1. Introduction
In Riemannian geometry, there are few appropriate maps among Riemannian manifolds that compare their geometric properties. In this direction, as a generalization of the notions of isometric immersions and Riemannian submersions, Riemannian maps between Riemannian manifolds were initiated by Fischer [
1], while isometric immersions and Riemannian submersions were widely studied in [
2] and [
3], respectively. However, the notion of Riemannian maps is a new research topic for geometers. More precisely, a differentiable map
between Riemannian manifolds
and
is called a Riemannian map (
where
and
) if it satisfies the following equation:
where
is the differentiable map of
Consequently, isometric immersions and Riemannian submersions are particular cases of Riemannian maps with
and
respectively [
1].
The other prominent basic map for comparing geometric structures between Riemannian manifolds is Riemannian submersion, and it was studied by O’Neill [
4] and Gray [
5]. In 1976, Watson [
6] studied Riemannian submersion between Riemannian manifolds equipped with differentiable structures. After that, several kinds of Riemannian submersions were introduced and studied, including Riemannian submersion [
3], H-anti-invariant submersion [
7], H-semi-invariant submersion [
8] and H-semi-slant submersion [
9].
Currently, one of the most inventive topics in differential geometry is the theory of Riemannian maps between different Riemannian manifolds. It is well known that differentiable maps between Riemannian manifolds have wide applications in differential geometry as well as in physics, such as in Yang–Mills theory [
10], Kaluza–Klein theory [
11], and supergravity and superstring theories [
12].
We also note that quarternionic manifolds have many applications, including for nonlinear
models with super symmetry [
12], in the theory of harmonic differential forms [
13] and obtaining estimates for the Betti numbers of the manifold [
14,
15]. In this paper, we have for the first time investigated
h-qhs Riemannian maps from almost quarternionic manifolds to Riemannian manifolds. Here, we mainly focus on the most fundamental and interesting geometric properties on the fibers and distributions of these maps.
Nowadays, Riemannian maps and related topics have been actively studied by many authors, such as invariant and anti-invariant Riemannian maps [
16], semi-invariant Riemannian maps [
17], slant Riemannian maps [
18], semi-slant Riemannian maps [
19,
20], hemi-slant Riemannian maps [
21], quasi-hemi-slant Riemannian maps [
22], almost
h-semi-slant Riemannian maps [
23], V-quasi-bi-slant Riemannian maps [
24] and Clairaut semi-invariant Riemannian maps [
25]. As a generalization of
h-slant Riemannian maps [
26],
h-semi-slant Riemannian maps [
9] and
h-hemi-slant Riemannian maps, we define and study
h-qhs Riemannian maps from almost Hermitian manifolds to Riemannian manifolds. In the near future, we plan to work on conformal
h-qhs submersions, conformal
h-qhs submersions,
h-qhs semi-Riemannian submersions, etc.
This paper is structured as follows. In
Section 2, we recall basic facts about Riemannian maps and almost Hermitian manifolds. In
Section 3, we define
h-qhs Riemannian maps and study the geometry of leaves of distributions that are involved in the definition of such maps. We give necessary and sufficient conditions for
h-qhs Riemannian maps to be totally geodesic. Finally, we provide two concrete examples of
h-qhs Riemannian maps.
2. Preliminaries
Let
and
be Riemannian manifolds and
be a
-Riemannian map [
1].
We define O’Neill’s tensors
and
[
4] by
for any vector fields
on
where ∇ is the Levi-Civita connection of
From Equations (2) and (3), we have
for
and
where
and
is basic.
Let
be a
map. The second fundamental form of
is given by
for
where
is the pullback connection [
27]. The map
is said to be a total geodesic if
for
.
