All language subtitles for [English] Understanding Laminar and Turbulent Flow [DownSub.com]

af Afrikaans
ak Akan
sq Albanian
am Amharic
ar Arabic
hy Armenian
az Azerbaijani
eu Basque
be Belarusian
bem Bemba
bn Bengali
bh Bihari
bs Bosnian
br Breton
bg Bulgarian
km Cambodian
ca Catalan
ceb Cebuano
chr Cherokee
ny Chichewa
zh-CN Chinese (Simplified)
zh-TW Chinese (Traditional) Download
co Corsican
hr Croatian
cs Czech
da Danish
nl Dutch
en English
eo Esperanto
et Estonian
ee Ewe
fo Faroese
tl Filipino
fi Finnish
fr French
fy Frisian
gaa Ga
gl Galician
ka Georgian
de German
el Greek
gn Guarani
gu Gujarati
ht Haitian Creole
ha Hausa
haw Hawaiian
iw Hebrew
hi Hindi
hmn Hmong
hu Hungarian
is Icelandic
ig Igbo
id Indonesian
ia Interlingua
ga Irish
it Italian
ja Japanese
jw Javanese
kn Kannada
kk Kazakh
rw Kinyarwanda
rn Kirundi
kg Kongo
ko Korean
kri Krio (Sierra Leone)
ku Kurdish
ckb Kurdish (Soranî)
ky Kyrgyz
lo Laothian
la Latin
lv Latvian
ln Lingala
lt Lithuanian
loz Lozi
lg Luganda
ach Luo
lb Luxembourgish
mk Macedonian
mg Malagasy
ms Malay
ml Malayalam
mt Maltese
mi Maori
mr Marathi
mfe Mauritian Creole
mo Moldavian
mn Mongolian
my Myanmar (Burmese)
sr-ME Montenegrin
ne Nepali
pcm Nigerian Pidgin
nso Northern Sotho
no Norwegian
nn Norwegian (Nynorsk)
oc Occitan
or Oriya
om Oromo
ps Pashto
fa Persian
pl Polish
pt-BR Portuguese (Brazil)
pt Portuguese (Portugal)
pa Punjabi
qu Quechua
ro Romanian
rm Romansh
nyn Runyakitara
ru Russian
sm Samoan
gd Scots Gaelic
sr Serbian
sh Serbo-Croatian
st Sesotho
tn Setswana
crs Seychellois Creole
sn Shona
sd Sindhi
si Sinhalese
sk Slovak
sl Slovenian
so Somali
es Spanish
es-419 Spanish (Latin American)
su Sundanese
sw Swahili
sv Swedish
tg Tajik
ta Tamil
tt Tatar
te Telugu
th Thai
ti Tigrinya
to Tonga
lua Tshiluba
tum Tumbuka
tr Turkish
tk Turkmen
tw Twi
ug Uighur
uk Ukrainian
ur Urdu
uz Uzbek
vi Vietnamese
cy Welsh
wo Wolof
xh Xhosa
yi Yiddish
yo Yoruba
zu Zulu
Would you like to inspect the original subtitles? These are the user uploaded subtitles that are being translated: 1 00:00:00,359 --> 00:00:06,759 This video from The Efficient Engineer is sponsored by Brilliant. 2 00:00:06,759 --> 00:00:10,849 One of the very first things you learn in fluid mechanics is the difference between 3 00:00:10,849 --> 00:00:12,599 laminar and turbulent flow. 4 00:00:12,599 --> 00:00:18,480 And for good reason - these two flow regimes behave in very different ways and, as we’ll 5 00:00:18,480 --> 00:00:25,830 see in this video, this has huge implications for fluid flow in the world around us 6 00:00:25,830 --> 00:00:29,539 Here we have an example of the laminar flow regime. 7 00:00:29,539 --> 00:00:32,610 It's characterised by smooth, even flow. 8 00:00:32,610 --> 00:00:37,620 The fluid is moving horizontally in layers, and there is a minimal amount of mixing between 9 00:00:37,620 --> 00:00:39,120 layers. 10 00:00:39,120 --> 00:00:44,590 As we increase the flow velocity we begin to see some bursts of random motion. 11 00:00:44,590 --> 00:00:49,170 This is the start of the transition between the laminar and turbulent regimes. 12 00:00:49,170 --> 00:00:54,970 If we continue increasing the velocity we end up with fully turbulent flow. 13 00:00:54,970 --> 00:00:59,680 Turbulent flow is characterised by chaotic movement and contains swirling regions called 14 00:00:59,680 --> 00:01:00,710 eddies. 15 00:01:00,710 --> 00:01:05,830 The chaotic motion and eddies result in significant mixing of the fluid. 