{"id":785,"date":"2026-08-12T00:32:13","date_gmt":"2026-08-12T00:32:13","guid":{"rendered":"https:\/\/physicsfundamentalsinfo.com\/blog\/?p=785"},"modified":"2026-08-24T13:03:43","modified_gmt":"2026-08-24T13:03:43","slug":"viscosity-units-examples","status":"publish","type":"post","link":"https:\/\/physicsfundamentalsinfo.com\/blog\/fluids\/viscosity-units-examples\/","title":{"rendered":"Viscosity: Definition, Units and Examples"},"content":{"rendered":"\n<div class=\"pf-citation\"><div class=\"eyebrow\">Definition<\/div><p>\n\nViscosity is a fluid&#8217;s resistance to flow, caused by internal friction as layers of the fluid slide past one another. It equals the shear stress divided by the velocity gradient, and its SI unit is the pascal second (Pa\u00b7s). Honey has high viscosity; water and air have low viscosity.\n\n<\/p><\/div>\n\n<p>Tip a jar of honey and a glass of water over at the same moment. The water is gone in a second; the honey is still deciding. Same gravity, same tilt \u2014 utterly different behaviour.<\/p>\n\n<p>That difference has a name, a formula and a unit, and it governs far more than breakfast. It sets how thick your engine oil needs to be in January, why blood struggles through narrowed arteries, and why a spoonful of custard turns solid when you stir it fast.<\/p>\n\n<h2>What Is Viscosity?<\/h2>\n\n<p>Viscosity is a measure of how strongly a fluid resists being sheared \u2014 that is, how hard it is to make one layer of the fluid slide over the layer beneath it. High viscosity means the fluid fights the motion; low viscosity means it gives way easily.<\/p>\n\n<p>Think of a deck of cards lying flat. Push the top card sideways and the cards below drag along a little, held back by <a href=\"https:\/\/physicsfundamentalsinfo.com\/blog\/mechanics\/what-is-friction\/\">friction between the surfaces<\/a>. A fluid does the same thing \u2014 except the &#8220;cards&#8221; are molecular layers, and the resistance between them is viscosity.<\/p>\n\n<p>Two details make this work. First, fluid touching a solid surface sticks to it and moves with it \u2014 the <strong>no-slip condition<\/strong>. Second, because the wall holds one edge still and something else drags the other edge along, the speed must change gradually across the gap.<\/p>\n\n<p>That change in speed with distance is the <strong>velocity gradient<\/strong>. Viscosity is simply the constant that links it to the force required.<\/p>\n\n<h2>The Viscosity Formula<\/h2>\n\n<p>The viscosity formula states that shear stress equals dynamic viscosity multiplied by the velocity gradient. This is Newton&#8217;s law of viscosity, and it is the definition from which every viscosity unit follows.<\/p>\n\n<div class=\"pf-formula\">\u03c4 = \u03bc(du\/dy)<\/div>\n\n<p>Each symbol carries a specific SI unit:<\/p>\n\n<ul>\n<li><strong>\u03c4<\/strong> (tau) \u2014 shear stress: the tangential force per unit area on a fluid layer, in pascals (Pa), equal to N\/m<sup>2<\/sup>.<\/li>\n<li><strong>\u03bc<\/strong> (mu) \u2014 dynamic viscosity, the fluid property itself, in pascal seconds (Pa\u00b7s).<\/li>\n<li><strong>du\/dy<\/strong> \u2014 velocity gradient or shear rate: how quickly flow speed changes across the gap, in reciprocal seconds (s<sup>\u22121<\/sup>).<\/li>\n<li><strong>u<\/strong> \u2014 local flow speed, in metres per second (m\/s).<\/li>\n<li><strong>y<\/strong> \u2014 distance measured perpendicular to the flow, in metres (m).<\/li>\n<\/ul>\n\n<p>Rearranged, \u03bc = \u03c4 \u00f7 (du\/dy). So dynamic viscosity is the shear stress needed per unit of shear rate \u2014 and that is exactly what a Pa\u00b7s means: one pascal of stress producing a shear rate of one per second.<\/p>\n\n<div style=\"background:#0A1628;border:1px solid #C8932A;border-radius:4px;padding:6px;margin:28px 0;\">\n<figure class=\"pf-figure\" style=\"margin:1.6em 0;\"><img src=\"https:\/\/physicsfundamentalsinfo.com\/blog\/wp-content\/uploads\/2026\/08\/viscosity-units-examples-moving-top-plate-stationary-bottom.webp\" width=\"1400\" height=\"846\" alt=\"Viscosity diagram showing a moving top plate, a stationary bottom plate, and the linear velocity gradient of the fluid between them\" loading=\"lazy\" decoding=\"async\" style=\"width:100%;height:auto;max-width:700px;display:block;margin:0 auto;\" \/><\/figure>\n<\/div>\n\n<p style=\"text-align:center;font-size:13px;font-style:italic;color:#1F2E47;\">Fluid sheared between two plates. The no-slip condition pins the fluid to each plate, producing a steady velocity gradient across the gap.