Abstract
In this article, we investigate anti-invariant Riemannian and Lagrangian submersions onto Riemannian manifolds from the Lorentzian para-Sasakian manifold. We demonstrate that, for these submersions, horizontal distributions are not integrable and their fibers are not totally geodesic. As a result, they are not totally geodesic maps. The harmonicity of such submersions is also examined. We specifically prove that they are not harmonic when the Reeb vector field is horizontal. Finally, we provide an illustration of our findings and mention some number-theoretic applications for the same submersions.
Keywords:
anti-invariant submersion; Lagrangian submersion; Lorentzian para-Sasakian manifold; homotopy groups MSC:
53C15; 53B20; 11F23
1. Introduction
The hypothesis of Riemannian submersions developed by O’Neill [1] and Gray [2] is now the most fascinating area of differential geometry research. Riemannian submersions among nearly-Hermitian manifolds were regarded as almost-Hermitian submersions by Watson [3]. After that, various subclasses of almost-Hermitian manifolds have been the subject of intense research with regard to almost-Hermitian submersions. Additionally, under the term of contact-Riemannian submersions, Riemannian submersions were expanded to include a number of subclasses of almost-contact manifolds. The book [4] contains vast investigations of Riemannian, nearly-Hermitian, and contact-Riemannian submersions.
Since Şahin [5] introduced such submersions along nearly-Hermitian manifolds onto Riemannian manifolds, the topic of Lagrangian submersions and anti-invariant submersions has become a particularly active research area. Anti-invariant and Lagrangian submersions have been researched in a variety of structures, including nearly-Kähler [6], Kähler [5,7], local-product Riemannian [8], almost-product [9], Sasakian [10,11,12,13], Kenmotsu [13,14], and cosymplectic structure [15].
It should be emphasized that the theory of anti-invariant Riemannian submersion has been enlarged into the concept of conformal anti-invariant submersion [16]. The bulk of the research on anti-invariant and Lagrangian submersions is reported in [17].
The following is how this document is structured. Section 2 introduces the background of the Lorentzian para-Sasakian manifold. Section 3 provides some context for Riemannian submersions. The authors review the definitions of anti-invariant and Lagrangian submersions in Section 4. Section 5 investigates anti-invariant submersions from Lorentzian para-Sasakian manifolds onto Riemannian manifolds conceding vertical Reeb vector fields, provides an example, and discusses some of its characteristics. Section 6 discusses the scenario where the Reeb vector field is horizontal. Section 7 investigates the geometry of vertical and horizontal distributions for Lagrangian submersions accommodating a vertical Reeb vector field. We also provide a necessary and sufficient condition for such harmonic submersions. Comparable investigations for Lagrangian submersions conceding horizontal Reeb vector fields are given at the end.
Lorentzian almost-para-contact manifolds were introduced by Matsumoto [18]. Following that, several geometers investigated various structures on these manifolds. After the work in [19,20,21], the study of Lorentzian para-Sasakian manifolds has become a topic of increasing scholarly interest.
2. Preliminaries
Let be a -dimensional Lorentzian manifold. Then, is called a Lorentzian almost-para-contact metric manifold [18] with the Riemannian metric if there exists a tensor of type and a global vector field , which is called the Reeb vector field [22] or the characteristic vector field, such that, if is the dual 1-form of , then we have
where . Furthermore, it is clear from the preceding arguments that
This structure is referred to as the Lorentzian para-contact metric structure
A Lorentzian para-contact metric structure on a connected manifold [23] is known as a Lorentzian para-Sasakian manifold if [18,20]
for all p and q tangent to , where ∇ indicates the Levi–Civita connection with respect to metric .
3. Riemannian Submersions
This section provides the necessary context for Riemannian submersions. Let and be Riemannian manifolds with and a surjective map is referred to as a Riemannian submersion [1] if the following conditions are met.
- (C1)
- Rank (.
In this scenario, for all points is a submanifold of with dimension t and is referred to as a fiber, where
If a vector field on is always tangent (resp. orthogonal) to fibers, it is claimed to be vertical (resp. horizontal). Confirmed all should be retained. If a horizontal vector field on is -related to a vector field on ℵ, then
for all where is the differential mapping of The projections on the vertical distribution and the horizontal distribution are denoted by and , respectively.
The manifold is termed the total manifold, and the manifold is called the base manifold of the submersion .
- (C2)
- The lengths of the horizontal vectors are preserved by .
This criterion implies that the derivative map of , constrained to is a linear isometry.