Let
be an almost quaternionic Hermitian manifold, where
is a Riemanian metric on the maniifold
and
E is a rank 3 subbundle of
such that for any point
within some neighborhood
U, there exists a local basis
of sections of
E on
U satisfying all
in which
for
where the indices are taken from
modulo 3 and
is called the quaternionic Hermitian basis. The structure
is called a quaternionic kähler manifold if there exist locally defined 1 forms
such that for
, we have
for
where the indices are taken from
modulo
If there exists a global parallel quaternionic Hermitian basis
of sections of
E on
, then
is called a hyperkähler. The structure
where
, a hyperkähler metric, is called a hyperkähler structure on
.
A map
is called an
-holomorphic map if for any point
and
, there exists
such that
A Riemannian submersion between quaternionic kähler manifolds
which is an
-holomorphic map, is known as a quaternionic kähler submersion (or a hyperkähler submersion) [
9]:
Definition 1 ([
23])
. A Riemannian map π from the almost quaternionic Hermitian manifold to the Riemannian manifold is called an h-semi-slant Riemannian map if, given a point with a neighborhood U, there exists a quaternionic Hermitian basis of sections of E on U such that for any , the following is true:in which the angle between and the space is constant for a non-zero and where is an orthogonal complement of in Furthermore, assume we have
Then, we call the map a strictly h-semi-slant Riemannian map, the basis a strictly h-semi-slant basis and the angle a strictly h-semi-slant angle.
3. h-Quasi-Hemi-Slant Riemannian Maps
Motivated by the studies given in
Section 2, we give the definition of the
h-qhs Riemannian map as follows:
Definition 2. A Riemannian map π from the almost quaternionic Hermitian manifold to the Riemannian manifold is called an h-qhs Riemannian map if, given a point with a neighborhood U, there exists a quaternionic Hermitian basis of sections of E on U such that for any , there is a distribution on U such thatand the angle between and the space is constant for a non-zero and where admits three orthogonal complementary distributions and such that D is invariant, is a slant with an angle and is anti-invariant. We call the basis an h-qhs basis and the angles h-qhs angles.
Furthermore, let us say we have
Then, we call the map a strictly h-qhs Riemannian map, the basis a strictly quasi-hemi-slant basis and the angle a strictly quasi-hemi-slant angle:
Definition 3. A Riemannian map π from the almost quaternionic Hermitian manifold to the Riemannian manifold is called an almost h-qhs Riemannian map if, given a point with a neighborhood U, there exists a quaternionic Hermitian basis of sections of E on U such that for any there is a distribution on U such thatand the angle between and the space is constant for a non-zero and where the vertical distribution admits three orthogonal complementary distributions and such that is invariant, is a slant with an angle and is anti-invariant. We call the basis an almost h-qhs basis and the angles almost h-qhs angles.
Let be an almost h-qhs Riemannian map. We can easily observe the following:
- (a)
If , and then is an almost proper h-semi-slant Riemannian map with a semi-slant angle ;
- (b)
If , and then is an almost h-hemi-slant Riemannian map.
We say that the almost h-qhs Riemannian map is proper if , and Thus, one can easily see that the h-hemi-slant Riemannian map, h-semi-invariant Riemannian map and h-semi-slant Riemannian map are examples of h-qhs Riemannian maps.
Obviously, is an invariant sub-bundle of with respect to the complex structure R.
For
we have
where
,
,
and
For
we obtain
where
,
and
For
we have
where
,
and
We will denote an almost h-qhs Riemannian map from a hyperkähler manifold onto a Riemannian manifold such that is an almost h-qhs basis by .
The following lemmas can be easily obtained:
Lemma 1. For , we getwhere Lemma 2. For , we havefor any , and Proof. Using Equations (9), (13) and (14), we can find all equations of Lemma 2: □
Lemma 3. With being an almost h-qhs Riemannian map, we then obtainfor , and Proof. Using Equations (4)–(7), (13) and (14), we can easily obtain Equations (15)–(22). □
Now, we define
for
,
and
Lemma 4. For , we findfor all , and Proof. Using Equations (15) and (16) as well as Equations (21)–(26), Lemma 4 follows. □
If the tensors
and
are parallel with respect to the linear connection
∇ on
, then
for all
and
:
Lemma 5. Let , be an almost h-qhs Riemannian map. Then, we obtainfor any non-zero vector field and , where } is an almost h-qhs basis with the almost h-qhs angles . Proof. For any non-zero vector field
and
, we have
and
where
is the
h-qhs angle.
