On semi-slant $\xi^\perp-$Riemannian submersions
Mehmet Akif Akyol, Ramazan Sar{\i}

TL;DR
This paper introduces and studies semi-slant 0-0-Riemannian submersions from Sasakian manifolds, generalizing existing submersion types, and explores their geometric properties, conditions for base manifolds, and examples.
Contribution
It defines semi-slant 0-0-Riemannian submersions, characterizes their geometry, and establishes conditions for base manifolds to be locally product, totally umbilical, or totally geodesic.
Findings
Characterization of semi-slant 0-0-Riemannian submersions
Conditions for base manifold to be locally product
Examples illustrating the submersions
Abstract
The aim of the present paper to define and study semi-slant Riemannian submersions from Sasakian manifolds onto Riemannian manifolds as a generalization of anti-invariant Riemannian submersions, semi-invariant Riemannian submersions and slant Riemannian submersions. We obtain characterizations, investigate the geometry of foliations which arise from the definition of this new submersion. After we investigate the geometry of foliations, we obtain necessary and sufficient condition for base manifold to be a locally product manifold and proving new conditions to be totally umbilical and totally geodesicness, respectively. Moreover, some examples of such submersions are mentioned.
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ON SEMI-SLANT RIEMANNIAN SUBMERSIONS
Mehmet Akif Akyol
Bingöl University, Faculty of Arts and Sciences, Deparment of Mathematics, 12000, Bingöl, Turkey
and
Ramazan Sarı
Amasya University, Merzifon Vocational Schools, 05300, Amasya, Turkey
Abstract.
The aim of the present paper to define and study semi-slant Riemannian submersions from Sasakian manifolds onto Riemannian manifolds as a generalization of anti-invariant Riemannian submersions, semi-invariant Riemannian submersions and slant Riemannian submersions. We obtain characterizations, investigate the geometry of foliations which arise from the definition of this new submersion. After we investigate the geometry of foliations, we obtain necessary and sufficient condition for base manifold to be a locally product manifold and proving new conditions to be totally umbilical and totally geodesicness, respectively. Moreover, some examples of such submersions are mentioned.
Key words and phrases:
Riemannian submersion, Sasakian manifold, anti-invariant Riemannian submersion, semi-invariant Riemannian submersion, slant Riemannian submersion.
2010 Mathematics Subject Classification:
53C15, 53C40.
1. Introduction
A differentiable map between Riemannian manifolds and is called a Riemannian submersion if is onto and it satisfies
[TABLE]
for vector fields tangent to , where denotes the derivative map. The study of Riemannian submersions were studied by O’Neill [26] and Gray [16] see also [15]. Later such submersions according to the conditions on the map , we have the following submersions: Riemannian submersions [24], almost Hermitian submersions [42], invariant submersions ([11, 37, 38]), anti-invariant submersions ([2, 5, 12, 17, 34, 37, 38]), lagrangian submersions ([43, 44]), semi-invariant submersions ([27, 35]), slant submersions ([13, 14, 18, 30, 36]), semi-slant submersions [1, 19, 28, 29], quaternionic submersions [40, 41], hemi-slant submersions ([3, 39]), pointwise slant submersions [21, 32] etc. We know that Riemannian submersions have several applications both in mathematics and in physics. Indeed, Riemannian submersions have their applications in the Kaluza-Klein theory ([9], [22]), supergravity and superstring theories ([23], [25]) and Yang-Mills theory ([8], [45]). Recently, in [20], Lee defined anti-invariant -Riemannian submersions from almost contact metric manifolds and then he studied the geometry of such maps. Then, in [12], Erken and Murathan introduced the notion of slant submersions from Sasakian manifolds.
On the other hand, as a generalization of anti-invariant -Riemannian submersions, Akyol et.al in [4] defined the notion of semi-invariant Riemannian submersions from almost contact metric manifolds and investigate the geometry of such maps. In this paper, as a generalization of anti-invariant Riemannian submersions, semi-invariant Riemannian submersions and slant Riemannian submersions, we define semi-slant Riemannian submersions from Sasakian manifolds onto Riemannian manifolds and investigate the geometry of the total space and the base space for the existence of such submersions.
