Nonsymmetric conical upper density and $k$-porosity
Antti K\"aenm\"aki, Ville Suomala

TL;DR
This paper investigates the distribution of Hausdorff measure in nonsymmetric cones and establishes an upper bound near $n-k$ for the dimension of $k$-porous sets, which have holes in multiple directions at small scales.
Contribution
It introduces new bounds on Hausdorff dimension for $k$-porous sets based on measure distribution in nonsymmetric cones.
Findings
Upper bound close to $n-k$ for Hausdorff dimension of $k$-porous sets
Distribution analysis of Hausdorff measure in nonsymmetric cones
Characterization of sets with holes in multiple directions
Abstract
We study how the Hausdorff measure is distributed in nonsymmetric narrow cones in . As an application, we find an upper bound close to for the Hausdorff dimension of sets with large -porosity. With -porous sets we mean sets which have holes in different directions on every small scale.
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Nonsymmetric conical upper density and -porosity
Antti Käenmäki
and
Ville Suomala
Department of Mathematics and Statistics
P.O. Box 35 (MaD)
FI-40014 University of Jyväskylä
Finland
Abstract.
We study how the Hausdorff measure is distributed in nonsymmetric narrow cones in . As an application, we find an upper bound close to for the Hausdorff dimension of sets with large -porosity. With -porous sets we mean sets which have holes in different directions on every small scale.
Key words and phrases:
Conical density, porosity, Hausdorff dimension.
2000 Mathematics Subject Classification:
Primary 28A75; Secondary 28A78, 28A80.
AK acknowledges the support of the Academy of Finland (project #114821)
1. Introduction
It is a well known fact that for a set with finite -dimensional Hausdorff measure, , we have
[TABLE]
for -almost every . For a proof, see, for example, [12, Theorem 6.2(1)]. This is analogous to the classical Lebesgue Density Theorem. Using this fact, we know roughly how much of there is in small balls. Mattila [11] studied how is distributed in such balls. He was able to estimate how much of there is near -planes. More precisely, assuming and denoting
[TABLE]
as , , , and , he proved that there exists a constant such that
[TABLE]
for -almost every whenever is such that . Here denotes the collection of all -dimensional linear subspaces of , see [12, §3.9]. Actually (1.2) is just a special case of Mattila’s result, as his theorem can be applied also for more general cones, see [11, Theorem 3.3].
In Theorem 2.5 we show that if is as above, then it cannot be concentrated in too small regions, not even inside the cones . More precisely, denoting
[TABLE]
for , , and , we prove under the same assumptions as in (1.2) that there exists a constant such that
[TABLE]
for -almost every . Here denotes the unit sphere of . To help the geometric visualization, it might be helpful to take and close to [math] and . Our method gives also a more elementary proof for (1.2) and it can also be used to obtain similar results for more general measures, see Theorem 2.7.
The nonsymmetric conical upper density theorem is essential in our application to -porous sets, that is, the sets with , see (1.5). The notation of porosity, or -porosity using our terminology, has arisen from the study of dimensional estimates related, for example, to the boundary behavior of quasiconformal mappings. See Koskela and Rohde [9], Martio and Vuorinen [10], Sarvas [15], Trocenko [17], and Väisälä [18]. The dimensional properties of -porous sets are well known. Using a version of (1.2), Mattila showed that if porosity is close to its maximum value , then the dimension cannot be much bigger than . More precisely,
[TABLE]
as . Here refers to the Hausdorff dimension. Later Salli [14] generalized this result for the Minkowski dimension, and found the correct asymptotics. The concept of -porosity has also been generalized for measures, and it leads to similar kind of dimension bounds. See Järvenpää and Järvenpää [4] and references therein.