<\/p>\n\n<div class=\"pf-sim-slot\"><div class=\"pf-sim-slot-header\"><span class=\"icon-dot\"><\/span><span class=\"label\">Viscosity Lab<\/span><\/div><div class=\"pf-sim-slot-body\"><style>.pf-sim-frame{width:100%;border:none;height:600px}@media(max-width:760px){.pf-sim-frame{height:1000px}}<\/style><iframe src=\"\/labs\/viscosity.html?embed=1\" class=\"pf-sim-frame\" loading=\"lazy\"><\/iframe><\/div><\/div>\n\n<h2>Units of Viscosity: Pa\u00b7s, Poise and Stokes<\/h2>\n\n<p>The SI unit of dynamic viscosity is the pascal second (Pa\u00b7s), also written N\u00b7s\/m<sup>2<\/sup> or kg\/(m\u00b7s). Older CGS units survive stubbornly in industry, which is why oil datasheets still speak in centipoise and centistokes.<\/p>\n\n<p>One poise (P) equals 0.1 Pa\u00b7s. One centipoise (cP) is a hundredth of that \u2014 exactly 10<sup>\u22123<\/sup> Pa\u00b7s, or one millipascal second. Water sits almost precisely at 1 cP at 20 \u00b0C, which is no accident: that convenient coincidence is why the unit stuck.<\/p>\n\n<div class=\"pf-table-scroll\" style=\"display:block;width:100%;max-width:100%;overflow-x:auto;-webkit-overflow-scrolling:touch;margin:1.5em 0;\">\n<table style=\"width:100%;border-collapse:collapse;\">\n<thead>\n<tr style=\"background:#0A1628;color:#FAF6EE;\">\n<th style=\"padding:10px;border:1px solid #D9CFB8;text-align:left;\">Quantity<\/th>\n<th style=\"padding:10px;border:1px solid #D9CFB8;text-align:left;\">SI unit<\/th>\n<th style=\"padding:10px;border:1px solid #D9CFB8;text-align:left;\">CGS unit<\/th>\n<th style=\"padding:10px;border:1px solid #D9CFB8;text-align:left;\">Conversion<\/th>\n<th style=\"padding:10px;border:1px solid #D9CFB8;text-align:left;\">Water at 20 \u00b0C<\/th>\n<\/tr>\n<\/thead>\n<tbody>\n<tr>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\"><strong>Dynamic viscosity (\u03bc)<\/strong><\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">pascal second, Pa\u00b7s<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">poise, P<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1 P = 0.1 Pa\u00b7s<br>1 cP = 10<sup>\u22123<\/sup> Pa\u00b7s<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1.002 \u00d7 10<sup>\u22123<\/sup> Pa\u00b7s (1.002 cP)<\/td>\n<\/tr>\n<tr style=\"background:#F5F2EA;\">\n<td style=\"padding:10px;border:1px solid #D9CFB8;\"><strong>Kinematic viscosity (\u03bd)<\/strong><\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">square metre per second, m<sup>2<\/sup>\/s<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">stokes, St<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1 St = 10<sup>\u22124<\/sup> m<sup>2<\/sup>\/s<br>1 cSt = 10<sup>\u22126<\/sup> m<sup>2<\/sup>\/s = 1 mm<sup>2<\/sup>\/s<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1.004 \u00d7 10<sup>\u22126<\/sup> m<sup>2<\/sup>\/s (1.004 cSt)<\/td>\n<\/tr>\n<tr>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\"><strong>Shear stress (\u03c4)<\/strong><\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">pascal, Pa<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">dyne\/cm<sup>2<\/sup><\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1 dyne\/cm<sup>2<\/sup> = 0.1 Pa<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">depends on shear rate<\/td>\n<\/tr>\n<tr style=\"background:#F5F2EA;\">\n<td style=\"padding:10px;border:1px solid #D9CFB8;\"><strong>Shear rate (du\/dy)<\/strong><\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">per second, s<sup>\u22121<\/sup><\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">per second, s<sup>\u22121<\/sup><\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">identical<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">set by the flow<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<\/div>\n\n<p>The value of 1.002 cP for water at 20 \u00b0C is not a textbook rounding. It was fixed by a decade-long capillary-flow determination at the US National Bureau of Standards, now NIST, and <a href=\"https:\/\/nvlpubs.nist.gov\/nistpubs\/jres\/048\/1\/V48.N01.A01.pdf\" target=\"_blank\" rel=\"noopener\">adopted in 1952 as the primary reference standard<\/a> against which other viscometers are still calibrated.<\/p>\n\n<h2>Dynamic vs Kinematic Viscosity<\/h2>\n\n<p>Dynamic viscosity measures resistance to shear on its own; kinematic viscosity measures that resistance relative to the fluid&#8217;s density. Divide one by the other and you get the second.<\/p>\n\n<div class=\"pf-formula\">\u03bd = \u03bc \/ \u03c1<\/div>\n\n<ul>\n<li><strong>\u03bd<\/strong> (nu) \u2014 kinematic viscosity, in m<sup>2<\/sup>\/s.<\/li>\n<li><strong>\u03bc<\/strong> (mu) \u2014 dynamic viscosity, in Pa\u00b7s.