Convolution integral and the Convolution Theorem.

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MIT OpenCourseWarehttp://ocw.mit.edu 18.034 Honors Differential Equations Spring 2009 For information about citing these materials or our Terms of Use, visit: http://ocw.mit.edu/terms. � � � LECTURE 22. CONVOLUTION Motivation: buildup of a pollutant in a lake. Let’s say we have a lake and a pollutant is being dumped into it at the variable rate f(t). The pollutant degrades over time exponentially. If the lake begins at t =0with no pollutant, how much is in the lake at time t> 0? The small drip of pollutant added to the lake between t1 and t1 +Δt, where Δt small, is f(t1)Δt. Later t>t1, the drip reduces to e−a(t−t1)f(t1)Δt, where a> 0is the decay constant. Adding them up, starting at the initial time t1 =0, we obtain that the amount is t (22.1) e −a(t−t1)f(t1)dt1. 0 Integral of this kind is called a convolution. We can solve this problem by setting up a differential equation. Let y(t) be the amount of pollutant in the lake at time t. Then, the amount of the chemical in the lake at time t +Δt is the amount at time t, minus the fraction that decayed plus the amount newly added: y(t +Δt)=y(t)− ay(t)Δt +f(t)Δt. Taking the limit as Δt → 0we obtain y +ay =f(t),y(0)=0. It is straightforward that (22.1) gives the solution of the above initial value problem. The convolution integral. The convolution of f and g is defined as t (22.2) (f ∗ g)(t)= f(t1)g(t − t1)dt1. 0 It gives the response at the present time t as a weighted superposition over the input at times t1

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A convolution integral is defined. The properties of convolution are stated and discussed. The convolution operator acts like ordinary multiplication for which distributive, commutative and associative rules hold. Convolution allows an easy passage from the s-domain to the t-domain and leads to explicit solutions for a general inhomogeneous term f(t). The Convolution Theorem is stated and proved. The tautochrone curve is defined and explained with the help of diagram. The aim is to determine the shape of the curve so that the y time of descent is independent of the starting point. A curve of this kind is called a tautochrone. Brachistochrone is discussed.
Instructor: Dr. Vera Mikyoung Hur, Maths, 18.034: Honors Differential Equations, Spring 2009: 19. Convolution: Massachusetts Institute of Technology: MIT Open Course Ware),http://ocw.mit.edu (Accessed 2 January, 2012). License: Creative Commons BY-NC-SA: http://ocw.mit.edu/terms/#cc

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