The Fourier orthogonality relation on this angular interval is
Projecting the outer boundary condition onto each angular eigenfunction gives
The solution is unique in the class of bounded harmonic functions with the prescribed boundary trace. For continuous boundary data, the difference of two solutions is zero on the boundary and bounded at the vertex, so the maximum principle for harmonic functions makes it zero throughout the sector. Equivalently all its Fourier sine series coefficients vanish. The usual convergence interpretation applies if the data are only piecewise smooth.
For separation of variables, take and divide the reaction-diffusion equation by this product wherever it is nonzero:
Each spatial term depends on a different variable and must be constant. Write and similarly for the other two factors. The Dirichlet boundary conditions give . A zero separation constant permits only a linear function and hence the zero solution; a positive value of likewise permits no nonzero function vanishing at both endpoints. The nontrivial choices are therefore
The temporal ordinary differential equation is
so, absorbing its constant multiplier into ,
The superposition principle and completeness of the Fourier sine series give the stated threefold expansion with these factors. For an initial density , orthogonality also determines the constants:
The separation of variables solution with Dirichlet boundary conditions on the cuboid is
The constants are fixed by the initial density through Fourier sine series. The fastest term again has . When , its growth rate becomes
Thus the precise condition for no exponentially growing term is
For example, gives , while gives : either a sufficiently flat or a sufficiently elongated cuboid suppresses growth despite its unchanged volume. The function decreases to its minimum at , then increases without bound. Hence there are two positive threshold values, with growth only between them; equality leaves one stationary term and all other terms decaying.
Write the equation as with the positive Sturm-Liouville operator from part (a). A Sturm-Liouville eigenfunction expansion therefore gives , where weighted orthogonal projection gives
Here the product-to-sum formulas reduce the integral to half the sum of the integrals of and . Consequently
At , use the continuous limits of the terms. The coefficients are , so the resulting endpoint series converges. Completeness is the ordinary Fourier sine series completeness after . For an independent check, solving with zero endpoint values gives
Its numerator vanishes at zero, and it has the same orthogonal projection coefficients. Positivity of proves uniqueness.
Use the Euler-Bernoulli beam equation for a uniform slender elastic beam, small deflection and small slope, neglecting axial tension, shear deformation, rotational inertia of a cross-section and damping. Let be Young's modulus, the second moment of area about the neutral axis, and the mass per unit length. If density instead denotes mass per volume, replace this by . The bending stiffness is ; the small-slope curvature is . The bending and kinetic energies are
Twice integrating the variation of by parts gives the restoring load per unit length. Newton's second law therefore gives
At a pivot, displacement is fixed but slope is free; zero end bending moment gives . This also follows from the natural boundary term in the variation.
With separation of variables, gives
Choose the time normalization . Initial rest removes the sine time term, so . The spatial characteristic roots are , giving
The two conditions at give and , hence . At , addition and subtraction of give and . Nontrivial positive-frequency modes therefore have and . Thus the simply supported beam normal modes are
The zero-frequency cubic solution also vanishes under these four endpoint conditions, so is not an additional mode.
For the specified release, small slope requires . Expand the initial deflection in the Fourier sine series. Its coefficients are
Writing , the resulting motion is
Only odd normal modes occur because the initial profile is symmetric about the midpoint, and their amplitudes decrease as . The frequencies grow as , so the motion is dispersive and is not a single shape multiplied by one cosine. Nevertheless the ideal undamped solution is exactly periodic with period . At all odd-mode cosines vanish, so the bar is instantaneously straight; at it has the opposite initial deflection. The first mode dominates displacement, with third-mode amplitude only of the first.
There is initial curvature incompatibility at a moment-free beam end: the prescribed parabola has , whereas a moment-free pivot requires zero curvature at an endpoint. Therefore the data do not define a classical solution with curvature continuous through the two end-time corners. They do define a finite-energy weak solution after release of the forces or end moments that prepared the initial shape. The sine expansion represents that solution: its displacement reproduces the initial parabola, each mode satisfies the released endpoint conditions, and gives finite bending energy. One must not differentiate the initial series twice at its endpoints and assign the interior parabola's curvature there. This qualification leaves the modal displacement prediction intact.
Figure 1.
Original modal evolution after releasing a parabolic elastic beam deflection
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The sine functions obey . The Parseval identity for the Fourier sine series gives
Consequently
The extremal equation is . For , its general solution is . The left endpoint forces , while the right endpoint and require . Therefore
In particular, each extremal has the requested Fourier sine series form . More strongly, for an individual extremal only the coefficient at can be nonzero. An arbitrary combination of distinct modes is an admissible function, but does not solve this one-eigenvalue equation.
An energy measurement selects the ground state with probability equal to the squared inner product with . Using and integration by parts,
Thus
The full Fourier sine series has , so , an independent wavefunction normalization check. However for every , hence diverges. This explicitly verifies the infinite-energy expectation qualification in part (b), without invalidating the individual projection probabilities.
The heat equation and its homogeneous Dirichlet boundary conditions are linear, so superposition of the separated modes gives
The Fourier sine basis represents the initial profile on the interior of the interval. At its Fourier sine series must equal . Multiplying by , integrating from to , and using orthogonality gives
Therefore the required Fourier sine coefficients are
For every , the exponential factors ensure convergence of the differentiated series, and every term satisfies the partial differential equation and the boundary conditions. The Fourier sine series recovers the smooth initial profile at every as .