<\/li>\n<li><strong>\u03c1<\/strong> (rho) \u2014 <a href=\"https:\/\/physicsfundamentalsinfo.com\/blog\/fluids\/density-formula\/\">density of the fluid<\/a>, in kg\/m<sup>3<\/sup>.<\/li>\n<\/ul>\n\n<p>Why bother with two? Because they answer different questions. Dynamic viscosity tells you the force you must supply to shear the fluid; kinematic viscosity tells you how readily the fluid&#8217;s own momentum spreads sideways compared with how much inertia it carries.<\/p>\n\n<p>Lubricant and fuel datasheets almost always quote kinematic viscosity in centistokes, because that is what a gravity-fed capillary viscometer measures directly. Converting to Pa\u00b7s means multiplying by density \u2014 a step it is easy to forget under exam pressure, and one you can check against our <a href=\"https:\/\/physicsfundamentalsinfo.com\/calculators\/viscosity-converter\">Viscosity Converter<\/a> when a datasheet gives you cSt and the question wants Pa\u00b7s.<\/p>\n\n<h2>How Viscosity Works Inside a Fluid<\/h2>\n\n<p>Viscosity arises from momentum being carried sideways between fluid layers, but the mechanism differs completely in liquids and gases. That difference produces one of the most counter-intuitive results in fluid mechanics.<\/p>\n\n<h3>Liquids: molecules that cling<\/h3>\n\n<p>In a liquid, molecules sit close together and attract one another. To shear the liquid you must repeatedly break and reform those bonds, and that costs force.<\/p>\n\n<p>Heat the liquid and the molecules jiggle harder, escaping each other&#8217;s pull more easily. So <strong>liquid viscosity falls as temperature rises<\/strong> \u2014 steeply. Water is about 3.6 times less viscous at 100 \u00b0C than at 20 \u00b0C, which is why hot oil pours like water and cold treacle barely moves.<\/p>\n\n<h3>Gases: molecules that trade places<\/h3>\n\n<p>Gas molecules are far apart and barely attract each other, so bonding is irrelevant. Instead, fast molecules from a quick-moving layer wander into a slower layer and speed it up, while slow molecules drift the other way and drag the fast layer back.<\/p>\n\n<p>This exchange of momentum <em>is<\/em> the gas&#8217;s viscosity. Heat the gas and the molecules cross between layers faster, so <strong>gas viscosity rises as temperature rises<\/strong> \u2014 the exact opposite of a liquid.<\/p>\n\n<div style=\"background:#0A1628;border:1px solid #C8932A;border-radius:4px;padding:6px;margin:28px 0;\">\n<figure class=\"pf-figure\" style=\"margin:1.6em 0;\"><img src=\"https:\/\/physicsfundamentalsinfo.com\/blog\/wp-content\/uploads\/2026\/08\/viscosity-units-examples-comparing-how-changes-temperature-falling.webp\" width=\"1400\" height=\"700\" alt=\"Graph comparing how viscosity changes with temperature, falling steeply for liquids and rising gently for gases\" loading=\"lazy\" decoding=\"async\" style=\"width:100%;height:auto;max-width:700px;display:block;margin:0 auto;\" \/><\/figure>\n<\/div>\n\n<p style=\"text-align:center;font-size:13px;font-style:italic;color:#1F2E47;\">Temperature dependence of viscosity. Liquids thin dramatically on heating; gases thicken slightly. Curves are schematic, not to scale.<\/p>\n\n<p>The no-slip condition that anchors all of this has a visible consequence: a thin layer where flow speed climbs from zero at a surface to the free-stream value. Engineers call it the boundary layer, and NASA&#8217;s aeronautics guide explains <a href=\"https:\/\/www1.grc.nasa.gov\/beginners-guide-to-aeronautics\/boundary-layer\/\" target=\"_blank\" rel=\"noopener\">how viscosity creates it around a wing<\/a>.<\/p>\n\n<h2>Real-World Examples of Viscosity<\/h2>\n\n<p>Viscosity spans an enormous range \u2014 roughly a million-fold between air and honey at room temperature. The table below lists measured values at 20 \u00b0C, with kinematic viscosity worked out from each fluid&#8217;s density.<\/p>\n\n<div class=\"pf-table-scroll\" style=\"display:block;width:100%;max-width:100%;overflow-x:auto;-webkit-overflow-scrolling:touch;margin:1.5em 0;\">\n<table style=\"width:100%;border-collapse:collapse;\">\n<thead>\n<tr style=\"background:#0A1628;color:#FAF6EE;\">\n<th style=\"padding:10px;border:1px solid #D9CFB8;text-align:left;\">Fluid (20 \u00b0C)<\/th>\n<th style=\"padding:10px;border:1px solid #D9CFB8;text-align:left;\">Dynamic \u03bc (Pa\u00b7s)<\/th>\n<th style=\"padding:10px;border:1px solid #D9CFB8;text-align:left;\">In cP<\/th>\n<th style=\"padding:10px;border:1px solid #D9CFB8;text-align:left;\">Density \u03c1 (kg\/m<sup>3<\/sup>)<\/th>\n<th style=\"padding:10px;border:1px