The paper is organized as follows. In Sect. 2, we give some basic informations and notions about Riemannian submersions, the second fundamental form of a map and Sasakian manifolds. In Sect. 3, we define semi-slant Riemannian submersions from Sasakian manifolds onto Riemannian manifolds. In Sect. 4, we investigate the geometry of leaves of the horizontal distribution and the vertical distribution and show that there are certain product structures on total space of a semi-slant Riemannian submersion. In Sect. 5, we find new conditions for a semi-slant Riemannian submersion to be totally umbilical and totally geodesicness, respectively. In Sect. 6, we give lots of examples of such submersions.
2. Riemannian submersions
Let and be Riemannian manifolds, where and A Riemannian submersion is a map of onto satisfying the following axioms:
(i) has maximal rank, and
(ii)The differential preserves the lenghts of horizontal vectors, that is is a linear isometry.
The geometry of Riemannian submersion is characterized by O’Neill’s two tensor and defined as follows:
[TABLE]
and
[TABLE]
for any where is the Levi-Civita connection on Note that we denote the projection morphisms on the vertical distribution and the horizontal distribution by and , respectively. One can easily see that is vertical, and is horizontal, We also note that
[TABLE]
for and
On the other hand, from (2.1) and (2.2), we obtain
[TABLE]
[TABLE]
[TABLE]
[TABLE]
for any and Moreover, if is basic then It is easy to see that for coincides with the fibers as the second fundamental form and reflecting the complete integrability of the horizontal distribution.
For each , is an dimensional submanifold of called a fiber. A vector field on is called vertical (resp. hozirontal) if it is always tangent to fibres. A vector field on is called horizontal if it is always orthogonal to fibres. A vector field on is called basic if is horizontal and related to a vector field on , i.e., for all .
Lemma 2.1**.**
(see [15], [26]). Let be a Riemannian submersion. If and basic vector fields on then we get:
- (i)
** 2. (ii)
* is a basic and * 3. (iii)
* is a basic, *related to where and are the Levi-Civita connection on and 4. (iv)
* is vertical, for any *
Let and be Riemannian manifolds and is a differentiable map. Then the second fundamental form of is given by
[TABLE]
for where is the pull back connection and the Levi-Civita connections of the metrics and
Finally, let be a dimensional Riemannian manifold and denote the tangent bundle of Then is called an almost contact metric manifold if there exists a tensor of type and global vector field and is a form of , then we have
[TABLE]
[TABLE]
where are any vector fields on In this case, is called the almost contact metric structure of The almost contact metric manifold is called a contact metric manifold if
[TABLE]
for any where is a form in defined by The form is called the fundamental form of A contact metric structure of is said to be normal if
[TABLE]
where is Nijenhuis tensor of . Any normal contact metric manifold is called a Sasakian manifold. Moreover, if is Sasakian [7, 31], then we have
[TABLE]
where is the connection of Levi-Civita covariant differentiation.
3. Semi-slant Riemannian submersions
Definition 3.1**.**
Let be a Sasakian manifold and be a Riemannian manifold. Suppose that there exists a Riemannian submersion such that is normal to . Then is called semi-slant Riemannian submersion if there is a distribution such that
[TABLE]
and the angle between and the space is constant for nonzero and , where is the orthogonal complement of in . As it is, the angle is called the semi-slant angle of the submersion.
Now, let be a semi-slant Riemannian submersion from a Sasakian manifold onto a Riemannian manifold . Then, for , we put
[TABLE]
where and For we have
[TABLE]
where and For we get
[TABLE]
where and are vertical (resp. horizontal) components of respectively. Similarly, for any we have
[TABLE]
where (resp. ) is the vertical part (resp. horizontal part) of Then, the horizontal distribution is decomposed as
[TABLE]
here is the orthogonal complementary distribution of and it is both invariant distribution of with respect to and contains By (2.9), (3.4) and (3.5), we have
[TABLE]
and
[TABLE]
for and From (3.4), (3.5) and (3.6), we get:
Lemma 3.1**.**
Let be a semi-slant Riemannian submersion from a Sasakian manifold onto a Riemannian manifold . Then we obtain
[TABLE]
for and
On the other hand, using (3.4), (3.5) and the fact that we obtain:
Lemma 3.2**.**
Let be a semi-slant Riemannian submersion from a Sasakian manifold onto a Riemannian manifold . Then we get
[TABLE]
where is the identity operator on the space of
Let be a Sasakian manifold and be a Riemannian manifold. Let be a semi-slant Riemannian submersion. We now examine how the Sasakian structure on effects the tensor fields and of a semi-slant Riemannian submersion .
