 00:05:49,840 you can cancel them out. 136 00:05:49,840 --> 00:05:52,070 And all you're left with then-- all 137 00:05:52,070 --> 00:05:55,670 you're left with is the differential of r. 138 00:05:55,670 --> 00:05:57,080 And since we lost the information 139 00:05:57,080 --> 00:05:58,496 that it's in the u-direction, I'll 140 00:05:58,496 --> 00:06:00,830 write here, the differential of r in the u-direction. 141 00:06:00,830 --> 00:06:02,891 I don't want to get the notation confused. 142 00:06:02,891 --> 00:06:04,140 This is just the differential. 143 00:06:04,140 --> 00:06:06,000 This is just how much r changed. 144 00:06:06,000 --> 00:06:08,820 This is not the partial derivative of r with respect 145 00:06:08,820 --> 00:06:09,455 to u. 146 00:06:09,455 --> 00:06:11,350 This right over here is, how much does r 147 00:06:11,350 --> 00:06:15,320 change given per unit change, per small change in u? 148 00:06:15,320 --> 00:06:19,190 This just says a differential in the direction of-- I 149 00:06:19,190 --> 00:06:22,530 guess as u changes, this is how much that infinitely small 150 00:06:22,530 --> 00:06:24,060 change that just r changes. 151 00:06:24,060 --> 00:06:27,460 This isn't change in r with respect to change in u. 152 00:06:27,460 --> 00:06:28,710 And we're going to cross that. 153 00:06:28,710 --> 00:06:31,775 Now, we're going to cross that with the partial of r, 154 00:06:31,775 --> 00:06:34,900 the partial of r in the v-direction. 155 00:06:34,900 --> 00:06:37,280 Now, this right over here, let's just conceptualize this. 156 00:06:37,280 --> 00:06:39,920 And this goes back to our original visions 157 00:06:39,920 --> 00:06:42,330 of what a surface integral was all about. 158 00:06:42,330 --> 00:06:44,314 If we're on a surface-- and I'll draw surface. 159 00:06:44,314 --> 00:06:45,480 Let me draw another surface. 160 00:06:45,480 --> 00:06:47,970 I won't use the one that I had already drawn on. 161 00:06:47,970 --> 00:06:51,077 If we draw a surface, and for a very small change in u-- 162 00:06:51,077 --> 00:06:52,910 and we're not going to think about the rate. 163 00:06:52,910 --> 00:06:56,220 We're just thinking about kind of the change in r. 164 00:06:56,220 --> 00:06:57,790 You're going in that direction. 165 00:06:57,790 --> 00:07:01,220 So if that thing looks like this, 166 00:07:01,220 --> 00:07:05,310 this is actually kind of a distance moved on the surface. 167 00:07:05,310 --> 00:07:08,060 Because remember, this isn't the derivative. 168 00:07:08,060 --> 00:07:09,350 This is the differential. 169 00:07:09,350 --> 00:07:11,840 So it's just a small change along the surface, 170 00:07:11,840 --> 00:07:13,510 that's that over there. 171 00:07:13,510 --> 00:07:16,710 And that this is a small change when you change v. So 172 00:07:16,710 --> 00:07:19,050 it's also a change along the surface. 173 00:07:19,050 --> 00:07:21,310 When you take the cross product of these two things, 174 00:07:21,310 --> 00:07:23,430 you get a vector that is orthogonal. 175 00:07:23,430 --> 00:07:26,570 You get a vector that is normal to the surface. 176 00:07:26,570 --> 00:07:33,740 So it is normal to the surface and its magnitude-- 177 00:07:33,740 --> 00:07:36,340 and we saw this when we first learned about cross products. 178 00:07:36,340 --> 00:07:40,080 Its magnitude is equal to the area that 179 00:07:40,080 --> 00:07:42,680 is defined by these two vectors. 180 00:07:42,680 --> 00:07:49,302 So its magnitude is equal to area. 181 00:07:49,302 --> 00:07:50,760 So in a lot of ways, you can really 182 00:07:50,760 --> 00:07:52,420 think of it-- you really could think 183 00:07:52,420 --> 00:07:57,020 of it as a unit normal vector times ds. 184 00:07:57,020 --> 00:07:59,960 And so the way that we would, I guess notationally do this, 185 00:07:59,960 --> 00:08:02,470 is we can call this-- because this is kind of a ds, 186 00:08:02,470 --> 00:08:04,045 but it's a vector version of the ds. 187 00:08:04,045 --> 00:08:06,760 Over here, this is just an area right over here. 188 00:08:06,760 --> 00:08:08,830 This is just a scalar value. 189 00:08:08,830 --> 00:08:12,250 But now, we have a vector that points normally 190 00:08:12,250 --> 00:08:14,930 from the surface, but its magnitude 191 00:08:14,930 --> 00:08:17,300 is the same thing as that ds that we were just 192 00:08:17,300 --> 00:08:18,340 talking about. 193 00:08:18,340 --> 00:08:22,070 So we can call this thing right over here, we can call this ds. 194 00:08:22,070 --> 00:08:25,140 And the key difference here is this is a vector now. 195 00:08:25,140 --> 00:08:28,240 So we'll call it ds with a little vector over it 196 00:08:28,240 --> 00:08:29,570 to know that this thing. 197 00:08:29,570 --> 00:08:33,200 This isn't the scalar ds that is just concerned with the area. 198 00:08:33,200 --> 00:08:34,970 But when you view things this way, 199 00:08:34,970 --> 00:08:39,289 we just saw that this entire thing simplifies to ds. 200 00:08:39,289 --> 00:08:43,419 Then our whole surface integral can be rewritten. 201 00:08:43,419 --> 00:08:45,200 Instead of writing it like this, we 202 00:08:45,200 --> 00:08:50,480 can write it as the integral or the surface 203 00:08:50,480 --> 00:08:54,050 integral-- those integral signs were too fancy. 204 00:08:54,050 --> 00:08:57,794 The surface integral of F dot. 205 00:08:57,794 --> 00:09:00,750 And instead of saying a normal vector times the scalar 206 00:09:00,750 --> 00:09:03,040 quantity, that little chunk of area on the surface, 207 00:09:03,040 --> 00:09:07,731 we can now just call that the vector differential ds. 208 00:09:07,731 --> 00:09:10,230 And I want to make it clear, these are two different things. 209 00:09:10,230 --> 00:09:12,280 This is a vector. 210 00:09:12,280 --> 00:09:14,130 This is essentially what we're calling it. 211 00:09:14,130 --> 00:09:16,655 This right over here is a scalar times a normal vector. 212 00:09:16,655 --> 00:09:18,030 So these are three different ways 213 00:09:18,030 --> 00:09:19,800 of really representing the same thing. 214 00:09:19,800 --> 00:09:22,175 And in different contexts, you will see different things, 215 00:09:22,175 --> 00:09:25,110 depending on what the author of whoever's trying to communicate 216 00:09:25,110 --> 00:09:26,820 is trying to communicate. 217 00:09:26,820 --> 00:09:29,990 This right over here is the one that we'll use most frequently 218 00:09:29,990 --> 00:09:34,192 as we actually try to calculate these surface integrals. 219 00:09:34,192 --> 00:09:34,692