How do we go from BVP to IVP in determining the Green's function?

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Hi PF!

I'm reading a text where the authors construct a Green's function for a given BVP by variation of parameters. The authors construct the Green's function by finding first the fundamental solutions (let's call these ##v_1## and ##v_2##) to the homogenous BVP. However, the authors determine ##v_1## and ##v_2## from initial conditions (not given anywhere in the physical setup) rather than boundary conditions.

Specifically, the boundary conditions initially presented are ##u'(s_0)+\mu u(s_0) = -u'(-s_0)+\mu u(-s_0) = 0:s\in[-s_0,s_0]##, where ##\mu## is a constant. The authors state that solving the BVP for the fundamental solutions is equivalent to solving the homogenous equation for the fundamental solutions ##v_1## and ##v_2## subject to ##v_1(0)=0,v_1'(0)=1## and ##v_2(0)=1,v_2'(0)=0##.

Can anyone help me understand how the went from the BVP to the IVP? I should say the governing differential equation (not shown here) does not change from the BVP to the IVP.
 
on Phys.org
I'm not sure what kind of differential equation is being solved here, but consider a BVP where the values of an unknown function ##f(x,y)## are given on a circular curve in the xy-plane, and then you make the circle larger and larger to make the shape of the boundary approach a straight line. Wouldn't this kind of a construction convert a boundary value problem to an initial value one?
 

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