17
ISRAEL JOURNAL OF MATHEMATICS 194 (2013), 259–275 DOI: 10.1007/s11856-012-0098-9 POINTWISE ESTIMATES FOR SOLUTIONS TO THE POROUS MEDIUM EQUATION WITH MEASURE AS A FORCING TERM BY Vitali Liskevich Department of Mathematics, Swansea University, Swansea SA2 8PP, UK e-mail: [email protected] AND Igor I. Skrypnik Institute of Applied Mathematics and Mechanics, Donetsk 83114, Ukraine e-mail: [email protected] ABSTRACT For porous media equations with a Radon measure on the right-hand side, we derive pointwise estimates for solutions via the Riesz potentials. 1. Introduction and main results Due to applications and interesting mathematical properties the porous media equations attracted much attention during the last decades. The results of the theory are well documented in monographs [1], [14], [15], [16] (see also [3, 4]). One of the important issues of the research is basic qualitative properties of solutions such as local boundedness, summability properties and alike. In this note we study weak solutions to porous media equations with measure as a forcing term. We provide pointwise estimates for solutions. The estimates are expressed in terms of the Riesz potential of the measure. For the case of the heat equation the corresponding result was recently given in [5]. The estimates obtained in this paper allow us to give a sharp condition of local boundedness Received March 10, 2011 and in revised form August 10, 2011 259

Pointwise estimates for solutions to the porous medium equation with measure as a forcing term

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Page 1: Pointwise estimates for solutions to the porous medium equation with measure as a forcing term

ISRAEL JOURNAL OF MATHEMATICS 194 (2013), 259–275

DOI: 10.1007/s11856-012-0098-9

POINTWISE ESTIMATES FOR SOLUTIONSTO THE POROUS MEDIUM EQUATIONWITH MEASURE AS A FORCING TERM

BY

Vitali Liskevich

Department of Mathematics, Swansea University, Swansea SA2 8PP, UK

e-mail: [email protected]

AND

Igor I. Skrypnik

Institute of Applied Mathematics and Mechanics, Donetsk 83114, Ukraine

e-mail: [email protected]

ABSTRACT

For porous media equations with a Radon measure on the right-hand side,

we derive pointwise estimates for solutions via the Riesz potentials.

1. Introduction and main results

Due to applications and interesting mathematical properties the porous media

equations attracted much attention during the last decades. The results of the

theory are well documented in monographs [1], [14], [15], [16] (see also [3, 4]).

One of the important issues of the research is basic qualitative properties of

solutions such as local boundedness, summability properties and alike.

In this note we study weak solutions to porous media equations with measure

as a forcing term. We provide pointwise estimates for solutions. The estimates

are expressed in terms of the Riesz potential of the measure. For the case of the

heat equation the corresponding result was recently given in [5]. The estimates

obtained in this paper allow us to give a sharp condition of local boundedness

Received March 10, 2011 and in revised form August 10, 2011

259

Page 2: Pointwise estimates for solutions to the porous medium equation with measure as a forcing term

260 V. LISKEVICH AND I. I. SKRYPNIK Isr. J. Math.

and for unbounded solutions they are useful for studying Lp properties, mem-

bership in other functional spaces etc. As an application we give a supremum

estimate for the solution of a model initial boundary value problem.

Let Ω be a domain in Rn, T > 0. Let μ be a Radon measure on Ω. We are

concerned with pointwise estimates for a class of non-homogeneous divergence

type quasi-linear parabolic equations of the type

(1.1) ut −Δ(|u|m−1u) = μ in ΩT = Ω× (0, T ), Ω ⊂ Rn, m > 1.

Before formulating the main results, let us remind the reader of the definition

of a weak solution to equation (1.1). We rewrite the equation in the divergence

form

ut −m div(|u|m−1∇u) = μ.

We say that u is a weak solution to (1.1) if

u ∈ C([0, T ];L2loc(Ω)) ∩ L2

loc(0, T ;W1,2loc (Ω)) |u|m ∈ L2

loc(0, T ;W1,2loc (Ω)),

and for any compact subset K of Ω and any interval [t1, t2] ⊂ (0, T ) the integral

identity

(1.2)∫Kuϕdx

∣∣∣t2t1+

∫ t2

t1

∫K

{−uϕτ +m|u|m−1∇u∇ϕ}dx dτ =

∫ t2

t1

∫Kϕμ(dx) dτ

holds for any ϕ ∈ C1(ΩT ).

The crucial role in the first main result is played by the truncated version of

the Riesz potential defined by

(1.3) Iμ2 (x,R) =

∫ R

0

μ(Br(x))

rn−2

dr

r.

In the sequel, γ stands for a constant depending only on n and m, which may

vary from line to line.

