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More limit cycles than expected in Liénard equations
Authors:Freddy Dumortier  Daniel Panazzolo  Robert Roussarie
Institution:Universiteit Hasselt, Campus Diepenbeek, Agoralaan - Gebouw D, B-3590 Diepenbeek, Belgium ; Instituto de Matemática e Estat' istica, Universidade de São Paulo, Rua do Matão, 1010 - São Paulo, SP, 05508-090, Brazil ; Institut de Mathématique de Bourgogne, U.M.R. 5584 du C.N.R.S., Université de Bourgogne, B.P. 47 870, 21078 Dijon Cedex, France
Abstract:The paper deals with classical polynomial Liénard equations, i.e. planar vector fields associated to scalar second order differential equations $ x'+f(x)x'+ x=0$ where $ f$ is a polynomial. We prove that for a well-chosen polynomial $ f$ of degree $ 6,$ the equation exhibits $ 4$ limit cycles. It induces that for $ n\geq 3$ there exist polynomials $ f$ of degree $ 2n$ such that the related equations exhibit more than $ n$ limit cycles. This contradicts the conjecture of Lins, de Melo and Pugh stating that for Liénard equations as above, with $ f$ of degree $ 2n,$ the maximum number of limit cycles is $ n.$ The limit cycles that we found are relaxation oscillations which appear in slow-fast systems at the boundary of classical polynomial Liénard equations. More precisely we find our example inside a family of second order differential equations $ \varepsilon x'+f_\mu(x)x'+x=0.$ Here, $ f_\mu$ is a well-chosen family of polynomials of degree $ 6$ with parameter $ \mu\in \mathbb{R}^4$ and $ \varepsilon$ is a small positive parameter tending to $ 0.$ We use bifurcations from canard cycles which occur when two extrema of the critical curve of the layer equation are crossing (the layer equation corresponds to $ \varepsilon =0)$. As was proved by Dumortier and Roussarie (2005) these bifurcations are controlled by a rational integral computed along the critical curve of the layer equation, called the slow divergence integral. Our result is deduced from the study of this integral.

Keywords:Limit cycles  Li\'enard equation  slow-fast equation  
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