The Gradient in Cylindrical Polar Coordinates

With respect to orthonormal Cartesian and cylindrical basis vectors  
\[( \mathbf{i} , \mathbf{j} , \mathbf{k} )\]
  and  
\[( \mathbf{e_r} , \mathbf{e_{\theta}} , \mathbf{e_z} )\]
  we can express the vector  
\[\mathbf{a}\]
  as
\[\mathbf{a} =a_1 \mathbf{i} +a_2 \mathbf{j} +a_3 \mathbf{k} = b_1 \mathbf{e_r} , b_2 \mathbf{e_{\theta}} + b_3 \mathbf{e_z} \]

We can take the dot product of  
\[\mathbf{a}\]
  with each of the cylindrical basis vectors gives
\[\mathbf{a} \cdot \mathbf{e_r} = b_1\]

\[\mathbf{a} \cdot \mathbf{e_{\theta}} = b_2\]

\[\mathbf{a} \cdot \mathbf{e_z} = b_3\]

Hence
\[\mathbf{a} = (\mathbf{a} \cdot \mathbf{e_r}) \mathbf{e_r} + (\mathbf{a} \cdot \mathbf{e_{\theta}}) \mathbf{e_{\theta}} + (\mathbf{a} \cdot \mathbf{e_z}) \mathbf{e_z}\]

Let  
\[\mathbf{a} = \mathbf{\nabla} f\]
  then
\[\mathbf{{\nabla}} = (\mathbf{{\nabla}} \cdot \mathbf{e_r}) \mathbf{e_r} + (\mathbf{{\nabla}} \cdot \mathbf{e_{\theta}}) \mathbf{e_{\theta}} + (\mathbf{{\nabla}} \cdot \mathbf{e_z}) \mathbf{e_z}\]

Now  
\[(ds)^2 = \sqrt{(dr)^2 + r^2 ( d \theta )^2 + (dz)^2} \rightarrow \frac{\partial r}{\partial s}= \frac{\partial z}{\partial s}=1, \: \frac{\partial s}{\partial \theta } = r \rightarrow \frac{\partial \theta}{\partial s}= \frac{1}{r} \]

\[\mathbf{e_r} \cdot (\mathbf{\nabla} f) = \frac{\partial f}{\partial s} |_{\theta , z = constant} = \frac{\partial r}{\partial s} \frac{\partial f}{\partial r} = \frac{\partial f}{\partial r}\]

\[\mathbf{e_\theta} \cdot (\mathbf{\nabla} f) = \frac{\partial f}{\partial s} |_{r , z = constant} = \frac{\partial \theta}{\partial s} \frac{\partial f}{\partial \theta} =\frac{1}{r} \frac{\partial f}{\partial \theta}\]

\[\mathbf{e_z} \cdot (\mathbf{\nabla} f) = \frac{\partial f}{\partial z} |_{r, \theta = constant} = \frac{\partial z}{\partial s} \frac{\partial f}{\partial z} = \frac{\partial f}{\partial z}\]

Hence  
\[\mathbf{\nabla} f = \frac{\partial f}{\partial r} \mathbf{e_r} _+ \frac{1}{r} \frac{\partial f}{\partial \theta} \mathbf{e_\theta}+ \frac{\partial f}{\partial z} \mathbf{e_z} \]
 

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