Let (x0, t0) ∈ ΩT . Consider the cylinder

(1.4) Q(r, τ) = Br(x0)× (t0 − τ, t0 + τ).

Further on, we assume that Q(r, τ) � ΩT .

The first main result of this paper is the following theorem.

Theorem 1.1: Let u be a weak solution to equation (1.1). For every λ ∈(0, 1/n) there exists γ > 0 depending on n,m and λ, such that for almost all

Page 3: Pointwise estimates for solutions to the porous medium equation with measure as a forcing term

Vol. 194, 2013 POROUS MEDIUM EQUATION 261

(x0, t0) ∈ ΩT such that Q0 = Q(r0, θ0) � ΩT we have

(1.5)

u(x0, t0) ≤ γ

{(1

rn+20

∫∫Q0

um+λ+ dx dτ

) 11+λ

+ supt∈(t0−θ,t0+θ)

1

rn0

∫Br0

u+ dx

+

(r20θ0

) 1m−1

+

(1 +

θ0r20

)Iμ2 (x0, 2r0)

}.

Also, the following version of the above estimate holds:

u(x0, t0) ≤ γ

{(1

rn+20

∫∫Q0

um+λ+ dx dτ

) 11+λ

+

(1

rn+20

∫∫Q0

um−1+2λ+ dx dτ

) 12λ

+1

θ0rn0

∫∫Q0

u+dx dτ +

(r20θ0

) 1m−1

+

(1 +

θ0r20

)Iμ2 (x0, 2r0)

}.

The estimate above is not homogeneous in u which is usual for such type

of equations [3, 14]. The proof of Theorem 1.1 is based on a suitable modi-

fications of De Giorgi’s iteration technique [2] following the adaptation of the

Kilpelainen–Maly technique [7] to parabolic equations with ideas from [10, 13].

A pointwise estimate for the evolutional p-Laplace equation was recently ob-

tained in [11].

An immediate application of the above result is the following corollary.

Corollary 1.2: Assume that there exists r0 > 0 such that for every Ω � Ω

the measure μ satisfies the condition

(1.6) supx∈Ω

Iμ2 (x, r0) < ∞.

Then every weak solution to (1.1) is locally bounded, that is u ∈ L∞loc(ΩT ).

In particular, if dμ(x) = f(x)dx with f ∈ Ln/2, 1(Ω) (Lorenz space) then (1.6)

is satisfied.

(See, e.g., [12] for relevant properties of the Riesz potential.)

Condition of local boundedness (1.6) is sharp, as one can easily see looking at

stationary solutions. If (1.6) does not hold, using local properties of the Riesz

potential (see, e.g., [12]) one can deduce summability properties of solutions to

(1.1) such as membership in Lp-spaces, Orlicz spaces etc. We will not dwell

upon this.

Page 4: Pointwise estimates for solutions to the porous medium equation with measure as a forcing term

262 V. LISKEVICH AND I. I. SKRYPNIK Isr. J. Math.

As another application of Theorem 1.1 we consider the following model initial

boundary value problem:

(1.7)

ut −Δ(um) =μ, (x, t) ∈ Q = BR × (0, T ),

u(x, t) =0, (x, t) ∈ S = ∂BR × (0, T ),

u(x, 0) =0, x ∈ BR.

First, let us remark on the well posedness of problem (1.7) in the sense of

weak solutions as defined above. The uniqueness can be verified in the same way

as in [9, Chap. 1, Sec. 12]. However, the most general result on the existence

of weak solutions to (1.7), known to the authors, requires dμ(x) = f(x)dx with

f ∈ L(m+1)/m (cf. [9, Theorem 12.2]). So the next result is a global a priori

bound on the solution.

Corollary 1.3: Let u be the solution to problem (1.7). Then

(1.8) supQ

u ≤ γ

(R2

T

) 1m−1

+ γ

(1 +

T

R2

)supx∈BR

Iμ2 (x, 2R).

Remark 1.4: 1. Based on the cases of the Laplacian and p-Laplacian it

is plausible to conjecture that (1.7) is well posed under the assumption

that supx∈BRIμ2 (x, 2R) < ∞. To identify the optimal class of measures

μ guaranteeing well posedness of problem (1.7) seems an interesting

open question.

2. Note that if dμ(x) = f(x)dx with f ∈ Ln/2,1(BR) and n ≥ 4, then by

the above-mentioned result of J.-L. Lions, (1.7) is well posed and (1.8)

becomes a posteriori supremum bound.

The approach we undertake in the proof of Theorem 1.1 allows for an ex-

tension of the result to the case of measures depending on (x, t) ∈ Rn+1. To

formulate the result we first restrict the geometry of the cylinders, compara-

tively to (1.4), namely, we introduce

Qr = Br(x0)× (t0 − r2, t0 + r2).

