Solution to Partial Differential Equations: Methods and Applications (Robert McOwen) Section 5.3
- Suppose u is a distribution solution of the nonhomogeneous heat equation ut=Δu+f(x,t) in U⊂Rn+1, where f∈C∞(U). Show that u∈C∞(U).
- Consider the heat equation ut=Δu in (x,t)∈Rn×(0,∞) with the initial condition u(x,0)=δ(x). Since ∫u(x,t)dx represents the total heat content in Rn at time t, we encounter the condition ∫u(x,t)dx=1 for all t≥0.
- Show that the choice α=−n/2, which was made to simplify (41) to (42), is a consequence of the scale invariance of ∫u(x,t)dx for t>0.
- Show that (43b) is a consequence of ∫u(x,t)dx<∞.
- Use ∫u(x,t)dx=1 to evaluate the constant C in (44), and conclude that u(x,t) coincides with the heat kernel.
- Suppose it is known that u(x,t)=tαw(x/√t) (see (39)). Then we use the change of variable to find
C=∫Rnu(x,t)dx=tα∫Rnw(x/√t)dx=tα∫Rnw(y)⋅√tndy=tα+n/2∫Rnw(y)dy.
Due to the t-independence, we have α=−n/2. The proof is complete. - From (43a), we have
w′+r2w=Ar1−n.
Multiplying it by er2/4, it yields(er2/4w)′=Ar1−ner2/4,
which givesw(r)=w(0)e−r2/4+Ae−r2/4∫r0s1−nes2/4dsfor r∈(0,∞).
From part (a), the condition ∫Rnu(x,t)dx<∞ implies ∫∞0rn−1w(r)dr<∞. This meansA∫∞0rn−1e−r2/4∫r0s1−nes2/4dsdr<∞.
Here we have used the fact that ∫∞0w(0)rn−1e−r2/4dr is finite. However, we apply L'Hôpital's rule to observe thatlimr→∞[r⋅rn−1e−r2/4∫r0s1−nes2/4ds]=limr→∞∫r0s1−nes2/4dsr−ner2/4=limr→∞r1−ner2/4−nr−n−1er2/4+r−ner2/4⋅r/2=limr→∞2−2nr−2+1=2.
This means the function rn−1e−r2/4∫r0s−1nes2/4ds∼1r as r sufficiently large, and the integral ∫∞0rn−1e−r2/4∫r0s−1nes2/4dsdr must be divergent. Therefore, A must be zero. - By (44) and ∫Rnu(x,t)dx=1, we have
1=Ctn/2∫Rnexp(−|x|24t)dt=Ctn/2n∏i=1∫Rexp(−x2i4t)dxi=Ctn/2n∏i=1⋅√4πt=Ctn/2⋅(4πt)n/2=(4π)n/2C.
Therefore, we get C=(4π)−n/2 and henceu(x,t)=1(4πt)n/2exp(−|x|24t),
which conincides with the heat kernel. - Apply the similarity method to the linear transport equation ut+aux=0 to obtain the special solutions u(x,t)=c(x−at)α.
- Consider the inviscid Burgers equation ut+uux=0.
- Use the similarity method to reduce this equation to the ODE ww′−(α+1)zw′+αw=0.
- Take α=−1 and obtain the rarefaction wave solutions discussed in Section 1.2.
- Let ˜u=ϵαu, ˜x=ϵβx and ˜t=ϵγt, where α, β and γ are constants, i.e.,
˜u(˜x,˜t)=ϵαu(ϵ−β˜x,ϵ−γ˜t).
To scale out the t-dependence means that we should take ϵγ=t−1 so that ˜t=1; that is if we introduce w(˜x)=˜u(˜x,1) and z=˜x, then u(x,t)=tα/γw(z) and z=t−β/γx defines the similarity transformation to the similarity variables w and z. For convenience, we take γ=1 and henceu(x,t)=tαw(z),z=t−βx.
The inviscid Burgers equation becomes0=ut+uux=αtα−1w(z)+tαw′(z)⋅−βt−β−1x+tαw(z)⋅tαw′(z)⋅t−β=αtα−1w(z)−βtα−1zw′(z)+t2α−βw(z)w′(z)
If we choose β=α+1, thenu(x,t)=tαw(z),z=t−α−1x.
Here w satisfiesw(z)w′(z)−(α+1)zw′(z)+αw(z)=0,
which is desired. - Taking α=−1, we get w′(z)−1=0, which gives w(z)=z+C. Therefore, we obtain
u(x,t)=t−1(z+C)=t−1(x+C)=x+Ct.
