For a separated nonzero solution , substitution and division by gives
The homogeneous Dirichlet boundary conditions impose . For a nonzero spatial factor, integration by parts gives , so the separation value is nonnegative. The zero value gives only a trivial linear under these boundary conditions. The nontrivial separated factors, for , are therefore
For the intended forward diffusion equation, assume . The superposition principle gives a Fourier sine series, whose coefficients must expand the initial ramp in the interior:
Consequently the standard heat-flow solution is
It satisfies both lateral boundary conditions for , and tends to as for , also converging to the ramp in the L2 norm. The exponential coefficient decay justifies differentiating the series for positive .
There is a genuine incompatibility in the printed data: at the lateral condition demands zero while the initial condition demands one. Thus no function satisfies every stated value at that corner. The displayed series solves the usual consistent interpretation with initial data on and lateral data for ; it cannot be continuous at the upper initial corner. This discrepancy is present in the original PDF.
The sign of is also unstated. If , the spatial equation with two zero endpoints forces , incompatible with the ramp. If , the separated Fourier coefficients grow like and fail to be square summable for every ; these data therefore have no forward solution in the standard L2 space class. The positive- assumption is essential to the stated heat-flow interpretation.
Termwise differentiation of a Fourier series, applied to the continuous periodic extension in part (c), gives for
Hence the required Fourier sine series is
The endpoint deserves care: at every term is zero, so the Fourier series sums to , the average of the periodic one-sided limits and . It therefore does not reproduce the specified endpoint value . Changing a value at one point does not change any Fourier coefficient, so this is still the Fourier series of the stated function on .
Evaluate the Fourier sine series of part (d) at the interior point . Only odd indices remain, with alternating signs:
Thus .
For the second identity, apply Parseval's identity to . From part (c), , and , so
The left side is , giving . Consequently
The first series is conditionally convergent, while the second converges absolutely by the P-series criterion.
Steady state. In the heat equation, time independence makes the second spatial derivative zero. The two endpoint temperatures therefore determine the linear profile
Insulation is along the sides; the endpoint reservoirs can still exchange heat with the rod.
Transient solution. Subtract the steady profile before applying separation of variables: let . Then , and for . Writing gives
The homogeneous Dirichlet boundary conditions exclude and select the eigenfunctions with eigenvalues , . Their orthogonality gives the Fourier sine series coefficients
Here integration by parts uses . Thus
Every summand satisfies the heat equation and the homogeneous endpoint conditions, while the steady profile supplies the prescribed endpoint values. The initial Fourier sine series equals in the open interval. At the initially cold rod and the suddenly imposed hot endpoint are incompatible; the formula describes the prescribed data for and the initial limit at interior points.
Heat absorption. Integrating in kills the even modes. With , the total heat relative to the initial state is
Consequently the net rate of heat absorption is
For each , any fixed number of differentiated modes is bounded by a polynomial in times . These bounds have finite sums, proving absolute convergence, uniform convergence on such time intervals and the validity of the integration and differentiation. In particular the displayed rate is finite for every , positive when , and tends to zero as equilibrium is approached. The same answer follows from the heat equation balance ; this subtracts loss at the cold endpoint from input at the hot endpoint.
Multiplication by puts the eigenvalue problem into Sturm-Liouville form, , with weight . If correspond to distinct eigenvalues , subtract their multiplied equations and integrate to get
The upper boundary term vanishes by the Dirichlet boundary condition. For a bounded solution near zero, has a limit because is integrable. A nonzero limit would force a divergence in , so that limit is zero; integration then gives . The lower boundary term therefore also vanishes, proving the weighted orthogonality.
Set . For , , and finiteness of gives . Thus with zero values at zero and . The radial Dirichlet spectrum in three dimensions gives
The zero and negative eigenvalues yield only the zero solution under these boundary conditions. Also .
For the forced equation, the same substitution gives . The Fourier sine series of on has coefficients
Expanding gives , hence
The value at zero is defined by a limit. In fact , so uniform convergence holds even there, by comparison with . An independent check comes from solving the constant-coefficient equation directly:
It satisfies both endpoint conditions and the forcing for , and its finite origin limit agrees with the series. For the homogeneous boundary value problem has no nonzero solution, so the solution is unique.
With constant positive thermal diffusivity , no internal heat source and one spatial coordinate, the heat equation is
Separation of variables makes each spatial mode decay by . The endpoint conditions determine whether the initial triangular profile is expanded in a Fourier sine series or a Fourier cosine series.
