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{{Differential equations}}
{{Short description|Procedure for solving differential equations}}In [[mathematics]], '''variation of parameters''', also known as '''variation of constants''', is a general method to solve [[inhomogeneous differential equation|inhomogeneous]]
For first-order inhomogeneous [[linear differential
Variation of parameters extends to linear [[partial differential equations]] as well, specifically to inhomogeneous problems for linear evolution equations like the [[heat equation]], [[wave equation]], and [[vibrating plate]] equation. In this setting, the method is more often known as [[Duhamel's principle]], named after [[Jean-Marie Duhamel]] (1797–1872) who first applied the method to solve the inhomogeneous heat equation. Sometimes variation of parameters itself is called Duhamel's principle and vice versa.
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The method of variation of parameters was first sketched by the Swiss mathematician [[Leonhard Euler]] (1707–1783), and later completed by the Italian-French mathematician [[Joseph Louis Lagrange|Joseph-Louis Lagrange]] (1736–1813).<ref>See:
* [[Forest Ray Moulton]], ''An Introduction to Celestial Mechanics'', 2nd ed. (first published by the Macmillan Company in 1914; reprinted in 1970 by Dover Publications, Inc., Mineola, New York), [https://books.google.com/books?id=URPSrBntwdAC&pg=PA431
* Edgar Odell Lovett (1899) [https://books.google.com/books?id=j7sKAAAAIAAJ&pg=PA47
A forerunner of the method of variation of a celestial body's orbital elements appeared in Euler's work in 1748, while he was studying the mutual perturbations of Jupiter and Saturn.<ref>Euler, L. (1748) [https://books.google.com/books?id=GtA6Ea1NlqwC&pg=PA1
Lagrange first used the method in 1766.<ref>Lagrange, J.-L. (1766) [https://books.google.com/books?id=XwVNAAAAMAAJ&pg=RA1-PA179
* Lagrange, J.-L. (1781) [https://books.google.com/books?id=UitRAAAAYAAJ&pg=PA199
* Lagrange, J.-L. (1782) [https://books.google.com/books?id=kW9PAAAAYAAJ&pg=PA169
* Lagrange, J.-L. (1783) [https://books.google.com/books?id=Lz7fp3OnutEC&pg=PA161
* Lagrange, J.-L. (1778) [https://books.google.com/books?id=F90_AAAAYAAJ&pg=PA60-IA55
* Lagrange, J.-L. (1778) [https://books.google.com/books?id=F90_AAAAYAAJ&pg=PA60-IA68
* Lagrange, J.-L. (1783) [http://gallica.bnf.fr/ark:/12148/bpt6k229223s/f498.image "Sur le probleme de la détermination des orbites des cometes d'après trois observations. Troisième mémoire, dans lequel on donne une solution directe et générale du problème."], ''Nouveaux Mémoires de l'Académie Royale des Sciences et Belles-lettres'' (Berlin), pages 296–332 [published in 1785].</ref> During 1808–1810, Lagrange gave the method of variation of parameters its final form in a third series of papers.<ref>See:
* Lagrange, J.-L. (1808) “Sur la théorie des variations des éléments des planètes et en particulier des variations des grands axes de leurs orbites,” ''Mémoires de la première Classe de l’Institut de France''. Reprinted in: Joseph-Louis Lagrange with Joseph-Alfred Serret, ed., ''Oeuvres de Lagrange'' (Paris, France: Gauthier-Villars, 1873), vol. 6, [http://gallica.bnf.fr/ark:/12148/bpt6k229225j/f715.image pages 713–768].
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== Description of method ==
Given an ordinary non-homogeneous [[linear differential equation]] of order ''n''
{{NumBlk|:|<math>y^{(n)}(x) + \sum_{i=0}^{n-1} a_i(x) y^{(i)}(x) = b(x).</math>|{{EquationRef|i}}}}
Let <math>y_1(x), \ldots, y_n(x)</math> be a [[
{{NumBlk|:|<math>y^{(n)}(x) + \sum_{i=0}^{n-1} a_i(x) y^{(i)}(x) = 0.</math>|{{EquationRef|ii}}}}
Then a [[
{{NumBlk|:|<math>y_p(x) = \sum_{i=1}^{n} c_i(x) y_i(x)</math>|{{EquationRef|iii}}}}
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:<math>c_i'(x) = \frac{W_i(x)}{W(x)}, \, \quad i=1,\ldots,n</math>
where <math>W(x)</math> is the [[Wronskian determinant]] of the
The particular solution to the non-homogeneous equation can then be written as
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Note that <math>A(x)</math> and <math> B(x)</math> are each determined only up to an arbitrary additive constant (the [[constant of integration]]). Adding a constant to <math>A(x)</math> or <math>B(x)</math> does not change the value of <math>Lu_G(x)</math> because the extra term is just a linear combination of ''u''<sub>1</sub> and ''u''<sub>2</sub>, which is a solution of <math>L</math> by definition.
==See also==▼
* [[Alekseev–Gröbner formula]], a generalization of the variation of constants formula.▼
* [[Reduction of order]]▼
== Notes ==
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| url = https://www.mat.univie.ac.at/~gerald/ftp/book-ode/
}}
▲==See also==
▲* [[Reduction of order]]
▲* [[Alekseev–Gröbner formula]], a generalization of the variation of constants formula.
== External links ==
*[http://tutorial.math.lamar.edu/classes/de/VariationofParameters.aspx Online Notes / Proof] by Paul Dawkins, [[Lamar University]].
*{{PlanetMath|VariationOfParameters}}
*[https://projecteuclid.org/download/pdf_1/euclid.mjms/1316092232 A NOTE ON LAGRANGE’S METHOD OF VARIATION OF PARAMETERS]
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