1 00:00:11,030 --> 00:00:12,980 PROFESSOR: So as a more technical aside, 2 00:00:12,980 --> 00:00:15,200 let's analyze more carefully the problem 3 00:00:15,200 --> 00:00:20,970 of release of viral load from a drop by process of diffusion. 4 00:00:20,970 --> 00:00:23,250 So here, again, I sketch a droplet, 5 00:00:23,250 --> 00:00:25,970 which would typically be an aerosol droplet in the size 6 00:00:25,970 --> 00:00:27,890 range of, let's say, microns. 7 00:00:27,890 --> 00:00:30,650 And the virion of interest has a size 8 00:00:30,650 --> 00:00:33,680 that is much smaller than that on the order of, let's say, 9 00:00:33,680 --> 00:00:35,480 100 nanometers. 10 00:00:35,480 --> 00:00:38,870 And this white path is showing how such a virion would 11 00:00:38,870 --> 00:00:43,430 go from its initial position R, let's say, as a radio position, 12 00:00:43,430 --> 00:00:45,380 to the boundary. 13 00:00:45,380 --> 00:00:48,800 Now, the general problem of finding 14 00:00:48,800 --> 00:00:53,510 the expected first passage time from the point inside a domain 15 00:00:53,510 --> 00:00:56,240 to a boundary is a classical problem 16 00:00:56,240 --> 00:00:59,480 in the theory of stochastic processes and random walks. 17 00:00:59,480 --> 00:01:01,830 And it has the following representation. 18 00:01:01,830 --> 00:01:04,340 So the mean are expected first passage 19 00:01:04,340 --> 00:01:14,120 time from a point to an absorbing surface 20 00:01:14,120 --> 00:01:16,120 solves the following problem. 21 00:01:16,120 --> 00:01:20,150 Is the Laplacian of that time with a minus sign 22 00:01:20,150 --> 00:01:22,870 is 1 over D where D is the diffusivity. 23 00:01:22,870 --> 00:01:25,010 And so this is the DV that I described before, 24 00:01:25,010 --> 00:01:26,780 the diffusivity of the virion. 25 00:01:26,780 --> 00:01:29,780 And the boundary condition for this equation 26 00:01:29,780 --> 00:01:33,530 is that it's an absorbing boundary, basically. 27 00:01:33,530 --> 00:01:35,810 So when the virion gets to the surface it's gone. 28 00:01:35,810 --> 00:01:40,430 And that's when the stochastic process finishes. 29 00:01:40,430 --> 00:01:46,030 So it's tau equals 0 on radius capital R, which 30 00:01:46,030 --> 00:01:47,280 is the radius of the droplets. 31 00:01:47,280 --> 00:01:49,440 So that's on the boundary. 32 00:01:49,440 --> 00:01:57,320 So in the case of a spherical drop, then 33 00:01:57,320 --> 00:02:01,980 we can write this equation in spherical coordinates. 34 00:02:01,980 --> 00:02:07,070 So that's minus 1 over r-squared, r derivative 35 00:02:07,070 --> 00:02:11,030 of r-squared D tau DR. And that's 36 00:02:11,030 --> 00:02:12,860 equal to 1 over capital D. 37 00:02:12,860 --> 00:02:14,450 And then again, our boundary condition 38 00:02:14,450 --> 00:02:17,850 is the tau of capital R is equal to zero. 39 00:02:17,850 --> 00:02:24,590 Another boundary condition we might mention is that D tau DR at R 40 00:02:24,590 --> 00:02:26,780 equals 0 is zero. 41 00:02:26,780 --> 00:02:28,329 That's a symmetry boundary condition. 42 00:02:28,329 --> 00:02:30,380 So when you're right in the middle, basically, 43 00:02:30,380 --> 00:02:31,700 there should be no-- 44 00:02:31,700 --> 00:02:36,350 there's no favorite direction for the diffusion process. 45 00:02:36,350 --> 00:02:38,150 And so, therefore, the derivative this time 46 00:02:38,150 --> 00:02:40,090 with respect to R must be 0 at the center 47 00:02:40,090 --> 00:02:42,200 because it's a symmetry boundary condition. 