solid #D9CFB8;text-align:left;\">Kinematic \u03bd (m<sup>2<\/sup>\/s)<\/th>\n<\/tr>\n<\/thead>\n<tbody>\n<tr>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">Air<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1.81 \u00d7 10<sup>\u22125<\/sup><\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">0.018<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1.20<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1.50 \u00d7 10<sup>\u22125<\/sup><\/td>\n<\/tr>\n<tr style=\"background:#F5F2EA;\">\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">Water<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1.00 \u00d7 10<sup>\u22123<\/sup><\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1.00<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">998<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1.00 \u00d7 10<sup>\u22126<\/sup><\/td>\n<\/tr>\n<tr>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">Mercury<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1.55 \u00d7 10<sup>\u22123<\/sup><\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1.55<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">13 534<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1.15 \u00d7 10<sup>\u22127<\/sup><\/td>\n<\/tr>\n<tr style=\"background:#F5F2EA;\">\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">Olive oil<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">8.4 \u00d7 10<sup>\u22122<\/sup><\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">84<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">915<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">9.2 \u00d7 10<sup>\u22125<\/sup><\/td>\n<\/tr>\n<tr>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">Glycerine<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1.41<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1 410<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1 261<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1.12 \u00d7 10<sup>\u22123<\/sup><\/td>\n<\/tr>\n<tr style=\"background:#F5F2EA;\">\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">Honey (typical)<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">about 10<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">about 10 000<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">1 420<\/td>\n<td style=\"padding:10px;border:1px solid #D9CFB8;\">7.0 \u00d7 10<sup>\u22123<\/sup><\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<\/div>\n\n<p>Honey values vary widely with water content and floral source, so treat that row as a typical figure rather than a constant. Everything else in the table is a standard measured value at 20 \u00b0C.<\/p>\n\n<p>Six places this actually matters:<\/p>\n\n<ul>\n<li><strong>Engine oil grades.<\/strong> A &#8220;5W-30&#8221; label is a viscosity specification \u2014 the oil must stay thin enough to pump when cold and thick enough to keep a film between bearing surfaces when hot.<\/li>\n<li><strong>Blood flow.<\/strong> Blood is roughly three to four times more viscous than water. Raised viscosity forces the heart to generate more pressure for the same flow.<\/li>\n<li><strong>Honey off a spoon.<\/strong> High viscosity means the shear stress from gravity produces only a tiny shear rate, so the strand thins slowly instead of breaking.<\/li>\n<li><strong>Paint and printing inks.<\/strong> Formulated to flow under the brush or roller, then stiffen fast enough not to run down the wall.<\/li>\n<li><strong>Volcanic lava.<\/strong> Silica-rich lava is thousands of times more viscous than basaltic lava, which is why some volcanoes ooze and others explode.<\/li>\n<li><strong>Aircraft skin friction.<\/strong> Air&#8217;s tiny viscosity still produces a large drag force, because aircraft skin area is huge and shear rates near the surface are enormous.<\/li>\n<\/ul>\n\n<figure style=\"margin:32px auto;max-width:640px;text-align:center;\">\n\n  <img decoding=\"async\" src=\"https:\/\/physicsfundamentalsinfo.com\/blog\/wp-content\/uploads\/2026\/08\/kashmiri-sidr-honey-dipper-resting-on-shallow-dish.webp\"\n\n       alt=\"High viscosity honey pouring slowly in an unbroken strand\"\n\n       loading=\"lazy\"\n\n       style=\"width:100%;height:auto;border-radius:4px;\" width=\"1024\" height=\"1024\">\n\n  <figcaption style=\"font-size:13px;color:#1F2E47;font-style:italic;margin-top:8px;\">Honey&#8217;s viscosity is roughly 10 000 times that of water, so gravity shears it only slowly.