Figure 1.
The same triangular initial temperature with cooled and insulated ends
. Original heat-equation solutions for several dimensionless times. Fixed zero-temperature ends cool the bar to zero; insulated ends preserve its initial mean and approach a uniform temperature. Details.
Set in the heat equation. Separation of variables gives . Zero endpoint temperatures impose Dirichlet boundary conditions , selecting for . The separated factors can therefore be chosen as
Zero and negative separation eigenvalues give only the zero spatial solution under these boundary conditions.
The initial profile is continuous and triangular, with midpoint height . Its Fourier sine series coefficients are
Consequently the heat flow from a triangular initial temperature is
For , each summand has magnitude at most . The Weierstrass M-test proves absolute and uniform convergence. The initial Fourier sine series equals the continuous piecewise smooth profile, and for the exponential factors justify termwise spatial and time differentiation on every time interval bounded away from zero.
Figure 1.
Cooling of a bar with a triangular initial temperature profile
. Original normalized solution snapshots, with horizontal coordinate , temperature divided by its initial maximum , and time . Both endpoints remain at zero while the midpoint corner is smoothed. Details.
Separation of variables in the wave equation with fixed endpoints selects and angular frequencies , . The time factors may be chosen as , . By Fourier sine series orthogonality, the initial data give
Hence . The factor in is required because differentiating the time sine supplies .
The given displacement is a symmetric triangular tent: it is zero at both endpoints and has height at . Integrating each linear half gives . Release from rest gives , so the midpoint-plucked fixed-end string is
Only odd modes occur, by symmetry about the midpoint. The initial slope corner makes this a finite-energy weak solution; it is a classical solution away from the propagating corner lines.
Figure 1.
Initial triangular pluck and later shapes of a fixed-end string
. Original normalized displacement and modal predictions. The initial tent reaches one at the midpoint; snapshots use time . The string passes through a straight configuration at and reverses its initial displacement at . Details.
Use separation of variables . The fixed-end Dirichlet boundary conditions select , , and each mode satisfies . In the physical resistance range , all normal modes are underdamped, with . The modal factor normalized by , is
Consequently the linearly damped string has solution
The coefficients are those of the initial Fourier sine series. Differentiating each normalized modal factor at zero confirms that the string starts from rest. Suitable initial data give convergence in the string's energy space; the piecewise linear profile here need not give a twice differentiable solution along every characteristic from its corner.
For the specified tent profile, integrating its two linear pieces by parts gives
For example the first piece gives , and the second gives the opposite cosine term and the same sine term. Hence
The zero even coefficients also follow from reflection symmetry about the midpoint. This is the Fourier sine series of a symmetric tent. If were read without the physical assumption , the same modal solution extends by replacing imaginary-frequency sine and cosine by their hyperbolic counterparts, and taking when .
Figure 1.
Evolution of a tent-shaped string released from rest with linear damping
. Details.
The substitution separates the uniform equilibrium from the decaying perturbation. Direct differentiation gives
Consequently the reaction-diffusion equation reduces to the heat equation . Its data become
When the three constants coincide, the Dirichlet boundary conditions for are homogeneous. Separation of variables gives and , selecting the normal modes for . Thus
Two integrations by parts give , while the constant term uses . Therefore the Fourier sine series is
For , its first coefficient is nonzero. Multiplying by and retaining the slowest-decaying mode gives
The remainder estimate holds uniformly in for sufficiently large positive time. If , the fundamental vanishes and the next possible mode has decay rate , explaining the exclusion.
There is an initial endpoint compatibility issue unless : the given polynomial profile vanishes at the endpoints, whereas the boundary values equal . The series realizes the initial data in L2 space and pointwise in the open interval, imposing the prescribed boundary values for . For nonzero it cannot also be continuous at both initial endpoint corners.
In logarithmic coordinates the eigenvalue problem becomes . A nonzero function with zero values at both ends requires : multiplying by and integrating gives . Write . The first endpoint gives , and the second requires , .
For vector normalization, . A positive real normalization constant therefore gives
The sine orthogonality identity also gives . Completeness is the usual completeness of the Fourier sine series on under the logarithmic coordinate transformation.