48 00:02:42,200 --> 00:02:45,260 OK, so we can now go ahead and solve this problem. 49 00:02:45,260 --> 00:02:47,740 Let me put the r-squared on their side and use primes 50 00:02:47,740 --> 00:02:49,380 with no derivatives. 51 00:02:49,380 --> 00:02:53,790 So let's write this as r-squared tau 52 00:02:53,790 --> 00:03:00,410 prime, prime equals minus r-squared over d. 53 00:03:00,410 --> 00:03:03,780 And if I now integrate both sides, 54 00:03:03,780 --> 00:03:07,970 I get r-squared tau prime equals-- 55 00:03:07,970 --> 00:03:11,810 and then here we get a minus r-cubed 56 00:03:11,810 --> 00:03:15,030 over 3D plus a constant. 57 00:03:17,579 --> 00:03:20,000 And that constant immigration according to the symmetry 58 00:03:20,000 --> 00:03:23,240 boundary condition has to be 0, because tau prime is 59 00:03:23,240 --> 00:03:25,910 0 at r equals 0. 60 00:03:25,910 --> 00:03:27,950 So we can simplify this and write 61 00:03:27,950 --> 00:03:34,150 tau prime is minus r over 3D. 62 00:03:34,150 --> 00:03:36,360 And so then I can integrate again. 63 00:03:36,360 --> 00:03:41,680 And I found that tau of r is-- 64 00:03:41,680 --> 00:03:44,260 well, I integrate this, I get r squared over 2 65 00:03:44,260 --> 00:03:45,040 is integral of r. 66 00:03:45,040 --> 00:03:47,680 So that gives that an r-squared over 6. 67 00:03:47,680 --> 00:03:52,210 So there will be a 6 D and minus r-squared. 68 00:03:52,210 --> 00:03:54,280 And there'll be a constant integration. 69 00:03:54,280 --> 00:03:57,370 And in order to satisfy this boundary condition of vanishing 70 00:03:57,370 --> 00:03:59,290 a capital R, you can see that I can 71 00:03:59,290 --> 00:04:00,910 write the constant this way. 72 00:04:00,910 --> 00:04:03,490 And I'll write it as capital R squared over 6D 73 00:04:03,490 --> 00:04:05,780 is a constant of integration. 74 00:04:05,780 --> 00:04:10,360 So basically, the profile of the main first passage time 75 00:04:10,360 --> 00:04:12,560 is essentially a parabola. 76 00:04:12,560 --> 00:04:19,269 So as a function of distance R from the center of the droplet, 77 00:04:19,269 --> 00:04:24,640 you have this shape to the mean transmission time. 78 00:04:24,640 --> 00:04:27,910 And the maximum here, the maximum value 79 00:04:27,910 --> 00:04:32,260 is tau 0 is the maximum value. 80 00:04:32,260 --> 00:04:36,720 And that is r-squared over 60. 81 00:04:36,720 --> 00:04:38,950 So that's if you happen to be unlucky and right 82 00:04:38,950 --> 00:04:39,540 in the middle. 83 00:04:39,540 --> 00:04:41,090 That's the longest you would expect 84 00:04:41,090 --> 00:04:44,040 to take from a particular part. 85 00:04:44,040 --> 00:04:45,920 Now on the other hand, as I've sketched here, 86 00:04:45,920 --> 00:04:48,320 in a typical droplet, if the virions are randomly 87 00:04:48,320 --> 00:04:51,409 distributed, some of them, like this guy over here, 88 00:04:51,409 --> 00:04:53,030 happen to be very close to the surface. 89 00:04:53,030 --> 00:04:55,280 So you're not going to have to wait this long for them 90 00:04:55,280 --> 00:04:55,790 to escape. 91 00:04:55,790 --> 00:04:58,340 So now we can ask the question, what is the average escape 92 00:04:58,340 --> 00:05:01,340 time over all the initial positions of the virus, 93 00:05:01,340 --> 00:05:04,100 or virion, assuming that the virions are uniformly 94 00:05:04,100 --> 00:05:08,130 distributed at random in the initial condition. 