Accumulation in space
For a continuous density on a suitable bounded solid , its mass is . For constant density one, the integral is the volume. Iterated integration slices the solid successively, provided the bounds actually describe ; Fubini's theorem applies under standard continuity and regularity assumptions.
Worked example
A tetrahedral solid
Let . The bounds , , give
The inner upper bound is the plane expressed as ; projecting onto the -plane gives the triangular outer bounds.
Cylindrical and spherical coordinates
Definition
Coordinate conventions and volume elements
Cylindrical coordinates use , , with and . Spherical coordinates here use
where , is the angle from the positive -axis and is azimuth. The volume element is . Other sources may exchange names of the two angles; check definitions before using a formula.
Proof
Why the spherical factor is
Differentiate the position vector with respect to . The absolute value of their scalar triple product is for . The three-dimensional change-of-variables theorem then supplies the volume element; coordinate singularities on the axis and at the origin are negligible in standard solid integrations.
Worked example
A sphere above a cone
Let be inside and above the cone . In spherical coordinates this is , , . Hence
The cone fixes an angle, and the sphere fixes a radius. Those geometric observations determine bounds before any integration.
Worked example
Cylindrical shells
For the solid , , use , , :
2. Derive spherical scale before using radial symmetry
Use coordinates
where is measured from the positive axis, , and is azimuth over one full turn. The derivative vectors have lengths and are mutually perpendicular with the corresponding positive orientation on the interior. Their scalar triple product is , giving
To verify the determinant explicitly, the derivative columns in the order are
Their triple product is when and . On the open parameter domain the map is one-to-one onto its slit image, with smooth inverse , and the usual smooth slit-plane azimuth. Thus the proved finite-dimensional change-of-variables theorem applies to every compact truncated parameter box inside that domain.
The omitted target regions also need estimates independent of the formula we are proving. The ball of radius is in a cube of volume . In a radius- ball, the two polar caps with angle at most from the axis lie in the box , , of volume . An azimuth seam of total angular width , with , lies in , , a box of volume . All three bounds vanish with their cutoff. Multiplying by a bound for the continuous target integrand controls its omitted integral, while the parameter estimates below control the other side. This completes the nonsingular-exhaustion argument without using spherical volume to justify its own formula.
The origin, poles and angular seam are coordinate-boundary exceptions. For bounded continuous integrands on a ball, use nonsingular truncated parameter regions and pass to their limit; the omitted parameter integral bounds tend to zero. For a bounded integrand, the radial factor near zero is bounded by a constant times , while a polar cap has factor and a shrinking azimuth seam has vanishing angle width. The formula is not a license to ignore an arbitrary unbounded singularity at those locations.
Choosing coordinates
Cartesian coordinates suit plane-bounded solids; cylindrical coordinates suit circular cross-sections around an axis; spherical coordinates suit spheres and cones about the origin. Transform the integrand as well as the bounds and include the Jacobian. Angles must cover the intended solid exactly once except for negligible coordinate seams. Triple integration computes signed accumulation if the integrand changes sign; geometric volume uses integrand .
Practice
- Find the volume of the box , , .
- Find the volume of the cylinder , using cylindrical coordinates.
- Find the volume of the ball using spherical coordinates.
- Rewrite and in the spherical convention of this unit.
Full solutions
- Integrate over the box: .
- .
- For , .
- They are and , respectively.
Synthesis
A triple integral is accumulated density over volume. Choose coordinates adapted to the solid, express every boundary and the integrand in those coordinates, and include the appropriate volume factor.