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Material Type: Exam; Professor: Fulling; Class: ADV ENGINEERING MATH; Subject: MATHEMATICS; University: Texas A&M University; Term: Unknown 1989;
Typology: Exams
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1.[20pts.] Below are listed four problems that can be solved using separation of variables and/or some combination of Fourier series and transforms.
Assume each problem has the maximum number of inhomogeneous boundary conditions. For each problem, pick the form of the expected solution from the following list.
(A) the sum of a steady-state solution and a Fourier series (B) the sum of both a Fourier series and two Fourier sine or cosine transforms (C) the sum of four Fourier series (D) Fourier transforms with respect to two different variables (E) a Fourier transform
2.[20pts.] Classify each of the following equations as linear homogeneous, linear inhomoge- neous, or nonlinear. Also, classify each as elliptic, parabolic, or hyperbolic.
(A) ∂^2 u ∂x^2
∂^2 u ∂y^2 −xyu = −(x + y) Linear nonhomogeneous, elliptic.
(B) ∂w
∂^2 w ∂x^2 = t^2 w Linear homogeneous, parabolic.
3.[40pts.] For the initial-value-problem
d^2 y dt^2
dy dt
find the first term of the regular expansion for the solution. Also, write down the equation you would use to find the second term in the expansion. DO NOT solve this equation, but use it to explain why the regular expansion will fail to be uniform. You may find helpful the trig identity
sin^3 x = −
sin 3x +
sin x.
Finally, describe briefly what you would do to remedy the situation. If y ∼ y 0 + y 1 then y^3 ∼ y 03 + 3y 1 y^20. The initial conditions translate to
y 0 (0) = 0, y′ 0 (0) = 1; y 1 (0) = 0, y 1 ′(0) = 0.
The equation becomes
0 ∼ y 0 ′′ + y 1 ′′ + 4y 0 + 4y 1 + y^30.
The ^0 problem is
y′′ 0 + 4y 0 = 0 with initial conditions =⇒ y 0 = 12 sin 2t.
The ^1 problem is
y′′ 1 + 4y 1 = −y^30 = −
2 sin 2t
= −^18 sin^3 2 t,
or
y 1 ′′ + 4y 1 =
sin 6t −
sin 2t.
Since the sin 2t term is resonant, the solution for y 1 will contain secular terms like t sin 2t; the approximation by regular perturbation theory is nonuniform. To improve the approximation by the distorted-time (Poincar´e) method, try a new time scale τ ∼ (1 + ω 1 )t and choose ω 1 to cancel the secular terms in the ODE for y 1. The improved y 0 is now a one-term approximation that already incorporates the effect of the perturbation to first order, in a more nearly uniform manner. The two-time method could also be used, but it is “overkill” for this problem.
4.[40pts.] Obtain a one-term uniformly valid composite expansion for the solution of
d^2 f dx^2
df dx
0 < 1 , f (0) = 1, f (2) = 3.
First find the lowest-order outer solution by just setting to 0 in the equation:
df 0 dx
This equation is separable (in the sense of ODEs):
∫ e+f^0 df 0 =
x dx =⇒ ef^0 =
x^2 2
x^2 2
The negative sign on the first derivative suggests a boundary layer on the right, so we enforce the left-end boundary condition 1 = f 0 (0) = ln C, or C = e. To construct the inner solution, let s = (2 − x)/, so that s vanishes at the right endpoint and is positive inside the interval. Then
d dx
d ds
, x = 2 − s,
so the ODE (multiplied by ) converts to
d^2 fi ds^2
dfi ds
Thus
dfi ds
= Ae−s, fi = −Ae−s^ + B.
The boundary condition (inherited from x = 2) is 3 = fi(0) = −A + B. So
fi = (3 + A) − Ae(x−2)/.
hence
B(ω) =
π
0
g(x) sin (ωx) dx.
For the second part, insert the formula for B, with x renamed z, into the formula for u, and exchange the order of integrations:
u(x, y) =
0
dz
0
dω
π
sin (ωx) sin (ωz)e−ωy^.
