I have read the most basic and important parts of vector calculus are gradient, divergence and curl. These three things are too important to analyse a vector field and I have gone through the physical meaning of gradient, divergence, and curl.

Gradient indicates the direction of maximum rate of change of a function, and it is defined as $\nabla u(\mathbf{x})\equiv\mathrm{grad} \, u(\mathbf{x})$ where $u(\mathbf{x})$ is a scalar function of the position vector $\mathbf{x}$.

Whereas divergence represents the volume density of the outward flux from an infinitesimal volume around a point and is defined as $\boldsymbol{\nabla} \boldsymbol{\cdot} \mathbf{A}(\mathbf{x})\equiv\mathrm{div} \, \mathbf{A}(\mathbf{x})$

And the curl signifies the infinitesimal rotation around a point and is defined as $\boldsymbol{\nabla} \boldsymbol{\times} \mathbf{A}(\mathbf{x})\equiv \mathrm{curl} \, \mathbf{A}(\mathbf{x})$

And now I have study and also mathematically formulate that $\boldsymbol{\nabla} \boldsymbol{\cdot} \left[\boldsymbol{\nabla} \boldsymbol{\times} \mathbf{A}(\mathbf{x})\right]=\mathrm{div} \left[\mathrm{curl} \mathbf{A}(\mathbf{x})\right]=0$.

And $\boldsymbol{\nabla} \boldsymbol{\times}\left[\nabla u(\mathbf{x})\right] =\mathrm{curl}\left[ \mathrm{grad} \, u(\mathbf{x})\right]= \boldsymbol{0}$ where u is a scalar function

Now my question is how can I interpret those two expressions? I mean, I want the physical significance of these two expressions in the sense of definition of gradient, divergence, curl, and also using graphical representation.

  • $\begingroup$ The first equation means that the curl of a vector function is either a uniform field or encloses on itself. The second means that a gradient do not enclose on itself. $\endgroup$
    – Tofi
    Commented Jun 24, 2016 at 19:41
  • $\begingroup$ I did not understand the last answer $\endgroup$
    – user101134
    Commented Jun 25, 2016 at 4:46
  • $\begingroup$ For curl see physics.stackexchange.com/q/211773 $\endgroup$
    – ProfRob
    Commented Jun 26, 2016 at 21:00
  • $\begingroup$ And together with divergence at physics.stackexchange.com/q/141582 makes this a duplicate. $\endgroup$
    – ProfRob
    Commented Jun 26, 2016 at 21:03
  • $\begingroup$ Not duplicates. OP wants an explanation of the identities in a physical/ graphical way. The links deal with physical meanings of div and curl, but no the identities. @NowIGetToLearnWhatAHeadIs has given an elegant answer explaining them. $\endgroup$
    – biryani
    Commented Jun 27, 2016 at 8:48

2 Answers 2


Since your question is how to gain an intuitive understanding of what the two equations $\nabla \cdot \nabla \mathbf{F} = 0$ and $\nabla \times \nabla f=\mathbf{0}$ mean, I will discuss the equations in a simple setting. The simpler, more intuitive setting I am thinking of is a discrete setting: the honeycomb lattice, shown below.

$\hskip 2 in$https://utmonehannay.files.wordpress.com/2014/07/honeycomb-lattice.png

Let me explain how vector calculus works on this lattice. A scalar function takes on values at the discrete vertices of the lattice.

A vector field takes on values on the edges of the lattice. This makes sense because vectors should represent movement from one point to another.

The gradient of a function $f$ has, on each edge, a magnitude equal to the difference between $f$ on the two ends of the edge, and the direction of the gradient, of course, is from the lower value to the higher value.

Now when you take the curl you get a function defined on each face (that is, hexagon) of the lattice. This makes sense because the curl is supposed to tell you how the vector field is going around in a "circle". In this case, the "circle" is really a hexagon. Let's see an example of taking the curl of a vector field.

enter image description here

In the above figure, the values of the vector field $\mathbf{F}$ are shown in red. Here I have taken the counter-clockwise direction to be positive, so a negative value means the vector actually points in the clockwise direction. The curl can be found by adding the values as you move counter-clockwise along the hexagon. So the value of the curl at the hexagon shown in the figure is $4$.

Now lets see why the curl of the gradient has to be zero.

enter image description here

Above, I have shown the values of the function in black at each vertex. The gradient is shown in red at each edge as in the previous picture. We find in this case that the curl is zero. The reason is simple. When you are taking the curl in this case, you are adding up the differences in the function values as you move around the hexagon. But since you end up where you started, the sum of the changes must be zero.

Now let's think about why the divergence of the curl must be zero. To take the divergence, we must move to three dimensions. So let's think about the soccer ball shape shown below.

enter image description here

As before, functions are defined on vertices, vectors are defined on edges, the curl is defined on faces. The new thing is that the divergence is defined on the volume enclosed by the soccer ball.

To see why the divergence of the curl is zero, lets just look at what is going on in the two hexagons closest to us.

enter image description here

In this case, we have a vector field $\mathbf{F}$, which can take on arbitrary values on the edges. I have picked random values for the sake of illustration. Again, the curl defined on each hexagon is the sum of $\mathbf{F}$ as you go around the hexagon counterclockwise. The counter-clockwise direction is important here. Notice the edge where $\mathbf{F}=4$ (the one shown in a box) is included in the calculation of the curl at both hexagons. In the lower hexagon, it has a positive sign, since this $\mathbf{F}$ does point in the counterclockwise direction as you go around the lower hexagon. However, it has a negative sign in the upper hexagon, since there this $\mathbf{F}$ points in the clockwise direction. Now since the divergence is the sum the values over all the faces, and the edge's contribution to the lower face is the opposite of the contribution to the upper face, we see that this edge has zero contribution to the divergence. But every single edge on the soccer ball lies on two faces, so each edge gives zero contribution to the divergence, and thus the divergence must be zero.

Now I should probably say a few words about how this relates to the situation of normal euclidean space. The situation is really very analogous. You can measure the curl of a vector field by taking its line integral around small circles. However, in the case of a gradient, the line integral tells you the total change in the function as you go around the circle. Since you end where you begin, the total change must be zero. Since these integrals must all be zero for the gradient, the curl of a gradient must be zero.

The divergence can be measured by integrating the field that goes through a small sphere. If you have a non-zero vector on the surface, then it will tend to create an outward pointing curl on its left, but an inward pointing curl on its right. These two contributions to the divergence cancel out, so you wind up with zero divergence.


Let us begin with $$\mathrm{div} \left[\mathrm{curl} \mathbf{A}(\mathbf{x})\right]=0$$

Consider the electrostatic field, it has sources to emerge from (positive charges) and sinks to go into (negative charges). Such a field has a non-zero divergence.

When we say that the divergence of $ \mathrm{curl} \mathbf{A}(\mathbf{x})$ is equal to zero, this means that the curl doesn't have any sources or sinks, its total flux out of a closed surface is always zero and it is usually either a uniform field or forms closed vortices (as the magnetic field). In general, any vector field with a zero divergence has to be a curl of some other field.

The second equation:$$\mathrm{curl}\left[ \mathrm{grad} \, u(\mathbf{x})\right]= \boldsymbol{0}$$ doesn't have much to deduce from. A field with zero curl is called irrotational. In a simply connected region, such a field is conservative (path independence and no vortices), but we already know this for a gradient.


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