Motivated by the fact that each has maximal -porosity, we introduce a porosity condition which describes also sets whose dimension is smaller than . For any integer , , , and we set
[TABLE]
Here is the inner product. The -porosity of at a point is defined to be
[TABLE]
and the -porosity of is given by
[TABLE]
This means that -porous sets have holes in orthogonal directions near each of its points in every small scale. We shall now give a concrete example where -porosity occurs naturally. Suppose and let be the usual -Cantor set, see [12, §4.10]. It is clearly a -porous set with . Mattila’s result (1.3) implies that as . Of course, we could obtain the same information just by calculating the Hausdorff dimension of the self-similar set and letting , but our aim was to provide the reader with an illustrative example. The sets and are clearly -porous with . For these sets (1.3) does not give any reasonable dimension bound. However, it would be desirable to see, also in terms of porosity, that and as . This follows as an immediate application of Theorem 3.2. Using our nonsymmetric conical upper density theorem, we show that
[TABLE]
as . Observe also that in the proof of Theorem 3.2 the orthogonality in (1) plays no rôle and we may replace it by an assumption of a uniform lower bound for the angles between and the -plane spanned by vectors , .
Let us now discuss the situation when porosity is small. It is well known (for example, see [10]) that if with for all and , then
[TABLE]
where depends only on , and refers to the Minkowski dimension, see [12, §5.3]. It might be possible to get a better estimate if is replaced by for some , but this condition does not feel very natural if the size of the holes is small. However, if is fixed and the condition is replaced by
[TABLE]
then in (1.6) can be replaced by , see Theorem 4.3. This is a rather immediate consequence of (1.6), but our main point is to give a simple proof for (1.6) using iterated function systems.
Acknowledgement*.*
The authors are indebted to Professor Pertti Mattila for his valuable comments for the manuscript. The authors thank also Esa Järvenpää, Maarit Järvenpää, Pekka Koskela, Tomi Nieminen, Kai Rajala and Eero Saksman for useful discussions during the preparation of this article.
2. Nonsymmetric conical upper density
We shall first prove a density theorem for nonsymmetric regions and then prove our main theorem by using a similar argument on -planes. The proofs rely on the following geometric fact.
Lemma 2.1**.**
For given , there is such that in any set of points in , there are always three points which determine an angle between and .
Remark 2.2*.*
Erdős and Füredi [1] have shown that for the smallest possible choice of it holds that
[TABLE]
For the convenience of the reader we shall give below a different proof which establishes the existence of some such . The estimate that we get here for is, however, quite bad compared to the best possible one.
Proof.
Let be a set of points in so that all angles formed by its points are less than . Let us fix and cover by cones , , where the constant depends only on and . To visualize the situation, note that if is close to , then is close to and cones are very narrow. To simplify the notation, we denote for .
For any index , where and for , we define sets in the following way: We begin by fixing and setting for . If has been defined, we choose and define for (if is empty, then so is ). We refer to as the corner of . It follows directly from the definition of the sets that
[TABLE]
Iterating this, we get
[TABLE]
The main point of the proof is the observation that if is chosen to be close enough to in the beginning, then the following is true: If and are the corners of and , respectively, and if , then . See Figure A. It follows by induction from the above fact that for given we have
[TABLE]
In particular, for any choice of . Combined with (2.1), this gives . This number depends only on and the claim follows. ∎
For we define
[TABLE]
Notice that and .
Lemma 2.3**.**
Suppose that , , , , and . If z\in\mathbb{R}^{n}\setminus\bigl{(}B(y,tr)\cup H(y,\theta,\gamma)\bigr{)}, then
[TABLE]
Proof.
Take such that it maximizes in the closure of . It suffices to prove that , see Figure B. It is straightforward to check that when . Denoting now , we have and thus
[TABLE]
which finishes the proof. ∎
Theorem 2.4**.**
Suppose and . Then there is a constant such that
[TABLE]
for almost every whenever with .
Proof.
Take and assume that there exists a Borel set with such that for each and there is for which
[TABLE]
It suffices to find a positive lower bound for in terms of , , and .
Using (1.1), and replacing by a suitable subset if necessary, we may assume that
[TABLE]
for all and . Moreover, using the lower estimate of (1.1), we find and such that
[TABLE]
Set , , and take . Let us fix such that the opening angle of is smaller than , and let be as in Lemma 2.1. We may cover the set by balls of radius with centers in . Using (2.4), we notice that there exists such that
[TABLE]
The set can also be covered by balls of radius with centers in . Whence, using (2.3) and (2.4),
[TABLE]
If , we find for which
[TABLE]
Choosing small enough and continuing in this manner, we find points with for , such that for each we have
[TABLE]
where .
