Take the spatial interval with , and write . A separated nonzero solution satisfies
The zero-endpoint Dirichlet boundary conditions rule out nonzero solutions for : linear or hyperbolic spatial factors cannot vanish at both ends. For , they give and , . The temporal factors solve , with the fixed-end standing wave frequencies . Superposition gives
The constants are arbitrary subject to the convergence and regularity required of the solution. For initial displacement and initial velocity , their Fourier sine series give and . Smooth compatible data give classical solutions; weaker data have the corresponding energy interpretation. A negative printed describes the interval with endpoints reversed and gives the same modes after using its positive length.
Seek a separated nonzero solution . Division by on intervals where the factors are nonzero gives . Write and , with both factors zero at their endpoints .
For , a nonpositive gives only the zero solution under the two endpoint conditions: linear functions vanish identically when , and the hyperbolic solutions do likewise for . For , the endpoints force with positive integer and . Applying the same argument to gives and , with positive integer .
The only positive integer pairs satisfying are and . By superposition,
To establish that this is the most general sufficiently regular solution, expand in the complete product Fourier sine series on the square. Substitution, or integration by parts against each sine mode, gives for every coefficient. Hence only the two displayed modes remain; all boundary terms vanish because of the given zero values. This is the eigenvalue- case of the Dirichlet eigensystem of a rectangle. The zero solution is included when .
Figure 1.
The two independent zero-boundary modes sharing Laplacian eigenvalue 25 on the square
. Details.
Set , so . The binomial theorem gives
Use and to obtain
This is a finite Fourier sine series, with only odd harmonics.
Take the odd extension on and then extend with period . It agrees with the required arch for and is continuous at its joins. Its Fourier sine series has
For clarity, let , so and . Two integrations by parts, with the first endpoint term zero, give
Consequently : the even coefficients vanish and the odd ones are . This proves
The Fourier sine series of an odd quadratic arch converges to this continuous extension; its coefficients are also absolutely summable. Finally evaluate at . The left side is and the sine factors are , so
The evaluation is at a continuity point, so it does not invoke a jump midpoint.
The original PDF contains the product ; the transcription drops the after the first sine. Using gives the finite Fourier sine series
Thus , , and all other sine coefficients vanish. No cosine or constant terms are present.
The required property is odd symmetry, , up to irrelevant changes on a set of measure zero when discussing Fourier coefficients. An odd function has zero mean, and its products with cosine are odd, so every cosine coefficient vanishes. Its sine coefficients may remain nonzero.
For pointwise representation, the Fourier series takes the average of the one-sided limits at a jump. In particular a pure Fourier sine series has value zero at the origin and at the endpoints; arbitrary assigned values there need not equal the series sum.
Use the double-angle identity . The Fourier series is already a finite trigonometric sum:
In the usual Fourier sine series convention, , all other vanish, and all cosine coefficients and the constant coefficient vanish.
For a nonzero separated solution of the reaction-diffusion equation, substitution and division by gives
The two sides depend on different variables, so both equal a separation constant. The homogeneous Dirichlet boundary conditions select a negative spatial constant, written :
For , . The boundary value at zero makes ; the boundary value at then requires , with . A zero spatial constant gives only a linear function vanishing at both endpoints, hence the zero function; a positive spatial constant similarly gives no nonzero admissible hyperbolic solution. Therefore
By superposition, the general solution with the stated boundary conditions is
The coefficients are fixed only if initial data are supplied: for , they are the Fourier sine series coefficients . Here they remain arbitrary subject to convergence. Every mode has the ordinary diffusive decay rate plus the additional reaction decay rate one.
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 .