The gradient is a differential operator on a scalar field, [tex]\phi[/tex]. The gradient, grad[tex]\phi[/tex], is a "vector field" defined by the requirement that
grad[tex]\,\phi\,\cdot[/tex] d
s = d[tex]\,\phi[/tex]
where d[tex]\,\phi[/tex] is the differential change in the scalar field, [tex]\phi[/tex], corresponding to the arbitrary space displacement, d
s, and from this,
d[tex]\,\phi[/tex] = | grad [tex]\,\phi\,[/tex]| |d
s| cos [tex]\theta[/tex], where is the angle between the displacement vector and the line formed between two points of interest in the scalar field.
Since cos [tex]\theta[/tex] has a maximum value of 1, that is when [tex]\theta[/tex]=0, it is clear that the rate of change is greatest if the differential displacement is in the direction of grad[tex]\,\phi\,[/tex], or stated another way,
"The direction of the vector grad[tex]\,\phi[/tex] is the direction of maximum rate of change (spatially-speaking) of [tex]\,\phi[/tex] from the point of consideration, i.e. direction in which [tex]\frac{d\phi}{ds}[/tex] is greatest."
The gradient of [tex]\phi[/tex] is considered 'directional derivative' in the direction of the maximum rate of change of the scalar field [tex]\phi[/tex].
Think of contours of elevation on a mountain slope. Points of the same (constant) elevation have the same gravitational potential, [tex]\phi[/tex]. Displacement along (parallel) to the contours produce no change in [tex]\phi[/tex] (i.e. d[tex]\phi[/tex] = 0). Displacements perpendicular (normal) to the equipotential are oriented in the direction of most rapid change of altitude, and d[tex]\phi[/tex] has the maximum value.
Isotherms are equipotentials with respect to heat flow.
See related discussion on the directional derivative (forthcoming).
Examples of scalar fields:
- density (mass distribution) in an object or matter (solid, liquid, gas, . . .)
- electrostatic (charge distribution)
Examples of vector fields:
- velocity at each point in a moving fluid (e.g. hurricane or tornado, river, . . .)
I am doing something similar for
div and
curl