The derivative, \( D/Dt \), defined by the previous slide, is commonly called the substantial derivative to remind us that it is computed for a particle of "substance." It is often also called the material derivative or particle derivative.
The physical significance of the terms is: \( \underbrace{\frac{D \vec{V}}{D t} = \vec{a}_p}_{\text{total acceleration of a particle}} = \underbrace{ v_x \frac{\partial \vec{V}}{\partial x} + v_y \frac{\partial \vec{V}}{\partial y} + v_z \frac{\partial \vec{V}}{\partial z} }_{\text{convective acceleration}} + \underbrace{ \frac{\partial \vec{V}}{\partial t} }_{\text{local acceleration}} \)
We recognize that a fluid particle moving in a flow field may undergo acceleration for either of two reasons:
The convective acceleration can be rewritten using the gradient operator \( \nabla \): \( v_x \frac{\partial \vec{V}}{\partial x} + v_y \frac{\partial \vec{V}}{\partial y} + v_z \frac{\partial \vec{V}}{\partial z} = (\vec{V} \cdot \nabla) \vec{V} \)
where \( \cdot \) is the dot product. Thus, the material derivative may be rewritten as: \( \frac{D \vec{V}}{D t} = \vec{a}_p = (\vec{V} \cdot \nabla) \vec{V} + \frac{\partial \vec{V}}{\partial t} \)
For a steady flow in three dimensions, the equation simplifies to: \( \frac{D \vec{V}}{D t} = \vec{a}_p = (\vec{V} \cdot \nabla) \vec{V} \)
which is not necessarily zero even though the flow is steady. Thus, a fluid particle may undergo a convective acceleration due to its motion, even in a steady velocity field.