O’Neill’s [1] tensors and describe the geometry of Riemannian submersions, which are defined as follows:
for any vector fields p and q on , wherein ∇ is the Levi–Civita connection of It is clear that the and operators are skew-symmetric on the tangent bundle of and reverse the horizontal and vertical distributions. The properties of the tensor field and are next outlined. Let be vertical vector fields and be horizontal vector fields on ; then, we gain
In addition, from Equations (5) and (6), we obtain
where . Furthermore, if is basic, then we get . It is easy to see that works as the second fundamental form, but operates on the horizontal distribution and measures the obstacle to its integrability. For further information on Riemannian submersions, see O’Neill’s work [1] and the book [4].
Let and be Riemannian manifolds and a smooth map. Then, the second fundamental form of is provided by
for where is the pull back connection, and we denote for convenience the Riemannian connections of the metrics and with ∇. It is well known that the second fundamental form is symmetric, wherein denotes the pull back connection and ∇ indicates the Riemannian connections of the metrics and for convenience. In addition, is said to be totally geodesic [24] if
for each , and is said to be a harmonic map [24] if
Example 1.
Let be a six-dimensional differentiable manifold where signifies the standard coordinates of a point in , and .
is the basis for the tangent space since it consists of a set of linearly independent vector fields at each point of the manifold . A definite positive metric g on is defined as follows. With , it is defined as
Let θ be a 1-form such that , where .
Thus, is a total manifold. In addition, let be the Levi–Civita connection with respect to g. Then, we have
where
Next, let us take a map as a submersion defined by
where
Then, the Jacobian matrix of Φ is given as
The Jacobi matrix of Φ has rank three at that point. This indicates that Φ is a submersion. Simple calculations produce
and
Also, direct computations yields
It is easy to observe that
Hence, we can easily observe that Φ meets the requirement (C2). As a result, Φ is a Θ.
4. Submersions from Lorentzain Para-Sasakian Manifolds
We begin by recalling the essence of an anti-invariant Riemannian submersion with a Lorentzian para-contact manifold as its total manifold.
Definition 1
([10,11]). Let be a -dimensional Lorentzian para-contact manifold with Lorentzian para-contact metric structure and N be a Riemannian manifold with Riemannian metric Let there exist a Riemannian submersion with a vertical distribution that is anti-invariant such that we have ; i.e., The Riemannian submersion Φ is then known as an anti-invariant Riemannian submersion. Such submersions will be denoted for short by Θ.
A horizontal distribution is decomposed in this situation as
wherein is the orthogonal complementary distribution of in and is invariant with regard to
We have an anti-invariant submersion with a vertical Reeb vector field (briefly, -RVF) if the Reeb vector field is tangent to and a horizontal Reeb vector field (briefly, ℏ-RVF) if the Reeb vector field is normal to . It is clear that contains the Reeb vector field (RVF) in the case that with the ℏ-RVF . For more information on anti-invariant submersions from various structures, see [10,11,14,15].
Remark 1.
In this article, we treat a Lorentzian para-Sasakian manifold [25] as a total manifold of a Θ.
Lagrangian submersion is a subcategory of . We next review the description of a Lagrangian submersion from a Lorentzian para-contact manifold onto a Riemannian manifold.
Definition 2
([12]). Let π be a Θ from a Lorentzian para-Sasakian manifold onto a Riemannian manifold . If it holds that
respectively, then we state that Φ is a Lagrangian submersion and it is denoted by
Remark 2.
This scenario has been investigated partially as a specific example of a Θ; for more information, see [10,11,12,14,15].
5. with Vertical Reeb Vector Field
We investigate conceding a -RVF from a Lorentizan para-Sasakian manifold in this section.
Let be a from a Lorentizan para-Sasakian manifold onto a Riemannian manifold . For any , we compose
wherein and . First, we investigate how the Lorentzian para-Sasakian structure affects and of the submersion
Lemma 1.
Let Φ be a Θ from a Lorentzian para-Sasakian manifold onto a Riemannian manifold admitting a -RVF. Then, we gain
wherein and .
Proof.
For any , using Equation (3), we find
Given that is vertical, we may take the horizontal and vertical components of Equation (24) to gain Equations (16) and (17), respectively.
Let and be any horizontal vector fields. We have Equation (3) once more.
Adopting Equations (11), (12), and (33), we get
We can simply generate Equations (22) and (23) by taking the horizontal and vertical portions of Equation (25) and employing the idea that is vertical.
The other assertions can be acquired in the same manner. □
In this section, we explore a from a Lorentzian para-Sasakian manifold onto a Riemannian manifold with a -RVF .
