Physical Chemistry Third Edition

(C. Jardin) #1

1244 B Some Useful Mathematics


or aCartesian tensor. Each of its components is multiplied by a product of two unit
vectors.
Thedivergenceof a vector functionFis denoted by∇·Fand is defined by

∇·F

(

∂Fx
∂x

)

+

(

∂Fy
∂y

)

+

(

∂Fz
∂z

)

(B-44)

The divergence is a scalar quantity. If the vector function represents the flow velocity of
a fluid, the divergence is a measure of the spreading out of the streaming curves along
which small elements of the fluid flow. A positive value of the divergence corresponds
to a decrease in density along a curve following the flow. See the discussion of the
equation of continuity in Section 11.2.
The divergence of the gradient of a scalar function is called theLaplacian. The
Laplacian of a scalar functionfis given in Cartesian coordinates by

∇^2 f

∂^2 f
∂x^2

+

∂^2 f
∂y^2

+

∂^2 f
∂z^2

(B-45)

The Laplacian is sometimes called “del squared.”
The vector derivative operators can be expressed in other coordinate systems. In
spherical polar coordinates, the gradient of the scalar functionfis

∇fer

∂f
∂r

+eθ

1

r

∂f
∂θ

+eφ

1

rsin(θ)

∂f
∂φ

(B-46)

whereeris the unit vector in therdirection (the direction of motion ifris increased
by a small amount, keepingθandφfixed),eθis the unit vector in theθdirection, and
eφis the unit vector in theφdirection. In spherical polar coordinates, the Laplacian is

∇^2 f

1

r^2

[


∂r

[

r^2

∂f
∂r

]

+

1

sin(θ)


∂θ

[

sin(θ)

∂f
∂θ

]

+

1

sin^2 (θ)

∂^2 f
∂φ^2

]

(B-47)

In cylindrical polar coordinates the three coordinates arez(same as in Cartesian coor-
dinates),φ(same as in spherical polar coordinates), andρ, equal to


x^2 +y^2. The
gradient of a scalar functionfis given by

∇feρ

∂f
∂ρ

+eφ

1

ρ

∂f
∂φ

+k

∂f
∂z

(B-48)

whereeρis the unit vector in theρdirection,eφis the unit vector in theφdirection,
andkis the unit vector in thezdirection.
For example, the liquid in a pipe with radiusRhas a velocity that depends onρ, the
distance from the center of the pipe such that

ukuz(ρ)kA(ρ^2 −R^2 ) (B-49)

whereAis a constant. All of the nine components of the gradient of this velocity will
vanish except for∂uz/∂ρ:

∇uzeρ

∂uz
∂ρ

eρ 2 Aρ (B-50)

The gradient of the flow velocity points at right angles to the velocity.
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