16 00:01:05,830 --> 00:01:11,080 If we record the velocity at a single point in steady laminar flow, we'll get data that 17 00:01:11,080 --> 00:01:14,320 looks like this. 18 00:01:14,320 --> 00:01:20,270 There are no random velocity fluctuations, and so in general laminar flow is fairly easy 19 00:01:20,270 --> 00:01:22,250 to analyse. 20 00:01:22,250 --> 00:01:26,880 For turbulent flow we’ll get data that looks like this. 21 00:01:26,880 --> 00:01:29,780 This flow is much more complicated. 22 00:01:29,780 --> 00:01:35,470 We can think of the velocity as being made up of a time-averaged component, and a fluctuating 23 00:01:35,470 --> 00:01:37,990 component. 24 00:01:37,990 --> 00:01:43,820 The larger the fluctuating component, the more turbulent the flow. 25 00:01:43,820 --> 00:01:49,410 Because of its chaotic nature, analysis of turbulent flow is very complex. 26 00:01:49,410 --> 00:01:54,740 Since laminar and turbulent flow are so different and need to be analysed in different ways, 27 00:01:54,740 --> 00:01:59,890 we need to be able to predict which flow regime is likely to be produced by a particular set 28 00:01:59,890 --> 00:02:01,710 of flow condition 29 00:02:01,710 --> 00:02:08,810 We can do this using a parameter which was defined by Osborne Reynolds in 1883. 30 00:02:08,810 --> 00:02:13,470 Reynolds performed extensive testing to identify the parameters which affect the flow regime, 31 00:02:13,470 --> 00:02:19,099 and came up with this non-dimensional parameter, which we call Reynolds number. 32 00:02:19,099 --> 00:02:23,620 It's used to predict if flow will be laminar or turbulent. 33 00:02:23,620 --> 00:02:30,190 Rho is the fluid density, U is the velocity, L is a characteristic length dimension, and 34 00:02:30,190 --> 00:02:33,400 Mu is the fluid dynamic viscosity. 35 00:02:33,400 --> 00:02:38,560 The equation is sometimes written as a function of the kinematic viscosity instead, which 36 00:02:38,560 --> 00:02:44,040 is just the dynamic viscosity divided by the fluid density. 37 00:02:44,040 --> 00:02:49,140 The characteristic length L will depend on the type of flow we are analysing. 38 00:02:49,140 --> 00:02:54,480 For flow past a cylinder it will be the cylinder diameter. 39 00:02:54,480 --> 00:02:59,430 For flow past an airfoil it will be the chord length. 40 00:02:59,430 --> 00:03:05,420 And for flow through a pipe it will be the pipe diameter. 41 00:03:05,420 --> 00:03:09,129 Reynolds number is useful because it tells us the relative importance of the inertial 42 00:03:09,129 --> 00:03:14,110 forces and the viscous forces. 43 00:03:14,110 --> 00:03:18,710 Inertial forces are related to the momentum of the fluid, and so are essentially the forces 44 00:03:18,710 --> 00:03:22,010 which cause the fluid to move. 45 00:03:22,010 --> 00:03:26,709 Viscous forces are the frictional shear forces which develop between layers of the fluid 46 00:03:26,709 --> 00:03:31,290 due to its viscosity. 47 00:03:31,290 --> 00:03:36,959 If viscous forces dominate flow is more likely to be laminar, because the frictional forces 48 00:03:36,959 --> 00:03:42,480 within the fluid will dampen out any initial turbulent disturbances and random motion. 49 00:03:42,480 --> 00:03:47,670 This is why Reynolds number can be used to predict if flow will be laminar or turbulent. 50 00:03:47,670 --> 00:03:51,849 If inertial forces dominate, flow is more likely to be turbulent. 51 00:03:51,849 --> 00:03:52,849 But if viscous forces dominate, it’s more likely to be laminar. 52 00:03:52,849 --> 00:03:58,260 And so smaller values of Reynolds number indicate that flow will be laminar. 53 00:03:58,260 --> 00:04:03,090 The Reynolds number at which the transition to the turbulent regime occurs will vary depending 54 00:04:03,090 --> 00:04:05,870 on the type of flow we are dealing with. 55 00:04:05,870 --> 00:04:09,690 These are the ranges usually quoted for flow through a pipe, for example. 