Abstract
Solutions of Laplace’s equation, ∂
2
V/∂
x
2
+ ∂
2
V/∂
y
2
+ ∂
2
V/∂
z
2
= 0 . . . . . (1. 11) are required in many branches of Applied Mathematics, such as hydrodynamics, electro-and magneto-statics, steady flow of heat or electricity, etc. The two-dimensional form of the equation, ∂
2
V/∂
x
2
+ ∂
2
V/∂
y
2
= 0, . . . . (1. 12) has a general solution V =
f
(
x + ɩy
) + F (
x – ɩy
), . . . (1. 21)
f
and F being arbitrary functions of their complex arguments. In the applications, one function alone is usually sufficient, and it is customary to write
w
=
ϕ
+ ɩψ =
f
(
z
). . . . . (1. 22) with
z
=
x
+ ɩ
y
, when
ϕ
and ψ usually have each some physical significance. Moreover, in most cases, the boundary conditions which have to be satisfied either are, or can be reduced to, the prescription of the boundary values of
ϕ
or ψ, of their derivatives.
Subject
General Earth and Planetary Sciences,General Environmental Science
Cited by
20 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献