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Disc integration
Disc integration
from Wikipedia

Disc integration, also known in integral calculus as the disc method, is a method for calculating the volume of a solid of revolution of a solid-state material when integrating along an axis "parallel" to the axis of revolution. This method models the resulting three-dimensional shape as a stack of an infinite number of discs of varying radius and infinitesimal thickness. It is also possible to use the same principles with rings instead of discs (the "washer method") to obtain hollow solids of revolution. This is in contrast to shell integration, which integrates along an axis perpendicular to the axis of revolution.

Definition

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Function of x

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If the function to be revolved is a function of x, the following integral represents the volume of the solid of revolution:

where R(x) is the distance between the function and the axis of rotation. This works only if the axis of rotation is horizontal (example: y = 3 or some other constant).

Function of y

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If the function to be revolved is a function of y, the following integral will obtain the volume of the solid of revolution:

where R(y) is the distance between the function and the axis of rotation. This works only if the axis of rotation is vertical (example: x = 4 or some other constant).

Washer method

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To obtain a hollow solid of revolution (the “washer method”), the procedure would be to take the volume of the inner solid of revolution and subtract it from the volume of the outer solid of revolution. This can be calculated in a single integral similar to the following:

where RO(x) is the function that is furthest from the axis of rotation and RI(x) is the function that is closest to the axis of rotation. For example, the next figure shows the rotation along the x-axis of the red "leaf" enclosed between the square-root and quadratic curves:

Rotation about x-axis

The volume of this solid is:

One should take caution not to evaluate the square of the difference of the two functions, but to evaluate the difference of the squares of the two functions.

(This formula only works for revolutions about the x-axis.)

To rotate about any horizontal axis, simply subtract from that axis from each formula. If h is the value of a horizontal axis, then the volume equals

For example, to rotate the region between y = −2x + x2 and y = x along the axis y = 4, one would integrate as follows:

The bounds of integration are the zeros of the first equation minus the second. Note that when integrating along an axis other than the x, the graph of the function which is furthest from the axis of rotation may not be obvious. In the previous example, even though the graph of y = x is, with respect to the x-axis, further up than the graph of y = −2x + x2, with respect to the axis of rotation the function y = x is the inner function: its graph is closer to y = 4 or the equation of the axis of rotation in the example.

The same idea can be applied to both the y-axis and any other vertical axis. One simply must solve each equation for x before one inserts them into the integration formula.

See also

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References

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from Grokipedia
Disc integration, commonly referred to as the disk method, is a fundamental technique in integral calculus for determining of a formed by rotating a bounded by a continuous, nonnegative function, an axis, and two vertical or horizontal lines around a fixed axis, such as the x-axis or y-axis. This method approximates the solid's volume by integrating the cross-sectional areas of thin circular disks perpendicular to the , where each disk's is the from the axis to the curve defining the . The disk method relies on the principle that the volume can be found by summing the volumes of infinitesimally thin disks, with the area of each disk given by πr2\pi r^2, where rr is the radius function. For rotation about the x-axis, if the region is bounded by y=f(x)y = f(x), the x-axis, x=ax = a, and x=bx = b, the volume VV is calculated as V=πab[f(x)]2dxV = \pi \int_a^b [f(x)]^2 \, dx. Similarly, for rotation about the y-axis, with the region bounded by x=g(y)x = g(y), the y-axis, y=cy = c, and y=dy = d, the formula becomes V=πcd[g(y)]2dyV = \pi \int_c^d [g(y)]^2 \, dy. This approach assumes the solid has no internal cavities; when a cavity is present, the method extends to the washer method by subtracting the inner disk volume from the outer. The disk method is particularly useful for regions where the axis of rotation aligns with the variable of integration, providing an efficient alternative to other techniques like cylindrical shells.

