The theorem on pointwise convergence of a piecewise smooth Fourier series gives the average of the two one-sided values of the corresponding periodic extension. Under the usual piecewise smooth interpretation of the paper's derivative assumption, the even extension is continuous at and at the joined endpoints . Thus
For the odd extension, the values on either side of zero are and ; those on either side of are and . Therefore
The endpoint values are also immediate because each sine term vanishes there. If or is nonzero, the Fourier sine series does not reproduce that endpoint value. Merely assuming that the derivative is locally piecewise continuous in the open interval would be weaker than the usual piecewise smooth hypothesis; the convergence assertion uses the standard endpoint regularity implicit in that hypothesis.
The Fourier cosine series and Fourier sine series use the respective forms
Their Fourier coefficients, obtained from Fourier orthogonality, are
In particular the constant term is . The Fourier cosine series is the Fourier series of the even extension , made -periodic. The Fourier sine series is the Fourier series of the odd extension, equal to for and for , again made -periodic.
Choose the scalar field
The allowed vector-valued Stokes identity gives
Every boundary point lies on the unit circle in the -plane, so throughout the boundary. Since the line integral of around a closed curve is the zero displacement,
Only the boundary value of this scalar field mattered: the interior of the surface need not be part of a sphere. Either consistent choice of orientation gives the same zero answer.
Use the outward orientation on the unit hemisphere and counterclockwise boundary orientation on the unit circle. With and , the vector line integral is
For the surface integral, and the outward unit normal vector is , since the radius is one. The cross product is
The integral of is zero by reflection symmetry. Using the same spherical polar coordinates as in ii, with , the other component is
Hence
verifying the vector-valued Stokes identity directly, component by component. The wedge symbol in the paper denotes the cross product here.
Choose the outward unit normal vector on the upper hemisphere. The curl of is
In spherical polar coordinates, put
Here and . The surface integral is therefore
The compatible boundary orientation follows increasing in , . On this circle,
Thus the line integral is
which agrees with the surface integral as required by the Stokes theorem.
Let be a compact, piecewise smooth oriented surface with piecewise smooth boundary, and let be continuously differentiable on an open neighbourhood of . The Stokes theorem states
The boundary orientation must agree with the chosen unit normal vector by the right-hand rule. For an upward orientation on a horizontal disk, its boundary is traversed counterclockwise when viewed from above. Reversing the orientation reverses both the line integral and the surface integral.
For each of the three constant Cartesian unit vectors , apply the divergence theorem to the vector field . Its divergence is , so
These are precisely the three components of
Thus the volume integral of the gradient is the boundary surface integral weighted by the vector surface element . The regularity needed here is that be continuously differentiable on a neighbourhood of the closure of .
One sufficient version of the divergence theorem is the following. Let be a bounded region in with a closed, piecewise smooth surface as its boundary, and let be a continuously differentiable function with values in on an open neighbourhood of the closure of . With the outward unit normal vector,
The boundary surface integral is the total outward flux integral. If the boundary has several components, each has the outward orientation relative to the material of ; inner components therefore point into the holes. Edges and isolated vertices may be omitted when assigning the unit normal vector, since they have zero surface area.
Write the centroid as . The region has reflection symmetry in the -axis: replacing by changes to and preserves and . Thus symmetry in integration gives
For the other first moment of area, use in polar coordinates:
Here the last integral has the value allowed in the paper. Dividing the first moment of area by the area found in i gives
The positive vertical coordinate agrees with the fact that the entire region lies above the -axis.
Use polar coordinates with and . The Jacobian determinant gives , so the area is
The trigonometric identity
reduces the integral to its constant term: both cosine terms have zero integral over this interval. Therefore
Assume . The velocity in polar coordinates is . Hence
Taking the dot product of the conserved Laplace-Runge-Lenz vector with gives
Consequently the polar equation of a conic is
Only angles for which the denominator is positive describe the physical trajectory. Its eccentricity is , giving an ellipse, parabola, or hyperbola when this ratio is respectively less than, equal to, or greater than .