- For n=1 and α=0, express the solution of (41) in terms of the error function
erf(y)=2√π∫y0e−s2ds.
- Use (a) to solve the heat equation on a half-line: ut=uxx for x,t>0 with u(x,0)=1 for x>0, and u(0,t)=0 for t>0.
- For n=1 and α=0, express the solution of (41) in terms of the error function
- For n=1 and α=0, equation (41) becomes
w″+12rw′=0.
Multiplying it by er2/4 and then integrating over [0,t], we get(er2/4w)′=0 ander2/4w′(r)=w′(0).
It is clear thatw(r)=w(0)+w′(0)∫r0e−t2/4dt=w(0)+2w′(0)∫r/20e−s2ds=w(0)+w′(0)√πerf(r/2).
- By (a), we get the solution u in the following form:
u(x,t)=w(z)=w(x√t)=w(0)+w′(0)√πerf(x√4t)for x,t>0.
Clearly, erf(0)=0 and limy→∞erf(y)=1. By the boundary condition u(0,t)=0, we get w(0)=0. Using the initial data u(x,0)=1 for x>0, we get w′(0)=1/√π. Therefore, we obtain the solution u given byu(x,t)=erf(x√4t)for x,t>0.
- Apply the similarity method to the porous medium equation ut=Δ(uγ) in Rn, where γ>1, to obtain Barenblatt's solution:
u(x,t)=tα(C−(γ−1)β|x|22γt2β)1/(γ−1),
where C is a positive constant, β=(n(γ−1)+2)−1, and α=−nβ.Remark. Here u(x,t) is defined and positive for (γ−1)β|x|2<C2γt2β, but may be extended by zero to a weak solution on Rn×(0,∞). In this way, u exhibits finite propagation speed, unlike the solution of the heat equation γ=1.
Solution
Pick ξ=(x0,t0)∈U and ϵ>0 so small that the ball B4ϵ(ξ)⊆U. Choose ϕ∈C∞0(B4ϵ(ξ)) with ϕ≡1 on B3ϵ(ξ). Let w(x,t)=ϕ(x,t)u(x,t) and v(x,t)=wt(x,t)−Δw(x,t)−f(x,t) in U, which are both distributions in U with support in B4ϵ(ξ). Clearly, v=0 on B3ϵ(ξ). In particular, the convolution(˜K∗v)(x,t)=∫Rn+1˜K(x−y,t−s)v(y,s)dyds=∫Rn+1˜K(y,s)v(x−y,t−s)dyds
is well-defined as a distribution. Butv(x−y,t−s)=wt(x−y,t−s)−Δw(x−y,t−s)−f(x−y,t−s)=(∂t−Δx)w(x−y,t−s)−f(x−y,t−s)=(−∂s−Δy)w(x−y,t−s)−f(x−y,t−s),
so for g∈C∞0(U), we find⟨˜K∗v,g⟩=∫U∫Rn+1˜K(y,s)[(−∂s−Δy)w(x−y,t−s)−f(x−y,t−s)]g(x,t)dydsdxdt=∫U∫Rn+1(∂s−Δy)˜K(y,s)w(x−y,t−s)g(x,t)dydsdxdt+∫U∫Rn+1˜K(y,s)f(x−y,t−s)g(x,t)dydsdxdt=∫U∫Rn+1[δ(y,s)w(x−y,t−s)+˜K(y,s)f(x−y,t−s)]g(x,t)dydsdxdt=∫U[w(x,t)+(˜K∗f)(x,t)]g(x,t)dxdt=⟨w+˜K∗f,g⟩.
In other words, ˜K∗(v−f)=w as distributions.Now we choose ψ∈C∞(Rn+1) with ψ≡0 on Bϵ(0) and ψ≡1 on Rn+1−B2ϵ(0). Then ψ vanishes in a neighborhood of the singularity of ˜K, so ψ˜K is smooth function, and hence so is (ψ˜K)∗(v−f). But for (x,t)∈Bϵ(ξ) and (y,s)∈supp(v)⊂B4ϵ(ξ)∩(Rn+1−B3ϵ(ξ)), we have |(x,t)−(y,s)|≥2ϵ, so ψ(x−y,t−s)=1. In other words, (ψ˜K∗(v−f))(x,t)=(˜K∗(v−f))(x,t)=w(x,t) for (x,t)∈Bϵ(ξ), which shows that w is smooth on Bϵ(ξ). But w(x,t)=ϕ(x,t)u(x,t), so u is also smooth on Bϵ(ξ). Since ξ∈U was arbitrary, we conclude that u is smooth on U.