The time-dependent analogue of the truncated Riesz potential is introduced by

Iμ2 (x, t, R) =

∫ R

0

μ(Qr)

rndr

r.

Theorem 1.5: Let u be a weak solution to equation (1.1). For every λ ∈(0, 1/n) there exists γ > 0 depending on n,m and λ, such that for almost all

Page 5: Pointwise estimates for solutions to the porous medium equation with measure as a forcing term

Vol. 194, 2013 POROUS MEDIUM EQUATION 263

(x0, t0) ∈ ΩT such that Q0 = Qr0 � ΩT we have

(1.9) u(x0, t0) ≤

γ{( 1

rn+20

∫∫

Q0

um+λ+ dx dτ

) 11+λ

+ supt∈(t0−r20,t0+r20)

1

rn0

Br0

u+ dx+1+Iμ2 (x0, t0, 2r0)

}.

The rest of the paper contains the proofs of the above statements.

2. Proofs

Proof of Theorem 1.1. Let Q(r, τ) be as above and ξ(x, t) be a cut-off function

such that

1Q(r/2,τ) ≤ ξ ≤ 1Q(r,τ), |∇ξ| ≤ γr−1, |ξt| ≤ γτ−1.

Further on, we assume that ut ∈ L2loc(ΩT ), since otherwise we can pass to

Steklov averages.

We start with some auxiliary integral estimates for the solutions of (1.1)

which are formulated in the next lemma.

Define

G(u) =

⎧⎨⎩u for u > 1,

u2−2λ for 0 < u ≤ 1.

Lemma 2.1: Let the conditions of Theorem 1.1 be fulfilled. Let u be a solution

to (1.1). Then there exists a constant γ > 0 depending only on n,m such that

for any l, δ > 0, any cylinder Q(r, τ) and any ξ as above,

(2.1)

δ2∫L(t)

G(u(x, t)− l

δ

)ξ(x, t)kdx

+

∫∫L

um−1(1 +

u− l

δ

)−1+λ(u− l

δ

)−2λ

|∇u|2ξ(x, t)kdx dt

≤γδ2

τ

∫∫L

(u− l

δ

)ξk−1dxdt+γ

δ2

r2

∫∫L

um−1(1+

u− l

δ

)1−λ(u− l

δ

)2λξk−2dxdt

+ γ τδμ(Br(x0)),

where L = Q(r, τ) ∩ {u > l}, L(t) = (Br(x0)× {t}) ∩ {u > l} and λ ∈ (0, 1/n),

k > 2.

Page 6: Pointwise estimates for solutions to the porous medium equation with measure as a forcing term

264 V. LISKEVICH AND I. I. SKRYPNIK Isr. J. Math.

Proof. First, note that

(2.2)

∫ u

l

(1 +

s− l

δ

)−1+λ(s− l

δ

)−2λ

ds ≤ γδ,

and

(2.3)

∫ u

l

dw

∫ w

l

(1 +

s− l

δ

)−1+λ(s− l

δ

)−2λ

ds

=

∫ u

l

(1 +

s− l

δ

)−1+λ(s− l

δ

)−2λ

(u − s)ds

≥1

2(u− l)

∫ u+l2

l

(1 +

s− l

δ

)−1+λ(s− l

δ

)−2λ

ds

=δ2

2

(u− l

δ

)∫ u−l2δ

0

(1 + z)−1+λz−2λdz

≥γδ2G(u− l

δ

).

Let η be the standard mollifier in Rn and as usual ησ(x) = η(x/σ). Set

uσ = ησ ∗ u. Let ε > 0. Test (1.2) by ϕ defined by

(2.4) ϕ(x, t) =

[ ∫ uσ(x,t)

l

(1 +

s− l

δ

)−1+λ(ε+

s− l

δ

)−2λ

ds

]+

ξ(x, t)k,

and t1 = t0 − τ , t2 = t.

Using first (2.2) on the right-hand side, then passing to the limit σ → 0 on

the left, after applying the Schwarz inequality we obtain for any t ∈ (0, t0)

∫L(t)

∫ u

l

dw

∫ w

l

(1 +

s− l

δ

)−1+λ(ε+

s− l

δ

)−2λ

dsξkdx

+

∫∫L

(1 +

u− l

δ

)−1+λ(ε+

u− l

δ

)−2λ

um−1|∇u|2ξkdxdt

≤γ

∫∫L

∫ u

l

dw

∫ w

l

(1 +

s− l

δ

)−1+λ(ε+

s− l

δ

)−2λ

ds|ξt|ξk−1dxdt

+ γr−2δ2∫∫

L

um−1(1+

u− l

δ

)1−λ(ε+

u− l

δ

)2λξk−2dx dt+γδτμ(Br(x0)).