According to Lemma 2.1, we may choose three points from the set such that for each there is for which y_{i}\in\mathbb{R}^{n}\setminus\bigl{(}B(y,t\delta r)\cup H(y,\theta,\gamma)\bigr{)}. We obtain, using Lemma 2.3, that for each there is such that
[TABLE]
Thus, applying (2.5), we have
[TABLE]
for all . Recalling (2.2), we conclude that . The proof is finished. ∎
Theorem 2.5**.**
Suppose and . Then there is a constant such that
[TABLE]
for almost every whenever with .
Proof.
For any , we set . With this metric is a compact metric space, see Salli [13]. Defining for each a set we notice that a finite number of these sets is still a cover. We assume that the sets assigned to the planes , where , cover . For any , it holds that with some . This implies . Thus, for each , there is such that
[TABLE]
for all and . We shall prove that if with , then
[TABLE]
for almost every from which the claim follows easily by using (2.6).
Take and assume that there is a Borel set with such that for each and there are and for which
[TABLE]
According to (1.1) we may assume that
[TABLE]
for all and . Using the lower estimate of (1.1), we find and such that
[TABLE]
Next we define
[TABLE]
Since , we infer from (2.8) that there is for which
[TABLE]
Let , choose as in the proof of Theorem 2.4, and define so that
[TABLE]
recall that so that this is possible. Since the set may be covered by balls of radius , there exists such that
[TABLE]
We now argue as in the proof of Theorem 2.4 above. We first observe that the slice S=B_{i_{0}}\cap B(x,r)\cap P_{V_{i_{0}}^{\bot}}^{-1}\bigl{(}B(y,\varepsilon r)\bigr{)} may be covered by balls of radius for a constant . Then we use (2.11), (2.7), and (2.10) to find points such that whenever and
[TABLE]
for all . Here . Now the same geometric argument as in the proof of Theorem 2.4 implies that there is a point such that for each we may find so that
[TABLE]
Since also
[TABLE]
see Figure C, we get
[TABLE]
by (2.12). Now and we conclude, using (2.9), that . This completes the proof. ∎
Remark 2.6*.*
Inspecting the proofs, one can read explicit expressions for the constants in Theorems 2.4 and 2.5. In Theorem 2.4, one gets and in Theorem 2.5, one obtains . The constants here depend only on . The estimates obtained in this way are probably rather far from being optimal, although the best values are not known.
Our method can be applied also in a more general setting. A similar proof as above gives the following result. If is a measure on , , and , we define and as the lower and upper limits, respectively, of the ratio \mu\bigl{(}B(x,r)\bigr{)}/h(r) as .
Theorem 2.7**.**
Suppose and is a function with
[TABLE]
as . Let be a measure on with for -almost all . For every , there is a constant such that
[TABLE]
for -almost every .
Let us make few comments related to the above theorem. Suppose that fulfills condition (2.13). Let be the generalized Hausdorff measure which is constructed using as a gauge function, see [12, §4.9]. If , where , then for -almost every , and thus Theorem 2.7 can be applied.
There are many natural gauge functions, such as where , which satisfy (2.13). However, some interesting cases, such as , are not covered by this condition.
It seems to be unknown whether a similar result as Theorem 2.7 holds if one replaces the condition by . The most interesting example falling into this category is obtained when and , where and . Here denotes the -dimensional packing measure, see [12, §5.10]. See also Suomala [16] for related theorems.
3. Sets with large -porosity
Mattila [11] proved Theorem 2.5 in the case . Using this, he obtained the desired dimension bounds for -porous sets, see (1.3). Our result for -porous sets follows applying a similar argument.
For we define
[TABLE]
Notice that as .
Lemma 3.1**.**
Suppose , , , , and . If is such that , then
[TABLE]
where .
Proof.