56 00:04:09,690 --> 00:04:14,930 Under very controlled conditions in a lab the onset of turbulence can be delayed until 57 00:04:14,930 --> 00:04:18,599 much larger Reynolds numbers. 58 00:04:18,599 --> 00:04:21,728 Most flows in the world around us are turbulent. 59 00:04:21,728 --> 00:04:26,060 The flow of smoke out of a chimney is usually turbulent. 60 00:04:29,540 --> 00:04:32,600 And so is the flow of air behind a car travelling at high speed. 61 00:04:41,920 --> 00:04:44,120 The flow of blood through vessels on the other 62 00:04:44,120 --> 00:04:52,289 hand is mostly laminar, because the characteristic length and velocity are small. 63 00:04:52,289 --> 00:04:56,580 This is fortunate because if it were turbulent the heart would have to work much harder to 64 00:04:56,580 --> 00:04:58,910 pump blood around the body. 65 00:04:58,910 --> 00:05:03,780 To understand why this is, let's look at how the flow regime affects flow through a circular 66 00:05:03,780 --> 00:05:05,629 pipe. 67 00:05:05,629 --> 00:05:09,539 The flow velocity right at the pipe wall is always zero. 68 00:05:09,539 --> 00:05:12,559 This is called the no-slip condition. 69 00:05:12,559 --> 00:05:17,899 For fully developed laminar flow, the velocity then increases to reach the maximum velocity 70 00:05:17,899 --> 00:05:19,649 at the centre of the pipe. 71 00:05:19,649 --> 00:05:24,249 The velocity profile is parabolic. 72 00:05:24,249 --> 00:05:27,789 For turbulent flow the profile is quite different. 73 00:05:27,789 --> 00:05:33,129 We still have the no-slip condition, but the average velocity profile is much flatter away 74 00:05:33,129 --> 00:05:34,669 from the wall. 75 00:05:34,669 --> 00:05:38,909 This is because turbulence introduces a lot of mixing between the different layers of 76 00:05:38,909 --> 00:05:43,939 flow, and this momentum transfer tends to homogenise the flow velocity across the pipe 77 00:05:43,939 --> 00:05:45,550 diameter. 78 00:05:45,550 --> 00:05:49,349 Note that I have shown the time-averaged velocity here. 79 00:05:49,349 --> 00:05:57,460 The instantaneous velocity profile will look something like this. 80 00:05:57,460 --> 00:06:03,319 In pipe flow one thing we are particularly interested in is pressure drop. 81 00:06:03,319 --> 00:06:07,169 Across any length of pipe there will be a drop in pressure due to the frictional shear 82 00:06:07,169 --> 00:06:10,589 forces acting within the fluid. 83 00:06:10,589 --> 00:06:15,750 The pressure drop in turbulent flow is much larger than in laminar flow, which explains 84 00:06:15,750 --> 00:06:21,449 why the heart would have to work harder if blood flow was mostly turbulent! 85 00:06:21,449 --> 00:06:26,870 We can calculate Delta-P along the pipe using the Darcy-Weisbach equation. 86 00:06:26,870 --> 00:06:32,649 It depends on the average flow velocity, the fluid density and a friction factor f. 87 00:06:32,649 --> 00:06:36,379 For laminar flow the friction factor can be calculated easily. 88 00:06:36,379 --> 00:06:39,529 It is just a function of the Reynolds number. 89 00:06:39,529 --> 00:06:43,809 If we combine these two equations we can see that the pressure drop is proportional to 90 00:06:43,809 --> 00:06:45,809 the flow velocity. 91 00:06:45,809 --> 00:06:49,770 But for turbulent flow calculating f is more complicated. 92 00:06:49,770 --> 00:06:52,550 It is defined by the Colebrook equation. 93 00:06:52,550 --> 00:06:57,279 f appears on both sides of the equation, so it needs to be solved iteratively. 