<\/figcaption>\n\n<\/figure>\n\n<h2>Newtonian vs Non-Newtonian Fluids<\/h2>\n\n<p>A Newtonian fluid has a viscosity that stays constant no matter how fast you shear it. Water, air, glycerine and most thin oils behave this way, so a single value of \u03bc describes them completely at a given temperature.<\/p>\n\n<p>Non-Newtonian fluids break that rule \u2014 their apparent viscosity changes with the shear rate itself. Two families cover most everyday cases.<\/p>\n\n<ul>\n<li><strong>Shear-thinning<\/strong> fluids get runnier the harder you work them. Ketchup, blood, paint and shampoo all thin under stress; this is why shaking the bottle works.<\/li>\n<li><strong>Shear-thickening<\/strong> fluids get stiffer. Cornflour-and-water paste is the classic demonstration \u2014 stir it slowly and it flows, punch it and it resists like a solid.<\/li>\n<\/ul>\n\n<p>A practical consequence: quoting &#8220;the viscosity of ketchup&#8221; without stating the shear rate is meaningless. For non-Newtonian fluids the number only exists alongside the conditions it was measured under.<\/p>\n\n<h2>Common Misconceptions About Viscosity<\/h2>\n\n<h3>1. &#8220;Viscosity is the same as density&#8221;<\/h3>\n\n<p>These are entirely independent properties, and the table above proves it. Mercury is 13.6 times denser than water yet only about 1.5 times as viscous \u2014 pour it and it splashes like water.<\/p>\n\n<p>Honey does the reverse: barely 1.4 times the density of water, but around 10 000 times the viscosity. Density is how much mass is packed in; viscosity is how hard the fluid resists shearing.<\/p>\n\n<h3>2. &#8220;Air is basically inviscid&#8221;<\/h3>\n\n<p>Air&#8217;s viscosity is small in absolute terms but never zero, and the consequences are not small. Skin-friction drag on an airliner comes entirely from air viscosity.<\/p>\n\n<p>Stranger still, air&#8217;s <em>kinematic<\/em> viscosity is about 15 times larger than water&#8217;s, because air&#8217;s density is so low. By that measure, air is the &#8220;thicker&#8221; fluid.<\/p>\n\n<h3>3. &#8220;Heating always lowers viscosity&#8221;<\/h3>\n\n<p>True for liquids, false for gases. Warm a gas and its viscosity climbs, because momentum transfer between layers speeds up. Sutherland&#8217;s law is built on exactly this behaviour.<\/p>\n\n<h3>4. &#8220;Thicker oil is always better lubrication&#8221;<\/h3>\n\n<p>Too viscous and the oil will not reach the bearing surfaces quickly on a cold start, and it wastes power as heat once running. Problem 7 below puts a number on that loss: 324 watts dissipated by a single sliding plate.<\/p>\n\n<h2>How Viscosity Relates to Drag, Flow and the Reynolds Number<\/h2>\n\n<p>Viscosity determines whether a flow is smooth or chaotic, and how strongly a fluid resists an object moving through it. The bridge between these ideas is the Reynolds number, a dimensionless ratio of inertial forces to viscous forces.<\/p>\n\n<div class=\"pf-formula\">Re = \u03c1vL \/ \u03bc = vL \/ \u03bd<\/div>\n\n<ul>\n<li><strong>Re<\/strong> \u2014 Reynolds number, dimensionless.<\/li>\n<li><strong>v<\/strong> \u2014 flow speed, in m\/s; <strong>L<\/strong> \u2014 characteristic length such as pipe diameter, in m.<\/li>\n<li><strong>\u03c1<\/strong>, <strong>\u03bc<\/strong>, <strong>\u03bd<\/strong> \u2014 density (kg\/m<sup>3<\/sup>), dynamic viscosity (Pa\u00b7s) and kinematic viscosity (m<sup>2<\/sup>\/s).<\/li>\n<\/ul>\n\n<p>In pipes, flow below roughly Re = 2000 is laminar and above about 4000 is turbulent. High viscosity keeps Re low and the flow orderly; that is why thick oil moves in smooth layers while water of the same speed tumbles.<\/p>\n\n<p>Viscosity also feeds directly into <a href=\"https:\/\/physicsfundamentalsinfo.com\/blog\/mechanics\/drag-force\/\">drag force<\/a>. At very low Reynolds numbers, Stokes&#8217; law gives drag on a sphere as F = 6\u03c0\u03bcrv, and setting that against gravity yields the <a href=\"https:\/\/physicsfundamentalsinfo.com\/blog\/mechanics\/terminal-velocity\/\">terminal velocity<\/a> of a falling ball bearing \u2014 the basis of the falling-sphere viscometer.<\/p>\n\n<p>For pipe flow, viscosity sets how much <a href=\"https:\/\/physicsfundamentalsinfo.com\/blog\/fluids\/pressure-in-physics\/\">pressure<\/a> you lose along the length. Poiseuille&#8217;s law, Q = \u03c0\u0394P r<sup>4<\/sup> \/ (8\u03bcL), shows flow rate falling inversely with viscosity and rising with the fourth power of radius.<\/p>\n\n<p>Compare that with <a href=\"https:\/\/physicsfundamentalsinfo.com\/blog\/fluids\/bernoullis-principle\/\">Bernoulli&#8217;s principle<\/a>, which assumes zero viscosity. Bernoulli predicts no pressure loss along a level pipe of constant width \u2014 real pipes always lose pressure, and viscosity is the reason.