All rectangle sides here are ordered with and ; for a simple region its continuous bounds satisfy everywhere. The complete Darboux and slicing proofs below preserve these assumptions.
From area sums to accumulated quantity
If is a density per unit area, multiplying a sampled density by a small area estimates the quantity in that cell. Add over cells and refine. The result is signed if can be negative: it is not automatically a physical mass or an unsigned volume.
Definition
Double integral on a rectangle
Let . Partition into subrectangles of areas and choose . If the sums approach the same limit as the maximum subrectangle diameter tends to zero, regardless of the choices, that limit is . Every continuous function on a closed rectangle is integrable.
For a bounded region with suitable boundary, define the integral over as the integral of over . This accommodates regions described by inequalities; sufficiently regular boundaries have area zero, so changing values only on the boundary does not alter the integral. The integral of over gives its area. For , is the volume under the graph above .
Theorem
Fubini and slicing
If is continuous on a rectangle , then
For continuous on a regular region bounded by continuous functions, the first formula becomes
The analogous horizontal-slice formula applies when is described by , .
The inner differential is integrated first. Its bounds may depend on variables held fixed, while the outer bounds are constants in this two-variable setup. A region may need splitting into pieces before one description is valid. These convenient sufficient assumptions do not cover every possible integrable function or irregular region.
Proof
Why slicing is natural
For a rectangle, group the two-dimensional Riemann sums by vertical columns. Within each column, the inner sum approximates the integral in for a fixed , and the remaining sum approximates the outer integral. Continuity on the compact rectangle supplies the uniform control needed for the limiting argument. For a simple region, integrate the indicator-extended function over a rectangle; slices outside the lower and upper boundaries contribute zero. This explains the formulas; the theorem supplies the full convergence justification.
Worked example
Draw the region before computing
Let be between and for . For ,
Horizontal slices have and , so the same integral is . The inequalities reverse roles; simply exchanging the differentials without changing the bounds changes the region.
Worked example
Switch order to make an integral elementary
Consider . The inner antiderivative is not elementary. The region is , so
The order change follows from continuity and the correct region description, not a formal interchange of symbols.
Let with . A grid consists of partitions of each coordinate interval. Its cells are closed subrectangles with disjoint interiors. For bounded , let be its infimum and supremum on cell , of area . Define and .
1. The definition and its useful criterion
Refining a grid raises lower sums and lowers upper sums. Given any two grids, their common refinement proves every lower sum is at most every upper sum. Thus the lower integral is at most the upper integral , and both are finite by boundedness. The function is Riemann integrable when these numbers agree, with common value .
Theorem: rectangular Darboux criterion
The bounded function is integrable if and only if for every some grid has .
Proof. If both integrals equal , choose a lower sum above and an upper sum below , then refine both grids. The new gap is below epsilon. Conversely any such grid bounds . Arbitrarily small gaps force equality. The proof is the supremum argument in two dimensions, not an assumption of Fubini's theorem.
Theorem: continuity implies proper integrability
If is continuous on , it is bounded and uniformly continuous there. Write . Choose a distance scale making output differences less than . A sufficiently fine grid has every cell diameter smaller than that scale, so each oscillation is at most . Therefore , proving integrability.
For any tags , the corresponding finite sum lies between the grid's lower and upper sums. Thus whenever the grid gap is small, its tagged approximation is close to the integral. This statement is a consequence of the definition, not a new limiting convention.
2. Prove the continuous rectangle Fubini theorem
Theorem
For continuous on ,
First, the iterated integrals exist. Each one-variable slice is continuous and integrable. Let . Uniform continuity of gives
Hence is continuous and integrable. The reversed inner-integral function is continuous by the same argument.
Next, squeeze them between the two-dimensional sums. On every cell, . For a fixed in its th strip, integrate these bounds over each interval and add:
Integrate over that strip and sum over . The result is . The double integral lies between the same bounds. Grids with arbitrarily small gap therefore force equality. Repeating with coordinates reversed proves the second equality. No order of an unproved infinite double sum was exchanged; only finite sums, ordinary integral inequalities and the Darboux criterion were used.
A separable continuous integrand consequently has integral . This is an integration identity under the stated hypotheses, not a claim about probabilistic independence in an unspecified experiment.
3. Why ordinary curved boundaries do not destroy proper integrability
Let with continuous , and let be continuous on . This is a compact set. Choose a bounding rectangle with . The clamping map
is continuous, maps into and fixes every point of . Consequently is a continuous extension to . In the estimates below write for this extension. Now set it to zero outside within . This zero extension may jump across the boundary, so one cannot cite continuity everywhere.
Instead control boundary cells. In a vertical grid strip, uniform continuity makes the oscillation of either boundary graph as small as desired. The cells meeting that graph can be covered by a rectangle whose height is at most that oscillation plus two vertical mesh widths. Summing strip widths shows the total area of these graph-boundary cells tends to zero as both mesh widths tend to zero. The two vertical end boundaries can likewise be covered by strips of arbitrarily small total area.
If , boundary cells contribute at most times their total area to the upper-lower gap. Cells away from the boundary lie wholly inside or wholly outside the region; inside, uniform continuity of makes their oscillations small, and outside the function is zero. Choose the boundary area small first and then the ordinary cell oscillation small. The total gap becomes arbitrarily small, proving integrability of the zero extension and therefore of over .
The same bounds show that its integral is : on each strip, changing the vertical endpoints and the input changes the inner integral by uniformly small amounts, while the vanishing boundary-cell area controls the endpoints. Explicitly, using the bounding rectangle's vertical span ,
so the inner-integral function is continuous, and the finite-strip Darboux squeeze applies after excluding the already controlled boundary cells. This establishes the common continuous-simple-region case. More general region or improper versions require their own hypotheses and are not inferred from this proof.
Properties and method selection
Linearity and additivity over nonoverlapping pieces reduce complicated expressions or regions. If throughout , then ; in particular . For a continuous density , mass is . When , the centroid is .
Use vertical slices when their limits are simpler; use horizontal slices when they simplify the region or inner antiderivative. Split the region only when a single pair of bounds cannot describe all slices. Polar or other changes of variables can simplify circular or transformed regions, but require a Jacobian and a separate change-of-variables theorem; they are not automatic replacements for .
Practice
- Evaluate .
- Reverse the order in and state the region.
- Compute the area between and for .
- A lamina occupies with density . Find its mass and centroid.
Full solutions
- .
- The region is . Horizontal slices give .
- The area is .
- . The first moment in is , and the first moment in is . Therefore .
Synthesis
The integral accumulates a quantity per unit area, while an iterated integral computes the same accumulation slice by slice under suitable hypotheses. Region geometry determines bounds; a reversed order must describe exactly the same set. Later coordinate changes and vector integral theorems build on this accounting of geometry and orientation.