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In mathematical physics, the Degasperis–Procesi equation : is one of only two exactly solvable equations in the following family of third-order, non-linear, dispersive PDEs: : where and ''b'' are real parameters (''b''=3 for the Degasperis–Procesi equation). It was discovered by Degasperis and Procesi in a search for integrable equations similar in form to the Camassa–Holm equation, which is the other integrable equation in this family (corresponding to ''b''=2); that those two equations are the only integrable cases has been verified using a variety of different integrability tests.〔Degasperis & Procesi 1999; Degasperis, Holm & Hone 2002; Mikhailov & Novikov 2002; Hone & Wang 2003; Ivanov 2005〕 Although discovered solely because of its mathematical properties, the Degasperis–Procesi equation (with ) has later been found to play a similar role in water wave theory as the Camassa–Holm equation.〔Johnson 2003; Dullin, Gottwald & Holm 2004; Constantin & Lannes 2007; Ivanov 2007〕 == Soliton solutions == (詳細はmultipeakon solutions, which are functions of the form : where the functions and satisfy〔Degasperis, Holm & Hone 2002〕 : These ODEs can be solved explicitly in terms of elementary functions, using inverse spectral methods.〔Lundmark & Szmigielski 2003, 2005〕 When the soliton solutions of the Degasperis–Procesi equation are smooth; they converge to peakons in the limit as tends to zero.〔Matsuno 2005a, 2005b〕 抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Degasperis–Procesi equation」の詳細全文を読む スポンサード リンク
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