Lemma 3.3**.**
Let be a Sasakian manifold and a Riemannian manifold. Let be a semi-slant Riemannian submersion. Then we have
[TABLE]
[TABLE]
[TABLE]
for all and .
Proof.
Given , by virtue of (2.10) and (3.4), we have
[TABLE]
By using (2.3), (2.4), (3.4) and (3.5), we get
[TABLE]
In (3.15), comparing horizontal and vertical parts, we get (3.9) and (3.10). The other assertions can be obtained in a similar method.
∎
As the proof of the following theorem is similar to semi-slant submanifolds (Theorem 5.1 of [10]), we omit it.
Theorem 3.1**.**
Let be a semi-slant Riemannian submersion from a Sasakian manifold onto a Riemannian manifold Then we have
[TABLE]
where denotes the semi-slant angle of .
By using (2.9), (3.4), (3.7), (3.8) we get:
Lemma 3.4**.**
Let be a semi-slant Riemannian submersion from a Sasakian manifold onto a Riemannian manifold with a semi-slant angle Then we have
[TABLE]
for any
4. Integrability, Totally Geodesicness and Decomposition Theorems
In this section, we shall study the integrability and totally geodesicness of the distributions which are involved in the definition of a semi-slant Riemannian submersions and obtain decomposition theorems of such submersions.
Theorem 4.1**.**
Let be a semi slant Riemannian submersion from a Sasakian manifold onto a Riemannian manifold with a semi-slant angle Then
- (i)
* is integrable * 2. (ii)
* is integrable *
for and
Proof.
Given and , since , we have Thus is integrable for Since is a Sasakian manifold, by (2.9) and (2.10), we have
[TABLE]
[TABLE]
Then, by (3.16) and (2.7), we conclude that
[TABLE]
After some calculations, we obtain
[TABLE]
which proves (i). The other assertion can be obtained in a similar method. ∎
We now investigate the geometry of leaves of and
Theorem 4.2**.**
Let be a semi slant Riemannian submersion from a Sasakian manifold onto a Riemannian manifold with a semi-slant angle Then the distribution is parallel if and only if
[TABLE]
and
[TABLE]
for and .
Proof.
By virtue of (4.1), (3.4) and (2.3), we have
[TABLE]
for and Since is a semi-slant Riemannian submersion, using (2.3) and (2.7), we arrive
[TABLE]
or
[TABLE]
which gives (4.2). On the other hand, from (2.9) and (2.10), we get
[TABLE]
for and Then using (3.4) and (3.5), we conlude that
[TABLE]
Also, using (2.3), (2.4) and the character of , we get
[TABLE]
Then (2.7) imply
[TABLE]
which gives (4.3). ∎
For , we get:
Theorem 4.3**.**
Let be a semi slant Riemannian submersion from a Sasakian manifold onto a Riemannian manifold with a semi-slant angle Then the distribution is parallel if and only if
[TABLE]
and
[TABLE]
for any and
Proof.
Given and using (4.1), (3.4) and (2.3), we get
[TABLE]
Since is a semi-slant Riemannian submersion, using (2.3) and (2.7), we arrive
[TABLE]
which completes (4.4). On the other hand, by using (4.1) and(3.4) we get
[TABLE]
for all and Then (2.4) and (3.16) imply that
[TABLE]
Now, using the character of and (2.4), we get
[TABLE]
After some calculations, we have
[TABLE]
which gives (4.5). ∎
Since is integrable, we only study the integrability of the distribution and then we investigate the geometry of leaves of and .
