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5️⃣Multivariable Calculus

Key Concepts of Double Integrals

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Why This Matters

Double integrals represent your first major leap from single-variable thinking into the world of multidimensional analysis. You're being tested on your ability to extend the fundamental idea of accumulation—adding up infinitely many infinitesimal pieces—from one dimension to two. This isn't just about computing integrals; it's about understanding how regions, coordinate systems, and transformation techniques work together to solve problems that single integrals simply can't handle.

The concepts here form the foundation for everything that follows in multivariable calculus: triple integrals, surface integrals, and the major theorems like Green's and Stokes'. Master these ideas and you'll see how geometric intuition, algebraic manipulation, and strategic coordinate choice combine to tackle real-world applications from physics to probability. Don't just memorize formulas—know why we switch to polar coordinates, when to change integration order, and what the Jacobian actually measures.


Foundations: What Double Integrals Actually Mean

Before computing anything, you need a rock-solid understanding of what double integrals represent. The double integral accumulates a function's values over a two-dimensional region, generalizing the "area under a curve" concept to "volume under a surface."

Definition of Double Integrals

  • Extends single integrals to two variables—instead of integrating along an interval, you're integrating over a region RR in the xyxy-plane
  • Notation Rf(x,y)dA\iint_R f(x, y) \, dA represents the limit of Riemann sums where dAdA is an infinitesimal area element
  • Accumulates quantities like volume, mass, or probability depending on what f(x,y)f(x, y) represents in context

Geometric Interpretation as Volume

  • Volume under a surface z=f(x,y)z = f(x, y) over region RR is the most common visualization
  • Positive values of ff contribute positive volume; negative values subtract from the total
  • Connects geometry to analysis—the integral transforms a surface equation into a single numerical quantity

Compare: Definition vs. Geometric Interpretation—the definition gives you the mechanics (limits of Riemann sums), while the volume interpretation gives you the intuition (what you're actually computing). FRQs often ask you to set up integrals for volume problems, so connect both perspectives.


Computation Techniques: Rectangular Regions

Rectangular regions are your starting point because the limits of integration are constants. Mastering these builds the foundation for handling more complex regions.

Iterated Integrals

  • Sequential single integrals—evaluate the inner integral first (treating the other variable as constant), then the outer
  • Breaks complexity into steps by reducing a double integral to two manageable single-variable problems
  • Inner integral produces a function of the remaining variable, which the outer integral then evaluates

Evaluating Over Rectangular Regions

  • Constant limits define the rectangle: axba \leq x \leq b and cydc \leq y \leq d
  • Either order works—compute as abcdf(x,y)dydx\int_a^b \int_c^d f(x,y) \, dy \, dx or cdabf(x,y)dxdy\int_c^d \int_a^b f(x,y) \, dx \, dy
  • Separable functions f(x,y)=g(x)h(y)f(x,y) = g(x)h(y) allow the integral to factor: (abg(x)dx)(cdh(y)dy)\left(\int_a^b g(x)\,dx\right)\left(\int_c^d h(y)\,dy\right)

Fubini's Theorem

  • Guarantees order doesn't matter when f(x,y)f(x, y) is continuous on a rectangular region
  • Enables strategic choice—pick the order that makes the antiderivative easier to find
  • Fails for discontinuous functions in certain cases, so always verify continuity conditions

Compare: Iterated Integrals vs. Fubini's Theorem—iterated integrals are the method, while Fubini's Theorem is the justification for switching order. If an FRQ asks why you can reverse integration order, cite Fubini and continuity.


Handling Complex Regions

Real problems rarely involve perfect rectangles. The key is describing the region with appropriate inequalities and setting up variable limits accordingly.

Non-Rectangular Regions

  • Variable limits replace constants—one integral's bounds depend on the other variable
  • Type I regions have axba \leq x \leq b with g1(x)yg2(x)g_1(x) \leq y \leq g_2(x); Type II regions reverse the roles
  • Sketch the region first—determining which type simplifies the integral often requires visualizing the boundaries

Changing Integration Order

  • Reverses which variable has constant limits and requires re-expressing the region's boundaries
  • Essential when one order is impossible—some integrands have no elementary antiderivative in one variable but do in the other
  • Sketch and re-describe the region using inequalities that match the new order

Compare: Type I vs. Type II regions—Type I integrates dydy first (vertical strips), Type II integrates dxdx first (horizontal strips). Choose based on which gives simpler limit expressions, not habit.


