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Convective derivative

The convective derivative (also commonly known as the advective derivative, substantive derivative, or the material derivative) is a derivative taken with respect to a coordinate system moving with velocity u, and is often used in fluid mechanics and classical mechanics.

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$φ$ is a scalar valued function of stationary spatial coordinates.

v is a vector valued function of stationary spatial coordinates.

The convective derivative is defined as:

$\frac{D\phi}{Dt} = \frac{\partial \phi}{\partial t} + (\mathbf{u}\cdot\nabla)\phi$

$\frac{D\mathbf{v}}{Dt} = \frac{\partial \mathbf{v}}{\partial t} + (\mathbf{u}\cdot\nabla)\mathbf{v}$

where $\nabla$ is the gradient operator del and $\frac{\partial}{\partial t}$ denotes the partial derivative with respect to t. The name is derived from the convection that is represented by the last term.

The convective derivative expresses the Eulerian derivative (written $\partial/\partial t$ ) in Lagrangian coordinates.

Consider water undergoing steady flow through a hosepipe that has a gradually decreasing cross section. Because water is incompressible in practice, conservation of mass requires that the flow is faster at the end of the pipe than at the start. Because the flow is steady, the Eulerian derivative of velocity is everywhere zero, but the convective derivative is nonzero because any individual parcel of fluid accelerates as it moves down the hose.

For tensor fields we usually want to take into account not only translation of the coordinate system due to the fluid movement but also its rotation and stretching. This is achieved by the upper convected time derivative.

There are many other names for this operator, including the Lagrangian derivative, total time derivative, Stokes derivative, particle derivative, and material derivative.

Proof

Proof is via the multivariate chain rule. In tensor notation (with the Einstein summation convention), the derivation may be written:

$\left[\frac{D\mathbf{B}}{Dt}\right]_j = \frac{D}{D t}(\hat{B_j}(t, x_i(t))) = \frac{\partial B_j}{\partial t} + \frac{\partial B_j}{\partial x_i} \frac{\partial x_i}{\partial t} = \frac{\partial B_j}{\partial t} + \frac{\partial x_i}{\partial t} \frac{\partial}{\partial x_i} B_j = \frac{\partial B_j}{\partial t} + \left[(\mathbf{u}\cdot\nabla)\mathbf{B}\right]_j$

References

Structure and Interpretation of Classical Mechanics. http://mitpress.mit.edu/SICM/book-Z-H-13.html#%_sec_Temp_122
Fluid Mechanics by Kundu and Cohen, 3rd Edition
Introduction to Continuum Mechanics by Lai, Rubin, and Krempl, 3rd edition

Category: Fluid dynamics

This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Convective_derivative". A list of authors is available in Wikipedia.

Convective derivative

Additional recommended knowledge

Better weighing performance in 6 easy steps

Recognize and detect the effects of electrostatic charges on your balance

What is the Correct Way to Check Repeatability in Balances?

Proof

See also

References

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