To simplify the notation, we assume , , and . This will not affect the generality. Let . We have to show that
[TABLE]
By the Pythagorean Theorem we have
[TABLE]
Using this, we obtain
[TABLE]
which implies (3.1). ∎
Theorem 3.2**.**
Suppose . Then
[TABLE]
as .
Proof.
Assume on the contrary that there exists such that for each there is a set for which and . Take and such a set . Now has a subset for which and for all and with some . Clearly also the closure of satisfies these conditions. Thus there is a closed set (for example, use [2, Theorem 5.4]) such that and
[TABLE]
Therefore, for any and , there are such that for , and for . Put .
Applying now Lemma 3.1 we have for every . Here and . Thus
[TABLE]
Put and take such that for every . Now choosing and small enough, we have, using (3.2), that
[TABLE]
Observe that the choice of and does not depend on and hence not on either. Figure D illustrates the situation. Using Theorem 2.5, we may fix and for which
[TABLE]
where . By (1.1) we may assume that also
[TABLE]
Combining (3.3)–(3.5), we have and hence
[TABLE]
But the constant does not depend on , and thus as giving a contradiction. ∎
4. Sets with small porosity
Finally, let us briefly discuss the situation when porosity is small. The proof of the following theorem can be found for example in Martio and Vuorinen [10]. We shall give here a different proof, and then show how the theorem can be improved when more information on the location of the holes is given.
Theorem 4.1**.**
Let be bounded and suppose that for all and . Then , where depends only on .
Proof.
We may assume that and . Let us denote by the collection of all closed dyadic cubes with side length . Let be the smallest integer with . It is easy to see that for any there is such that and . Let us fix one such for each . Next we define a set by setting
[TABLE]
For any , let be the corner of which is nearest to the origin, and let . If we define by setting
[TABLE]
where int denotes the interior of a given set, then obviously , see also [7]. The set is the limit set of the iterated function system defined by the similitudes , , see Figure E. For any , there are similitudes among with contraction ratio . Since the open set condition is clearly satisfied, the dimension is given by
[TABLE]
see Hutchinson [3, §5]. This reduces to
[TABLE]
and since \log_{2}(1+x)\geq x/\bigl{(}(1+x)\log 2\bigr{)} for , we have
[TABLE]
where c=\bigl{(}2/(5\log 2)\bigr{)}2^{-3n}n^{-n/2}. Because and , we conclude that also . ∎
In the above proof, the use of the self-similar set is not a necessity, but it concretizes the situation. The key point in the proof is that for any cube which is small enough, one can find subcubes such that and , where is given by (4.2). From this the desired dimension bound follows easily.
Remark 4.2*.*
In a sense the above result is the best possible one. There is a constant and sets , , with , and for all and . See, for example, Koskela and Rohde [9], or estimate the Hausdorff dimension of the set from below.
Theorem 4.3**.**
Let be bounded and suppose that there is such that for all and one has
[TABLE]
Then , where depends only on and .
Proof.
Without losing the generality we may assume that , , and . Let be, as before, the collection of all closed dyadic cubes with side length , and let and . Here is the orthogonal projection onto . Furthermore, let be the smallest integer with .
We define a set as in the proof of Theorem 4.1. For we let denote the minimum number of cubes from the collection that are needed to cover . The proof of Theorem 4.1 yields that
[TABLE]
where is an absolute constant.
It is straightforward to convince oneself of the following fact: If and , then there is such that , , and . From this observation it follows that given , only cubes from the collection touch the set . Thus only cubes from the collection are needed to cover . Using (4.4), we calculate
[TABLE]
The proof is finished. ∎
Remark 4.4*.*
Suppose that is fixed and is such that (4.3) holds for every and , where depends on the point . It follows immediately from Theorem 4.3 that , where is as in Theorem 4.3 and denotes the packing dimension, see [12, §5.9]. The above dimension estimates are also sharp. Consider, for example, sets of the form , where is as in the proof of Theorem 4.1.
Remark 4.5*.*
After the submission of this article in May 2004, there has been considerable progress in the study of conical densities and porosities. Most notably, the question posed after Theorem 2.7 has been answered positively in [8]. For improvements of Theorems 3.2 and 4.1, see [6] and [5], respectively.
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