The annulus is in polar coordinates. Their Jacobian determinant supplies , so
The original double integral covers the triangle . By Fubini's theorem, after reversing the order, runs from to and from to . Since a continuous function is integrable on this bounded region,
For the square pyramid, a horizontal section at height is a square of side : each vertex moves linearly from the base towards . Hence its cross-sectional area is , and its volume is . To use the identity just proved, choose :
Start with the solid between the elliptic paraboloid and the upper plane . Its projection is the disk
since their vertical separation is . The second lower bound, , removes the part between the elliptic paraboloid and this lower plane wherever
Call this second disk . Its centre is distance from the centre of , and
because . Thus lies wholly inside . In particular the lower plane never exceeds the upper plane on , so the subtraction describes exactly the requested solid.
Figure 1.
Nested projections of the upper and lower planar faces in Question 3(c)
. The blue disk has centre and radius ; the orange disk has centre and radius . Over the lower plane replaces the elliptic paraboloid as the bottom of the solid. Details.
The nested-disk subtraction for paraboloid volumes therefore gives a difference of two double integrals:
Translate polar coordinates to the centre of each disk. A general integral of this form is
Using and gives

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