94 00:06:57,279 --> 00:07:02,270 Unlike laminar flow, for which the pressure drop is proportional to the flow velocity, 95 00:07:02,270 --> 00:07:07,029 it turns out that for turbulent flow it is proportional to the flow velocity squared. 96 00:07:07,029 --> 00:07:10,619 And it also depends on the roughness of the pipe surface. 97 00:07:10,619 --> 00:07:15,719 Epsilon is the height of the pipe surface roughness, and the term Epsilon/D is 98 00:07:15,719 --> 00:07:18,129 called the relative roughness. 99 00:07:18,129 --> 00:07:22,659 Surface roughness is important for turbulent flow because it introduces disturbances into 100 00:07:22,659 --> 00:07:27,069 the flow, which can be amplified and result in additional turbulence. 101 00:07:27,069 --> 00:07:31,800 For laminar flow it doesn't have a significant effect because these disturbances are dampened 102 00:07:31,800 --> 00:07:35,469 out more easily by the viscous forces. 103 00:07:35,469 --> 00:07:40,419 Since the Colebrook equation is so difficult to use, engineers usually use its graphical 104 00:07:40,419 --> 00:07:48,889 representation, the Moody diagram, to look up friction factors for different flow conditions. 105 00:07:48,889 --> 00:07:53,331 Where flow is laminar the friction factor is only a function of Reynolds number, so 106 00:07:53,331 --> 00:07:56,939 we get a straight line on the Moody diagram. 107 00:07:56,939 --> 00:08:02,360 For turbulent flow you select the curve corresponding to the relative roughness of your pipe, and 108 00:08:02,360 --> 00:08:08,360 you can look up the friction factor for the Reynolds number of interest. 109 00:08:08,360 --> 00:08:13,800 So we know that if Reynolds number is large, inertial forces dominate, and the flow is 110 00:08:13,800 --> 00:08:14,800 turbulent. 111 00:08:14,800 --> 00:08:19,159 But even for turbulent flow viscous forces can be significant in the boundary layers 112 00:08:19,160 --> 00:08:22,880 that develop at solid walls. 113 00:08:26,680 --> 00:08:32,110 Because of the no-slip condition, shear stresses are large close to a wall. 114 00:08:32,110 --> 00:08:37,440 This means that in a turbulent boundary layer there remains a very thin area close to the 115 00:08:37,440 --> 00:08:42,448 wall where viscous forces dominate and flow is essentially laminar. 116 00:08:42,448 --> 00:08:45,890 We call this the laminar, or viscous, sublayer. 117 00:08:45,890 --> 00:08:50,250 Its thickness decreases as Reynolds number increases. 118 00:08:50,250 --> 00:08:55,360 Above the laminar sublayer there is the buffer layer, where both viscous and turbulent effects 119 00:08:55,360 --> 00:08:56,740 are significant. 120 00:08:56,740 --> 00:09:00,589 And above the buffer layer turbulent effects are dominant. 121 00:09:00,589 --> 00:09:04,670 If the roughness of a surface is contained entirely within the thickness of the laminar 122 00:09:04,670 --> 00:09:10,180 sublayer, the surface is said to be hydraulically smooth, because the roughness has no effect 123 00:09:10,180 --> 00:09:13,379 on the turbulent flow above the sublayer. 124 00:09:13,379 --> 00:09:18,519 This is important in pipe flow because, as can be seen from the Moody diagram, flow in 125 00:09:18,519 --> 00:09:23,440 smooth pipe has a lower friction factor and so smaller pressure drop than flow in rough 126 00:09:23,440 --> 00:09:25,290 pipe. 127 00:09:25,290 --> 00:09:29,959 We can see that for a given roughness the friction factors converge to a constant value 128 00:09:29,959 --> 00:09:34,561 to the right of this dashed line, meaning that at high Reynolds number the friction 129 00:09:34,561 --> 00:09:37,540 depends only on the relative roughness. 