Solution
Solution
Let ˜u=ϵαu, ˜x=ϵβx and ˜t=ϵγt, where α, β and γ are constants, i.e.,˜u(˜x,˜t)=ϵαu(ϵ−β˜x,ϵ−γ˜t).
To scale out the t-dependence means that we should take ϵγ=t−1 so that ˜t=1; that is if we introduce w(˜x)=˜u(˜x,1) and z=˜x, then u(x,t)=tα/γw(z) and z=t−β/γx defines the similarity transformation to the similarity variables w and z. For convenience, we take γ=1 and henceu(x,t)=tαw(z),z=t−βx.
The linear transport equation becomes0=ut+aux=αtα−1w(z)+tαw′(z)⋅−βt−β−1x+atαw′(z)⋅t−β=αtα−1w(z)+atα−βw′(z)−βtα−β−1xw′(z)=αtα−1w(z)−βtα−1zw′(z)+atα−βw′(z)=tα−1(αw(z)−βzw′(z))+atα−βw′(z).
If we choose β=1, thenu(x,t)=tαw(z),z=x/t.
Here w satisfiesαw(z)+(a−z)w′(z)=0,
which can be solved by w(z)=c|z−a|α. Therefore, we obtainu(x,t)=tα⋅c|z−a|α=tα⋅c|xt−a|α=c|x−at|α.
Solution
Solution
Solution
Let ˜u=ϵαu, ˜x=ϵβx and ˜t=ϵδt, where α, β and δ are constants, i.e.,˜u(˜x,˜t)=ϵαu(ϵ−β˜x,ϵ−δ˜t).
To scale out the t-dependence means that we should take ϵδ=t−1 so that ˜=1; that if we introduce w(˜x)=˜u(˜x,1) and z=˜x, then u(x,t)=tα/δw(z) and z=t−β/δx defines the similarity transformation to the similarity variables w and z. For convenience, we take δ=1 and henceu(x,t)=tαw(z),z=t−βx.
The porous medium equation becomes0=ut−Δ(uγ)=αtα−1w(z)+tα∇w(z)⋅−βt−β−1x−tαγΔx(wγ(z))=αtα−1w(z)−βtα−1z⋅∇w(z)−tαγ∇x⋅(t−βγwγ−1(z)∇w(z))=αtα−1w(z)−βtα−1z⋅∇w(z)−γtαγ−β[t−β(γ−1)wγ−2(z)|∇w(z)|2+t−βwγ−1(z)Δw(z)]=αtα−1w(z)−βtα−1z⋅∇w(z)−γtαγ−2β[(γ−1)wγ−2(z)|∇w(z)|2+wγ−1(z)Δw(z)].
In order to obtain a time-independent partial differential equation for w, the powers of t must agree, which gives α−1=αγ−2β, and hence β=(α(γ−1)+1)/2. Thus, we find thatu(x,t)=tαw(z),z=t−(α(γ−1)+1)/2x.
Here w satisfiesαw(x)−βz⋅∇w(z)−γ[(γ−1)wγ−2(z)|∇w(z)|2+wγ−1(z)Δw(z)]=0.
Now we assume that w is radial, i.e., ˜w(r)=w(z) for |z|=r. Then ˜w satisfiesα˜w(r)−β⋅r˜w′(r)−γ[(γ−1)˜wγ−2(r)˜w′2(r)+wγ−1(z)(˜w″(r)+n−1r˜w′(r))]=0,
which impliesα˜w(r)−β⋅r˜w′(r)−[(wγ(r))″+n−1r(˜wγ(r))′]=0.
If we choose α=−nβ, then we observe that rn−1(α˜w−βr˜w′(r))=−β(rn˜w)′. Multiplying the differential equation by rn−1, we obtain(rn−1(˜wγ)′)′+β(rn˜w)′=0,
which impliesrn−1(˜wγ)′+βrn˜w=A.
For the sake of simplicity, we assume that w and w′ decay to zero as r tends to infinity, and hence A=0. Thus, we get˜wγ−2˜w′=−βγr,
which gives us˜wγ−1(r)=C−(γ−1)β2γr2.
Therefore, we arrive atw(z)=(C−(γ−1)β2γ|z|2)1/(γ−1),u(x,t)=tαw(t−βx)=tα(C−(γ−1)β2γt2β|x|2)1/(γ−1),
where α=−n(n(γ−1)+2)−1 and β=(n(γ−1)+2)−1.
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