Passing to the limit ε → 0 on the right-hand side of the above inequality and

Page 7: Pointwise estimates for solutions to the porous medium equation with measure as a forcing term

Vol. 194, 2013 POROUS MEDIUM EQUATION 265

using the Fatou lemma on the left, by (2.3) we obtain the required (2.1).

Let us set

v =1

δ

[ ∫ u

l

(1 +

s− l

δ

)− 1−λ2(s− l

δ

)m−1−2λ2

ds

]+

,(2.5)

w =1

δ

[ ∫ u

l

(1 +

s− l

δ

)− 1−λ2(s− l

δ

)−λ

ds

]+

.(2.6)

With this notation the next lemma is a consequence of Lemma 2.1.

Lemma 2.2: Let the conditions of Lemma 2.1 be fulfilled. Then

(2.7)∫L(t)

G

(u− l

δ

)ξkdx + δm−1

∫∫L

|∇v|2ξkdxdt + lm−1

∫∫L

|∇w|2ξkdxdt

≤γτ−1

∫∫L

(u− l

δ

)ξk−1dxdt

+ γr−2

∫∫L

um−1

(1 +

u− l

δ

)1−λ(u− l

δ

)2λ

ξk−2dxdt

+ γ τδ−1μ(Br(x0)).

Let (x0, t0) ∈ ΩT , R0 ≤ 12 dist(x0, ∂Ω), θ0 ≤ 1

2 min{t0, T − t0}.For j = 0, 1, 2, . . . set rj = R02

−j, θj = θ02−j, Bj = Brj(x0).

We define the sequence (lj)j∈N inductively, and then the sequences

(δj)j∈N∪{0}, (Δj)j∈N∪{0} by setting δi = li+1 − li and Δi = max{li, δi}. Set

l0 = 0. Suppose that l1, . . . , lj have been chosen. Let us show how to choose

lj+1.

For l > lj we define

(2.8) δj(l) = l − lj, Δj(l) = max{δj(l), lj}, τj(l) = min

{θj ,

r2j

Δm−1j (l)

}.

Next we introduce the cylinder Qj and the set Lj by

Qj = Bj × Ij(l), Ij(l) = (t0 − τj(l), t0 + τj(l)),

Lj = Qj ∩ ΩT ∩ {u(x, t) > lj}, Lj(t) =((Bj ∩ Ω)× {t}) ∩ {u > l}.

Page 8: Pointwise estimates for solutions to the porous medium equation with measure as a forcing term

266 V. LISKEVICH AND I. I. SKRYPNIK Isr. J. Math.

Let ξj ∈ C∞0 (Qj) be such that

ξj(x, t) = 1 for (x, t) ∈ Bj+1 × (t0 − 1

2τj(l), t0 +

1

2τj(l)),

|∇ξj | ≤ γr−1j , |∂ξj/∂t| ≤ γτj(l)

−1.

For l ≥ lj set

(2.9)

Aj(l) =1

τ1+ n

2j (l)Δ

(1+n2 )(m−1)

j (l)

∫∫˜Lj

um−1

(u− ljδj(l)

)1+λ

ξk−2j dxdt

+ supt∈Ij(l)

1

τn2

j (l)Δn2 (m−1)j (l)

∫˜Lj(t)

G

(u− ljδj(l)

)ξkj dx.

Note that Aj(l) is continuous as a function of l and Aj(l) → 0 as l → ∞.

Fix a number κ ∈ (0, 1) depending on n,m, c1, c2, which will be specified

later. For j = 0, 1, 2, . . . , if

(2.10) Aj

(lj +

(r2jθj

) 1m−1

)≤ κ,

we set

lj+1 = lj +

(r2jθj

) 1m−1

.

If, on the other hand,

(2.11) Aj

(lj +

(r2jθj

) 1m−1

)> κ,

then there exists

l > lj +

(r2jθj

) 1m−1

such that Aj(l) = κ. In this case we set lj+1 = l and δj(lj+1) = lj+1 − lj in

both cases. Hence

Δj := Δj(lj+1) ≥(r2jθj

) 1m−1

so that

τj := τj(lj+1) =r2j

Δm−1j

.

Page 9: Pointwise estimates for solutions to the porous medium equation with measure as a forcing term

Vol. 194, 2013 POROUS MEDIUM EQUATION 267

After choosing lj+1 we have from (2.9)

(2.12) Aj(lj+1) =

1

rn+2j

∫∫Lj

um−1

(u− ljδj

)1+λ

ξk−2j dxdt + sup

t∈Ij

1

rnj

∫Lj(t)

G

(u− ljδj

)ξkj dx,

where

Ij = (t0 − τj , t0 + τj), Qj = Bj × Ij , Lj = Qj ∩ΩT ∩ {u > lj}.

First, we note that Δj ≥ Δj−1 and therefore τj ≤ τj−1, which implies that

Qj ⊂ Qj−1.

