1. Introduction
As a dual notion to the isometric immersions, O’Neill and Gray introduced independently the concept of Riemannian submersions in [
1,
2], respectively. Riemannian submersions play an important role in mathematical and theoretical physics, especially due to their usage in the superstring, Yang–Mills, Kaluza–Klein and supergravity theories [
3,
4,
5,
6,
7,
8]. For more information on Riemannian submersions, we refer to the monographs [
9,
10].
In [
11], Taştan, Şahin and Yanan introduced and investigated hemi-slant submersions from almost Hermitian manifolds onto Riemannian manifolds. This class of submersions appears as a natural generalization of invariant, anti-invariant, semi-invariant and slant submersions, four families of Riemannian submersions with remarkable geometric properties thoroughly investigated by Şahin [
12,
13,
14,
15]. Later, these submersions were studied for different ambient spaces by various authors who obtained several results regarding their geometry (see, e.g., [
16,
17,
18,
19,
20,
21,
22,
23]).
One of the most important curvature invariants for a Riemannian manifold
was introduced by Chen [
24] as follows:
where
is scalar curvature of
M and
In ref. [
25], B.-Y. Chen established a general optimal inequality involving the intrinsic invariant
and the squared mean curvature of a submanifold
M isometrically immersed in a real space form
of constant sectional curvature
c. This result gave rise to a whole theory, known as the theory of Chen’s invariants, which gained an exponential development in the following years (see the monograph [
26] and the recent articles [
27,
28,
29,
30,
31,
32], as well as the references cited therein). The main purpose of this new theory is to prove answers to a fundamental problem in the geometry of submanifolds, namely “
establish simple relationships between the main extrinsic invariants and the main intrinsic invariants of a submanifold” [
26]. Recently, Chen-like inequalities have been investigated in the setting of Riemannian submersions (see, e.g., [
19,
33,
34,
35,
36]).
Motivated by the studies indicated above, we obtain in this work various Chen-like inequalities for hemi-slant Riemannian submersions from complex space forms onto Riemannian manifolds and discuss the equality case of the obtained inequalities. The paper is organized as follows. In Section cid2, we recall the definition and some fundamental properties of hemi-slant submersions. In Section cid3, we derive the main inequalities: we first establish a Chen-like inequality involving the Ricci curvature and then state a Chen–Ricci inequality for the vertical and the horizontal distributions of hemi-slant Riemannian submersions with total space a complex space form, and with base an arbitrary Riemannian manifold. We also discuss the equality case of the obtained inequalities. In Section cid4, we provide examples of hemi-slant Riemannian submersions to show that the equality cases of the main inequalities can be attained.
2. Hemi-Slant Riemannian Submersions
In this study, manifolds, mappings, vector fields, sections, and so on, will always be supposed of class . We first recall the following definition.
Definition 1 ([
11]).
Let be an almost Hermitian manifold and be a Riemannian manifold. A Riemannian submersion is said to be a hemi-slant submersion if there is a distribution such thatand the angle between and the space is constant for nonzero and , where is the orthogonal complement of in . In this case, θ is called the hemi-slant angle of σ. Moreover, the hemi-slant submersion σ is called proper if and .
Throughout this paper, we will assume all horizontal vector fields as basic vector fields.
Let
be a hemi-slant submersion. For
, we obtain
where
and
. For
, we obtain
where
and
. We have
where
is the orthogonal complement of
in
and is invariant under
J. Let us consider the O’Neill’s tensors
and
given by [
1]
for any vector fields
and
on
M, where
and
denote the vertical and horizontal projections of the submersion, and
∇ is the Levi-Civita connection of
g. On the other hand, for any
and
from (
5), we obtain
where
.
We denote by
R,
,
and
the Riemannian curvature tensors of Riemannian manifolds
M,
N, the vertical distribution
and the horizontal distribution
, respectively. Then, the Gauss–Codazzi type equations are given by [
1]
where
for all
and
.
Moreover, the mean curvature vector field
of any fiber of Riemannian submersion
is given by
where
is an orthonormal basis of the vertical distribution
. Furthermore,
has totally geodesic fibers if
vanishes identically.
