George Green George Green (14 July 1793 – 31 May 1841) was a British mathematical physicist who wrote: An Essay on the Application of Mathematical Analysis.

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Presentation transcript:

George Green George Green (14 July 1793 – 31 May 1841) was a British mathematical physicist who wrote: An Essay on the Application of Mathematical Analysis to the Theories of Electricity and Magnetism (Green, 1828). The essay introduced several important concepts, among them a theorem similar to the modern Green's theorem, the idea of potential functions as currently used in physics, and the concept of what are now called Green's functions. Green was the first person to create a mathematical theory of electricity and magnetism and his theory formed the foundation for the work of other scientists such as James Clerk Maxwell, William Thomson, and others. His work on potential theory ran parallel to that of Carl Friedrich Gauss.James Clerk Maxwell William ThomsonCarl Friedrich Gauss Green's life story is remarkable in that he was almost entirely self-taught. He received only about one year of formal schooling as a child, between the ages of 8 and 9

The Diffusion Equation  Consider the Following Problem  Two point spills of mass M 1 and M 2 occur at two different locations x 1 and x 2.  Describe how the concentration field evolves.

Hopefully you gut said This is absolutely correct – but the question is why? Here’s a question for you: Is the ADE a linear or a nonlinear equation?

Linear Superposition  Answer:  The ADE is a linear equation, which means we can add solutions together (principle of linear superposition), i.e. where We can use this same idea for any initial condition, no matter how complex

One step back What is the delta function? An infinitely narrow, infinitely tall pulse Which integrates to unity It also acts as a filter with the following useful property i.e. it picks out the value of f(x) and x=x 0

Arbitrary Initial Condition How do we represent this as the sum of several point spills? Which will allow us to solve in the same way as before. Well by definition we can always write: That is we can represent any initial condition as the sum (integral) of infinitely many delta functions weighted by C 0. Each delta evolves with the fundamental solution of the diffusion equation

This is pretty amazing….  Each evolves as  Therefore  We call the fundamental solution for initial condition the Greens function We can do this for any linear equation!!

More Generally for the ADE  Consider the diffusion equation with an additional source term The solution of which is given by the general expression Where for the diffusion equation

Example 1 Consider the diffusion equation with a more complex initial condition H(x) is the Heaviside step function where H(x)=1 for x>0 =0 for x <0 This is a step initial condition where C=1 for x 0

Example 2 This problem is a lot harder than it seems it should be… Consider the diffusion equation with an additional source term We have a domain that is initially empty of contaminant and there is a source located at x=0, which is continuously injecting mass in at x=0.

Finite Domains  So far we have only considered infinite domains, which of course is an idealization of reality. What about when the domains are finite and have boundary conditions?  Amazingly we can still use the Greens function approach – the form of the Greens function just changes to reflect the domain of interest.  See handout with notes from Polyanin’s book.