Theorem 4.4**.**
Let be a semi slant Riemannian submersion from a Sasakian manifold onto a Riemannian manifold with a semi-slant angle Then the distribution is integrable if and only if
[TABLE]
and
[TABLE]
for and
Proof.
From (4.1), (2.9) and (2.10), we have
[TABLE]
for and Then by (3.5), we have
[TABLE]
From (2.4), we get
[TABLE]
Using (2.7), we obtain
[TABLE]
which gives (4.6). In a similar way, by virtue of (4.1), (2.9) and (2.10), we have
[TABLE]
for and Then by (3.16) and (2.6), we arrive
[TABLE]
Now, using the character of , (2.6) and (2.7) imply that
[TABLE]
so with some elementary calculations, we find
[TABLE]
which completes (4.7). ∎
For the geometry of leaves , we obtain:
Theorem 4.5**.**
Let be a semi slant Riemannian submersion from a Sasakian manifold onto a Riemannian manifold with a semi-slant angle Then the distribution is parallel if and only if
[TABLE]
and
[TABLE]
for and
Proof.
Given and , by (2.9) and (2.10), we have
[TABLE]
Thus, from (3.5), we find
[TABLE]
Taking into account that is a semi-slant Riemannian submersion, we get
[TABLE]
By (2.7), we obtain
[TABLE]
which gives (4.8). On the other hand, for , by virtue of (2.9), (2.10), we obtain
[TABLE]
From (3.4) and (3.5), we arrive
[TABLE]
Since is a semi-slant Riemannian submersion, using (3.16) and the character of we get
[TABLE]
Now, using (2.7), we obtain
[TABLE]
which gives (4.9). ∎
Similarly, we get:
Theorem 4.6**.**
Let be a semi slant Riemannian submersion from a Sasakian manifold onto a Riemannian manifold with a semi-slant angle Then the distribution is parallel if and only if
[TABLE]
for any and
Proof.
By virtue of (2.9) and (2.10), we have
[TABLE]
for and Then, from (3.4), we arrive
[TABLE]
Now, by (3.4), (3.5) and (3.16), we obtain
[TABLE]
By virtue of (2.7), (2.3) and the character of we arrive
[TABLE]
so with some elementary calculations, we get
[TABLE]
which completes (4.9). ∎
We now recall the following characterization for locally (usual) product Riemannian manifold from [33]. Let be a Riemannian metric tensor on the manifold and assume that the canonical foliations and intersect perpendicularly everywhere. Then is the metric tensor of a usual product of Riemannian manifolds if and only if and are totally geodesic foliations.
By virtue of Theorem 4.2, Theorem 4.3 and Theorem 4.5, we have the following theorem;
Theorem 4.7**.**
Let be a semi slant Riemannian submersion from a Sasakian manifold onto a Riemannian manifold with a semi-slant angle Then the total space is a locally product manifold of the leaves of , and i.e., if and only if
[TABLE]
[TABLE]
[TABLE]
[TABLE]
and
[TABLE]
[TABLE]
for and
From Theorem 4.5 and Theorem 4.6, we have the following theorem;
Theorem 4.8**.**
Let be a semi-slant Riemannian submersion from a Sasakian manifold onto a Riemannian manifold with a semi-slant angle Then the total space is a locally (usual) product manifold of the leaves of and i.e., if and only if
[TABLE]
[TABLE]
and
[TABLE]
for and
5. Totally umbilical and Totally geodesicness of
In this section, we are going to examine the totally umbilical fibres and the totally geodesicness of a semi-slant Riemannian submersion. First we give a new condition for a semi-slant Riemannian submersion to be totally umbilical. Let be a Riemannian submersion from a Riemannian manifold onto a Riemannian manifold . is called a Riemannian submersion with totally umbilical fibres if
[TABLE]
for where is mean curvature vector field of the fibres [35]. Then we have the following result.
Theorem 5.1**.**
Let be a semi-slant Riemannian submersion with totally umbilical fibres from a Sasakian manifold onto a Riemannian manifold then
Proof.
