1
1 Introduction
Throughout paper, we will use some abbreviations as follows:
| Riemannian Manifold |
RS |
| Riemannian Submersion |
RS |
| Conformal Generic Submersions |
CGS |
| Locally Product Riemannian |
l.p.R. |
| grad |
|
One of the most popular areas of study in differential geometry is submanifold theory, and establishing proper smooth maps between two manifolds is one of the quickest ways to compare them and transfer certain structures from one manifold to another. If there are two manifolds, then a differential map is said to be an immersion (submersion) if its rank coincide with the dimension of the source manifold (target manifold). Moreover, these are called isometric immersions (isometric submersions) if the maps defined between manifolds are isometric. O’Neill (1966) and Gray (1997) were the first to address the idea of Riemannian submersions between Riemannian manifolds. The Riemannian submersions are being used extensively in both mathematics and physics. Particularly in the context of the Yang-Mills theory (Bourguignon and Lawson, 1981; Baird and Wood, 2003), Kalauza-Klien theory (Bourguignon, 1990), super-gravity and super-string theories (Ianus and Visinescu, 1991; Ianus and Visinescu, 1987), redundant robotic chains (Altafini, 2004) etc.
Riemannian submersions eventually developed into a suitable approach for describing the geometry of RMs with differential structures. The first study of RS between RMs equipped with an additional structure of almost complex type was executed by Watson (1976). In most instances, Watson established that the structure of the base manifold and each fiber is the same as that of the total space by defining an almost Hermitian submersion between almost Hermitian manifolds. In this case, the RS is also a complex mapping and consequently, the vertical and horizontal distributions are invariant with respect to the almost complex structure of the total manifold of the submersion. Almost Hermitian submersions have been extended to the almost contact manifolds (Chinea, 1985), locally conformal Kaheler manifolds (Marrero and Rocha, 1994) and QR manifolds (Ianus et al., 2008). Escobales (Escobales, 1978) studied RS from complex projective space onto a RM under the assumption that the fibres are connected, complex, totally geodesic submanifolds. In fact this assumption also implies that the vertical distribution is invariant with respect to the almost complex structure.
The vertical and horizontal distributions are invariant, which is a characteristic shared by all the submersions mentioned above. Then, in 2010, B. Sahin presented the notion of anti-invariant RS, which is referenced in (Şahin, 2010). Anti-invariant RS are the RS from almost Hermitian manifolds to RMs such that the vertical distributions (or, for that matter the fibres) are anti-invariant under the almost complex structure of total manifold. Such submersions are demonstrated to exhibit a wealth of geometrical characteristics and are helpful for assessing the geometry of the total manifold of the submersion. The vertical and horizontal distributions are reversed by the almost complex structure of the total manifold in a Lagrangian submersion, which is a special case of an anti-invariant RS. (Şahin, 2010; Şahin, 2011; Tastan, 2014). Following that, many RS have been investigated such as Semi-invariant submersion (Şahin, 2011), Slant submersion (Şahin, 2011), Semi-slant submersion (Park and Prasad, 2013), Generic submersion (Ali and Fatima, 2013) etc.
On the other hand, horizontally conformal submersions caught attention in 1992 and studied by Gudmundsson and Wood (1997). Horizontally conformal submersions are the generalization of RS and unlikely to the RS, horizontally conformal submersions do not preserve the distance between the points but they preserve the angles between the vector fields. This property allows one to transfer specific properties of a manifold to another manifold by deforming such properties. Recently, M. A. Akyol and B. Sahin defined conformal anti-invariant submersion (Akyol and Şahin, 2016) and later on conformal semi-invariant, conformal slant, conformal semi-slant and CGS are studied by M. A Akyol and others (we refer to Akyol and Şahin, 2017; Akyol, 2017; Akyol and Şahin, 2019; Akyol, 2017; Akyol, 2021 Özdemir et al., 2017).
The current article’s objective is to investigate CGS from l.p.R manifolds onto RMs. The manuscript is structured as follows: Section 2 reviews the fundamental ideas of RS and horizontally conformal submersions and Section 3 explains the requirement for a l.p.R manifold. In Section 4, the definition and an example of CGS are covered. Then, several fundamental conclusions are reached, including equivalent criteria for the distributions’ integrability and conditions that are required and adequate for the distributions to describe completely geodesic foliations. Section 4 also lists the criteria for CGS to be a harmonic map. The sectional curvature relations of the total manifold, fibers and manifolds are the only focus of Section 5.
2
2 Conformal Riemannian Submersions
We shall review the concept of conformal submersions, which are one of a large class of conformal maps, but in this study, we won’t look at these maps.
