Vibrations of Single-DOF Systems

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dynamics vibrations natural frequency damping spring-mass systems free vibration

Core Idea

A single-degree-of-freedom vibrating system consists of a mass, a restoring element (spring), and optionally a damping element (dashpot). For undamped free vibration, Newton's second law yields the equation of motion m*x'' + k*x = 0, with the natural frequency omega_n = sqrt(k/m) and period tau = 2*pi/omega_n. The general solution x(t) = A*sin(omega_n*t + phi) describes simple harmonic motion. When viscous damping is added, the equation becomes m*x'' + c*x' + k*x = 0, characterized by the damping ratio zeta = c/(2*m*omega_n). If zeta < 1 (underdamped), the system oscillates with exponentially decaying amplitude at the damped frequency omega_d = omega_n*sqrt(1 - zeta^2). If zeta = 1 (critically damped) or zeta > 1 (overdamped), the system returns to equilibrium without oscillation. The logarithmic decrement delta = ln(x_n/x_{n+1}) = 2*pi*zeta/sqrt(1 - zeta^2) provides a practical way to measure damping from experimental decay data.

How It's Best Learned

Derive the equation of motion from Newton's second law for a spring-mass-dashpot system, identify the natural frequency and damping ratio from the coefficients, and then write the solution form based on the damping regime. Work problems that ask for period, frequency, maximum displacement, and the number of cycles for amplitude to decay by a given factor. For rotational systems, draw the analogy: I*theta'' + c_t*theta' + k_t*theta = 0, with omega_n = sqrt(k_t/I).

Common Misconceptions

Explainer

From your study of simple harmonic motion, you know that a restoring force proportional to displacement produces sinusoidal oscillation. Single-degree-of-freedom vibration analysis is what happens when you apply Newton's second law to a spring-mass system systematically, extract the governing parameters, and then generalize to damped systems. The architecture of the whole subject flows from a single equation of motion.

For an undamped spring-mass system, Newton's second law gives m*x'' = −k*x, which rearranges to m*x'' + k*x = 0. Every coefficient carries physical meaning: m is inertia (resisting acceleration) and k is stiffness (providing the restoring force). Dividing through by m gives x'' + (k/m)*x = 0, and the quantity ω_n = √(k/m) is the natural frequency — the rate at which the system oscillates if displaced and released. You should read ω_n physically: a stiffer spring (larger k) or lighter mass (smaller m) gives higher natural frequency. The solution x(t) = A sin(ω_n t + φ) is exactly the simple harmonic motion you already know, with amplitude A and phase φ set by initial conditions.

Adding a dashpot (viscous damper with constant c) introduces a velocity-proportional force: the equation becomes m*x'' + c*x' + k*x = 0. Two new parameters emerge. The critical damping coefficient c_c = 2m*ω_n is the value at which the system returns to equilibrium in minimum time without oscillating. The damping ratio ζ = c / c_c compares the actual damping to critical. The three regimes flow directly from ζ: if ζ < 1 (underdamped), the system oscillates at the reduced damped natural frequency ω_d = ω_n√(1−ζ²) with amplitude that decays as e^(−ζω_n t); if ζ = 1 (critically damped), the system returns to equilibrium as fast as possible with no overshoot; if ζ > 1 (overdamped), return is even slower and also non-oscillatory. Automobile suspensions are tuned to ζ ≈ 0.3–0.7 to balance ride comfort against unwanted oscillation.

The logarithmic decrement δ = ln(x_n / x_{n+1}) bridges theory and experiment. Because successive peaks of an underdamped oscillation decay by the factor e^(−ζω_n T_d) per cycle, the log of consecutive peak amplitudes directly yields ζ. This makes it practical to measure damping from recorded vibration data without ever knowing m, k, or c individually — a tool used routinely in structural health monitoring, modal testing, and machine diagnostics. The entire single-DOF framework — equation of motion, natural frequency, damping ratio, response regimes — repeats structurally for every vibrating system from a guitar string to a skyscraper; only m, k, and c take different physical forms.

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 MomentsCenter of MassConservation of Linear MomentumElastic CollisionsInelastic CollisionsCoefficient of RestitutionCollision Analysis and Real-World ApplicationsTwo-Body Collisions in the Center-of-Mass FrameReduced Mass and Two-Body ProblemsKinematics in Two DimensionsProjectile MotionCurvilinear Kinematics of ParticlesNewton's Second Law Applied to Particle DynamicsVibrations of Single-DOF Systems

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