130 00:09:37,540 --> 00:09:42,839 At these high Reynolds numbers the thickness of the laminar sublayer is extremely thin, 131 00:09:42,840 --> 00:09:47,800 and so the effect of the surface roughness is governing. 132 00:09:49,940 --> 00:09:54,420 Modelling turbulent flow through a pipe is fairly simple, but most scenarios are far 133 00:09:54,420 --> 00:09:55,580 more complex. 134 00:09:55,580 --> 00:10:00,770 It’s worth talking more about why analysis of turbulent flow is so complicated, and a 135 00:10:00,770 --> 00:10:05,709 lot of it has to do with the turbulent eddies we saw at the start of the video. 136 00:10:05,709 --> 00:10:09,209 Large eddies contain a lot of kinetic energy. 137 00:10:09,209 --> 00:10:13,889 Over time the energy in these large eddies feeds the creation of progressively smaller 138 00:10:13,889 --> 00:10:19,970 eddies, until at the smallest scale the turbulent energy in minuscule eddies dissipates as heat, 139 00:10:19,970 --> 00:10:24,170 due to frictional forces caused by the fluid viscosity. 140 00:10:24,170 --> 00:10:28,390 We can think of the energy in the flow as cascading from the largest to the smallest 141 00:10:28,390 --> 00:10:32,930 eddies, and so this concept is called the energy cascade. 142 00:10:32,930 --> 00:10:38,839 The energy cascade was summarised in a very elegant way by the physicist Lewis Fry Richardson, 143 00:10:38,839 --> 00:10:44,089 who wrote that "Big whirls have little whirls that feed on their velocity, and little whirls 144 00:10:44,089 --> 00:10:48,680 have lesser whirls, and so on to viscosity". 145 00:10:48,680 --> 00:10:53,870 Because of this behaviour, turbulence involves a huge range of length and time scales. 146 00:10:53,870 --> 00:10:58,689 This makes analysis of turbulent flow very complex, to the point that it is probably 147 00:10:58,689 --> 00:11:03,889 the most significant challenge facing the field of Fluid Mechanics. 148 00:11:03,889 --> 00:11:09,740 For complex scenarios like flow past an airfoil, we can't accurately describe the fluid behaviour 149 00:11:09,740 --> 00:11:11,629 using simple equations. 150 00:11:11,629 --> 00:11:17,181 So to analyse the flow we have to use either experimentation or numerical methods, or a 151 00:11:17,181 --> 00:11:19,769 combination of the two. 152 00:11:19,769 --> 00:11:25,320 Modelling flow using numerical methods is the field of Computational Fluid Dynamics. 153 00:11:25,320 --> 00:11:30,300 It essentially involves using computational power to solve the Navier-Stokes equations, 154 00:11:30,300 --> 00:11:34,860 which is a system of partial differential equations that describes the behaviour of 155 00:11:34,860 --> 00:11:38,279 fluids, but is difficult to solve. 156 00:11:38,279 --> 00:11:43,990 To do this we model the fluid domain around the airfoil as a mesh of discrete elements, 157 00:11:43,990 --> 00:11:48,319 define boundary conditions and fluid properties, and apply an appropriate assessment technique 158 00:11:48,320 --> 00:11:50,380 to find a solution. 159 00:11:50,380 --> 00:11:55,140 I mentioned earlier that one of the main challenges when dealing with turbulence is capturing 160 00:11:55,149 --> 00:11:59,870 the wide range of length scales associated with the turbulent eddies. 161 00:11:59,870 --> 00:12:04,939 There are three main techniques which are used to simulate flow in CFD, and they differ 162 00:12:04,939 --> 00:12:09,339 mainly in how they treat turbulence on these different scales. 163 00:12:09,339 --> 00:12:12,230 First we have Direct Numerical Simulation. 