Example 3.10. Show
that, if
is
is the principal square root function given by
,
where the domain is restricted to be
, then
the derivative is given by
,
for every point in the domain
.
Explore Solution 3.10.
Solution. We
write
,
and
.
Thus,
,
and
.
Moreover, the partial derivatives
are
continuous in the domain
(note
the strict inequality in
).
By Theorem 3.5,
, is
differentiable in the domain
. Therefore,
using Equation (3-23) and
(3-24), we
have
And an alternative calculation is
Note that
is
discontinuous on the negative real axis and is undefined at the
origin.
Using the terminology of Section
2.4, the negative real axis
is a branch cut, and the origin is a branch point for this
function.
We are done.
Aside. Both
and
can assist us in finding the partial derivatives.
Aside. The Mathematica solution uses the commands.
Mathematica shows that the polar form of the Cauchy-Riemann
equations (3-22) are
satisfied for all
,
,
and
.
Aside. The Maple commands are similar.
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Maple shows that the polar form of the Cauchy-Riemann
equations (3-22) are
satisfied for all
,
,
and
.
The Cauchy-Riemann
equations hold all points
in
the complex plane,
therefore
is
an analytic function,
for all except at points that lie on the negative
-axis
and
.
Verify that the derivative can be calculated with either of the
formulas:
(3-23)
,
or
(3-24)
.
Aside. The Mathematica solution uses the commands.
Aside. The Maple commands are similar.
>
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>
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>
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>
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Both Mathematica and Maple have shown that
if
,
where the domain is restricted to be
, then
the derivative is given by
,
where
.
We are really done.
Aside. Figure
E.3.10 a, shows the graphs of
and
.
The partial derivatives of
are
and
,
and the partial derivatives of
are
and
.
They satisfy the
Cauchy-Riemann
equations (3-22) because they
are the real and imaginary parts of an analytic
function.
At the point
, we
have
and
, and
these partial derivatives
appear along the edges of the surfaces for
at
the points
and
,
respectively. Similarly, at the
point
, we
have
and
and
these
partial derivatives appear along the edges of the surfaces
for
at
the points
and
, respectively.
.
.
Figure
E.3.10 a
, and
, and
.
.
Figure
E.3.10 b
, and
, and
.
.
Remark.
It is difficult to visualize
and
because
these partial derivatives
are
taken with respect to changes in the polar
angle
, and
so they cannot be visualized as an "ordinary slope."
Figure
E.3.10 c
For
the function
we
see that
, and
.
Figure
E.3.10
We are really really done.
Aside. We can let Mathematica check out the calculations given above.
Remark. In this
book the use of computers is optional.
Hopefully this text will promote their use and understanding.
This solution is complements of the authors.
This material is coordinated with our book Complex Analysis for Mathematics and Engineering.
(c) 2011 John H. Mathews, Russell W. Howell