Also note that our choices guarantee that

(2.13) Aj(lj+1) ≤ κ.

The following lemma is a key in the Kilpelainen–Maly technique [7].

Lemma 2.3: Let the conditions of Theorem 1.1 be fulfilled. There exists γ > 0

depending on the data, such that for all j ≥ 1 we have

(2.14) δj ≤ 2−1

m−1 δj−1 + γ

(r2jθj

) 1m−1

+ γ

(1 +

θ0r20

)1

rn−2j

μ(Bj).

Proof. Fix j ≥ 1. Without loss assume that

(2.15) δj > 2−1

m−1 δj−1, δj >

(r2jθj

) 1m−1

,

since otherwise (2.14) is evident. The second inequality in (2.15) guarantees

that Aj(lj+1) = κ and Qj = Qj.

Next we claim that

(2.16)1

rn+2j

∫∫Lj

um−1dx dt ≤ γκ.

Indeed, for (x, t) ∈ Lj one has

(2.17)u(x, t)− lj−1

δj−1= 1 +

u(x, t)− ljδj−1

≥ 1.

Page 10: Pointwise estimates for solutions to the porous medium equation with measure as a forcing term

268 V. LISKEVICH AND I. I. SKRYPNIK Isr. J. Math.

Hence we have, by (2.17),

(2.18)

1

rn+2j

∫∫Lj

um−1dx dt ≤ 1

rn+2j

∫∫Lj

um−1

(u− lj−1

δj−1

)1+λ

ξk−2j−1 dx dt

≤γ1

rn+2j−1

∫∫Lj−1

um−1

(u− lj−1

δj−1

)1+λ

ξk−2j−1 dx dt

≤γAj−1(lj) ≤ γκ.

Let us estimate the terms in the right-hand side of (2.12). For this we de-

compose Lj as Lj = L′j ∪ L′′

j ,

(2.19) L′j =

{(x, t) ∈ Lj :

u(x, t)− ljδj

< ε

}, L′′

j = Lj \ L′j,

where ε ∈ (0, 1), depending on n, p, c1, c2, is small enough to be determined

later.

By (2.16) we have

(2.20)

1

rn+2j

∫∫L′

j

um−1

(u− ljδj

)1+λ

ξk−2j dx dt ≤ γ

ε1+λ

rn+2j

∫∫L′

j

um−1dx dt ≤ γε1+λκ.

Let vj and wj be defined by (2.5) and (2.6), respectively, with δj in place of

δ and lj in place of l. Note that λ ≤ 1/n due to the assumption.

The following inequalities are easy to verify

(2.21)

vj ≤γ

(u(x, t)− lj

δj

)m−λ2

for (x, t) ∈ Lj, and

vj ≥γ

(u(x, t)− lj

δj

)m−λ2

for (x, t) ∈ L′′j .

Similarly,

(2.22)

wj ≤γ

(u(x, t)− lj

δj

) 1−λ2

for (x, t) ∈ Lj, and

wj ≥γ

(u(x, t)− lj

δj

) 1−λ2

for (x, t) ∈ L′′j .

Page 11: Pointwise estimates for solutions to the porous medium equation with measure as a forcing term

Vol. 194, 2013 POROUS MEDIUM EQUATION 269

Hence we have

(2.23)

1

rn+2j

∫∫L′′

j

um−1

(u− ljδj

)1+λ

ξk−2j dxdt

≤ γδm−1j

rn+2j

∫∫L′′

j

(u− ljδj

)m+λ

ξk−2j dxdt+ γ

lm−1j

rn+2j

∫∫L′′

j

(u− ljδj

)1+λ

ξk−2j dxdt

≤ γ(ε)δm−1j

rn+2j

∫∫L′′

j

v2m+λ

m−λ

j ξk−2j dxdt+ γ(ε)

lm−1j

rn+2j

∫∫L′′

j

w2 1+λ

1−λ

j ξk−2j dxdt.

The integrals on the right-hand side of (2.23) are estimated by using the

Gagliardo–Nirenberg inequality in the form given in [8, Chapter II, Theo-

rem 2.2], as follows:

(2.24)

RHS of (2.23) ≤γ

(supt∈Ij

1

rnj

∫Lj(t)

v2

m−λ

j dx

)2n(δm−1j

rnj

∫∫Lj

∣∣∣∇(vjξ

k−22

j

)∣∣∣2dxdt)

(supt∈Ij

1

rnj

∫Lj(t)

w2

1−λ

j dx

)2n(lm−1j

rnj

∫∫Lj

∣∣∣∇(wjξ

k−22

j

)∣∣∣2dxdt).

