In fluid mechanics and hydraulics, **open-channel flow** is a type of liquid flow within a conduit with a free surface, known as a channel.^{[1]}^{[2]} The other type of flow within a conduit is pipe flow. These two types of flow are similar in many ways but differ in one important respect: open-channel flow has a free surface, whereas pipe flow does not, resulting in flow dominated by gravity but not hydraulic pressure.

Open-channel flow can be classified and described in various ways based on the change in flow depth with respect to time and space.^{[3]} The fundamental types of flow dealt with in open-channel hydraulics are:

**Time as the criterion***Steady flow*- The depth of flow does not change over time, or if it can be assumed to be constant during the time interval under consideration.

*Unsteady flow*- The depth of flow does change with time.

**Space as the criterion***Uniform flow*- The depth of flow is the same at every section of the channel. Uniform flow can be steady or unsteady, depending on whether or not the depth changes with time, (although unsteady uniform flow is rare).

*Varied flow*- The depth of flow changes along the length of the channel. Varied flow technically may be either steady or unsteady. Varied flow can be further classified as either rapidly or gradually-varied:
*Rapidly-varied flow*- The depth changes abruptly over a comparatively short distance. Rapidly varied flow is known as a local phenomenon. Examples are the hydraulic jump and the hydraulic drop.

*Gradually-varied flow*- The depth changes over a long distance.

- The depth of flow changes along the length of the channel. Varied flow technically may be either steady or unsteady. Varied flow can be further classified as either rapidly or gradually-varied:
*Continuous flow*- The discharge is constant throughout the reach of the channel under consideration. This is often the case with a steady flow. This flow is considered continuous and therefore can be described using the continuity equation for continuous steady flow.

*Spatially-varied flow*- The discharge of a steady flow is non-uniform along a channel. This happens when water enters and/or leaves the channel along the course of flow. An example of flow entering a channel would be a road side gutter. An example of flow leaving a channel would be an irrigation channel. This flow can be described using the continuity equation for continuous unsteady flow requires the consideration of the time effect and includes a time element as a variable.

The behavior of open-channel flow is governed by the effects of viscosity and gravity relative to the inertial forces of the flow. Surface tension has a minor contribution, but does not play a significant enough role in most circumstances to be a governing factor. Due to the presence of a free surface, gravity is generally the most significant driver of open-channel flow; therefore, the ratio of inertial to gravity forces is the most important dimensionless parameter.^{[4]} The parameter is known as the Froude number, and is defined as:where is the mean velocity, is the characteristic length scale for a channel's depth, and is the gravitational acceleration. Depending on the effect of viscosity relative to inertia, as represented by the Reynolds number, the flow can be either laminar, turbulent, or transitional. However, it is generally acceptable to assume that the Reynolds number is sufficiently large so that viscous forces may be neglected.^{[4]}

It is possible to formulate equations describing three conservation laws for quantities that are useful in open-channel flow: mass, momentum, and energy. The governing equations result from considering the dynamics of the flow velocity vector field with components . In Cartesian coordinates, these components correspond to the flow velocity in the x, y, and z axes respectively.

To simplify the final form of the equations, it is acceptable to make several assumptions:

- The flow is incompressible (this is not a good assumption for rapidly-varied flow)
- The Reynolds number is sufficiently large such that viscous diffusion can be neglected
- The flow is one-dimensional across the x-axis

The general continuity equation, describing the conservation of mass, takes the form:where is the fluid density and is the divergence operator. Under the assumption of incompressible flow, with a constant control volume , this equation has the simple expression . However, it is possible that the cross-sectional area can change with both time and space in the channel. If we start from the integral form of the continuity equation:it is possible to decompose the volume integral into a cross-section and length, which leads to the form:Under the assumption of incompressible, 1D flow, this equation becomes:By noting that and defining the volumetric flow rate , the equation is reduced to:Finally, this leads to the continuity equation for incompressible, 1D open-channel flow:

The momentum equation for open-channel flow may be found by starting from the incompressible Navier-Stokes equations :where is the pressure, is the kinematic viscosity, is the Laplace operator, and is the gravitational potential. By invoking the high Reynolds number and 1D flow assumptions, we have the equations:The second equation implies a hydrostatic pressure , where the channel depth is the difference between the free surface elevation and the channel bottom . Substitution into the first equation gives:where the channel bed slope . To account for shear stress along the channel banks, we may define the force term to be:where is the shear stress and is the hydraulic radius. Defining the friction slope , a way of quantifying friction losses, leads to the final form of the momentum equation:

To derive an energy equation, note that the advective acceleration term may be decomposed as:where is the vorticity of the flow and is the Euclidean norm. This leads to a form of the momentum equation, ignoring the external forces term, given by:Taking the dot product of with this equation leads to:This equation was arrived at using the scalar triple product . Define to be the energy density:Noting that is time-independent, we arrive at the equation:Assuming that the energy density is time-independent and the flow is one-dimensional leads to the simplification:with being a constant; this is equivalent to Bernoulli's principle. Of particular interest in open-channel flow is the specific energy , which is used to compute the hydraulic head that is defined as:

with being the specific weight. However, realistic systems require the addition of a head loss term to account for energy dissipation due to friction and turbulence that was ignored by discounting the external forces term in the momentum equation.

- HEC-RAS
- Streamflow
**Fields of study****Types of fluid flow****Fluid properties****Other related articles**

**^**Chow, Ven Te (2008).*Open-Channel Hydraulics*(PDF). Caldwell, NJ: The Blackburn Press. ISBN 978-1932846188.**^**Battjes, Jurjen A.; Labeur, Robert Jan (2017).*Unsteady Flow in Open Channels*. Cambridge, UK: Cambridge University Press. ISBN 9781316576878.**^**Jobson, Harvey E.; Froehlich, David C. (1988).*Basic Hydraulic Principles of Open-Channel Flow*(PDF). Reston, VA: U.S. Geological Survey.- ^
^{a}^{b}Sturm, Terry W. (2001).*Open Channel Hydraulics*(PDF). New York, NY: McGraw-Hill. p. 2. ISBN 9780073397870.

- Nezu, Iehisa; Nakagawa, Hiroji (1993).
*Turbulence in Open-Channel Flows*. IAHR Monograph. Rotterdam, NL: A.A. Balkema. ISBN 9789054101185. - Syzmkiewicz, Romuald (2010).
*Numerical Modeling in Open Channel Hydraulics*. Water Science and Technology Library. New York, NY: Springer. ISBN 9789048136735.

- Caltech lecture notes:
- Open-Channel Flow
- Open Channel Flow Concepts
- What is a Hydraulic Jump?
- Open Channel Flow Example
- Simulation of Turbulent Flows (p. 26-38)

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