<\/p>\n\n<h2>Worked Problems<\/h2>\n\n<div class=\"pf-problem\"><div class=\"pf-problem-num\">Problem 1<\/div><div class=\"pf-problem-question\">A flat plate slides over a 4.0 mm layer of oil at 2.0 m\/s. The oil has dynamic viscosity 0.50 Pa\u00b7s. Find the velocity gradient, the shear stress, and the force needed if the plate contacts 0.20 m^2 of oil.<\/div><details><summary>Show Solution<\/summary><div class=\"pf-problem-solution\">\n<p><strong>Solution:<\/strong><\/p>\n<p>Step 1: With no-slip at both surfaces the profile is linear, so du\/dy = U \/ h.<\/p>\n<p>Step 2: du\/dy = 2.0 m\/s \u00f7 (4.0 \u00d7 10<sup>\u22123<\/sup> m) = 500 s<sup>\u22121<\/sup><\/p>\n<p>Step 3: \u03c4 = \u03bc(du\/dy) = 0.50 Pa\u00b7s \u00d7 500 s<sup>\u22121<\/sup> = 250 Pa<\/p>\n<p>Step 4: F = \u03c4A = 250 Pa \u00d7 0.20 m<sup>2<\/sup> = 50 N<\/p>\n<p><strong>Answer: du\/dy = 500 s<sup>\u22121<\/sup>, \u03c4 = 250 Pa, F = 50 N<\/strong><\/p>\n<\/div><\/details><\/div>\n\n<div class=\"pf-problem\"><div class=\"pf-problem-num\">Problem 2<\/div><div class=\"pf-problem-question\">An engine oil is quoted as 250 cP. Express this dynamic viscosity in Pa\u00b7s and in poise.<\/div><details><summary>Show Solution<\/summary><div class=\"pf-problem-solution\">\n<p><strong>Solution:<\/strong><\/p>\n<p>Step 1: By definition, 1 P = 0.1 Pa\u00b7s and 1 cP = 0.01 P = 10<sup>\u22123<\/sup> Pa\u00b7s.<\/p>\n<p>Step 2: \u03bc = 250 cP \u00d7 10<sup>\u22123<\/sup> Pa\u00b7s\/cP = 0.250 Pa\u00b7s<\/p>\n<p>Step 3: \u03bc = 250 cP \u00f7 100 cP\/P = 2.50 P<\/p>\n<p><strong>Answer: 0.250 Pa\u00b7s, which is 2.50 poise<\/strong><\/p>\n<\/div><\/details><\/div>\n\n<div class=\"pf-problem\"><div class=\"pf-problem-num\">Problem 3<\/div><div class=\"pf-problem-question\">A hydraulic oil has kinematic viscosity 46 cSt and density 870 kg\/m^3. Find its dynamic viscosity in Pa\u00b7s.<\/div><details><summary>Show Solution<\/summary><div class=\"pf-problem-solution\">\n<p><strong>Solution:<\/strong><\/p>\n<p>Step 1: \u03bd = \u03bc \/ \u03c1, so rearranging gives \u03bc = \u03bd\u03c1.<\/p>\n<p>Step 2: Convert the unit: 1 cSt = 10<sup>\u22126<\/sup> m<sup>2<\/sup>\/s, so \u03bd = 46 \u00d7 10<sup>\u22126<\/sup> m<sup>2<\/sup>\/s.<\/p>\n<p>Step 3: \u03bc = (46 \u00d7 10<sup>\u22126<\/sup> m<sup>2<\/sup>\/s)(870 kg\/m<sup>3<\/sup>) = 0.0400 kg\/(m\u00b7s)<\/p>\n<p>Step 4: kg\/(m\u00b7s) is identical to Pa\u00b7s, so no further conversion is needed.<\/p>\n<p><strong>Answer: \u03bc = 0.040 Pa\u00b7s (40 mPa\u00b7s, or 40 cP)<\/strong><\/p>\n<\/div><\/details><\/div>\n\n<div class=\"pf-problem\"><div class=\"pf-problem-num\">Problem 4<\/div><div class=\"pf-problem-question\">Water at 20 \u00b0C (\u03c1 = 998 kg\/m^3, \u03bc = 1.00 \u00d7 10^-3 Pa\u00b7s) flows at 0.60 m\/s through a pipe of internal diameter 25 mm. Find the Reynolds number and classify the flow.<\/div><details><summary>Show Solution<\/summary><div class=\"pf-problem-solution\">\n<p><strong>Solution:<\/strong><\/p>\n<p>Step 1: Re = \u03c1vd \/ \u03bc, taking the characteristic length as the pipe diameter.<\/p>\n<p>Step 2: Re = (998 kg\/m<sup>3<\/sup>)(0.60 m\/s)(0.025 m) \u00f7 (1.00 \u00d7 10<sup>\u22123<\/sup> Pa\u00b7s)<\/p>\n<p>Step 3: Numerator = 14.97 kg\/(m\u00b7s), so Re = 14.97 \u00f7 1.00 \u00d7 10<sup>\u22123<\/sup> = 1.497 \u00d7 10<sup>4<\/sup><\/p>\n<p>Step 4: Re is well above 4000, so the flow is turbulent.<\/p>\n<p><strong>Answer: Re \u2248 1.5 \u00d7 10<sup>4<\/sup> \u2014 turbulent flow<\/strong><\/p>\n<\/div><\/details><\/div>\n\n<div class=\"pf-problem\"><div class=\"pf-problem-num\">Problem 5<\/div><div class=\"pf-problem-question\">A steel ball of radius 2.0 mm and density 7800 kg\/m^3 falls through glycerine (density 1260 kg\/m^3, viscosity 1.41 Pa\u00b7s). Find its terminal velocity. Take g = 9.81 m\/s^2.<\/div><details><summary>Show Solution<\/summary><div class=\"pf-problem-solution\">\n<p><strong>Solution:<\/strong><\/p>\n<p>Step 1: At terminal velocity, weight = buoyancy + viscous drag, using Stokes&#8217; law F = 6\u03c0\u03bcrv.<\/p>\n<p>Step 2: (4\/3)\u03c0r<sup>3<\/sup>\u03c1_s g = (4\/3)\u03c0r<sup>3<\/sup>\u03c1_f g + 6\u03c0\u03bcrv<\/p>\n<p>Step 3: Rearranging gives v = 2r<sup>2<\/sup>(\u03c1_s \u2212 \u03c1_f)g \/ (9\u03bc)<\/p>\n<p>Step 4: Numerator = 2(2.0 \u00d7 10<sup>\u22123<\/sup> m)<sup>2<\/sup>(7800 \u2212 1260 kg\/m<sup>3<\/sup>)(9.81 m\/s<sup>2<\/sup>) = 0.5133<\/p>\n<p>Step 5: Denominator = 9 \u00d7 1.41 Pa\u00b7s = 12.69, so v = 0.5133 \u00f7 12.69 = 0.0404 m\/s<\/p>\n<p>Step 6: Check Stokes&#8217; law applies: Re = \u03c1_f v d \/ \u03bc = 0.14, comfortably below 1.