Uniform Continuity

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Core Idea

A function f is uniformly continuous on a set S if for every ε > 0, there exists δ > 0 (independent of the point) such that for all x, y ∈ S, |x - y| < δ implies |f(x) - f(y)| < ε. This is stronger than pointwise continuity: δ works at all points simultaneously. It is essential for convergence of integrals and derivatives.

How It's Best Learned

Show f(x) = x is uniformly continuous but f(x) = x² is not on ℝ (though it is on [0,1]). Prove f(x) = 1/x is not uniformly continuous on (0,1) but is on [1,∞).

Common Misconceptions

Explainer

From your study of ε-δ continuity, you know what it means for a function f to be continuous at a single point x₀: for every ε > 0, there exists δ > 0 such that |x − x₀| < δ implies |f(x) − f(x₀)| < ε. The δ you find typically depends on both ε and the particular point x₀. Uniform continuity strengthens this by demanding that a single δ works at all points simultaneously. Formally, f is uniformly continuous on a set S if: for every ε > 0, there exists δ > 0 such that for all x, y ∈ S, |x − y| < δ implies |f(x) − f(y)| < ε. The δ depends only on ε, not on the location within S.

The distinction is about how the "required δ" varies across the domain. For f(x) = x on ℝ, continuity is trivially uniform: choosing δ = ε works everywhere, because |f(x) − f(y)| = |x − y| < δ = ε. The function's "rate of change" is constant (slope 1), so the same δ suffices at every point. For f(x) = x² on ℝ, the situation is different. To ensure |x² − y²| = |x + y||x − y| < ε when |x − y| < δ, you need δ < ε/|x + y|. As x grows, |x + y| ≈ 2|x| grows without bound, forcing the required δ toward 0. No single δ can work for all x ∈ ℝ simultaneously, so f(x) = x² is continuous but not uniformly continuous on ℝ.

The same function can be uniformly continuous on one domain but not another. f(x) = 1/x is not uniformly continuous on (0, 1) — near x = 0, the function grows arbitrarily steep, and any proposed δ fails for sufficiently small x. But on [1, ∞), the slope |f'(x)| = 1/x² ≤ 1 is bounded, so δ = ε works everywhere by the mean value theorem. The key structural fact is the Heine-Cantor theorem: every continuous function on a compact set is uniformly continuous. Since [a, b] is compact and (0, 1) is not, the theorem explains why continuity on [a, b] automatically upgrades to uniform continuity, while continuity on open or unbounded domains need not.

Uniform continuity matters because it is the condition needed to guarantee that function-level operations behave well. The proof that continuous functions on [a, b] are Riemann integrable relies on uniform continuity: it lets you choose a single mesh size δ for the partition that controls the oscillation of f on every subinterval simultaneously. Without uniform continuity, you would need finer and finer partitions in different parts of the domain, and the integral might not exist. Similarly, uniform continuity is the hypothesis (stronger than pointwise continuity) that ensures certain limits can be interchanged with integration. Understanding when continuity is automatically uniform — and when it is not — is one of the key practical skills in real analysis.

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 ValueIntegers and the Number LineOpposites and Additive InversesAbsolute ValueAdding IntegersSubtracting IntegersMultiplying IntegersDividing IntegersUnit RatesProportionsPercent ConceptConverting Between Fractions, Decimals, and PercentsOperations with Rational NumbersTwo-Step EquationsSolving Multi-Step EquationsEquations with Variables on Both SidesLiteral EquationsSlope-Intercept FormPoint-Slope FormWriting Linear EquationsParallel and Perpendicular Line SlopesGraphing Linear EquationsPiecewise FunctionsOne-Sided LimitsContinuity DefinitionEpsilon-Delta ContinuityUniform Continuity

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