Let be a admitting a -RVF from a Lorentzian para-Sasakian manifold onto a Riemannian manifold . Then, adopting Equation (33) and the condition (C2), we deduce
for every and , which entails that
Theorem 1.
Let be a Lorentzian para-Sasakian manifold of dimension and a Riemannian manifold of dimension s. Let be a Θ such that . Then, the RVF ς is vertical and .
Proof.
With the hypothesis , for any we gain
This demonstrates that the RVF is vertical.
Now, let be an orthonormal set of , wherein . Since
with an orthonormal set of . So, in light of Equation (33), we get , which entails that . □
Theorem 2.
Let be a Θ admitting a -RVF; then, the fibers are not totally umbilical.
Proof.
Adopting Equations (9) and (3), we get
for any , and with totally umbilical fibers, one can get
wherein is the mean curvature vector field of any fiber. Since , we get , which demonstrates that fibers are minimal. Consequently, the fibers are totally geodesic, which is inappropriate to the condition . □
Lemma 2.
Let Φ be an be a Θ admitting a -RVF from a Lorentzian para-Sasakian manifold to a Riemannian manifold . Then, we gain
for any .
Lemma 3.
Let Φ be an be a Θ admitting a -RVF from a Lorentzian para-Sasakian manifold to a Riemannian manifold . Then, we gain
for and .
6. Anti-Invariant Submersions with ℏ-RVF
Example 2.
Let be a nine-dimensional Riemannian space given by
Then, we choose a Lorentzian para-contact structure on , such as
wherein , are vector fields. Thus, is a Lorentzian para-Sasakian manifold.
Next, consider a mapping defined by
where is the Riemannian metric of . Then, the Jacobian matrix of Φ is
As the rank of the Jacobian matrix is 5, the map Φ is a submersion. However, we can easily show that Φ meets the requirement (C2). As a result, Φ is a Lorentzian submersion. Now, after some calculations, we arrive at
and
Furthermore, we can observe that for , which indicates
Hence, Φ is a Θ and ς is a ℏ-RVF.
Let be a from a Lorentzian para-Sasakian manifold onto a Riemannian manifold . For any , we compose
wherein and . We begin by investigating how the Lorentzian para-Sasakian manifold affects the tensor fields and of the submersion
Lemma 4.
Let Φ be a Θ from a Lorentzian para-Sasakian manifold onto a Riemannian manifold admitting a ℏ-RVF. Then, we gain
wherein and .
Proof.
The proof is pretty similar to the Lemma 1 proof. As a result, we leave it out. □
In this part, we examine a from a Lorentzian para-Sasakian manifold onto a Riemannian manifold with a ℏ-RFV .
Using Equation (33), we have
Assume that q is a vertical vector field and is a horizontal vector field. Applying the aforementioned relationship and Equation (3), we get
We have this last relationship , which implies that
Equations (3) and (33) entail the following lemma.
Lemma 5.
Let Φ be a Θ admitting a ℏ-RVF from a Lorentzian para-Sasakian manifold onto a Riemannian manifold . Then, we gain
for any .
Lemma 6.
Let Φ be a Θ with a ℏ-RVF from a Lorentzian para-Sasakian manifold onto a Riemannian manifold . Then, we have
for and .
Proof.
In light of Equations (4), (12), and (33), we get Equation (43). Adopting Equations (4) and (10), we get Equation (44). Since is horizontal and is vertical, for and , we get Equation (45). Then, employing Equation (45), we get
for and . Then, adopting Equations (3) and (11), we have
Since , we get Equation (46).
7. Lagrangian Submersions with -RVFs from Lorentzian Para-Sasakian Manifolds
In this section, we examine the integrability and total geodesicity of the horizontal distribution of conceding a -RVF from a Lorentzian para-Sasakian manifold. Initially, we estimate the behavior of the tensor of . In light of Lemma 4, one can obtain the following outcomes.
Corollary 1.
Let Φ be a Ξ with a -RVF from a Lorentzian para-Sasakian manifold onto a Riemannian manifold . Then, we gain
for and .
Proof.
Remark 3.
Referring to [26], it can be noted that tensor T vanishes if the fibers of a Riemannian submersion are totally geodesic.
Corollary 1 entails that the tensor cannot vanish. Hence, in light of Remark 3, we can articulate the following.
Theorem 3.
Let Φ be a Ξ with a -RVF from a Lorentzian para-Sasakian manifold onto a Riemannian manifold . Then, the fibers of Φ are not totally geodesic.
In addition, we provide a few findings about the characteristics of the tensor of .
Corollary 2.