<\/p>\n<p><strong>Answer: v \u2248 0.040 m\/s (about 4.0 cm\/s)<\/strong><\/p>\n<\/div><\/details><\/div>\n\n<div class=\"pf-problem\"><div class=\"pf-problem-num\">Problem 6<\/div><div class=\"pf-problem-question\">Water (\u03bc = 1.00 \u00d7 10^-3 Pa\u00b7s) flows through a horizontal tube of radius 1.0 mm and length 0.50 m under a pressure difference of 4.0 kPa. Find the volume flow rate, then state the effect of halving the radius.<\/div><details><summary>Show Solution<\/summary><div class=\"pf-problem-solution\">\n<p><strong>Solution:<\/strong><\/p>\n<p>Step 1: Poiseuille&#8217;s law for laminar flow gives Q = \u03c0\u0394P r<sup>4<\/sup> \/ (8\u03bcL).<\/p>\n<p>Step 2: Numerator = \u03c0(4000 Pa)(1.0 \u00d7 10<sup>\u22123<\/sup> m)<sup>4<\/sup> = 1.257 \u00d7 10<sup>\u22128<\/sup><\/p>\n<p>Step 3: Denominator = 8(1.00 \u00d7 10<sup>\u22123<\/sup> Pa\u00b7s)(0.50 m) = 4.00 \u00d7 10<sup>\u22123<\/sup><\/p>\n<p>Step 4: Q = 1.257 \u00d7 10<sup>\u22128<\/sup> \u00f7 4.00 \u00d7 10<sup>\u22123<\/sup> = 3.14 \u00d7 10<sup>\u22126<\/sup> m<sup>3<\/sup>\/s = 3.1 mL\/s<\/p>\n<p>Step 5: Q depends on r<sup>4<\/sup>, so halving r divides the flow by 2<sup>4<\/sup> = 16, giving 0.20 mL\/s.<\/p>\n<p><strong>Answer: Q \u2248 3.1 \u00d7 10<sup>\u22126<\/sup> m<sup>3<\/sup>\/s (3.1 mL\/s); halving the radius drops it to \u2248 0.20 mL\/s<\/strong><\/p>\n<\/div><\/details><\/div>\n\n<div class=\"pf-problem\"><div class=\"pf-problem-num\">Problem 7<\/div><div class=\"pf-problem-question\">A 0.30 m \u00d7 0.30 m plate slides at 1.5 m\/s over a 0.50 mm oil film of viscosity 0.80 Pa\u00b7s. Find the viscous force resisting the motion and the power dissipated as heat.<\/div><details><summary>Show Solution<\/summary><div class=\"pf-problem-solution\">\n<p><strong>Solution:<\/strong><\/p>\n<p>Step 1: du\/dy = U \/ h = 1.5 m\/s \u00f7 (0.50 \u00d7 10<sup>\u22123<\/sup> m) = 3000 s<sup>\u22121<\/sup><\/p>\n<p>Step 2: \u03c4 = \u03bc(du\/dy) = 0.80 Pa\u00b7s \u00d7 3000 s<sup>\u22121<\/sup> = 2400 Pa<\/p>\n<p>Step 3: A = 0.30 m \u00d7 0.30 m = 0.090 m<sup>2<\/sup>, so F = \u03c4A = 2400 Pa \u00d7 0.090 m<sup>2<\/sup> = 216 N<\/p>\n<p>Step 4: P = Fv = 216 N \u00d7 1.5 m\/s = 324 W<\/p>\n<p><strong>Answer: F = 216 N, and 324 W is dissipated as heat in the oil film<\/strong><\/p>\n<\/div><\/details><\/div>\n\n<div class=\"pf-problem\"><div class=\"pf-problem-num\">Problem 8<\/div><div class=\"pf-problem-question\">At 20 \u00b0C water has \u03bc = 1.00 \u00d7 10^-3 Pa\u00b7s and \u03c1 = 998 kg\/m^3, while air has \u03bc = 1.81 \u00d7 10^-5 Pa\u00b7s and \u03c1 = 1.20 kg\/m^3. Find the kinematic viscosity of each and decide which fluid is &#039;more viscous&#039;.<\/div><details><summary>Show Solution<\/summary><div class=\"pf-problem-solution\">\n<p><strong>Solution:<\/strong><\/p>\n<p>Step 1: \u03bd = \u03bc \/ \u03c1 for both fluids.<\/p>\n<p>Step 2: \u03bd_water = 1.00 \u00d7 10<sup>\u22123<\/sup> \u00f7 998 = 1.00 \u00d7 10<sup>\u22126<\/sup> m<sup>2<\/sup>\/s<\/p>\n<p>Step 3: \u03bd_air = 1.81 \u00d7 10<sup>\u22125<\/sup> \u00f7 1.20 = 1.51 \u00d7 10<sup>\u22125<\/sup> m<sup>2<\/sup>\/s<\/p>\n<p>Step 4: Dynamic comparison: 1.00 \u00d7 10<sup>\u22123<\/sup> \u00f7 1.81 \u00d7 10<sup>\u22125<\/sup> = 55, so water wins by 55 times.<\/p>\n<p>Step 5: Kinematic comparison: 1.51 \u00d7 10<sup>\u22125<\/sup> \u00f7 1.00 \u00d7 10<sup>\u22126<\/sup> = 15, so air wins by 15 times.<\/p>\n<p><strong>Answer: \u03bd_water \u2248 1.0 \u00d7 10<sup>\u22126<\/sup> m<sup>2<\/sup>\/s and \u03bd_air \u2248 1.5 \u00d7 10<sup>\u22125<\/sup> m<sup>2<\/sup>\/s. Water is 55 times more viscous dynamically; air is 15 times more viscous kinematically. The question is incomplete without stating which viscosity is meant.<\/strong><\/p>\n<\/div><\/details><\/div>\n\n<h2>Frequently Asked Questions<\/h2>\n\n<details class=\"pf-faq-item\"><summary>What is viscosity in simple terms?<\/summary><div class=\"pf-faq-item-answer\">\n\nViscosity is how strongly a fluid resists flowing. It comes from internal friction between fluid layers sliding past one another. Honey has high viscosity because those layers grip each other tightly; water has low viscosity because they slide easily. Formally, viscosity is the shear stress divided by the resulting velocity gradient.\n\n<\/div><\/details>\n\n<details class=\"pf-faq-item\"><summary>What is the SI unit of viscosity?