The scan explicitly prints on ; it must not silently become . For , the interior profile tends to at the right endpoint, whereas the prescribed boundary condition is zero for . The solution is therefore not continuous at the corner , although it satisfies every condition on the printed open ranges. A solution continuous on the closed space-time domain with these data would require .[ref]
For the Fourier sine series write . Orthogonality of trigonometric functions gives
In the second half of the integral put ; then and . Hence
Every even coefficient is zero. For odd , part (a) or the supplied integral yields
Putting therefore gives
This is the Fourier sine series of a symmetric tent. The absolute values of its terms are uniformly bounded by a summable sequence, giving absolute convergence and uniform convergence; the piecewise smooth odd extension and the Dirichlet convergence theorem for Fourier series identify its value with the continuous , including the zero endpoints and the peak.
The printed lower limit is an error. The original PDF visibly has this lower limit. It omits the nonzero fundamental coefficient . In particular, the printed series equals , rather than . At it gives instead of . The corrected lower limit is displayed explicitly above.
Apply separation of variables to each mode of the damped wave equation , assuming . The spatial ordinary differential equation is . Its general solution is . The boundary condition at gives ; a nonzero mode at requires
Only odd occur in the initial Fourier sine series. Put and . The temporal equation has roots . Define
For distinct roots, let the full amplitude be . The initial displacement and zero initial velocity impose and . Solving gives
Thus the physically consistent superposition is
For there is overdamping, with two real decaying exponentials. For there is underdamping; set ; the equivalent real expression is
At critical damping, the repeated-root case , take the limit, giving . These formulas all satisfy and .
Three source qualifications matter. First, the sum must start at , for the same reason as in (b). Second, the printed cannot hold for a single separated mode: the tent has on each open linear segment but , contradicting for positive , and its peak is not twice differentiable. Separation applies mode by mode, with the initial tent recovered by superposition. Third, no finite “large” makes every mode overdamped, because . The two-exponential expression permits complex conjugate roots, while a repeated root requires its displayed limiting form. The tent initial data are naturally interpreted through the convergent modal solution, rather than as a single smooth separated product.
Substitute the proposed Fourier sine series into the heat equation:
Projecting onto each sine using orthogonality gives for every mode with . The initial condition fixes , since already describes the initial amplitude. Hence
For a mode with , the value of is immaterial and the same convention is convenient. The positive thermal diffusivity damps every mode, with higher frequencies decaying faster. For square-integrable initial data the damping justifies termwise differentiation for and recovery of the initial data in L2 norm convergence as .
The left panel illustrates the Fourier series in part (b). The right panel is a self-generated example with and , showing the two normal modes decaying at rates and .
A Fourier sine series automatically meets the zero-temperature boundary conditions because . Equivalently, extend oddly from to and then periodically with period . Its Fourier series has only sine terms, with
The coefficient formula follows from the orthogonality identity
For piecewise smooth initial data the series equals at interior continuity points and the average of its one-sided values at interior jumps. More general square-integrable data have convergence in L2 norm convergence. A classical solution continuous at the initial corners additionally requires , in agreement with the prescribed boundary conditions.
The reference to part “(c)(i)” in the source is circular; the relevant modes are those verified in part (b)(i). Linearity of the heat equation and its homogeneous Dirichlet boundary conditions allows superposition of those modes:
Match the initial uniform interior temperature using the orthogonality of the Fourier sine series:
Thus for even integers and for odd integers , giving
For every , the exponential factor makes the series and the derivatives needed in the heat equation converge uniformly on later time intervals. At , the Fourier sine series equals at interior points but zero at the endpoints: the instantaneous cooling boundary condition is incompatible with the pre-immersion endpoint values. This corner mismatch is physically the idealization of an instantaneous bath contact and does not invalidate the solution for .
Figure 1.
Cooling profiles in a zero-temperature bath and the mean temperature retained after insulation
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For nonnegative nonzero integrable initial data on , the first coefficient in the normalized Fourier sine series is strictly positive, because the first sine eigenfunction is positive throughout the interval. For with zero Dirichlet boundary conditions, the first decay rate is . Every higher rate exceeds it by , so smoothing for positive time and the spectral gap imply uniformly. Thus all interior points share the growth/decay threshold ; the endpoints remain zero. At equality the limiting profile is nonzero and stationary.
For the radial Laplace operator on , require a finite value at the origin and . The map preserves the norm from to and sends to . The regular endpoint condition becomes . The self-adjoint realization therefore corresponds to the ordinary Dirichlet boundary conditions for the one-dimensional second derivative. Its eigenvalues and eigenfunctions are displayed above, with understood by a limit. Their squared weighted norm is . Completeness and orthogonality follow from the Fourier sine series on .
On , integration by parts gives the displayed Fourier sine series. For normalized Dirichlet eigenfunctions , indexed from , it has the form , with and . Its Rayleigh quotient for is , since and . Reflection symmetry forces , because that first excited eigenfunction is antisymmetric about . Thus the first excited state's contribution to the error is exactly zero; the first nonzero correction is .
For with zero vertical-side values on , the Fourier coefficient obeys the Cauchy-Euler differential equation . Boundedness at removes the negative indicial root, leaving . Bounded top coefficients give absolute convergence of the Fourier sine series below the top boundary.
On a shell with homogeneous Dirichlet boundary conditions, put and . The radial heat equation in three dimensions becomes , with zero values at both endpoints. Expanding in a Fourier sine series gives the displayed solution, with . Each radial mode decays at the square of its wave number. The positive inner radius makes division by harmless throughout the shell.
Stress-free convection growth-rate polynomial Created 2026-10-06 Updated 2026-11-05
For a fixed-temperature layer with stress-free boundary conditions, a vertical Fourier sine series has , where is horizontal wavenumber. The coupled vertical velocity and temperature amplitudes satisfy the displayed quadratic for their growth rate . Its roots are real for positive Rayleigh number, while both roots have negative real parts for negative Rayleigh number. Setting gives the free-slip convection neutral curve.