Second-Order System Time Response

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damping-ratio natural-frequency percent-overshoot settling-time second-order

Core Idea

A standard second-order system has the transfer function G(s) = ωₙ²/(s² + 2ζωₙs + ωₙ²), characterized by natural frequency ωₙ and damping ratio ζ. The damping ratio determines qualitative behavior: underdamped (ζ < 1) produces oscillatory overshoot, critically damped (ζ = 1) gives the fastest non-overshooting response, and overdamped (ζ > 1) gives a sluggish monotone response. Key performance metrics — percent overshoot (%OS = e^{−πζ/√(1−ζ²)}×100), rise time, peak time Tₚ = π/ωd, and settling time Ts ≈ 4/(ζωₙ) — are analytically derivable from ζ and ωₙ. Most control design specifications are stated in terms of these metrics.

How It's Best Learned

Plot step responses for ζ = 0.1, 0.5, 0.707, 1.0, and 2.0 to internalize how damping affects behavior. Derive the overshoot formula and settling time approximation so they become second nature — these are the most frequently used formulas in control design.

Common Misconceptions

Explainer

From your study of first-order systems, you know that a single time constant τ fully describes how fast a system approaches its final value — the response is always a decaying exponential, never oscillatory. A second-order system introduces a new possibility: the system can overshoot its target and ring back and forth before settling. This happens because a second-order system has energy storage in two different elements (think of a mass with both spring and dashpot), and those elements can exchange energy with each other. The two parameters that replace τ are the natural frequency ωₙ and the damping ratio ζ.

The natural frequency ωₙ sets the intrinsic speed of the system — how fast it would oscillate if there were no damping at all (ζ = 0). Think of it as the frequency of an undamped spring-mass system from your simple harmonic motion prerequisite. The damping ratio ζ measures how aggressively the system dissipates energy relative to that natural oscillation. When ζ = 0, the system oscillates forever. When ζ = 1 (critically damped), dissipation exactly prevents any overshoot. When ζ > 1 (overdamped), the system is sluggish — imagine a door closer in thick oil. The most practically useful regime is underdamped (0 < ζ < 1), where the system overshoots but settles quickly. The actual oscillation frequency you observe in the step response is the damped natural frequency ωd = ωₙ√(1−ζ²), which is always lower than ωₙ because damping slows the oscillations.

The performance metrics follow directly from ζ and ωₙ. Percent overshoot depends only on ζ: %OS = e^(−πζ/√(1−ζ²)) × 100. This is a pure function of ζ — if you want less than 5% overshoot, you need ζ > 0.69. Peak time Tₚ = π/ωd tells you when the first overshoot peak occurs — it decreases as ωd increases, meaning a faster (higher ωₙ) or less-damped system peaks sooner. Settling time Ts ≈ 4/(ζωₙ) depends on both parameters: to settle faster, you need either more damping or a higher natural frequency. This is the essential design tradeoff — ζ controls the overshoot; ωₙ scales the overall speed.

The value ζ ≈ 0.707 (= 1/√2) deserves special attention. It is not critically damped, but it achieves a near-optimal compromise: the step response is fast, the overshoot is only about 4.3%, and the settling is clean. Many practical specifications target this region. In the s-plane, increasing ωₙ moves the closed-loop poles radially outward (faster), while increasing ζ rotates them toward the negative real axis (less oscillatory). When you move to designing controllers like PID, every gain adjustment is really an attempt to place those poles at the right combination of ωₙ and ζ — so internalizing the relationship between pole location and these time-domain metrics is foundational to everything that follows.

Practice Questions 5 questions

Prerequisite Chain

Counting to 10Counting to 20Understanding ZeroThe Number ZeroCounting to FiveOne-to-One CorrespondenceCombining Small Groups Within 5Addition Within 10Addition Within 20Two-Digit Addition Without RegroupingTwo-Digit Addition with RegroupingAddition Within 100Repeated Addition as MultiplicationMultiplication Facts Within 100Division as Equal SharingDivision as Grouping (Measurement Division)Division: Grouping (Repeated Subtraction) ModelDivision: Fair Sharing ModelDivision as Equal SharingDivision as GroupingBasic Division FactsDivision Facts Within 100Two-Digit by One-Digit DivisionDivision with RemaindersRemainders and Quotients in DivisionDivision Word ProblemsIntroduction to Long DivisionFactors and MultiplesPrime and Composite NumbersEquivalent FractionsRelating Fractions and DecimalsDecimal Place ValueReading and Writing DecimalsComparing and Ordering DecimalsAdding and Subtracting DecimalsMultiplying DecimalsDividing DecimalsDividing FractionsMixed Number ArithmeticOrder of OperationsInteger Order of OperationsVariable ExpressionsCombining Like TermsOne-Step EquationsTwo-Step EquationsSolving Multi-Step EquationsEquations with Variables on Both SidesAngle Pairs: Complementary, Supplementary, and VerticalParallel Lines and TransversalsCorresponding AnglesAlternate Interior AnglesTriangle Angle Sum TheoremExterior Angle TheoremTriangle Inequality TheoremSimilar Triangles: AA SimilaritySimilar Triangles: SSS and SAS SimilarityProportions in Similar TrianglesRight Triangle Trigonometry IntroductionTrigonometric Ratios ReviewRadian MeasureConverting Between Degrees and RadiansThe Unit CircleGraphing Sine and CosineGraphing Tangent and Reciprocal Trigonometric FunctionsDerivatives of Trigonometric FunctionsAntiderivativesIterated Integrals and Fubini's TheoremDouble Integrals in Cartesian CoordinatesDouble Integrals over Rectangular RegionsDouble Integrals in Polar CoordinatesDouble Integrals: Definition and SetupIterated Integrals and Fubini's TheoremDouble Integrals over Rectangular RegionsDouble Integrals over General RegionsApplications of Double Integrals: Area, Mass, and MomentsTriple Integrals in Cartesian CoordinatesTriple Integrals in Cylindrical and Spherical CoordinatesChange of Variables and the Jacobian DeterminantApplications of Triple Integrals: Volume and MassVector Fields and Their RepresentationsLine Integrals of Vector FieldsGreen's TheoremSurface Integrals and Flux of Vector FieldsSurface Integrals and Flux of Vector FieldsDivergence Theorem: Flux and OutflowDivergence TheoremElectric FluxGauss's LawConductors in Electrostatic EquilibriumCapacitance and CapacitorsDielectricsDielectric Constant and Relative PermittivityElectric Field Inside Dielectric MaterialsDielectric Materials and PolarizationDielectric Susceptibility and PermittivityEnergy Density in Electric FieldsElectric Current and Current DensityElectrical Resistance and ResistivityOhm's Law and Circuit ElementsElectromotive Force (EMF) and BatteriesKirchhoff's Circuit Laws: Voltage and CurrentDC Circuit Network Analysis MethodsTransient Response in RC CircuitsRC CircuitsLC and RLC CircuitsSecond-Order Transient Circuit ResponseFeedback Control FundamentalsLaplace Transform Methods for ControlTransfer Functions and System ModelingFirst-Order System Time ResponseSecond-Order System Time Response

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