Introduction

Overview

Disc integration, also known as the disk method, is a fundamental technique in integral calculus for calculating the volume of solids of revolution generated by rotating a region bounded by a continuous function around an axis. This method approximates the solid's volume by summing the volumes of infinitesimally thin cylindrical disks, whose areas are integrated over the interval of rotation to yield the exact total volume via a definite integral. The process relies on the geometry of rotation: when a plane region under a curve is revolved around an axis, the resulting solid features circular cross-sections perpendicular to that axis, each forming a disk with radius determined by the distance from the axis to the curve. These cross-sections are stacked along the axis, and their infinitesimal volumes π[R(x)]2dx\pi [R(x)]^2 \, dx accumulate to form the solid. The general formula for the volume VV is V=πab[R(x)]2dx,V = \pi \int_a^b [R(x)]^2 \, dx, where R(x)R(x) represents the function, and the integration limits aa to bb span the bounded interval along the axis. This approach assumes the is continuous, the region is bounded, and rotation occurs around a fixed axis external to or along the boundary of the region.

Historical Context

The origins of disc integration lie in the 17th-century contributions of Italian mathematician , who developed the method of indivisibles as a precursor to integral calculus for approximating areas and volumes. In his seminal work Geometria indivisibilibus continuorum (1635), Cavalieri applied this approach to solids of revolution, such as , , and spheroids generated by rotating conic sections around an axis, by summing collections of planar elements—effectively thin disks—to determine volume ratios, like that of a cone to a cylinder as 1:3. This technique prefigured the disk method by conceptualizing volumes as aggregates of similar cross-sections without invoking explicit limits or infinitesimals. The method gained rigor through the independent invention of integral calculus by and in the late 1660s and 1670s. Newton's fluxional calculus, outlined in his unpublished De Analysi (1669) and later works, treated integration as the inverse of differentiation to compute fluents like volumes under curves, directly applicable to revolving regions around an axis to form solids. Similarly, Leibniz's 1675 development of the sum (∫) notation enabled precise summation of cross-sectional areas πy² dx for volumes of revolution, as published in his 1686 paper on integral calculus. Their fundamental theorem linking differentiation and integration provided the theoretical foundation for disc integration as a systematic tool. Leonhard Euler advanced these ideas in the , integrating them into a cohesive framework in his (1748) and the multi-volume Institutionum calculi integralis (1768–1794). Euler explicitly used definite integrals to derive volumes of solids of revolution, such as spheres and paraboloids, by revolving curves and summing disk-like elements, while clarifying notation and extending applications to more complex geometric forms. His treatises emphasized the method's versatility, establishing it as a core component of analytical geometry. In the , refinements continued. A key milestone came with William Thomson (later ) and Peter Guthrie Tait's Treatise on Natural Philosophy (1867), which incorporated disc integration into , demonstrating its use for modeling rotational solids in and through illustrative examples. By the early , disc integration had evolved into a standard topic in textbooks, with concise presentations in works like William F. Osgood's A First Course in the Differential and Integral Calculus (revised edition, 1914).

Mathematical Prerequisites

Solids of Revolution

A solid of revolution is a three-dimensional geometric figure generated by rotating a two-dimensional region bounded by a curve, such as y=f(x)y = f(x) or x=g(y)x = g(y), and the coordinate axes around a fixed axis, typically the x-axis or y-axis. This rotation sweeps out the region to form a solid whose shape depends on the original curve and the axis of rotation. Solids of revolution can be classified by the extent of and the presence of internal voids. A full , typically 360 degrees, produces complete symmetric shapes like spheres from semicircles or tori from circles offset from the axis, while partial rotations yield incomplete forms such as spherical caps. Simple solids lack holes and form when the rotated region touches the axis, resulting in filled interiors; those with holes arise when the region is separated from the axis, creating annular voids akin to a . To visualize these solids, consider cross-sections taken perpendicular to the axis of rotation, which appear as circles for simple solids or annuli (ring-shaped regions) for those with holes. These circular slices highlight the radial inherent in the rotation process. A key non-integral method for computing volumes of such solids is , which states that the volume equals the product of the region's area and the distance traveled by its during rotation. Specifically, for rotation around an external axis, the volume V=2πrˉAV = 2\pi \bar{r} A, where AA is the area and rˉ\bar{r} is the distance from the to the axis. This theorem provides an alternative to integration-based approaches by leveraging geometric properties of the .

