Some important equations in log-polar coordinates Log-polar coordinates




1 important equations in log-polar coordinates

1.1 laplace s equation
1.2 cauchy–riemann equations
1.3 euler s equation





some important equations in log-polar coordinates
laplace s equation

laplace s equation in 2 dimensions given by











∂

2


u


∂

x

2





+




∂

2


u


∂

y

2





=
0


{\displaystyle {\frac {\partial ^{2}u}{\partial x^{2}}}+{\frac {\partial ^{2}u}{\partial y^{2}}}=0}



in cartesian coordinates. writing same equation in polar coordinates gives more complicated equation







r


∂

∂
r




(
r



∂
u


∂
r



)

+




∂

2


u


∂

θ

2





=
0


{\displaystyle r{\frac {\partial }{\partial r}}\left(r{\frac {\partial u}{\partial r}}\right)+{\frac {\partial ^{2}u}{\partial \theta ^{2}}}=0}



or equivalently









(
r


∂

∂
r



)


2


u
+




∂

2


u


∂

θ

2





=
0


{\displaystyle \left(r{\frac {\partial }{\partial r}}\right)^{2}u+{\frac {\partial ^{2}u}{\partial \theta ^{2}}}=0}



however, relation



r
=

e

ρ




{\displaystyle r=e^{\rho }}

follows



r


∂

∂
r



=


∂

∂
ρ





{\displaystyle r{\frac {\partial }{\partial r}}={\frac {\partial }{\partial \rho }}}

laplace s equation in log-polar coordinates,











∂

2


u


∂

ρ

2





+




∂

2


u


∂

θ

2





=
0


{\displaystyle {\frac {\partial ^{2}u}{\partial \rho ^{2}}}+{\frac {\partial ^{2}u}{\partial \theta ^{2}}}=0}



has same simple expression in cartesian coordinates. true coordinate systems transformation cartesian coordinates given conformal mapping. thus, when considering laplace s equation part of plane rotational symmetry, e.g. circular disk, log-polar coordinates natural choice.


cauchy–riemann equations

a similar situation arises when considering analytical functions. analytical function



f
(
x
,
y
)
=
u
(
x
,
y
)
+
i
v
(
x
,
y
)


{\displaystyle f(x,y)=u(x,y)+iv(x,y)}

written in cartesian coordinates satisfies cauchy–riemann equations:










∂
u


∂
x



=



∂
v


∂
y



,
 
 
 
 
 
 



∂
u


∂
y



=
−



∂
v


∂
x





{\displaystyle {\frac {\partial u}{\partial x}}={\frac {\partial v}{\partial y}},\ \ \ \ \ \ {\frac {\partial u}{\partial y}}=-{\frac {\partial v}{\partial x}}}



if function instead expressed in polar form



f
(
r

e

i
θ


)
=
r

e

i
Φ




{\displaystyle f(re^{i\theta })=re^{i\phi }}

, cauchy–riemann equations take more complicated form







r



∂
log
⁡
r


∂
r



=



∂
Φ


∂
θ



,
 
 
 
 
 
 



∂
log
⁡
r


∂
θ



=
−
r



∂
Φ


∂
r



,


{\displaystyle r{\frac {\partial \log r}{\partial r}}={\frac {\partial \phi }{\partial \theta }},\ \ \ \ \ \ {\frac {\partial \log r}{\partial \theta }}=-r{\frac {\partial \phi }{\partial r}},}



just in case laplace s equation, simple form of cartesian coordinates recovered changing polar log-polar coordinates (let



p
=
log
⁡
r


{\displaystyle p=\log r}

):










∂
p


∂
ρ



=



∂
Φ


∂
θ



,
 
 
 
 
 
 



∂
p


∂
θ



=
−



∂
Φ


∂
ρ





{\displaystyle {\frac {\partial p}{\partial \rho }}={\frac {\partial \phi }{\partial \theta }},\ \ \ \ \ \ {\frac {\partial p}{\partial \theta }}=-{\frac {\partial \phi }{\partial \rho }}}



the cauchy–riemann equations can written in 1 single equation as








(


∂

∂
x



+
i


∂

∂
y



)

f
(
x
+
i
y
)
=
0


{\displaystyle \left({\frac {\partial }{\partial x}}+i{\frac {\partial }{\partial y}}\right)f(x+iy)=0}



by expressing





∂

∂
x





{\displaystyle {\frac {\partial }{\partial x}}}

,





∂

∂
y





{\displaystyle {\frac {\partial }{\partial y}}}

in terms of





∂

∂
ρ





{\displaystyle {\frac {\partial }{\partial \rho }}}

,





∂

∂
θ





{\displaystyle {\frac {\partial }{\partial \theta }}}

equation can written in equivalent form








(


∂

∂
ρ



+
i


∂

∂
θ



)

f
(

e

ρ
+
i
θ


)
=
0


{\displaystyle \left({\frac {\partial }{\partial \rho }}+i{\frac {\partial }{\partial \theta }}\right)f(e^{\rho +i\theta })=0}



euler s equation

when 1 wants solve dirichlet problem in domain rotational symmetry, usual thing use method of separation of variables partial differential equations laplace s equation in polar form. means write



u
(
r
,
θ
)
=
r
(
r
)
Θ
(
θ
)


{\displaystyle u(r,\theta )=r(r)\theta (\theta )}

. laplace s equation separated 2 ordinary differential equations









{




Θ
″

(
θ
)
+

ν

2


Θ
(
θ
)
=
0





r

2



r
″

(
r
)
+
r

r
′

(
r
)
−

ν

2


r
(
r
)
=
0








{\displaystyle {\begin{cases}\theta (\theta )+\nu ^{2}\theta (\theta )=0\\r^{2}r (r)+rr (r)-\nu ^{2}r(r)=0\end{cases}}}



where



ν


{\displaystyle \nu }

constant. first of these has constant coefficients , solved. second special case of euler s equation








r

2



r
″

(
r
)
+
c
r

r
′

(
r
)
+
d
r
(
r
)
=
0


{\displaystyle r^{2}r (r)+crr (r)+dr(r)=0}



where



c
,
d


{\displaystyle c,d}

constants. equation solved ansatz



r
(
r
)
=

r

λ




{\displaystyle r(r)=r^{\lambda }}

, through use of log-polar radius, can changed equation constant coefficients:








p
″

(
ρ
)
+
(
c
−
1
)

p
′

(
ρ
)
+
d
p
(
ρ
)
=
0


{\displaystyle p (\rho )+(c-1)p (\rho )+dp(\rho )=0}



when considering laplace s equation,



c
=
1


{\displaystyle c=1}

,



d
=
−

ν

2




{\displaystyle d=-\nu ^{2}}

equation



r


{\displaystyle r}

takes simple form








p
″

(
ρ
)
−

ν

2


p
(
ρ
)
=
0


{\displaystyle p (\rho )-\nu ^{2}p(\rho )=0}



when solving dirichlet problem in cartesian coordinates, these equations



x


{\displaystyle x}

,



y


{\displaystyle y}

. thus, once again natural choice domain rotational symmetry not polar, rather log-polar, coordinates.







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