Using Equations (9) and (13), we obtain
From Equations (29) and (30), Equation (27) follows. □
Theorem 1. Let π be an h-qhs Riemannian map from an almost hyperkahler manifold to a Riemannian manifold . Then, the following cases are equivalent:
- (a)
is integrable;
- (b)
for and ; - (c)
for and ; - (d)
for and
Proof. For
,
,
and
, since
we have
Thus,
is integrable ⇔
Now, using Equations (4) and (12)–(14), we have
Since
is R-invariant, we have
Therefore, we obtain the result. □
Theorem 2. The following cases are equivalent for the map π defined in Theorem 1:
- (a)
is integrable;
- (b)
for all and ; - (c)
for all and ; - (d)
for all and
Proof. For
,
,
and
, since
, we have
Thus,
is integrable ⇔
Using Equations (
4), (
5), (
12) and (
13) as well as Lemma
we have
which gives
Since
is an R-slant distribution, therefore, we obtain
Therefore, we find the result. □
Theorem 3. For the h-qhs Riemannian map π defined in Theorem 1, is always integrable.
Proof. We can easily prove the Theorem as hemi-slant case given in [
21]. □
Theorem 4. For the h-qhs Riemannian map π defined in Theorem 1, any one of the following assertions implies the others:
- (a)
defines a totally geodesic foliation on ;
- (b)
for and ; - (c)
for and ; - (d)
for and
Proof. For
and
, using Equations (6), (7) and (12)–(14) as well as Lemma 5, we have
Therefore, the result follows. □
Theorem 5. The following conditions are equivalent for the h-qhs Riemannian map π:
- (a)
defines a totally geodesic foliation on ;
- (b)
for and ; - (c)
for and ; - (d)
for and
Proof. For
and
, using Equations (
4), (
5) and (
12)–(
14) as well as Lemma 5, we have
Therefore, the result follows. □
Theorem 6. Let π be an h-qhs Riemannian map from an almost hyperkahler manifold to a Riemannian manifold . Then, any one of the following assertions implies the others:
- (a)
defines a totally geodesic foliation on ;
- (b)
for and ; - (c)
for and ; - (d)
for and
Proof. For
and
, using Equations (
4), (
12) and (
13), we have
Moreover, using Equations (
4), (
12) and (
14), we obtain
Therefore, the result follows. □
Theorem 7. With being an h-qhs Riemannian map, the following conditions are equivalent:
- (a)
defines a totally geodesic foliation on ;
- (b)
for and ; - (c)
for and ; - (d)
for and
Proof. For
and
, using Equations (
5), (
12) and (
13) as well as Lemma
we have
which gives
Moreover, from Equations (5), (13) and (14) as well as Lemma 5, we have
Therefore, the result follows. □
Theorem 8. For the h-qhs Riemannian map π defined in Theorem 1, any one of the following assertions implies the others:
- (a)
defines a totally geodesic foliation on ;
- (b)
for and ; - (c)
for and ; - (d)
for and
Proof. For
and
, using Equations (5), (12) and (13), we have
Again, using Equations (5), (13) and (14), we have
Therefore, the result follows. □
Theorem 9. Let π be an h-qhs Riemannian map from an almost hyperkahler manifold to a Riemannian manifold . Then, the following conditions are equivalent:
- (a)
π is a totally geodesic map;
- (b)
for and ; - (c)
for and ; - (d)
for and
Proof. Since π is a Riemannian map, therefore, we have
for
For
,
and
, using Equations (
4), (
5) and (
12)–(
14) as well as Lemma 5, we have
Moreover, using Equations (
4), (
5) and (
12)–(
14) as well as Lemma 5, we have
Thus, the theorem is proven. □