If , the angle is undefined, but the same dot product identity gives the circular orbit . If , the trajectory is radial and the displayed division degenerates; for , and on a fixed ray, so the identity does not determine as a function of a varying angle.
With , a gives constant , and the polar coordinates basis satisfies , . Also . Differentiating the proposed Laplace-Runge-Lenz vector therefore gives
For this to vanish for arbitrary , including nonzero , the central force must satisfy
Attraction requires . The condition “for any value of ” matters: with alone, the Laplace-Runge-Lenz vector is constant on each radial ray for any central force, so that special case would not determine the force law.
Let . It is a symmetric matrix, and . By the spectral theorem for real symmetric matrices, choose an orthonormal basis of eigenvectors of , with nonnegative eigenvalues .
For each , take the unit parallelogram parametrized by , . Its surface area is . Moreover,
The image parallelogram consequently has area . By the assumption this equals for all three pairs, giving
No eigenvalue can be zero. Dividing the equations and using positivity yields . Hence
Thus testing all surfaces is stronger than necessary: the three unit parallelograms in these principal directions already determine the result. This is the three-dimensional characterization of linear surface-area isometries.
Let parametrize . Then parametrizes its image, with tangent vectors and . An orthogonal matrix preserves dot products, so the Lagrange identity for the cross product gives, for any ,
The area element of a surface is therefore the same pointwise before and after applying . Integrating proves
This includes orthogonal transformations with determinant : reversal of orientation does not affect the Euclidean norm in the surface area formula.
The endpoint radii are and , but substituting those two numbers in the finite conical frustum formula is invalid. A rotation about the -axis preserves the horizontal angle between the endpoint position vectors; here and are not parallel. The radius along the generating segment is not linear in height.
Parametrize the actual segment by
Its rotated circle at height has radius
Thus the rotated image is the surface of revolution . Applying the conical frustum formula to infinitesimal pieces of this radial profile, or directly using the cross product as in ii, gives the surface area of a surface of revolution
To evaluate it explicitly, put . Then . Define
The chain rule gives , so the answer is
The positive logarithm arguments make this a real-valued expression. Rotating the segment's endpoints independently into one vertical plane before joining them would instead create a different surface, with surface area .
Figure 1.
The rotated segment has a curved radial profile, although its three-dimensional generator is straight.
Details.
For the parametrized surface in i,
These tangent vectors are orthogonal, and their Euclidean norms are and , respectively. Their cross product therefore has Euclidean norm . Integration gives
This is the lateral surface area of a conical frustum, with no end disks included.
Interpolate the radius and height by
A parametrized surface for the conical frustum is
The strict positivity of gives . Since , the height identifies uniquely; the angle then identifies a point of each circle uniquely modulo . Hence this covers the lateral surface of revolution once. If , it is the lateral surface of a circular cylinder.
Represent the quadratic form by the symmetric matrix
The spectral theorem for real symmetric matrices gives an orthogonal matrix and real eigenvalues such that . In the orthogonal change of coordinates , the equation becomes .
If both eigenvalues are positive, this is an ellipse with semiaxes and . Conversely, a zero eigenvalue makes the set either empty or unbounded along that coordinate, while two negative eigenvalues give the empty set. Opposite signs give an unbounded hyperbola. A negative eigenvalue together with a zero one also gives the empty set. None of those cases is an ellipse. Therefore the exact condition is that be a symmetric positive-definite matrix.
The sum and product of its eigenvalues are its matrix trace and determinant:
Two real numbers are both positive precisely when their sum and product are positive. Thus
An orthogonal transformation preserves area. Using i gives the quadratic-form ellipse area
The altitude of a triangle through has equation , and the altitude of a triangle through has equation . Their normal vectors and are linearly independent because the triangle is nondegenerate. Consequently these two lines meet in exactly one point .
Substitute its position vector in the supplied identity. Its first term vanishes by the first altitude of a triangle equation, and its second term vanishes by the second altitude of a triangle equation. Hence
This is exactly the condition that lies on the altitude of a triangle through . The three lines therefore meet in a unique point, the orthocenter. This argument includes right triangles and triangles whose orthocenter lies outside them.

Pinned article: Introduction to the OurBigBook Project

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