From (2.3), we have
[TABLE]
for any Now, using (3.4) and (3.5), we get
[TABLE]
By virtue of (2.9) and (2.10) imply that
[TABLE]
Taking inner product in above equation with , we obtain
[TABLE]
From (5.1), we have
[TABLE]
Interchanging and in (5.2), we get
[TABLE]
Subtracting (5.2) and (5.3), we get which shows that ∎
Now, we give some conditions for a semi-slant Riemannian submersion from a Sasakian manifold to be totally geodesic map. Recall that a differential map between two Riemannian manifolds is called totally geodesic if [6]. It is known that the second fundamental form is symmetric.
Theorem 5.2**.**
Let be a semi slant Riemannian submersion from a Sasakian manifold onto a Riemannian manifold with a semi-slant angle Then is a totally geodesic map if
[TABLE]
for any and where and
Proof.
By virtue of (2.5), (2.9) and (2.10), we have
[TABLE]
for any and . Now, from (2.7), we arrive
[TABLE]
By using (2.5), (2.6), (3.4) and (3.5) we get
[TABLE]
for any , where and Thus taking into account the vertical parts, we obtain
[TABLE]
which gives our assertion. ∎
Theorem 5.3**.**
Let be a semi slant Riemannian submersion from a Sasakian manifold onto a Riemannian manifold with a semi-slant angle Then is a totally geodesic map if and only if
- (i)
** 2. (ii)
** 3. (iii)
**
for any and .
Proof.
(i) Given and , from (2.7), (2.9) and (2.10), we have
[TABLE]
By using (2.5) and (2.10), we obtain
[TABLE]
From (2.3), we get
[TABLE]
which gives (i).
(ii) By virtue of (2.7), (2.9) and (2.10), we get
[TABLE]
for Then using (3.4), (3.5) and (2.10), we obtain
[TABLE]
Taking into account that is a semi-slant Riemannian submersion, using (2.3) imply that
[TABLE]
Now, from (2.7) and (3.16), we obtain
[TABLE]
so with some elementary calculations, we arrive
[TABLE]
which completes (ii).
(iii) If , then by using (2.7), (2.9) and (2.10), we have
[TABLE]
Using (2.9), (3.4) and (3.5), we get
[TABLE]
By virtue of (2.4), (3.2), (3.4) and (3.5), we obtain
[TABLE]
[TABLE]
From the above equation, we obtain (iii). ∎
In a similar way, we obtain the following lemma:
Theorem 5.4**.**
Let be a semi slant Riemannian submersion from a Sasakian manifold onto a Riemannian manifold with a semi-slant angle Then is a totally geodesic map if and only if
- (i)
** 2. (ii)
** 3. (iii)
**
for and .
6. Examples
Example 6.1**.**
Every invariant submersion from a Sasakian manifold to a Riemannian manifold is a semi-slant Riemannian submersion with and .
Example 6.2**.**
Every slant Riemannian submersion from a Sasakian manifold to a Riemannian manifold is a semi-slant Riemannian submersion with .
Now, we construct some non-trivial examples of semi-slant Riemannian submersion from a Sasakian manifold. Let denote the manifold with its usual Sasakian structure given by
[TABLE]
[TABLE]
[TABLE]
where are the Cartesian coordinates. Throughout this section, we will use this notation.
Example 6.3**.**
Let be a submersion defined by
[TABLE]
with Then it follows that
[TABLE]
and
[TABLE]
Hence we have , . Thus it follows that and is a slant distribution with slant angle Thus is a semi-slant submersion with semi-slant angle Also by direct computations, we obtain
[TABLE]
[TABLE]
where and denote the standard metrics (inner products) of and . Thus is a semi-slant Riemannian submersion.
Example 6.4**.**
Let be a submersion defined by
[TABLE]
Then the submersion is a semi-slant Riemannian submersion such that and with semi-slant angle
Example 6.5**.**
Let be a submersion defined by
[TABLE]
with Then the submersion is a semi-slant Riemannian submersion such that and with semi-slant angle
Example 6.6**.**
Let be a submersion defined by
[TABLE]
*Then the submersion is a semi-slant Riemannian submersion such that and with semi-slant angle
**Acknowledgement
**This paper is supported by Bingöl University research project (BAP-FEF.2016.00.011).
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