Let Φ be a Ξ with a -RVF from a Lorentzian para-Sasakian manifold onto a Riemannian manifold . Then, we get
for and .
Proof.
Remark 4.
We can observe that the tensor cannot vanish for the submersion from Equation (54). Then, we get the following theorem.
Theorem 4.
Let Φ be a Ξ with a -RVF from a Lorentzian para-Sasakian manifold onto a Riemannian manifold . Then, the horizontal distribution of Φ is not integrable.
Remark 5.
A mapping between Riemannian manifolds is considered to be totally geodesic if preserves parallel translation. According to Vilms [26], a Riemannian submersion Φ is totally geodesic if and only if both tensors T and A vanish.
Now, referring to Theorem 3 or Theorem 4 and Remark 5, we gain the following outcome.
Theorem 5.
Let Φ be a Ξ with a -RVF from a Lorentzian para-Sasakian manifold onto a Riemannian manifold . Then, the submersion Φ is not a totally geodesic map.
Finally, we provide a necessary and sufficient condition for to be harmonic.
Theorem 6.
Let Φ be a Ξ with a -RVF from a Lorentzian para-Sasakian manifold onto a Riemannian manifold . Then, Φ is harmonic if and only if
for , wherein is the restriction of to .
Proof.
In view of [27], is harmonic if and only if has minimal fibers. Let be an orthonormal set of .
Thus, is harmonic ⇔ . Since it follows that is harmonic ⇔ Now, we compute By orthonormal expansion, we can write
wherein is an orthonormal frame of Since is skew-symmetric, we get
From Equation (48), we have
As are linearly independent, in view of Equation (55), we arrive at
Example 3.
Let , wherein are the standard coordinates in , and be a Lorentzian para-Sasakian manifold, as in the example in Equation (2).
Now, let us assume the map defined by the following:
where is the Riemannian metric of . Thus, the Jacobian matrix of Φ is given as:
Since the rank of the matrix is equal to 2, the map Φ is a submersion. On the other hand, we can observe that Φ obeys the condition (C2). Then, by a direct estimation, we arrive at
and
It is easy to identify that , , and entail that
Consequently, Φ is a Ξ such that ς is a -RVF.
8. Lagrangian Submersions with ℏ-RVFs from Lorentzian Para-Sasakian Manifolds
We analyze admitting ℏ-RVFs from Lorentzian para-Sasakian manifolds onto Riemannian manifolds in this section.
Theorem 7.
Assume a Lorentzian para-Sasakian manifold of dimension and a Riemannian manifold of dimension s. Let be a Ξ admitting ℏ-RVFs. Then, .
Proof.
Let be an orthonormal set of , where . As such, , generated from an orthonormal set of . So, from Equation (26), we get , which implies that . □
It should be emphasized that the proof of Theorem 7 is highly analogous to the proof of Theorem 8.1 in [10], but we include it for clarification.
From Lemma 1, we get the following corollary.
Corollary 3.
Let Φ be a Ξ with a ℏ-RVF from a Lorentzian para-Sasakian manifold onto a Riemannian manifold Then, we have
for and .
Proof.
We can see from Equation (61) that the tensor cannot vanish; hence, we have the following result.
Theorem 8.
Let Φ be a Ξ with a ℏ-RVF from a Lorentzian para-Sasakian manifold onto a Riemannian manifold Then, the fibers of Φ are not totally geodesic.
Corollary 4.
Let Φ be a Ξ with a ℏ-RVF from a Lorentzian para-Sasakian manifold onto a Riemannian manifold Then, we get
for and .
Proof.
It is clear from Equations (62) and (63) that the tensor cannot vanish. As a result of Remark 4, we gain the desired result.
Theorem 9.
Let Φ be a Ξ with a ℏ-RVF from a Lorentzian para-Sasakian manifold onto a Riemannian manifold The horizontal distribution of Φ is hence not integrable.
Based on Remark 5 from Theorem 8 or Theorem 9, we obtain the following outcome.
Theorem 10.
Let Φ be a Ξ with a ℏ-RVF from a Lorentzian para-Sasakian manifold onto a Riemannian manifold Then, the submersion Φ is not a totally geodesic map.
Lastly, we can present a finding relating to the harmonicity of .
Theorem 11.
Let Φ be a Ξ with a ℏ-RVF from a Lorentzian para-Sasakian manifold onto a Riemannian manifold Then, Φ is not harmonic.
Proof.
Let be an orthonormal set of . Then, is an orthonormal set of Thus, we arrive at
Applying the skew-symmetry of and Equation (59), we derive
We can conclude from Equation (66) that
This ensures that are linearly independent. □
Remark 6.
