Tangent Planes to Surfaces

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Core Idea

For a surface z = f(x, y), the tangent plane at (x₀, y₀, z₀) has equation z − z₀ = f_x(x₀, y₀)(x − x₀) + f_y(x₀, y₀)(y − y₀). The normal vector is n = ⟨f_x, f_y, −1⟩, and ∇f lies in the plane.

Explainer

In single-variable calculus, the tangent line at a point (x₀, y₀) on the curve y = f(x) has equation y − y₀ = f'(x₀)(x − x₀). It is the best linear approximation to f near x₀. The tangent plane for a surface z = f(x, y) is the direct 3D extension: a flat plane that best approximates the surface near the point (x₀, y₀, z₀). Instead of one derivative, there are two — f_x and f_y, the partial derivatives you know from the gradient — and the plane accounts for the slope in each independent direction.

The tangent plane equation z − z₀ = f_x(x₀, y₀)(x − x₀) + f_y(x₀, y₀)(y − y₀) can be read as: "the change in z is approximately the x-slope times the change in x, plus the y-slope times the change in y." Hold y fixed (set y = y₀) and the equation becomes z − z₀ = f_x(x − x₀), which is exactly the tangent line in the xz-plane. Hold x fixed and you recover the tangent line in the yz-plane. The tangent plane combines both tangent lines simultaneously — it is the unique plane containing both.

The gradient ∇f = ⟨f_x, f_y⟩ encodes both partial derivatives but lives in the xy-plane, not in 3D. The normal vector to the tangent plane is n = ⟨f_x, f_y, −1⟩. To see why: rewrite the tangent plane as f_x(x − x₀) + f_y(y − y₀) − (z − z₀) = 0, which is the equation n · ⟨x − x₀, y − y₀, z − z₀⟩ = 0 — the standard form of a plane with normal n. The third component is −1 because z appears with coefficient −1 when you move it to the left side. This is why the statement "∇f lies in the plane" is true: the 2D gradient vector is not the 3D normal; the normal has an additional z-component.

For a surface given implicitly as F(x, y, z) = c (rather than explicitly as z = f(x,y)), the 3D gradient ∇F = ⟨F_x, F_y, F_z⟩ is the normal vector to the surface. This is the more general form: since F is constant on the surface, any tangent direction v must satisfy ∇F · v = 0, making ∇F normal to every tangent direction. The explicit case z = f(x,y) is a special case: define F(x,y,z) = f(x,y) − z, so ∇F = ⟨f_x, f_y, −1⟩, recovering the normal vector from the Core Idea. This unification — the gradient of an implicit equation is always the normal to the corresponding surface — is one of the most reusable ideas in multivariable calculus.

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 DefinitionLimit Definition of the DerivativeDerivative as Slope of Tangent LinePartial Derivatives: Definition and ComputationDifferentiability in Multiple VariablesDifferentiability in Multivariable FunctionsTotal Differential and Linear ApproximationTangent Planes and Linear ApproximationTangent Planes and Linear ApproximationTangent Planes to Surfaces

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