Let us estimate separately the first factors in both terms of the right hand

side of (2.24):

(2.25)

supt

1

rnj

∫Lj(t)

v2

m−λ

j dx+ supt

1

rnj

∫Lj(t)

w2

1−λ

j dx

by (2.21), (2.22)

≤ c−1 supt

1

rnj

∫Lj(t)

u− ljδj

dx

by (2.15)

≤ 2c−1 supt

1

rnj

∫Lj(t)

u− lj−1

δj−1ξkj−1 dx

by (2.17), (2.12)

≤ γ supt

1

rnj−1

∫Lj−1(t)

G

(u− lj−1

δj−1

)ξkj−1 dx

by (2.13)

≤ γκ.

Combining (2.23), (2.24) and (2.25) we obtain

1

rn+2j

∫∫L′′

j

um−1

(u− ljδj

)1+λ

ξk−2j dxdt

≤ γ(ε)κ2n

(δm−1j

rnj

∫∫Lj

∣∣∣∇(vjξ

k−22

j

)∣∣∣2 dxdt+ lm−1j

rnj

∫∫Lj

∣∣∣∇(wjξ

k−22

j

)∣∣∣2 dxdt).

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270 V. LISKEVICH AND I. I. SKRYPNIK Isr. J. Math.

To estimate the right hand side of the above inequality we start with the terms

containing ∇ξj :

(2.26)δm−1j

rnj

∫∫Lj

v2j |∇ξj |2 ξk−4j dx dt+

lm−1j

rnj

∫∫Lj

w2j |∇ξj |2 ξk−4

j dx dt

≤γ1

rn+2j

(δm−1j

∫∫Lj

(u− ljδj

)m−λ

dx dt+ lm−1j

∫∫Lj

(u− ljδj

)1−λ

dx dt

)

( by (2.15))

≤γ1

rn+2j

∫∫Lj

um−1

(u− lj−1

δj−1

)1−λ

ξk−2j−1 dx dt

(by using the decomposition (2.19) and (2.16))

≤γε1−λκ + γ

1

rn+2j−1

∫∫Lj−1

um−1

(u− lj−1

δj−1

)1+λ

ξk−2j−1 dx dt ≤ γκ.

For the terms with ∇vj and ∇wj we use Lemma 2.2:

(2.27)

δm−1j

rnj

∫∫Lj

|∇vj |2ξk−2j dx dt+

lm−1j

rnj

∫∫Lj

|∇wj |2ξk−2j dx dt

≤γ1

τjrnj

∫∫Lj

u− ljδj

ξk−3j dxdt

+ γ1

rn+2j

∫∫Lj

um−1

(1 +

u− ljδj

)1−λ(u− ljδj

)2λ

ξk−4j dxdt

+ γτjrnj

δ−1j μ(Bj).

For the first term on the right-hand side of (2.27) we have

(2.28)

1

τjrnj

∫∫Lj

u− ljδj

ξk−3j dxdτ ≤γ

1

rnjsupt∈Ij

∫Lj(t)

u− ljδj−1

dx

≤γ1

rnjsupt∈Ij

∫Lj−1(t)

G

(u− lj−1

δj−1

)ξkj−1dx

≤γκ.

The second term of the right-hand side of (2.27) is estimated by γκ using

the decomposition (2.19).

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Vol. 194, 2013 POROUS MEDIUM EQUATION 271

Thus we obtain the following estimate for the first term of Aj(lj+1):

(2.29)1

rn+2j

∫∫Lj

um−1

(u− ljδj

)1+λ

ξk−2j dxdτ

≤ γε1+λκ + γ(ε)κ

2n

(κ +

τjrnj

δ−1j μ(Bj)

).

Let us estimate the second term in the right-hand side of (2.9). By Lemma 2.2

with l = lj, δ = δj , using the decomposition (2.19), (2.16) and finally estimate

(2.29), we have

(2.30) supt∈Ij

1

rnj

∫Lj(t)

G

(u− ljδj

)ξkj dx

≤ γε1+λκ + γ(ε)κ

2n

(κ + δ−1

j

τjrnj

μ(Bj)

)+ γδ−1

j

τjrnj

μ(Bj).

Combining (2.12), (2.29) and (2.30), and choosing ε appropriately, we can

find γ1 and γ such that

(2.31) κ ≤ γ1κ2n

(κ + δ−1

j

τjrnj

μ(Bj)

)+ γδ−1

j

τjrnj

μ(Bj).

Now choosing κ < 1 such that κp/n = 1/2γ1 we have

(2.32) δj ≤ γτjrnj

μ(Bj) = γ1

rn−2j Δm−1

j

μ(Bj).

Taking into account that

Δm−1j ≥ Δm−1

0 = δm−10 ≥ r20

θ 0,

we obtain

δj ≤ γθ0r20

1

rn−2j

μ(Bj),

which completes the proof of the lemma.