Theorems 8, 9, and 10 also hold for a Θ allowing a ℏ-RVF.
9. Some Number Theoretic Applications to Riemannian Submersions
The sumberison is a smooth Hopf fibration [28]. Moreover, a large class of submersions are submersions between spheres of higher dimensions, such as
whose fibers have the dimension m. The Hopf fibration asserts that a fibration generalizes the idea of a fiber bundle and plays a significant role in algebraic topology [29].
Every fiber in a fibration is closely connected to the homotopy group and satisfies the homotopy property [30]. The homotopy group of spheres essentially describes how several spheres of different dimensions may twist around one another. We can obtain the j-th homotopy group in which the j-dimensional sphere can be mapped continuously onto the r-dimensional sphere .
Now, we have the following remark:
Remark 7.
We aim to figure out the homotopy groups for positive k using the formula . The homotopy groups with are known as stable homotopty groups of spheres and are denoted by . They are finite abelian groups for . In view of Freudenthal’s suspension Theorem [31], the groups are known as unsteady homotopy groups of spheres for .
Now, in light of Theorem 1 and using Remark (7), we get the following outcomes.
Theorem 12.
Let be a Lorentzian para-Sasakian manifold of dimension , and is a Riemannian manifold of dimension s. Let be a Θ. Then, the homotopy group of Θ is
Example 4.
Let us adopt the example from Equation (2). We have anti-invariant submersions with a ℏ-RVF wherein is a Lorentzian para-Sasakian manifold.
Next, consider a mapping
where is the Riemannian metric of . Then, according to Hopf fibration (the fiber bundle), we have homotopy groups:
Therefore, the above remark entails that ; i.e., . Thus, the homotopy groups are unstable homotopy groups.
Remark 8.
For a prime number p, the homotopy p-exponent of a topological space , denoted by , is defined to be the largest such that some homotopy group has an element of order . Cohen et al. [32] proved that
For a prime number p and an integer z, the p-adic order of z is given by = .
Example 5.
In view of Equation (67) and Remark (8), the homotopy p-exponent of homotopy group of the anti-invariant submersions Φ with ℏ-RVFs is
Moreover, the homotopy group of anti-invariant submersions Φ with ℏ-RVFs has an element of the p-adic order 9e, where
Through the above observation, in 2007, Davis and Sun proved an interesting inequality in terms of homotopy groups. For more details, see Theorem 1.1, page 2, in [33]. According to them, for any prime p and , some homotopy group contains an element of order ; i.e., the strong and elegant lower bound for the homotopy p-exponent of the homotopy group is then
where is a special unitary group of degree n.
Therefore, using Davis and Sun’s result (Theorem 1.1 [33]) with Theorem 12, we gain an interesting inequality.
Theorem 13.
For any prime number p and , some homotopy group of Θ contains an element of order , and we get the inequality
10. Conclusions
This study explored the possibility that, if an anti-invariant Riemannian submersion admits a vertical Reeb vector field, the fiber of the anti-invariant Riemannian submersion is not totally umbilical. Also, if a Lagrangian submersion admits a vertical Reeb vector field, the fiber of the Lagrangian submersion is not totally geodesic, and under the same condition, the horizontal distribution of the submersion is not integrable. In addition, this implies a necessary and sufficient condition for a Lagrangian submersion to be harmonic, and a Lagrangian submersion with a horizontal Reeb vector field is not totally geodesic. Furthermore, if a Lagrangian submersion admits a horizontal Reeb vector field, the horizontal distribution of the same submersion is not integrable. Finally, this Riemannian submersion from Lorentzian para-Sasakian manifolds can be used to construct a homotopy group and find the lower bound for the same homotopy group of the Riemannian submersion.
Author Contributions
Conceptualization, M.D.S.; formal analysis, M.D.S. and A.H.H.; investigation, M.D.S. and A.H.H.; methodology, M.D.S.; funding A.H.H.; validation, M.D.S. and A.H.H.; writing—original draft, M.D.S. All authors have read and agreed to the published version of the manuscript.
Funding
This research received no external funding.
Data Availability Statement
Not applicable.
Acknowledgments
We thank the anonymous reviewers for their careful reading of our manuscript and their many insightful comments and suggestions.
Conflicts of Interest
The authors declare no conflict of interest.
Acronyms
| anti-invariant Riemannian submersion | |
| J | Lagrangian submersion |
| -RVF | vertical Reeb vector field |
| ℏ-RVF | horizontal Reeb vector field |
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