Maxima, minima and saddle points for functions of two variables 359
36.3 Procedure to determine
maxima, minima and saddle
points for functions of two
variables
Givenz=f(x,y):
(i) determine
∂z
∂x
and
∂z
∂y
(ii) for stationary points,
∂z
∂x
=0and
∂z
∂y
=0,
(iii) solve the simultaneous equations
∂z
∂x
=0and
∂z
∂y
=0forxandy, which gives the co-ordinates
of the stationary points,
(iv) determine
∂^2 z
∂x^2
,
∂^2 z
∂y^2
and
∂^2 z
∂x∂y
(v) for each of the co-ordinates of the stationary
points,substitutevaluesofxandyinto
∂^2 z
∂x^2
,
∂^2 z
∂y^2
and
∂^2 z
∂x∂y
and evaluate each,
(vi) evaluate
(
∂^2 z
∂x∂y
) 2
for each stationary point,
(vii) substitute the values of
∂^2 z
∂x^2
,
∂^2 z
∂y^2
and
∂^2 z
∂x∂y
into the equation
=
(
∂^2 z
∂x∂y
) 2
−
(
∂^2 z
∂x^2
)(
∂^2 z
∂y^2
)
and evaluate,
(viii) (a) if> 0 then the stationary point is a
saddle point.
(b) if< 0 and
∂^2 z
∂x^2
< 0 , then the stationary
point is amaximum point,
and
(c) if< 0 and
∂^2 z
∂x^2
> 0 , then the stationary
point is aminimum point.
36.4 Worked problems on maxima,
minima and saddle points for
functions of two variables
Problem 1. Show that the function
z=(x− 1 )^2 +(y− 2 )^2 has one stationary point only
and determine its nature. Sketch the surface
represented byzand produce a contour map in the
x-yplane.
Following the above procedure:
(i)
∂z
∂x
= 2 (x− 1 )and
∂z
∂y
= 2 (y− 2 )
(ii) 2(x− 1 )= 0 ( 1 )
2 (y− 2 )= 0 ( 2 )
(iii) From equations (1) and (2),x=1andy=2, thus
the only stationary point exists at (1, 2).
(iv) Since
∂z
∂x
= 2 (x− 1 )= 2 x− 2 ,
∂^2 z
∂x^2
= 2
and since
∂z
∂y
= 2 (y− 2 )= 2 y− 4 ,
∂^2 z
∂y^2
= 2
and
∂^2 z
∂x∂y
=
∂
∂x
(
∂z
∂y
)
=
∂
∂x
( 2 y− 4 )= 0
(v)
∂^2 z
∂x^2
=
∂^2 z
∂y^2
=2and
∂^2 z
∂x∂y
= 0
(vi)
(
∂^2 z
∂x∂y
) 2
= 0
(vii) =( 0 )^2 −( 2 )( 2 )=− 4
(viii) Since<0and
∂^2 z
∂x^2
>0,the stationary point
(1, 2) is a minimum.
The surfacez=(x− 1 )^2 +(y− 2 )^2 isshowninthree
dimensions in Fig. 36.7. Looking down towards the
x-yplane from above, it is possible to produce acon-
tour map. A contour is a line on a map which gives
places having the same vertical height above a datum
line (usuallythe mean sea-level on a geographical map).