In
fluid dynamics
In physics, physical chemistry and engineering, fluid dynamics is a subdiscipline of fluid mechanics that describes the flow of fluids – liquids and gases. It has several subdisciplines, including (the study of air and other gases in motion ...
, Couette flow is the flow of a
viscous
Viscosity is a measure of a fluid's rate-dependent resistance to a change in shape or to movement of its neighboring portions relative to one another. For liquids, it corresponds to the informal concept of ''thickness''; for example, syrup h ...
fluid
In physics, a fluid is a liquid, gas, or other material that may continuously motion, move and Deformation (physics), deform (''flow'') under an applied shear stress, or external force. They have zero shear modulus, or, in simpler terms, are M ...
in the space between two surfaces, one of which is moving
tangent
In geometry, the tangent line (or simply tangent) to a plane curve at a given point is, intuitively, the straight line that "just touches" the curve at that point. Leibniz defined it as the line through a pair of infinitely close points o ...
ially relative to the other. The relative motion of the surfaces imposes a
shear stress
Shear stress (often denoted by , Greek alphabet, Greek: tau) is the component of stress (physics), stress coplanar with a material cross section. It arises from the shear force, the component of force vector parallel to the material cross secti ...
on the fluid and induces flow. Depending on the definition of the term, there may also be an applied
pressure gradient
In hydrodynamics and hydrostatics, the pressure gradient (typically of air but more generally of any fluid) is a physical quantity that describes in which direction and at what rate the pressure increases the most rapidly around a particular locat ...
in the flow direction.
The Couette configuration models certain practical problems, like the
Earth's mantle
Earth's mantle is a layer of silicate mineral, silicate rock between the Earth's crust, crust and the Earth's outer core, outer core. It has a mass of and makes up 67% of the mass of Earth. It has a thickness of making up about 46% of Earth's ...
and
atmosphere
An atmosphere () is a layer of gases that envelop an astronomical object, held in place by the gravity of the object. A planet retains an atmosphere when the gravity is great and the temperature of the atmosphere is low. A stellar atmosph ...
, and flow in lightly loaded
journal bearings
Plain bearing on a 1906 S-Motor locomotive showing the axle, bearing, oil supply and oiling pad
A sliding table with four cylindrical bearings
A wheelset from a Great Western Railway (GWR) wagon showing a plain, or journal, bearing end
A pl ...
. It is also employed in
viscometry and to demonstrate approximations of
reversibility.
It is named after
Maurice Couette
Maurice Marie Alfred Couette (9 January 1858, Tours – 18 August 1943, Angers) was a French physicist known for his studies of Viscosity#Fluidity, fluidity.
Couette is best known for his contributions to rheology and the theory of fluid flow. He ...
, a Professor of Physics at the French
University of Angers
The University of Angers () is a public university in western France, with campuses in Angers, Cholet, and Saumur.
It is part of the Angers-Le Mans University Community.
History
The University of Angers was initially established during the 11 ...
in the late 19th century.
Isaac Newton
Sir Isaac Newton () was an English polymath active as a mathematician, physicist, astronomer, alchemist, theologian, and author. Newton was a key figure in the Scientific Revolution and the Age of Enlightenment, Enlightenment that followed ...
first defined the problem of Couette flow in Proposition 51 of his
''Philosophiæ Naturalis Principia Mathematica'', and expanded upon the ideas in Corollary 2.
Planar Couette flow

Couette flow is frequently used in undergraduate physics and engineering courses to illustrate
shear-driven fluid motion. A simple configuration corresponds to two infinite, parallel plates separated by a distance
; one plate translates with a constant relative velocity
in its own plane. Neglecting pressure gradients, the
Navier–Stokes equations
The Navier–Stokes equations ( ) are partial differential equations which describe the motion of viscous fluid substances. They were named after French engineer and physicist Claude-Louis Navier and the Irish physicist and mathematician Georg ...
simplify to
:
where
is the spatial coordinate normal to the plates and
is the velocity field. This equation reflects the assumption that the flow is ''unidirectional'' — that is, only one of the three velocity components
is non-trivial. If the lower plate corresponds to
, the boundary conditions are
and
. The exact solution
:
can be found by integrating twice and solving for the constants using the boundary conditions.
A notable aspect of the flow is that
shear stress
Shear stress (often denoted by , Greek alphabet, Greek: tau) is the component of stress (physics), stress coplanar with a material cross section. It arises from the shear force, the component of force vector parallel to the material cross secti ...
is constant throughout the domain. In particular, the first derivative of the velocity,
, is constant. According to
Newton's Law of Viscosity (
Newtonian fluid
A Newtonian fluid is a fluid in which the viscous stresses arising from its flow are at every point linearly correlated to the local strain rate — the rate of change of its deformation over time. Stresses are proportional to the rate of cha ...
), the shear stress is the product of this expression and the (constant) fluid
viscosity
Viscosity is a measure of a fluid's rate-dependent drag (physics), resistance to a change in shape or to movement of its neighboring portions relative to one another. For liquids, it corresponds to the informal concept of ''thickness''; for e ...
.
Startup
In reality, the Couette solution is not reached instantaneously. The "startup problem" describing the approach to steady state is given by
:
subject to the initial condition
: