On certain orbits of geodesic flow and (a,b)-continued fractions
Manoj Choudhuri

TL;DR
This paper characterizes special geodesic orbits on the Modular surface using a two-parameter family of continued fractions, extending the connection between dynamics and number theory.
Contribution
It introduces a new characterization of exceptional geodesic orbits via (a,b)-continued fractions, expanding the Dani correspondence framework.
Findings
Identification of two types of exceptional orbits
Extension of Dani correspondence to new continued fraction families
Enhanced understanding of geodesic flow and Diophantine approximation
Abstract
In this article, we characterize two kinds of exceptional orbits of the geodesic flow associated with the Modular surface in terms of a two-parameter family of continued fraction expansion of endpoints of the lifts to the hyperbolic plane of the corresponding geodesics. As a consequence, we obtain an extension of Dani correspondence between homogeneous dynamics and Diophantine approximation.
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Taxonomy
TopicsMathematical Dynamics and Fractals · Advanced Differential Equations and Dynamical Systems · Quantum chaos and dynamical systems
On certain orbits of geodesic flow and -continued fractions
Manoj Choudhuri,
Institute of Infrastructure Technology Research and Management,
*Near Khokhara Circle, Maninagar (East),
Ahmedabad-380026, Gujarat, India
*email: [email protected]
Abstract
In this article, we characterize two kinds of exceptional orbits of the geodesic flow associated with the Modular surface in terms of a two-parameter family of continued fraction expansion of endpoints of the lifts to the hyperbolic plane of the corresponding geodesics. As a consequence, we obtain an extension of Dani correspondence between homogeneous dynamics and Diophantine approximation.
Keywords : Geodesic flow; Modular surface; continued fractions; coding of geodesics.
Mathematics Subject Classification: 37A17, 11J70, 53C22.
1 Introduction
Let be the upper half plane endowed with the hyperbolic metric . The group acting by fractional linear transformations (see [11]), is the orientation preserving isometry group of . The discrete group acting properly discontinuously on gives rise to the modular surface , which is topologically a sphere with two singularities and one cusp. Let be the unit tangent bundle of the hyperbolic plane which is the collection with in and being a tangent vector of norm one in ; acts on as well and the quotient space can be identified with the unit tangent bundle of , which we denote by . We denote by . Any determines a unique geodesic in . If we consider the geodesic along with its tangent vector at each point, then it is the orbit of under the geodesic flow. This orbit is denoted by , where denotes the geodesic flow on . It is well known that the geodesic flow on is ergodic with respect to the Liouville measure (see [5] for more details and original references). This means in particular that with respect to the Liouville measure, the orbits of almost all in are equidistributed, i. e., if denotes the (normalized) Liouville measure on , then for almost all ,
[TABLE]
for any measurable , where denotes the characteristic function of the set . Apart from these generic orbits there are many interesting orbits of geodesic flow associated with the modular surface. By Dani correspondence (see [3], [4] for details), we know that badly approximable numbers (see [9] for definition) correspond to bounded orbits and rational numbers correspond to divergent orbits. In this article, we are going to characterize two kinds of orbits in terms of their asymptotic rate of time spent in cusp neighbourhoods. One of these kinds of orbits contains the bounded orbits and the other one contains the divergent orbits. These characterizations are done in terms of the continued fraction expansions of certain real numbers associated with those orbits. In order to do so, we use arithmetic coding of geodesics on the modular surface which was originated in the 1924 paper of E. Artin ([1]), who proved the existence of a dense geodesic using classical continued fraction. A more precise description of this machinery using classical continued fraction can be found in [15]. We do not restrict ourselves to only classical continued fraction, rather we consider a two-parameter family of continued fractions and obtain the characterizations in terms of that family, from which the characterizations in terms of the classical continued fraction follow.
The two-parameter family of continued fractions we are going to consider in this article is known as -continued fractions with , satisfying a technical condition (see next section for more details about -continued fractions). Using these continued fraction expansions of real numbers, in [14], S. Katok and I. Ugarcovicci describe a coding of geodesics on the modular surface, which enables one to give a symbolic description of the geodesic flow associated with the modular surface. We use this coding of geodesics, which also relies on another paper ([13]) by the same authors, as a base of the arguments, used to prove the results of the present article. In this article, we consider -continued fractions for in a particular subset of , where is given as follows:
.
Note that this excludes the possibilities and , though in the work of Katok and Ugarcovicci ([13], [14]) those possibilities were also considered with . Also let be the exceptional set discussed in [13], the elements of which do not satisfy the finiteness (see next section for the definition) condition. Let
[TABLE]
(see next section for definition of cycle properties) and
[TABLE]
Now let and be given by
[TABLE]
where denotes the imaginary part of the complex number , and denotes the set of unit tangent vectors in . Let denote both the projections from to and from to . Also let and . Note that is a typical neighbourhood of the cusp in . We say that an orbit visits the cusp with frequency [math], if there exists some such that as . On the other hand, an orbit is said to visit the cusp with frequency , if for all , as . Now let and be its -continued fraction expansion. Given and , we define the modified partial quotients of the -continued fraction expansion of as follows:
[TABLE]
Theorem 1.1**.**
For a given , let be the corresponding geodesic in , and be one of its lifts to the hyperbolic plane. Let be the attracting end point of . For , let the -continued fraction expansion of be given by . Also for , let be the modified sequence of partial quotients as defined above, and
[TABLE]
*Then,
the forward orbit visits the cusp with frequency [math] if and only if
as for some , and
visits the cusp with frequency if and only if as .*
Remark 1.2**.**
The restriction of the parameters to the set ensures that any geodesic in is -equivalent to an -reduced geodesic (a notion to be made clear in the next section). This is essential for this article as we are not looking at a generic set of orbits of the geodesic flow. It follows from Theorem of [13] that if and have the strong cycle property, then every geodesic in is -equivalent to an -reduced geodesic, whereas in [12], the same statement was shown to be true for . It is easy to see that -continued fraction expansion of a real number is nothing but the classical continued fraction expansion of with alternating signs (see [12] for details). A similar relation holds between -continued fraction expansion and the nearest integer continued fraction expansion of a real number. Then the characterizations in Theorem 1.1 in terms of the classical and the nearest integer continued fractions follow from the characterizations in terms of and -continued fractions respectively.
If we consider the algebraic description of the geodesic flow, then Theorem 1.1 may be thought of as an extension of Dani correspondence between homogeneous dynamics and Diophantine approximation. We know that can be identified with (see [11] for details), where the identification is given by
for , here denotes the unit tangent vector based at the point and pointing upwards. Similarly can be identified with . The right action of the one parameter subgroup
on , which is given by the following:
, for ,
where we denote by , corresponds to the geodesic flow on . Given a real number , let
[TABLE]
Then the simplest form of Dani correspondence says that the orbit is bounded (relatively compact) in if and only if is a badly approximable number. On the other hand is divergent if and only if is rational. It is well known (see [9] for instance) that a real number is badly approximable if and only if the partial quotients in the classical continued fraction of are bounded. The same is true for -continued fraction expansion of with and because the -continued fraction expansion of is nothing but the classical continued fraction expansion of with alternating signs. In Remark of [2], it was shown that a number is badly approximable if and only if the partial quotients in its -continued fraction expansion are bounded. By the same reasoning (with the help of Proposition 2.5), the same assumption is true for -continued fraction as well for . So, in the statement of Dani correspondence, the term badly approximable can be replaced by partial quotients in the -continued fraction expansion of being bounded, and the rational numbers can be replaced by having a finite -continued fraction expansion. Then one may think of Theorem 1.1 as en extension of Dani correspondence stated above.
Remark 1.3**.**
Let
[TABLE]
and
[TABLE]
Then has Hausdorff dimension , since it contains the set of badly approximable numbers and it was shown by Jarnik in [10] that the set of badly approximable numbers has Hausdorff dimension . On the other hand, it was shown in [6] that if (see below for definition) is the classical continued fraction expansion of , then the set of those for which as , has Hausdorff dimension . Then it follows that has Hausdorff dimension .
Above remark ensures that is a bigger set than the set of rational numbers as the set of rational numbers has Hausdorff dimension [math]. Now we show that contains some very well approximable numbers. A real number is said to be very well approximable if there exists , such that holds for infinitely many and . Recall that each real number has a classical continued fraction expansion
[TABLE]
written as with denoting the th convergent (see [9] for more details). Now construct a real number using classical continued fraction with the choice of ’s as follows. Fix some , choose and arbitrarily, and inductively choose for . Then as is an increasing sequence, is also an increasing sequence and consequently as . Hence, . On the other hand, it follows from the construction of , that the sequence of convergents satisfy the inequality for all , showing that is a very well approximable number. Note that can not contain all very well approximable numbers as the set of very well approximable numbers has Hausdorff dimension ([10]) and has Hausdorff dimension .
Summary of revisions over the previous version:
We have done some rearrangements and modifications in the introduction which leads to a modification in the exposition of the article. Accordingly, we have chosen a better-suited title and modified the abstract. 2. 2.
In the present version of the article, the set of parameters which is an important object in Theorem 1.1, now has a more restricted description compared to the one in the previous version.
2 (a,b)-continued fractions and geodesic flow
Following S. Katok and I. Ugarcovicci ([13]), for , the -continued fraction expansion of a real number can be defined using a generalized integral part function:
[x]_{a,b}:=\left\{\begin{array}[]{lr}[x-a]\hskip 11.38092pt\text{if}\hskip 5.69046pt\text{x<a}\\ 0\hskip 42.67912pt\text{if}\hskip 5.69046pt\text{a\leq x<b}\\ \lceil x-b\rceil\hskip 11.38092pt\text{if}\hskip 5.69046pt\text{x\geq b},\end{array}\right.
where , being the largest integer . For , every irrational number can be expressed uniquely as an infinite -continued fraction of the form (see [13] for details)
[TABLE]
which we denote by . Here , and , for and is called the th partial quotient. The rational number is called the th convergent. The sequence is eventually increasing and converges to . As mentioned earlier, a particular case of -continued fraction, viz. the -continued fraction (also called the alternating continued fraction) is closely related to the classical continued fraction. If is the sequence of partial quotients in the classical continued fraction expansion of a real number , then is the sequence of partial quotients in the -continued fraction expansion of . A similar relation holds between the nearest integer continued fraction (also known as Hurwitz’s continued fraction introduced by Hurwitz) expansion and -continued fraction expansion of any real number. Note that we write the -continued fraction expansion of any real number as in (1) using minus sign, while in the case of classical or nearest integer continued fraction expansion it is written using plus sign. The use of minus sign while writing the -continued fraction expansion, presents some advantages which will be clear when we discuss the coding of geodesics using these continued fractions.
Let and be defined by
f_{a,b}(x):=\left\{\begin{array}[]{lr}x+1\hskip 11.38092pt\text{if}\hskip 5.69046pt\text{x<a}\\ -\frac{\displaystyle 1}{\displaystyle x}\hskip 19.91684pt\text{if}\hskip 5.69046pt\text{a\leq x<b}\\ x-1\hskip 11.38092pt\text{if}\hskip 5.69046pt\text{x\geq b}.\end{array}\right.
Note that is defined using the standard generators and of the modular group , and the continued fraction algorithm described above can be obtained using the first return map of to the interval . The main object of study in [13] is a two dimensional realization of the natural extension map , of , which is defined as follows:
F_{a,b}(x,y):=\left\{\begin{array}[]{lr}(x+1,y+1)\hskip 11.38092pt\text{if}\hskip 5.69046pt\text{x<a}\\ (-\frac{\displaystyle 1}{\displaystyle x},-\frac{\displaystyle 1}{\displaystyle y})\hskip 28.45274pt\text{if}\hskip 5.69046pt\text{a\leq x<b}\\ (x-1,y-1)\hskip 11.38092pt\text{if}\hskip 5.69046pt\text{x\geq b}.\end{array}\right.
The following theorem is just a restatement of the main result of [13] for the restricted set of parameters .
Theorem 2.1**.**
*([13]) There exists a one-dimensional Lebesgue measure zero, uncountable set contained in , such that for all ,
the map has an attractor on which is essentially bijective.
The set consists of two (or one in degenerate cases) connected components each having finite rectangular structure, i.e., bounded by non-decreasing step-functions with finitely many steps.
Every point of the plane () is mapped to after finitely many iterations of .*
In [13], to deduce the above theorem, a crucial role in the arguments used, is played by the orbits of and under , viz. to , the upper orbit (i.e., the orbit of ) and the lower orbit (i.e., the orbit of ), and to , the upper orbit (i.e., the orbit of ) and the lower orbit (i.e., the orbit of ). Let us denote the set by the symbol . It was proved in [13] that if , then satisfies the finiteness condition. This means that for both and , their upper and lower orbits are either eventually periodic, or they satisfy the cycle property, i.e., they meet forming a cycle, in other words there exist integers such that
[TABLE]
where and are the ends of the cycles. If the products of transformations over the upper and lower sides of the cycle of (respectively ) are equal, (respectively ) is said to have strong cycle property, otherwise it has weak cycle property. Let
\mathcal{L}_{a}=\left\{\begin{array}[]{lr}\mathcal{O}_{l}(a)\hskip 128.0374pt\text{if ahas no cycle property}\\ \text{lower part ofa-cycle}\hskip 51.21504pt\text{if ahas strong cycle property}\\ \text{lower part ofa-cycle}\cup\{0\}\hskip 19.91684pt\text{if a has weak cycle property},\end{array}\right.
\mathcal{U}_{a}=\left\{\begin{array}[]{lr}\mathcal{O}_{u}(a)\hskip 128.0374pt\text{if ahas no cycle property}\\ \text{upper part ofa-cycle}\hskip 51.21504pt\text{if ahas strong cycle property}\\ \text{upper part ofa-cycle}\cup\{0\}\hskip 19.91684pt\text{if a has weak cycle property}\end{array}\right.
and , be defined similarly. Also let and . So, satisfies the finiteness condition means that both the sets and are finite, which is true when . In [13], first a set , having finite rectangular structure, was constructed (see Theorem in [13]) using the values in the sets and , and then it was shown (Theorem in [13]) that actually coincides with the attractor . The upper component of is bounded by non-decreasing step functions with values in the set and the lower component of is bounded by non-decreasing step functions with values in the set .
Making use of the properties of the map and the attractor , in a subsequent paper ([14]), S. Katok and I. Ugarcovicci developed a general method of coding geodesics on the modular surface and gave a symbolic description of the geodesic flow associated with the modular surface. We first recall from [14], the notion of -reduced geodesics, which plays a crucial role in determining the cross-section for the geodesic flow needed for coding purposes.
Definition 2.2**.**
A geodesic in with real endpoints and , being the attracting and being the repelling endpoints, is called -reduced if , where
[TABLE]
Given any geodesic in , one can obtain an -reduced geodesic -equivalent to by using the reduction property (rd assertion in Theorem 2.1) of the map . More precisely, if is a geodesic which is not -reduced and if is the attracting end point of , then there exists some positive integer such that is an -reduced geodesic (see [14] for details). Now let be an -reduced geodesic with attracting and repelling endpoint and respectively, and be the -continued fraction expansion of . Using the essential bijectivity of the map , one can extend the sequence in the past as well to get a bi-infinite sequence , called the coding sequence of and written as
,
where (see Section of [14] for details).
Now we recall from [14], the description of the cross-section. Let
be the upper half of the unit circle and denote the standard fundamental domain for the action of on , given by
.
Using the definition of -reduced geodesic it is easy see the following fact.
Proposition 2.3**.**
([14]) For , every -reduced geodesic intersects .
Given an -reduced geodesic with attracting and repelling endpoints and respectively, the cross-section point on is the intersection point of with . Let be defined by
,
where is the cross-section point on the geodesic joining and , and is the unit vector tangent to at . The map is clearly injective and after composing with the Canonical projection we obtain a map
.
Let . Then is a cross-section for the geodesic flow associated with the modular surface (see [14] for details). The lift of to restricted to the unit tangent vectors having base points on the fundamental domain , can be described as follows:
(see Figure ),
where consists of unit tangent vectors on the circular boundary of the fundamental region and pointing inward such that the corresponding geodesic on is -reduced; consists of unit tangent vectors with base points on the right vertical boundary of and pointing inward such that if is the geodesic corresponding to one such unit vector, then is -reduced; consists of unit tangent vectors with base points on the left vertical boundary of and pointing inward such that if is the geodesic corresponding to one such unit vector, then is -reduced.
Now let and be the corresponding geodesic in and be an -reduced lift of it inside . Also let be the Canonical projection of onto . The following theorem from [14] provides the base for coding geodesics on the modular surface using -continued fractions.
Theorem 2.4**.**
([14]) Let and be as above. Then each geodesic segment of between successive returns to , while extended to a geodesic, produces an -reduced geodesic on , and each -reduced geodesic -equivalent to is obtained in this way.The first return of to corresponds to a left shift of the coding sequence of .
Let be the orbit of the geodesic flow on corresponding to the geodesic , i.e., and let be the segment of the geodesic corresponding to the portion of the orbit between th and th returns to the cross-section . We call the segment the th excursion of the geodesic into the cusp. Let be the attracting end point of and . Then the segment of between and , denoted by is a lift of to the hyperbolic plane. Assuming the geodesics to be parameterized by arc length, the time between the th and the th return of to the cross-section, called the th return time, is given by
[TABLE]
where stands for the hyperbolic length of the geodesic segment. Also let .
Proposition 2.5**.**
If , then is contained inside a compact subset of .
Proof.
The structure of is discussed in detail in Theorem of [13]. has two connected components, the lower one we denote by and the upper one we denote by . Both the sets and have finite rectangular structure i.e., bounded by non-decreasing step functions with finite number of steps. For the values of the step function are given by the set , and for the values of the step function are given by the set . The structure of the boundary (see Figure for a typical picture of ) of consists
of finite number of horizontal segments at different points of the set , called the different levels of and consecutive levels are joined by vertical segments, where the highest level is . has a similar description with the lowest level being . Let be the -coordinate of the vertical segment joining two consecutive levels and of with , and be the -coordinate of the vertical segment joining two consecutive levels and with . Similarly, let be the -coordinate of the vertical segment joining two consecutive levels and of with , and be the -coordinate of the vertical segment joining two consecutive levels and with . Also let be the level above and next to ; be the level below and next to .
It follows from these assertions and the definition of , that a geodesic with attracting and repelling endpoints and respectively with , is -reduced if and only if
[TABLE]
On the other hand if , then is -reduced if and only if
[TABLE]
We show that , and , .
For , let and be positive integers such that and . Let , , then the the proof of Lemma of [13] shows that the vertical segment joining and has -coordinate greater than , and the vertical segment joining and has -coordinate less than . Therefore, in these cases we have , and , . Now we consider the situation when , . Note that can never be , for if , then since , but we have assumed that . So, . Now if either or is , then from the explicit cycle description of and discussed in [13], we see that there is always one level between and ; similarly there is always one level between and . As the statement of Lemma of [13] guarantees that the vertical segment joining and has -coordinate greater than or equal to and the vertical segment joining and has -coordinate less than or equal to , it follows that , and , in these cases as well.
From the discussion above we have, and . Now let be the intersection point of the geodesic joining [math] and , and ; be the intersection point of the geodesic joining and , and . We chose one of and , which has -coordinate less than or equal to the other and denote it by . Also let be the intersection point of and the vertical geodesic based at the point . Then any -reduced geodesic having attracting endpoint , intersects the segment joining and of (see Figure ). Consequently the cross-section point for any -reduced geodesic having positive attracting endpoint, has -coordinate uniformly bounded away from [math]. The same is true for any -reduced geodesic with negative attracting endpoint as well, which can be shown similarly by using the fact that and . This completes the proof of the proposition. ∎
3 Cusp excursions with extreme frequencies
In this section, we prove the main results of this article. The results are about classifying two kinds of forward orbits of geodesic flow apart from the generic ones. This is done by relating the time spent by the orbits in cusp neighbourhoods compared to the total time parameter, and the average growth rate of the partial quotients of the continued fraction expansion of the attracting end points of the corresponding geodesics. It is worth mentioning that there are many interesting results relating cusp excursions of geodesics on hyperbolic 2-orbifolds and Diophantine approximation. For example, see [7], [8] and the references given there (As there is a large body of literature around this phenomena, the reference list given here is not complete by any means). In [7] and [8], various aspects of cusp excursions of a generic set of geodesics have been studied and analogue of various results from classical Diophantine approximation in the context of Fuchsian groups have been obtained, while restricting to the case of the modular surface these produce new proofs of classical results (see [7], [8] for details). For example, it was shown in [8] that for and for almost all , if is the subsequence of which intersect , then .
In this article, we consider a certain class of geodesics apart from the generic ones and look at their behaviour in terms of spending time inside cusp neighbourhoods compared to their length parameter. Let , , , be as in the previous section. The partial quotients of the continued fraction expansion of determine how much further the orbit of the geodesic flow goes into a typical neighbourhood of the cusp before returning to the cross-section. This particular fact is easier to see when the cross-section is contained inside a compact set which is the case when . Whereas for , the cross-section is not contained inside a compact set. In this case we use the formula for return times given by S. Katok and I. Ugarcovicci and some other facts which are particular to the -continued fraction.
3.1
Lemma 3.1**.**
*Let be a positive integer.
Assume that . Then intersects or does not intersect accordingly as or .
Assume that . Then intersects or does not intersect accordingly as or .*
Proof.
If , then the attracting endpoint of lies in the interval
and the repelling endpoint is contained in the interval . So, in this case, lies above the geodesic , where is the geodesic joining and . Also, lies below the geodesic , where is the geodesic joining and . So, if the radius of is less than , then does not intersect ; on the other hand if the radius of is greater than , then does intersect . Now a simple calculation gives the assertion of the lemma in the case . If , then lies above the geodesic joining and , and lies below the geodesic joining and . Again a simple calculation gives the assertion of the lemma in the case . ∎
The following two lemmas which are crucial to the arguments to follow, can be proved easily using the fact that the cross-section is contained inside a compact set in . The proof of similar statements for the particular case is contained in [2] (Proposition and Proposition respectively) and the same proofs work for any as well.
Lemma 3.2**.**
Let be such that , then if is nonempty, is the only connected component of .
Lemma 3.3**.**
Let , be the corresponding geodesic in , and be an -reduced lift of inside . Let be the attracting end point of and be the th return time for the corresponding orbit of the geodesic flow. Then there exist a constant such that
[TABLE]
Remark 3.4**.**
The asymptotic estimates for values of binary quadratic forms at integer points were obtained in [2] in terms of -continued fraction expansion of the coefficients of the quadratic forms, and the -continued fraction coding of geodesics on the modular surface was used to obtain the estimates. The facts that the cross-section for geodesic flow corresponding to the -continued fraction coding, is contained inside a compact subset of and the return times can be bounded uniformly by the partial quotients as in (2), were used crucially to obtain those estimates. Since the above two properties hold for -continued fraction coding as well for , one can obtain similar estimates as in [2] for values of binary quadratic forms at integer points in terms of the -continued fraction expansions of its coefficients as well.
Given , let , , and
\mathfrak{j}_{\underline{d}}^{N}=\#\big{(}0\leq j<N:\text{either}\hskip 2.84544pta_{j}>\underline{d}^{+}\hskip 5.69046pt\text{if}\hskip 5.69046pta_{j}>0\hskip 5.69046pt\text{or}\hskip 5.69046pta_{j}<-\underline{d}^{-}\hskip 5.69046pt\text{if}\hskip 5.69046pta_{j}<0\big{)}.
Let , , and
\mathfrak{j}_{\bar{d}}^{N}=\#\big{(}0\leq j<N:\text{either}\hskip 2.84544pta_{j}>\bar{d}_{+}\hskip 5.69046pt\text{if}\hskip 5.69046pta_{j}>0\hskip 5.69046pt\text{or}\hskip 5.69046pta_{j}<-\bar{d}_{-}\hskip 5.69046pt\text{if}\hskip 5.69046pta_{j}<0\big{)}.
Let . Also let
[TABLE]
where denotes the characteristic function of the neighbourhood of the cusp and .
It is evident from Lemma 3.1, Lemma 3.2 and Lemma 3.3 that the th excursion of the geodesic goes more and more into the cusp as the value of gets bigger and bigger and vice versa. The following proposition uses this fact to characterize those orbits of geodesic flow which visit the cusp with full frequency. It is easy to see that to conclude about the extreme behaviour of , it is enough to consider .
Proposition 3.5**.**
*Let , be the corresponding geodesic on and be an -reduced lift of in . Let be the attracting endpoint of . Then as for all , if and only if,
as .*
Proof.
We enumerate those for which either for , or for
, by the subsequence , and by we mean the sum
.
On the other hand, we enumerate those for which if , or if , by the subsequence , and by we mean the sum
.
Now suppose as which implies by Lemma 3.3, that as .
Let be such that . Now for any , let
[TABLE]
Then
[TABLE]
As both the quantities and are bounded, and
as , it follows that as .
To prove the converse statement, we show that if as , then there is some such that can not go to as . Now as means that there is a subsequence and such that for all , which again means, by Lemma 3.3, that for some and for all . Since as for all implies as , which again by Lemma 3.3 implies as , we may assume that there exists some and such that (if needed by considering a subsequence of and denoting it again by ) for all . Now
[TABLE]
Since the cross-section point for any -reduced geodesic, is uniformly bounded away from the real line, it follows that has a uniform lower bound, i.e., for some and all . Since and for all , it follows that , for all . Hence as , a contradiction. ∎
Let us now concentrate on those orbits whose frequency of visiting the cusp is zero. A complete characterization of such orbits is given by the following proposition.
Proposition 3.6**.**
If as for some , then as for all . On the other hand if as for some , then as for all .
Proof.
From Lemma 3.3, we have
[TABLE]
where is as in that Lemma. Note that implies as . Then from (6), we conclude that is equivalent to as .
Now for any ,
,
which tends to [math] as since is bounded below by .
To prove the converse statement, let us assume that as , and . Suppose as . Then using another version of (6), with replaced by , there is a subsequence and , such that for all . Note that, as when , we have as . Because if as , then for some and for infinitely many . Then , for infinitely many , which in turn implies that for infinitely many , where . This is a contradiction to the fact that as .
Now let denote the least upper bound of the distances from the cross-section point on to the horizontal line , for all -reduced geodesics. Then
[TABLE]
Since as , it follows that there is some such that
for all . Therefore, from (7) and (8), we conclude that there exists some , such that for sufficiently large . Which is a contradiction to the assumption that as . This completes the proof of the proposition. ∎
Now the proof of Theorem 1.1 for follows from Proposition 3.5 and Proposition 3.6.
Remark 3.7**.**
Note that in Proposition 3.5 and Proposition 3.6, we have considered an -reduced lift of , whereas in Theorem 1.1, we have considered any lift of to . This does not lead to any ambiguity because if we obtain an -reduced geodesic with attracting end point , from a geodesic with attracting end point , then for some .
3.2
Now we concentrate on the special case . Recall that the coding of geodesics on the modular surface using this particular continued fraction is discussed in detail in [12], where it is called the alternating continued fraction coding. The name alternating continued fraction comes from the fact that the partial quotients of the -continued fraction expansion of a real number has alternate signs. This particular coding procedure does not provide a cross-section contained in a compact subset of . Recall form [12], that a geodesic in is called -reduced (-reduced with our convention), if its attracting endpoint and repelling endpoint satisfy and respectively. So the cross-section point for an -reduced geodesic can be as close to the real line as one wants, showing that the cross-section is not contained inside a compact set in . So the th return time may not be at a bounded distance from . But can be controlled using a couple of preceding and couple of succeeding entries in the sequence of partial quotients. We recall from [12], the following formula for the th return time:
[TABLE]
Now assume that , then it follows from the definition of -reduced geodesics that . Since the partial quotients have alternate signs, we also have and consequently . Then,
[TABLE]
Now using the assumption that and consequently , , it is easy to see that
[TABLE]
where is some real number such that . Then it follows that,
[TABLE]
By a similar reasoning,
[TABLE]
with , and it follows that,
[TABLE]
Using the continued fraction expansions for and , we obtain similar estimates for other quantities in the above inequality involving . The case can be treated similarly and we get the following estimate for the return time :
[TABLE]
here is some constant which is independent of . On the other hand, considering the definition of -reduced geodesics, and the fact that the length of the geodesic segment joining the point and is at a bounded distance from , independent of , it is easy to see that
[TABLE]
where can be taken as the hyperbolic length of the segment of the unit circle joining the point and .
Also note that in this special case, whenever is non-empty, the number of connected components of can be more than one, in fact it can be at most three. One component is ; one of the other two may be the segment starting from the cross-section point up to the intersection point of with the horocycle , where is the image of the horocycle under as shown in Figure ; the third component may be a similar one coming from near the other end of . In Figure , the geodesic is the geodesic which is tangent to the horizontal line and passes through the intersection point of the vertical line based at and the horocycle . Let be the hyperbolic length of the segment of joining the pair of points where it cuts the horocycle and where it touches the line . Then . On the other hand, let denote the hyperbolic distance between the points and the horizontal line . Then if , . Using these observations, the following two propositions from which the proof of Theorem 1.1 follows in the case , can be proved by adopting the similar strategies as in the proofs of Proposition 3.5 and Proposition 3.6 respectively.
Proposition 3.8**.**
*Let , be the corresponding geodesic on and be an -reduced lift of in . Let be the attracting endpoint of . Then as for all if and only if
as .*
Proposition 3.9**.**
If as for some , then there exists , such that as for all . On the other hand, if as for some , then there exist such that as for all .
**Proof of Theorem 1.1 in the case of -continued fraction.
**It follows easily from (9) and (10), that as is equivalent to as . Now let
[TABLE]
Then for , from (9) we get
[TABLE]
Therefore, if as for some , which also implies as , then it follows from (11), that
as for all . On the other hand, it follows easily from (10), that if for some , which also implies as , there exists , such that
as for all . With these observations, now the proof of Theorem 1.1 in the case of -continued fraction, follows from Proposition 3.8 and Proposition 3.9.
4 Acknowledgements
The author is thankful to S. G. Dani for suggesting the problem and his constant help in writing the paper. Thanks are also due to the referee of this version for valuable suggestions which have helped to improve the exposition of the article. The author thanks Indian Statistical Institute Bangalore, Harish Chandra Research Institute Allahabad and Indian Statistical Institute Kolkata for their hospitality during the author’s stay there, which has made this work possible. Financial support from the National Board for Higher Mathematics India through NBHM post-doctoral fellowship is duly acknowledged.
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