Let
M be an almost Hermitian manifold with an almost complex structure
J and a Hermitian metric
g. If
J is parallel with respect to the Levi–Civita connection
∇ on
M, that is
for all vector fields
X and
Y on
M, then
is called a Kähler manifold. A complete and simply connected Kähler manifold
M is said to be a complex space form if it has constant holomorphic sectional curvature
c. In this case, the complex space form is denoted by
. The curvature tensor of the complex space form
is given by
for any
.
The following theorem gives us a characterization of hemi-slant submersions (see [
11]).
Theorem 1. Let σ be a Riemannian submersion from an almost Hermitian manifold onto a Riemannian manifold . Then, σ is a hemi-slant Riemannian submersion with hemi-slant angle θ if and only if there exist a distribution and a constant such that
- (i)
;
- (ii)
, for all , where is the orthogonal complement of in .
Furthermore, we have
By virtue of (
3) and (
4), we have the following result.
Lemma 1. Let , be a complex space form and a Riemannian manifold, respectively. If is a hemi-slant Riemannian submersion, then the following relations are valid for any .
3. Chen–Ricci Inequality
In the present section, we aim to obtain some inequalities involving the Ricci curvature and the scalar curvature on the vertical and horizontal distributions for hemi-slant Riemannian submersions from a complex space form to a Riemannian manifold. We will also discuss the equality cases of these inequalities.
Let
be a proper hemi-slant Riemannian submersion from a complex space form
onto a Riemannian manifold
and
. For every
, we consider
an orthonormal basis of
and
an orthonormal basis of
, respectively, such that
is an orthonormal basis of
, while
is an orthonormal basis of
. We will call this basis an adapted hemi-slant basis of
. Obviously, we have
and
Besides from (
10), (
11) and (
15), we have
for all vector fields
and
for all vector fields
.
Theorem 2. Let be a proper hemi-slant Riemannian submersion from a complex space form onto a Riemannian manifold Then, we have for a unit vector field , where r is the dimension of the vertical distribution. The equality case of (19) holds identically for any unit vector field if and only if each fiber is totally geodesic. Proof. From (
17), we obtain
where
If
, then choosing an adapted hemi-slant basis
of
, one derives
Using last equation in (
20), we derive (
19). On the other hand, it is clear that the equality case of (
19) holds identically for any unit vector field
if and only if
which means that the fibers are totally geodesic (see [
9]). □
In a similar way, using an adapted hemi-slant basis of , we obtain the following results.
Theorem 3. Let be a proper hemi-slant Riemannian submersion from a complex space form onto a Riemannian manifold Then, we have for a unit vector field . The equality case of (23) holds identically for any unit vector field if and only if each fiber is totally geodesic. Theorem 4. Let be a proper hemi-slant Riemannian submersion from a complex space form onto a Riemannian manifold Then, we have for .
Theorem 5. Let be a proper hemi-slant Riemannian submersion from a complex space form onto a Riemannian manifold . Then we have As a consequence of the last theorem, we derive the following.
Corollary 1. Let be a proper hemi-slant Riemannian submersion from a complex space form onto a Riemannian manifold Then, we have The equality case of (26) holds if and only if each fiber is totally geodesic. Proof. The inequality (
26) is clear from (
25). On the other hand, the equality case of (
26) holds if and only if
which implies
for all
. Replacing
U by
in (
27), where
, and using the symmetry of the O’Neill tensor
for vertical vector fields, we obtain
. Hence, the fibers of the submersion are totally geodesic. □
Now, if
is an orthonormal basis of
and
is an orthonormal basis of
, we denote
where
and
, and
where
and
. From [
35], we use
Moreover, if
, then
and
From the Binomial theorem, we have the following relation between the components of the O’Neill tensor field
and the squared mean curvature
:
Theorem 6. Let be a proper hemi-slant Riemannian submersion from a complex space form onto a Riemannian manifold . Suppose U is a unit vertical vector field. Then:
(i) If , we have (ii) If , we have Moreover, the equality cases of (37) and (38) hold if and only if there exist two orthonormal bases and of and , respectively, such that and , for . Proof. Let be an adapted hemi-slant basis of .
Due to the fact that one can choose the above adapted hemi-slant basis such that
, it suffices to prove (
38) for
.