This has the desired Green function form with
G(x, y, z) =
0
dω
π
sin (ωx) sin (ωz)e−ωy
2 π
0
dω [eiω(x+z)^ − eiω(x−z)^ − eiω(z−x)^ + e−iω(x+z)]e−ωy
2 π
−∞
dω[eiω(x−z)^ − eiω(x+z)]e−|ω|y
y/π (x − z)^2 + y^2
y/π (x + z)^2 + y^2
(This is the same as the Green function for the entire upper half plane together with an “image charge” term to force the solution to zero at the vertical boundary of the quadrant.)
(B) Solve
∂u ∂t
∂^2 u ∂x^2
, 0 < x < π, 0 < t < ∞,
∂u ∂x
(t, 0) = N,
∂u ∂x
(t, π) + βu(t, π) = C,
u(0, x) = f (x),
where N, C, and β are prescribed constants, β is positive, and f is a prescribed function. Cite any appropriate theorems needed to justify your answer.
Because of the nonhomogeneous, but time-independent, terms N and C, we need to peel off a steady-state solution. Let u = v + w, where v = v(x) satisfies
v′′^ = 0, v′(0) = N, v′(π) + βv(π) = C.
Then v(x) = Ax + B where N = A and C = A + β(Aπ + B). Thus
v(x) = Nx +
β
− πN.
Write h(x) for f (x) − v(x). The other part of the solution, w, satisfies the homogeneous boundary-value problem
wt = wxx , wx(t, 0) = 0 = wx(t, π) + βw(t, π), w(0, x) = h(x).
Assuming a separated solution w = X(x)T (t) with an oscillatory eigenfunction (positive eigenvalue) leads to
T ′ T
= −ω^2.
The eigenvalue problem is
X′′^ + ω^2 X = 0, X′(0) = 0, X′(π) + βX(π) = 0.
The solutions are X(x) = cos(ωx) with −ω sin(ωπ)+β cos(ωπ) = 0. The allowed eigenvalues satisfy
ω β
= cot(ωπ).
The two sides of this equation can be easily sketched, showing that there are infinitely many positive roots ω 1 , ω 2 ,... , each ωj being greater than (j − 1)π and increasingly close to the latter as j increases. Negative ω’s give nothing new. The general theory of Sturm– Liouville problems guarantees that the eigenfunctions form a complete set and that there are no nonreal eigenvalues. The only nontrivial question is whether there could be a negative or zero eigenvalue (corresponding to a pure imaginary ω). The easiest way to exclude this possibility (which you were not expected to do) is again to appeal to general theory: Assume X is an eigenfunction and Integrate by parts in
ω^2
∫ (^) π
0
X(x)^2 dx = −
∫ (^) π
0
XX′′^ dx = βX(π)^2 +
∫ (^) π
0
X′(x)^2 dx.
Since all the squares are positive, the assumption that ω^2 is strictly positive is vindicated. The general Sturm–Liouville theorem guarantees that the eigenfunctions are complete and orthogonal, so the full solution for w has the form
w(t, x) =
j=
cj cos(ωj x)e−ω
(^2) j t .
h(x) =
j=
cj cos(ωj x) =⇒ cj =
(^0) ∫ cos( ωj^ x)h(x)^ dx 1 0 cos
(^2) (ωj x) dx
(C) Solve, by the method of your choice, the wave equation
∂^2 u ∂t^2
∂^2 u ∂x^2
, u(t, 0) = 0 = u(t, 1),
u(0, x) = f (x),
∂u ∂t
(0, x) = 0.
This can be solved either by separation of variables or by d’Alembert’s method (with the odd extension of the initial data through each endpoint to enforce the Dirichlet boundary conditions). Please see the lecture notes for details.
(D) Solve the heat equation in a disk (0 ≤ r < 1),
∂u ∂t
∂^2 u ∂r^2
r
∂u ∂r
r^2
∂^2 u ∂θ^2
u(t, 1 , θ) = 0, u(0, r, θ) = g(r) cos θ.
(The special choice of initial data assures that only one particular Bessel function appears in the answer; however, you will need to sum over something else.)