95 00:05:08,130 --> 00:05:12,090 So if we do that, then we're solving for the-- 96 00:05:12,090 --> 00:05:14,180 that's all [INAUDIBLE],, so I'll put it over here. 97 00:05:17,670 --> 00:05:24,600 The average escape time or first passage time for the virus 98 00:05:24,600 --> 00:05:27,150 will be tau bar. 99 00:05:27,150 --> 00:05:29,210 Well, what I'll do is I'll integrate over 100 00:05:29,210 --> 00:05:31,770 all the positions and then divide by the volume 101 00:05:31,770 --> 00:05:33,550 because a uniform distribution. 102 00:05:33,550 --> 00:05:35,909 So I'll write the integral over the volume 103 00:05:35,909 --> 00:05:39,840 as 4 pi, the solid angle times integral from 0 to capital 104 00:05:39,840 --> 00:05:47,340 R of tau of r r-squared DR. And I'll divide by the total volume 105 00:05:47,340 --> 00:05:51,720 4/3 pi capital r-cubed. 106 00:05:51,720 --> 00:05:55,900 OK, so if we do this integral here, 107 00:05:55,900 --> 00:05:57,820 so when we plug-in this, first of all, 108 00:05:57,820 --> 00:06:01,470 we can see that we get, obviously, 109 00:06:01,470 --> 00:06:03,540 for the constant term, r-squared over 60, 110 00:06:03,540 --> 00:06:06,810 we just have a ratio of volume over volume, which is one. 111 00:06:06,810 --> 00:06:10,380 So we get r squared over 6D is the first term, 112 00:06:10,380 --> 00:06:12,850 just integrating that constant. 113 00:06:12,850 --> 00:06:15,040 But then it's 1 minus. 114 00:06:15,040 --> 00:06:16,980 And then instead of r-squared, you 115 00:06:16,980 --> 00:06:18,940 have r-squared times this r-squared. 116 00:06:18,940 --> 00:06:20,440 It says r to fourth. 117 00:06:20,440 --> 00:06:21,600 So you integrate that. 118 00:06:21,600 --> 00:06:23,780 You get r to the fifth over 5. 119 00:06:23,780 --> 00:06:26,800 And so then you get 1/5 over this 1/3 here. 120 00:06:26,800 --> 00:06:28,460 And that gives you 3/5. 121 00:06:31,000 --> 00:06:33,490 And so that gives, when I subtract one minus 3/5, 122 00:06:33,490 --> 00:06:34,750 I get 2/5. 123 00:06:34,750 --> 00:06:37,120 And 2 over 6 is 1/3. 124 00:06:37,120 --> 00:06:42,940 And so this ends up being r-squared over 15D 125 00:06:42,940 --> 00:06:45,490 as we had previously quoted. 126 00:06:45,490 --> 00:06:47,830 So it's worth going through the calculation just to see. 127 00:06:47,830 --> 00:06:49,659 This number 15 is an order of magnitude. 128 00:06:49,659 --> 00:06:51,530 It's larger than 10. 129 00:06:51,530 --> 00:06:54,070 So while we normally estimate diffusion times 130 00:06:54,070 --> 00:06:57,640 to be of order length squared divided by D, 131 00:06:57,640 --> 00:07:00,010 so r-squared over d, this calculation 132 00:07:00,010 --> 00:07:03,130 shows that the actual average time is much smaller 133 00:07:03,130 --> 00:07:05,110 than that by a factor of 15. 134 00:07:05,110 --> 00:07:07,870 And that's precisely because the virus virions sometimes 135 00:07:07,870 --> 00:07:09,700 find themselves initially near the surface. 136 00:07:09,700 --> 00:07:10,870 So they get out more easily. 137 00:07:10,870 --> 00:07:12,490 So you don't have to wait for diffusion 138 00:07:12,490 --> 00:07:13,690 across the entire drop. 139 00:07:13,690 --> 00:07:15,370 That sets the overall scale. 140 00:07:15,370 --> 00:07:18,340 But the average drop diffusion time 141 00:07:18,340 --> 00:07:20,760 is actually less than that.