Using (
28) in (
25), we can write
If (
36) is used in (
39), then (
39) can be rewritten as
Thus, from (
40) we derive
Furthermore, taking
,
in (
10), we obtain
Using (
42) in (
41), we derive
Considering (
44) in (
43), we derive
On the other hand, since
is a complex space form, its curvature tensor
R satisfies (
15) and we get
As
, we obtain immediately
and therefore (
46) can be written as
Considering now the last equation in (
45), we get
and the conclusion is now clear.
Due to the fact that in this case one can choose the adapted hemi-slant basis
such that
, it suffices to prove (
38) for
.
With similar arguments as in case
, we obtain
and
As
, we obtain immediately
and therefore (
49) can be written as
Considering now the last equation in (
48), we get
and inequality (
38) is clear.
Now, we remark that the equality case of (
37) holds if and only if the equality is attained in (
41). However, this happens if and only if
and
, for
and
. On the other hand, the equality case of (
38) holds if and only, with respect to the hemi-slant adapted basis considered in the proof, we have
and
, for
and
. Using a reordering of the vectors in the basis of
, we derive the conclusion. □
Theorem 7. Let be a proper hemi-slant Riemannian submersion from a complex space form onto a Riemannian manifold . Then, we have Moreover, the equality holds in (51) if and only if the horizontal distribution is integrable. Proof. Using the anti-symmetry of
and (
18), we obtain
where
is an orthonormal basis of
. Now, using (
31) in (
52) we obtain
and inequality (
51) follows immediately. Moreover, it is clear that the equality case of (
51) holds if and only if
, for
and the proof is now complete due to the fact that the vanishing of the O’Neill tensor
is equivalent to the integrability of the horizontal distribution (see, e.g., [
9]). □
Theorem 8. Let be a proper hemi-slant Riemannian submersion from a complex space form onto a Riemannian manifold . If is an orthonormal basis of , then we have Proof. By using (
29) in (
53), we have
Thus, (
55) can be written as
Moreover, taking
in (
11), we obtain
Using (
57) in (
56), we derive
Since
is a complex space form, its curvature tensor
R satisfies the equality (
15) and we obtain
Then, from (
58) and (
59), taking into account that
we get
and equality (
54) follows immediately. □
As an outcome of the above result, we have the following.
Theorem 9. Let be a proper hemi-slant Riemannian submersion from a complex space form onto a Riemannian manifold . If X is a unit horizontal vector field, then we have Moreover, the equality case of the above inequality holds identically for all unit horizontal vector fields if and only if the horizontal distribution is integrable.
Proof. Inequality (
62) is clear from Theorem 8 because in (
54) we can select
to be any arbitrary unit horizontal vector field. This is due to the fact that one can always choose in Theorem 8 an orthonormal basis
of
with
.
Now, if the horizontal distribution is integrable, then
, for
, and it is clear that we have equality in (
62). Conversely, if the equality case of (
62) holds identically for all unit horizontal vector fields, then it follows that
, for
and
,
, which means
, for all
. However, due to the skew-symmetry of
for horizontal vector fields, it is obvious that
. Hence,
for
, and therefore the horizontal distribution is integrable. □
Now, we are going to state the Chen–Ricci inequality between the vertical and horizontal distributions for a hemi-slant Riemannian submersion
from a complex space form
onto a Riemannian manifold
. Suppose
is an orthonormal basis of
and
is an orthonormal basis of
. Then, for the scalar curvature
of
, we have
Next, let us denote as usual (see [
35]):
Theorem 10. Let be a proper hemi-slant Riemannian submersion from a complex space form onto a Riemannian manifold . Suppose is an orthonormal basis of and is an orthonormal basis of .
(i) If , then (ii) If , then The equality case of (69) and (70) holds if and only if for , .