In order to complete the proof of Theorem 1.1 we sum up (2.14) with respect

to j from 1 to J − 1

(2.33)

lJ ≤γδ0 + γ

∞∑j=1

(r2jθj

) 1m−1

+ γ

∞∑j=1

r2−nj μ(Bj)

≤γ

(δ0 + γ

(r20θ0

) 1m−1

+ γ

(1 +

θ0r20

)Iμ2 (x0, r0)

).

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272 V. LISKEVICH AND I. I. SKRYPNIK Isr. J. Math.

Let us estimate δ0. There are two cases to consider. Either

l1 = δ0 =

(r20θ0

) 1m−1

,

or l1 and δ0 are defined by A0(l1) = κ.

In this case

θ0Δm−10 > r20 .

Then by (2.12) we have

(2.34)

κ =1

rn+20

∫∫Q0

um−1

(u+

δ0

)1+λ

ξk−20 dx dτ + sup

tr−n0

∫B0

G

(u+

δ0

)ξk0 dx

≤ 1

rn+20

∫∫Q0

um−1

(u+

δ0

)1+λ

ξk−20 dx dτ + sup

tr−n0

∫B0

u+

δ0ξk0 dx.

Hence we obtain that

(2.35) δ0 ≤ γ

(1

rn+20

∫∫Q0

um+λ+ dxdt

) 11+λ

+ γ1

rn0supt

∫B0

u+dx.

This proves the first assertion.

By Lemma 2.2

(2.36)

r−n0

∫L0(t)

G

(u

δ0

)ξk0dx ≤γτ−1

0 r−n0

∫∫L0

u+

δ0ξk−10 dxdτ

+ γr−2−n0

∫∫L0

um−1(1 +

u

δ0

)1−λ(u+

δ0

)2λξk−20 dxdτ

+ γθ0r20

r2−n0 δ−1

0 μ(B0(x0))

≤γτ−10 r−n

0

∫∫L0

u+

δ0ξk−10 dxdτ

+ γr−2−n0

∫∫Q0

um−1(u+

δ0

)2λξk−20 dxdτ

+ γr−2−n0

∫∫Q0

um−1(u+

δ0

)1+λ

ξk−20 dxdτ

+ γθ0r20

r2−n0 δ−1

0 μ(B0(x0)).

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Vol. 194, 2013 POROUS MEDIUM EQUATION 273

Hence we obtain from (2.12) that

(2.37)

δ0 ≤γ

(1

rn+20

∫∫Q0

um+λ+ dxdτ

) 11+λ

+ γ

(1

rn+20

∫∫Q0

um−1+2λ+ dxdτ

) 12λ

+r20θ0

1

rn+20

∫∫Q0

u+dxdτ + γθ0r20

r2−n0 μ(B0(x0)).

This completes the proof of the second assertion.

Proof of Corollary 1.3. Direct analysis of the proof of Theorem 1.1 shows that

for the solution to (1.7), estimate (1.5) holds for any (x0, t0) ∈ Q = BR× (0, T ).

Let M := supQ u. Hence from Theorem 1.1 we have

(2.38)

M ≤γ

(1

Rn+2

∫∫Q

um+λdx dt

) 11+λ

+ γ supt

∫BR

udx

+ γ

(R2

T

) 1m−1

+ γ

(1 +

T

R2

)supx∈BR

Iμ2 (x, 2R).

Using

ϕ =u

u+ ε, ε > 0,

as a test function and subsequently passing to the limit ε → 0, we obtain

(2.39) supt

1

Rn

∫BR×{t}

udx ≤ T

Rnμ(BR) ≤ T

R2Iμ2 (0, 2R).

Let us estimate the first integral on the right-hand side of (2.38). By the

Poincare inequality we have

1

Rn+2

∫∫Q

um+λdx dt ≤ 1

Rn

∫∫Q

um+λ−2|∇u|2dx dt.

Multiplying the equation by u(u + ε)λ−1 with ε > 0, integrating by parts and

passing to the limit as ε → 0, we obtain∫∫Q

um+λ−2|∇u|2dx dt ≤∫∫

Q

uλdμ dt ≤ MλTμ(BR).

Taking the above into account and applying the Young inequality we see that(

1

Rn+2

∫∫Q

um+λdx dt

) 11+λ

≤γMλ

λ+1

(T

R2Iμ2 (0, 2R)

) 1λ+1

≤1

2M + γ

T

R2Iμ2 (0, 2R).

This completes the proof of (1.8).

Page 16: Pointwise estimates for solutions to the porous medium equation with measure as a forcing term

274 V. LISKEVICH AND I. I. SKRYPNIK Isr. J. Math.

Proof of Theorem 1.5. The proof follows the same lines as the proof of Theo-

rem 1.1. So we only explain the required modifications.