Basic Integration Review

The definite represents the net signed area under the curve of a f(x)f(x) over the interval [a,b][a, b], denoted as abf(x)dx\int_a^b f(x) \, dx. When f(x)0f(x) \geq 0 on [a,b][a, b], this computes the exact area between the curve and the x-axis; for regions where f(x)f(x) changes sign, positive and negative areas are added algebraically. This foundational concept extends the notion of area from simple geometric shapes to more complex curves, providing a limit-based measure that approximates the region with increasingly fine partitions. Riemann sums form the basis for defining the definite by approximating the area under the curve through finite sums of rectangular areas. For a partition of [a,b][a, b] into nn subintervals of width Δx=(ba)/n\Delta x = (b - a)/n, the Riemann sum is i=1nf(xi)Δx\sum_{i=1}^n f(x_i^*) \Delta x, where xix_i^* is a sample point in the ii-th subinterval (such as the left endpoint, right endpoint, or ). As nn \to \infty and Δx0\Delta x \to 0, the limit of these sums converges to the definite abf(x)dx\int_a^b f(x) \, dx, enabling volume approximations in higher dimensions by integrating cross-sectional areas. This process ensures the integral captures the precise accumulation, regardless of the choice of sample points for Riemann-integrable functions. Finding antiderivatives, or indefinite integrals, is essential for evaluating definite integrals via the , with basic rules tailored to polynomial-like functions common in radius expressions. The power rule states that for n1n \neq -1, xndx=xn+1n+1+C\int x^n \, dx = \frac{x^{n+1}}{n+1} + C, directly applicable to terms like squared distances where exponents are even integers greater than or equal to 2. Integration by substitution reverses the chain rule: for composites of the form f(g(x))g(x)f(g(x)) g'(x), set u=g(x)u = g(x) so du=g(x)dxdu = g'(x) \, dx, transforming f(g(x))g(x)dx\int f(g(x)) g'(x) \, dx into f(u)du\int f(u) \, du, which is then integrated and substituted back. These techniques simplify expressions involving powers or compositions, such as those arising from radial functions in rotated solids. A common pitfall in integration arises with over unbounded regions or discontinuous functions, requiring limits to assess convergence. For instance, an like af(x)dx\int_a^\infty f(x) \, dx is defined as limbabf(x)dx\lim_{b \to \infty} \int_a^b f(x) \, dx; if the limit exists and is finite, the improper integral converges to that value, but occurs otherwise, potentially leading to infinite volumes in unbounded solids of revolution. Similarly, integrals with discontinuities inside [a,b][a, b] split at the point of issue and evaluate limits from both sides. Failing to recognize these cases can yield misleading finite results for inherently divergent accumulations.

Core Methods

Disc Method for X-Axis Rotation

The disc method for x-axis rotation applies to finding the volume of a solid formed by revolving a region bounded by the curve y=f(x)y = f(x), the x-axis, and the vertical lines x=ax = a and x=bx = b (where f(x)0f(x) \geq 0) around the x-axis. This generates a solid of revolution composed of stacked circular discs perpendicular to the x-axis, with each disc's radius equal to the function value f(x)f(x) at that point. The derivation begins by considering thin rectangular strips of width Δx\Delta x along the x-axis, from xx to x+Δxx + \Delta x. Revolving the region in this strip around the x-axis generates a thin disk with radius f(x)f(x) and thickness Δx\Delta x. The volume of this disk is ΔV=π[f(x)]2Δx\Delta V = \pi [f(x)]^2 \Delta x. Summing these volumes over the interval using Riemann sums and taking the limit as Δx0\Delta x \to 0 yields the definite integral for the total volume: V=πab[f(x)]2dx.V = \pi \int_a^b [f(x)]^2 \, dx. This formula represents the integral of the cross-sectional area A(x)=π[f(x)]2A(x) = \pi [f(x)]^2 along the axis of rotation. To apply the method, first identify the bounds aa and bb as the x-intercepts or specified limits of the . The radius of each disc is simply the y-value f(x)f(x), and no is needed since the region touches the axis of rotation. Substitute into the integral formula and evaluate using standard techniques such as computation or substitution. A classic example is computing of a of rr, obtained by rotating the y=r2x2y = \sqrt{r^2 - x^2}
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