164 00:12:12,230 --> 00:12:17,600 This involves solving the Navier-Stokes equations down to even the smallest scales, and so all 165 00:12:17,600 --> 00:12:22,709 turbulent eddies are fully resolved, meaning that they are simulated explicitly. 166 00:12:22,709 --> 00:12:27,149 This is very computationally expensive, and isn’t a practical solution for the vast 167 00:12:27,149 --> 00:12:29,850 majority of fluid flow problems. 168 00:12:29,850 --> 00:12:32,930 Next we have Large Eddy Simulation. 169 00:12:32,930 --> 00:12:37,699 This technique resolves the large scale eddies explicitly, but small scale eddies are filtered 170 00:12:37,699 --> 00:12:42,620 out and are modelled, using what is known as a subgrid-scale model. 171 00:12:42,620 --> 00:12:47,660 LES is much less computationally expensive than DNS. 172 00:12:47,660 --> 00:12:51,300 Finally we have the Reynolds-Averaged Navier-Stokes technique, 173 00:12:51,300 --> 00:12:55,240 which is the least computationally expensive of the three techniques. 174 00:12:55,280 --> 00:13:00,320 This is a time-averaged method which doesn’t resolve eddies explicitly at all. 175 00:13:00,330 --> 00:13:06,870 Instead it models the effect of eddies using the concept of turbulent viscosity. 176 00:13:06,870 --> 00:13:12,550 Several different turbulence models exist, like the K-Epsilon or K-Omega models, with 177 00:13:12,550 --> 00:13:16,889 different models being better suited to different problem types. 178 00:13:16,889 --> 00:13:22,610 As is so often the case in engineering, experience and intuition will need to be used to determine 179 00:13:22,610 --> 00:13:27,230 which techniques and models are best suited to a particular problem. 180 00:13:27,230 --> 00:13:31,550 When it comes to troubleshooting problems in the real world, the importance of engineering 181 00:13:31,550 --> 00:13:33,999 intuition can’t be overstated. 182 00:13:33,999 --> 00:13:37,999 And that’s why I’d like to introduce you to Brilliant. 183 00:13:37,999 --> 00:13:43,089 Brilliant is a math and science learning website and app that has courses covering a wide range 184 00:13:43,089 --> 00:13:50,240 of topics, including differential equations, energy, momentum, and even dimensional analysis, 185 00:13:50,240 --> 00:13:53,899 to name just a few which are relevant to Fluid Mechanics. 186 00:13:53,899 --> 00:13:58,720 But the Scientific Thinking course in particular is great for engineers. 187 00:13:58,720 --> 00:14:04,059 We know all too well that traditional engineering teaching tends to be very math-heavy, which 188 00:14:04,060 --> 00:14:10,360 can make even relatively simple topics seem complex, and can get in the way of true understanding. 189 00:14:10,360 --> 00:14:15,420 And that’s what I love about this course - it intentionally ditches the math and puts 190 00:14:15,420 --> 00:14:21,689 the emphasis on concepts, using fun puzzles to help you develop your engineering intuition. 191 00:14:21,689 --> 00:14:26,670 So if you’d like to start having fun actively developing your problem-solving intuition, 192 00:14:26,670 --> 00:14:32,970 and support this channel at the same time, head over to brilliant.org/EfficientEngineer 193 00:14:32,970 --> 00:14:34,899 and sign up for free. 194 00:14:34,900 --> 00:14:43,880 The first 200 people to sign up using this link will get 20% off the annual Premium subscription. 195 00:14:46,949 --> 00:14:50,040 That's it for this look at laminar and turbulent flow. 196 00:14:50,040 --> 00:14:51,319 Thanks for watching. 19851

Can't find what you're looking for?
Get subtitles in any language from opensubtitles.com, and translate them here.