Coordinate Transformations

Choosing the right coordinate system can transform an impossible integral into a straightforward one. The Jacobian ensures your answer remains correct after the transformation.

Polar Coordinates

  • Ideal for circular symmetry—regions bounded by circles, sectors, or radial lines become simple rectangles in rθr\theta-space
  • Transformation equations x=rcos(θ)x = r\cos(\theta), y=rsin(θ)y = r\sin(\theta) with x2+y2=r2x^2 + y^2 = r^2
  • Area element becomes dA=rdrdθdA = r \, dr \, d\theta—the extra rr factor is critical and commonly forgotten on exams

Change of Variables (Jacobian)

  • Generalizes coordinate transformations beyond polar to any substitution (x,y)=(g(u,v),h(u,v))(x, y) = (g(u, v), h(u, v))
  • Jacobian determinant J=(x,y)(u,v)=xuxvyuyvJ = \frac{\partial(x, y)}{\partial(u, v)} = \begin{vmatrix} \frac{\partial x}{\partial u} & \frac{\partial x}{\partial v} \\ \frac{\partial y}{\partial u} & \frac{\partial y}{\partial v} \end{vmatrix} measures how areas scale
  • New integral becomes Rf(g(u,v),h(u,v))Jdudv\iint_{R'} f(g(u,v), h(u,v)) \, |J| \, du \, dvalways use absolute value of JJ

Compare: Polar Coordinates vs. General Change of Variables—polar is a specific case where J=rJ = r. Understanding the Jacobian framework helps you handle elliptical regions, sheared coordinates, or any custom transformation an FRQ might require.


Applications: Why We Compute Double Integrals

Double integrals aren't just abstract computations—they solve concrete problems. Each application interprets f(x,y)f(x, y) and dAdA differently.

Area, Volume, and Mass

  • Area of region RR uses f(x,y)=1f(x, y) = 1, giving R1dA\iint_R 1 \, dA
  • Volume under surface uses f(x,y)=f(x, y) = the height function; this is the default geometric interpretation
  • Mass with variable density ρ(x,y)\rho(x, y) computed as Rρ(x,y)dA\iint_R \rho(x, y) \, dA

Center of Mass

  • Coordinates (xˉ,yˉ)(\bar{x}, \bar{y}) found via xˉ=1MRxρ(x,y)dA\bar{x} = \frac{1}{M}\iint_R x \rho(x, y) \, dA and similarly for yˉ\bar{y}
  • Total mass MM is the denominator—compute it first using the mass integral
  • Balances the region at the point where weighted position averages to zero

Probability and Statistics

  • Joint probability density f(x,y)f(x, y) integrates to 1 over all possible outcomes
  • Probability over region RR equals Rf(x,y)dA\iint_R f(x, y) \, dAthe integral gives the likelihood of outcomes in RR
  • Marginal distributions obtained by integrating out one variable: fX(x)=f(x,y)dyf_X(x) = \int_{-\infty}^{\infty} f(x, y) \, dy

Compare: Mass vs. Probability applications—both integrate a "density" function, but mass density has units (kg/m²) while probability density is dimensionless and must integrate to 1. The setup is identical; the interpretation differs.


Quick Reference Table

ConceptBest Examples
Basic DefinitionRiemann sum limit, notation RfdA\iint_R f \, dA
Rectangular RegionsConstant limits, separable functions
Fubini's TheoremOrder reversal, continuity requirement
Non-Rectangular RegionsType I (vertical strips), Type II (horizontal strips)
Polar CoordinatesCircular regions, dA=rdrdθdA = r \, dr \, d\theta
JacobianGeneral substitution, area scaling factor
Volume ApplicationsSurface z=f(x,y)z = f(x,y) over region RR
Physical ApplicationsMass, center of mass, density functions
ProbabilityJoint PDF, marginal distributions

Self-Check Questions

  1. When evaluating Rf(x,y)dA\iint_R f(x, y) \, dA over a non-rectangular region, what determines whether you should use Type I or Type II setup?

  2. Compare and contrast: How does the area element dAdA change when converting from Cartesian to polar coordinates, and why does this factor appear?

  3. If 01x1ey2dydx\int_0^1 \int_x^1 e^{y^2} \, dy \, dx cannot be evaluated as written, what technique would you use, and what would the new limits be?

  4. Two laminas have the same shape but different density functions. Which double integral quantities would be the same, and which would differ?

  5. Explain why Fubini's Theorem requires continuity—what could go wrong if f(x,y)f(x, y) has discontinuities in region RR?