Proof. Since
is a complex space form, using (
64) and (
32) we get
On the other hand, using the Gauss–Codazzi type Equations (
10)–(
12), we derive
Therefore, using (
30) and (
36) in (
72), we obtain
Using now (
42), (
57) and (
71) in (
73), we get
Hence, in view of (
65)–(), the equality (
74) implies
If
, then considering (
47) and (
59) in (
75), in view of (
60) we obtain (
69). Similarly, if
, then using (
50), (
59) and (
60) in (
75), we obtain (
70). Finally, the equality of (
69) and (
70) holds if and only if we have equality in (
75), which happens if and only if
and
, for all
and
. This completes the proof. □
Remark 1. If is a proper hemi-slant Riemannian submersion from a complex space form onto a Riemannian manifold , then from (71) and (72) we get From (76) we derive immediately that Moreover, it is clear that the equality case of (77) holds for all if and only if the horizontal distribution is integrable, while the equality cases of (78) hold for all if and only if the fibers of σ are totally geodesic submanifolds of . In particular, we deduce the following result. Theorem 11. Let be proper a hemi-slant Riemannian submersion from a complex space form onto a Riemannian manifold with totally geodesic fibers. Then, we have Moreover, the equality case of (79) holds for all if and only if the horizontal distribution is integrable. We now recall the following result, which we will use a little later.
Lemma 2 ([
37]).
Let be n real numbers . Thenwith equality iff .
Theorem 12. Let be a proper hemi-slant Riemannian submersion from a complex space form onto a Riemannian manifold . Then we have Equality case of (80) holds for all if and only σ has totally umbilical fibers. Proof. Applying Lemma 2 in (
81), we get
which gives (
80). Equality case of (
80) holds for all
if and only if the components of the O’Neill tensor
satisfy
and
, for
,
,
. The conclusion is now clear. □
Using a similar proof as in Theorem 12, we deduce the following result.
Theorem 13. Let be a proper hemi-slant Riemannian submersion from a complex space form onto a Riemannian manifold . Then we have The equality case of the above inequality holds for all if and only if the components of the O’Neill tensor with respect to some suitable orthonormal bases of the horizontal and vertical distributions satisfy and , for and , .
4. Examples
In this section, we provide examples of hemi-slant Riemannian submersions, illustrating the main results stated above.
From [
11], we know that the concept of hemi-slant submersion generalizes in a natural way the notions of invariant, anti-invariant, semi-invariant and slant submersions. More precisely, if we denote the dimension of
and
by
and
, respectively, then we have the following:
If
, then
M is a semi-invariant submersion [
12].
If
and
, then
M is an invariant submersion [
15,
38].
If
and
, then
M is an anti-invariant submersion [
13].
If
, then
M is a slant submersion with slant angle
[
14].
We would like to point out that there is a special type of anti-invariant submersion, called Lagrangian submersion, for which the almost complex structure of the total space of the submersion reverses
and
(see [
39]). Examples of invariant, anti-invariant, Lagrangian, semi-invariant, slant and hemi-slant submersions, as well as various interesting results regarding the geometry of these submersions, can be found in [
11,
12,
13,
14,
15,
39]. At this point, we would just like to note that according to Theorem 4.5 of [
39], it follows that the horizontal distribution of a Lagrangian submersion with total space a complex space form is integrable. However, such submersions do not provide us suitable examples to illustrate the equality case of the inequalities stated in Theorems 7, 9 and 11, because a Lagrangian submersion is not a proper hemi-slant submersion.
Next, we will construct the first example of proper hemi-slant submersion satisfying the equality case of all inequalities established in the above section.
Example 1. Consider the Kähler manifold equipped with the canonical Euclidean metric and the complex structure J given by: Define now a map by where and is the standard canonical Euclidean metric on . Then, it is easy to check that σ is a hemi-slant submersion such that Moreover, the hemi-slant angle of σ is. A straightforward computation shows that fibers of the submersions are totally geodesic and the horizontal distribution is integrable. Hence, we conclude that the inequalities stated in Theorems 2, 3, 6, 7, 9–11 and 13 are satisfied with equality sign.
Similarly, the following map illustrates the equality case of the above-mentioned inequalities.
Example 2. Consider the Euclidean space equipped with the standard metric (denoted by ) and the compatible almost complex structure J given by Then, is a Kähler manifold and we define a map by and is the standard canonical Euclidean metric on . A direct computation shows that σ is a hemi-slant submersion with the hemi-slant angle such that We derive immediately that fibers of the submersions are totally geodesic and the horizontal distribution is integrable. Hence, we have again that σ satisfies the equality case of the inequalities stated in Theorems 2, 3, 6, 7, 9–11 and 13.