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Ordinary differential equations

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First order odeSecond order odeLinear odeSystems of odeSeries solutionsEigenvalue problemsAutonomous differential equationAutonomous systemNon autonomous systemNon homogeneous differential equationExact differential equationInexact differential equationSeparable differential equationBernoulli differential equationMatrix differential equationDifference equationAlgebraic differential equationDifferential algebraic system of equationsPartial differential algebraic equationDelay differential equationFractional differential equationsDifferential variational inequalitySystem of differential equationsDynamic equationFree motion equationCharacteristic equation calculusForcing function differential equationsIsoclineFundamental matrix linear differential equationAbels identityLiouvilles formulaVariation of parametersReduction of orderIntegrating factorMethod of undetermined coefficientsAnnihilator methodExponential response formulaPower series solution of differential equationsFrobenius methodMethod of averagingSingular perturbationMagnus expansionOrdered exponentialAdomian decomposition methodQuasilinearizationNumerical methods for ordinary differential equationsSingular solutionFuchss theoremFuchsian theoryFloquet theoryMonodromy matrixCharacteristic multiplierExponential dichotomyInitial value problemCauchy problemWell posed problemPicard lindelof theoremPeano existence theoremCaratheodory existence theoremCaratheodorys existence theoremKnesers theorem differential equationsLienards theoremOscillation theoryQualitative theory of differential equationsLiouvilles theorem differential algebraIsomonodromic deformationSchlesinger equationsLoewy decompositionLoewy decomposition of linear differential equationsMalmquists theoremNeural differential equationOde filterOde im correspondenceAdams williamson equationRadiodromeLaser diode rate equationsHolonomic function

A Damped Spiral That Rings Down to One, Not to Zero

The characteristic roots of u'' + u' + u are the primitive cube roots of unity, so the homogeneous part decays with envelope e to the minus x over two and oscillates with period 4 pi over root 3, which is 7.2552. Substituting that homogeneous solution back into the equation leaves a residual of exactly minus one, and that residual is the whole distance between the common wrong answer and the right one. The constant u = 1 solves the equation by itself, so every solution settles on 1, and the constant trial works only because the coefficient on u is not zero.

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