<\/summary><div class=\"pf-faq-item-answer\">\n\nThe SI unit of dynamic viscosity is the pascal second (Pa\u00b7s), which can also be written N\u00b7s\/m<sup>2<\/sup> or kg\/(m\u00b7s). Kinematic viscosity uses m<sup>2<\/sup>\/s. The older CGS units still appear on datasheets: 1 poise = 0.1 Pa\u00b7s, 1 centipoise = 10<sup>\u22123<\/sup> Pa\u00b7s, and 1 centistokes = 10<sup>\u22126<\/sup> m<sup>2<\/sup>\/s.\n\n<\/div><\/details>\n\n<details class=\"pf-faq-item\"><summary>What is the difference between dynamic and kinematic viscosity?<\/summary><div class=\"pf-faq-item-answer\">\n\nDynamic viscosity (\u03bc) measures resistance to shear directly, in Pa\u00b7s. Kinematic viscosity (\u03bd) is that value divided by density, in m<sup>2<\/sup>\/s, so it compares viscous effects with the fluid&#8217;s inertia. The two are linked by \u03bd = \u03bc \/ \u03c1. Datasheets usually quote kinematic viscosity because capillary viscometers measure it directly.\n\n<\/div><\/details>\n\n<details class=\"pf-faq-item\"><summary>Does viscosity increase or decrease with temperature?<\/summary><div class=\"pf-faq-item-answer\">\n\nIt depends on whether the fluid is a liquid or a gas. Liquid viscosity falls sharply as temperature rises, because thermal motion lets molecules escape each other&#8217;s attraction. Gas viscosity rises with temperature, because faster molecules carry momentum between layers more effectively. Water at 100 \u00b0C is about 3.6 times less viscous than at 20 \u00b0C.\n\n<\/div><\/details>\n\n<details class=\"pf-faq-item\"><summary>Is viscosity the same as density?<\/summary><div class=\"pf-faq-item-answer\">\n\nNo, viscosity and density are independent properties. Density is mass per unit volume; viscosity is resistance to shearing. Mercury is 13.6 times denser than water but only about 1.5 times as viscous. Honey is only 1.4 times denser than water yet roughly 10 000 times more viscous. A dense fluid can be very runny.\n\n<\/div><\/details>\n\n<details class=\"pf-faq-item\"><summary>What is a Newtonian fluid?<\/summary><div class=\"pf-faq-item-answer\">\n\nA Newtonian fluid has a viscosity that does not change with shear rate, so shear stress stays proportional to the velocity gradient. Water, air, glycerine and most light oils are Newtonian. Non-Newtonian fluids such as ketchup, blood and cornflour paste change apparent viscosity when sheared, so their viscosity must be quoted with a shear rate.\n\n<\/div><\/details>\n\n<details class=\"pf-faq-item\"><summary>How is viscosity measured?<\/summary><div class=\"pf-faq-item-answer\">\n\nViscosity is measured with a viscometer. Capillary viscometers time how long a fixed volume drains through a narrow tube, giving kinematic viscosity directly. Falling-sphere viscometers use a ball&#8217;s terminal velocity and Stokes&#8217; law. Rotational viscometers spin a spindle in the fluid and measure torque, which suits non-Newtonian fluids because the shear rate can be varied.\n\n<\/div><\/details>\n","protected":false},"excerpt":{"rendered":"<p>Viscosity measures a fluid&#8217;s resistance to flow, set by the shear stress needed to slide one layer of fluid over another. This guide covers the formula, SI and CGS units, six everyday examples and worked problems.<\/p>\n","protected":false},"author":1,"featured_media":786,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[160],"tags":[],"class_list":["post-785","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-fluids"],"_links":{"self":[{"href":"https:\/\/physicsfundamentalsinfo.com\/blog\/wp-json\/wp\/v2\/posts\/785","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/physicsfundamentalsinfo.com\/blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/physicsfundamentalsinfo.com\/blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/physicsfundamentalsinfo.com\/blog\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/physicsfundamentalsinfo.com\/blog\/wp-json\/wp\/v2\/comments?post=785"}],"version-history":[{"count":7,"href":"https:\/\/physicsfundamentalsinfo.com\/blog\/wp-json\/wp\/v2\/posts\/785\/revisions"}],"predecessor-version":[{"id":1460,"href":"https:\/\/physicsfundamentalsinfo.com\/blog\/wp-json\/wp\/v2\/posts\/785\/revisions\/1460"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/physicsfundamentalsinfo.com\/blog\/wp-json\/wp\/v2\/media\/786"}],"wp:attachment":[{"href":"https:\/\/physicsfundamentalsinfo.com\/blog\/wp-json\/wp\/v2\/media?parent=785"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/physicsfundamentalsinfo.com\/blog\/wp-json\/wp\/v2\/categories?post=785"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/physicsfundamentalsinfo.com\/blog\/wp-json\/wp\/v2\/tags?post=785"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}