In Lemmas 2.1 and 2.2 the obvious modification is to replace τμ(Br(x0)) by

μ(Qr). The sequence (lj) will start from l0 = 1, and the formula for τj(l) in (2.8)

is replaced by τj(l) = r2j /Δm−1j (l). In the alternative (2.10), (2.11) governing

the choice of lj+1 the quantity(r2j /θj

) 1m−1 should be replaced by μ(Qrj ). In

the formulation of Lemma 2.3 inequality (2.14) is replaced by

δj ≤ 2−1

m−1 δj−1 + γ1

rnjμ(Qrj ).

The last terms in the right-hand sides of (2.27), (2.29), (2.30) require obvious

replacement of τjμ(Qrj ). Inequality (2.33) will be rewritten as

lJ ≤ γ(δ0 + Iμ2 (x0, t0, r0)).

One can also provide the analogue of the second assertion of Theorem 1.1

with obvious changes in (2.36) and (2.37). We leave this to the reader.

Acknowledgement. This paper was completed when the first-named author

was visiting the Department of Mathematics at the Technion. The support

of the British Technion Society is gratefully acknowledged. The first-named

author would like to thank the Department of Mathematics at the Technion for

its warm hospitality. Special thanks go to Moshe Marcus and Yehuda Pinchover

for useful discussions.

References

[1] P. Daskalopoulos and C. Kenig, Degenerate Diffusions. Initial Value Problems and Local

Regularity Theory, EMS Tracts in Mathematics, 1, European Mathematical Society,

Zurich, 2007.

[2] E. De Giorgi, Sulla differenziabilita e l’analiticita delle estremali degli integrali multi-

pli regolari, Memorie dell’Accademia delle Scienze di Torino. Classe di Scienze Fisiche,

Matematiche e Naturali 125 (1957), 25–43.

[3] E. DiBenedetto, U. Gianazza and V. Vespri, Harnack’s Inequality for Degenerate and

Singular Parabolic Equations, Springer, 2012.

[4] E. DiBenedetto, J. M. Urbano and V. Vespri, Current issues on singular and degenerate

evolution equations, in Handbook of Differential Equations. Evolutionary Equations.

Vol. I (C. Dafermos and E. Feireisl, eds.), Elsevier, Amsterdam, 2004, pp. 169–286.

[5] F. Duzaar and G. Mingione, Gradient estimates via non-linear potentials, American

Journal of Mathematics 133 (2011), 1093–1149.

Page 17: Pointwise estimates for solutions to the porous medium equation with measure as a forcing term

Vol. 194, 2013 POROUS MEDIUM EQUATION 275

[6] M. de Guzman, Differentiation of Integrals in Rn, Lecture Notes in Mathematics 481,

Springer, Berlin, 1975.

[7] T. Kilpelainen and J. Maly, The Wiener test and potential estimates for quasilinear

elliptic equations, Acta Mathematica 172 (1994), 137–161.

[8] O. A. Ladyzhenskaja, V. A. Solonnikov and N. N. Uraltceva, Linear and Quasilinear

Equations of Parabolic Type, Translations of Mathematical Monographs, Vol. 23, Amer-

ican Mathematical Society, Providence, RI, 1967.

[9] J.-L. Lions, Quelques methodes de resolution des problemes aux limites non lineaires

(French), Dunod; Gauthier-Villars, Paris, 1969.

[10] V. Liskevich and I. I. Skrypnik, Harnack inequality and continuity of solutions to quasi-

linear degenerate parabolic equations with coefficients from Kato-type classes, Journal

of Differrential Equations 247 (2009), 2740–2777.

[11] V. Liskevich, I. I. Skrypnik and Z. Sobol, Potential estimates for quasi-linear parabolic

equations, Advanced Nonlinear Studies 11 (2011), 905–915.

[12] J. Maly and W. Ziemer, Fine Regularity of Solutions of Elliptic Partial Differential

Equations, Mathematical Surveys and Monographs, 51, American Mathematical Society,

Providence, RI, 1997.

[13] I. I. Skrypnik, On the Wiener criterion for quasilinear degenerate parabolic equations

(Russian), Rosiıskaya Akademiya Nauk. Dokladi Akademii Nauk 398 (2004), 458–461.

[14] J. L. Vazquez, Smoothing and Decay Estimates for Nonlinear Diffusion Equations. Equa-

tions of Porous Medium Type, Oxford Lecture Series in Mathematics and its Applica-

tions, 33, Oxford University Press, Oxford, 2006.

[15] J. L. Vazquez, The Porous Medium Equation. Mathematical Theory, Oxford Mathemat-

ical Monographs, The Clarendon Press, Oxford University Press, Oxford, 2007.

[16] Zh. Wu, J. Zhao, J. Yin and H. Li, Nonlinear Diffusion Equations, World Scientific,

Singapore, 2001.