After multiplying the initial field by , the dependence is exactly the cosine mode. Its orthogonality therefore gives when . For , the remaining Fourier coefficient in the Fourier sine series is
Thus
The coefficients are independent of , because the initial exponential exactly cancels the drift-removing weight. Substitution into the preceding expansion gives the full subsequent solution, with decay rates .
Assume the struck interval lies within the string, so . The initially stationary straight string has . Write its initial velocity as a Fourier sine series . Then
Thus . Immediately after the strike all the energy is kinetic energy:
The orthogonality integral assigns energy to mode . Since the ideal modes evolve independently, their total kinetic-plus-elastic energies remain constant. Therefore the modal energy of a localized velocity impulse on a string gives
The centre factor selects modes having significant motion at the impact location; the width factor accounts for cancellation across the finite hammer footprint. Parseval's identity ensures . The velocity discontinuities are understood in the mean-square sense and do not alter the energy integrals.
For each sine normal mode, the temporal characteristic equation is , with roots . Since , the first modes are overdamped and all higher modes are underdamped. No integer gives critical damping.
The zero initial displacement excludes the hyperbolic cosine and cosine terms. Hence
where
To impose the initial velocity, let be its Fourier sine series coefficients. Differentiating the expansion at gives for the overdamped modes and for the underdamped modes. These determine all coefficients. Despite the hyperbolic sine, the first modes decay: , so both temporal exponential rates are negative.
Here and . Let
Two applications of integration by parts give
Solving these equations,
Consequently the required amplitudes are
The stated initial velocity is nonzero at the fixed endpoints, whereas a classical solution differentiable there would require zero endpoint velocity. Thus it is understood on the open interval, or as an L2 space initial datum in the usual finite-energy solution. Its Fourier sine series takes value zero at the endpoints; this changes no initial energy or interior initial data.
First decompose the initial dependence using . Only the cosine indices and occur. Expand the remaining factor in a Fourier sine series:
For , two integrations by parts give
Thus even vanish, while for odd . The nonzero double-series coefficients are and . Their separate heat-mode decay factors give
At the bracket is , which recovers the initial profile with the displayed sine coefficients. Each term satisfies the mixed Dirichlet boundary conditions and Neumann boundary conditions.
Set and write . Then
so the two first-derivative contributions cancel exactly, leaving
The Dirichlet spectrum of on this interval is , . If , the linear or hyperbolic solutions cannot satisfy both zero endpoints nontrivially, so no additional modes have been omitted. Thus
To verify normalization, use :
This proves weighted orthonormality and also transfers completeness from the ordinary Fourier sine series. The construction is the cubic-coordinate reduction of a singular Sturm-Liouville operator. The positive constant shifts the entire spectrum down; a zero eigenvalue occurs if , so the no-zero-eigenvalue proviso in part (a)(iii) must be imposed separately if that inverse formula is used here.
Expand in the complete Fourier sine series and apply Fourier inversion. Substitution of part (ii) gives
To check the source normalization, apply mode by mode. It cancels the denominator; the remaining inverse transform gives , and completeness gives
The endpoints vanish termwise. These identities establish the equation in the distributional sense, with classical validity wherever the series and derivatives converge suitably.
The displayed real-axis integrals in the paper are not ordinary convergent integrals at their poles. One definite choice is the Cauchy principal value at each . If a causal solution is wanted, use instead. Its inverse transform is , so the causal solution is
when the past integral exists. The principal-value choice instead uses the time-symmetric kernel . No temporal initial data are given, so homogeneous sine and cosine modes remain permissible additions. This is the causal Fourier resolvent of a point-driven fixed string.
Apply separation of variables with and temporal factor . The spatial eigenvalue equation is
The nontrivial solutions of these Dirichlet boundary conditions are sine eigenfunctions. Normalizing in the usual inner product on gives
with . The superposition principle and the Fourier sine series then give
The constants are the initial-data coefficients . Here physical diffusion means .
Let . The first normalized Fourier sine series coefficient is
Strict positivity follows because , has positive total mass, and everywhere inside the interval. In particular, there is no cancellation that could remove the slowest term. This is the positivity of the first Dirichlet reaction-diffusion coefficient.
For finite initial mass , all coefficients satisfy . The eigenfunction expansion therefore gives the uniform bound
The positive first profile thus controls the long-time behavior. We recover exactly the threshold , with decay below it and unbounded positive growth at every interior point above it. The finite-mass condition is the usual meaning of an initial density profile here; standard positive-time smoothing gives the same conclusion in the usual broader admissible data classes.