Definition 1
(Baird and Wood, 2003) “ Let
and
be two RMs with dimensions m and n, respectively, and let
be a
– differentiable map between them. If either
-
, or
-
maps horizontal space
conformally onto
, i.e.,
is surjective and there exists a number
such that
(1)
for any
.
Then,
is called horizontally weakly conformal or semi conformal at
. ”.
In the definition above, if “
is met, we say that p is a critical point of
and if
is met we refer point p as a regular point. At a critical point,
has rank 0 where as at a regular point
has rank n and represents submersion. The number
, which is necessarily non-negative, is called the square dilation of
at p. The square root
is called the dilation of
at p. The map
is called horizontally weakly conformal or semi conformal on M if it is horizontally weakly conformal at every point of M. It is clear that we refer to a horizontally conformal submersion if
has no critical points. Let
be a submersion. A vector field E on
is said to be projectable if there exists a vector field
on
, such that
for all
. In this case E and
are called
– related. A horizontal vector field
on
is called basic, if it is projectable. It is well known fact that if
is a vector field on
, then there exists a unique basic vector field Z on
, such that Z and
are
– related. The vector field Z is called the horizontal lift of
(O’Neill, 1966).”.
In (O’Neill, 1966), the basic tensors of submersions were presented. They function similar to the second fundamental form of immersion. More precisely, O’Neill’s tensors
and
defined for any vector fields
by
(2)
(3)
where
and
are the vertical and horizontal projections of
and
(see Falcitelli et al., 2004). On the other hand, from (2) and (3 ), we have
(4)
(5)
(6)
(7)
for any
and
, where
. If
is basic, then
. It is easily seen that for any
and
, the linear operators
are skew-symmetric, that is
for all
and
. The restriction of
to the vertical distribution
is precisely the same as the second fundamental form of the fibers, as can also be seen. We conclude that
has totally geodesic fibres if and only if
because
is skew-symmetric. The following are the results for the horizontal conformal submersion:
Proposition 1
(Gudmundsson, 1992) “Let
be a horizontally conformal submersion with dilation
be horizontal vectors fields, then
(8)
We see that the skew-symmetric part of
measures the obstruction integrability of the horizontal distribution
.
The following curvature relations for horizontally conformal submersion are now brought to mind from (Gromoll et al., 1975 and Gudmundsson, 1992).
Theorem 1
“Let
and
be two RMs, where
. Let R and
be the curvature tensors on
and
, respectively. Let
be a horizontally conformal submersion, with dilation
and let
be the curvature tensor of the fibres of the submersion. If
are horizontal
vertical vectors, then
(9)
(10)
(11)
(12)
“Let
and
be RMs and suppose that
is a smooth map between them. The differential of
of
can be viewed a section of the bundle
, where
is the pullback bundle which has fibres
,
.
has a connection
induced from the Levi–Civita connection
and the pullback connection. Then, the second fundamental form of
is given by
defined by
(13)
for
, where
is the pullback connection.” The symmetry of the second fundamental form is well recognised. “A smooth map
is said to be harmonic if
. On the other hand, the tension field of
is the section
of
defined by
(14)
where
is the orthonormal frame on
. Thus, it follows that
is the neccesary and sufficient condition under which
is harmonic.” For more information, see (Baird and Wood, 2003).
Lemma 1
(Urakawa, 1993) “Consider that
is a smooth map between the RMs
and
. Then
(15)
for any
.”
Last but not least, consider the following (Baird and Wood, 2003).
Lemma 2
“Assume that the submersion
is horizontally conformal. Then, for any vertical fields
and horizontal vector fields
,
-
;
-
;
-
.”
4
4 Conformal generic submersions
This section assesses the study of CGS as the total space of the submersions is l.p.R. manifold. We define the CGS and provide a non-trivial example to assure the existence of such submersion.
Definition 2
Let
be a l.p.R. manifold with the product structure
and
be a RM. Consider a horizontally conformal submersion
. Then
is called CGS if there are two orthogonal complementary distributions
and
of
such that
(18)
where
, a complex subspace of a vertical space
, has a constant dimension along
and defines a differentiable distribution on
. The distribution
is called the purely real distribution.
As observed that the vertical distribution
is integrable. Therefore, this defintion simply implies that integral manifolds,
of the submersion are generic submanifold of M. For generic submersions, we refer to (Chen, 1981).
Let
be a CGS from a l.p.R. manifold
onto a RM
. For any
,
(19)
where
and
. Also for any
,
(20)
where
and
. Then,
is decomposed as
(21)
where
denotes the orthogonal complement of
in
and is invariant under the almost product structure
.
We now present a non-trivial example of CGS whose total space is an almost product manifold.
Consider an Euclidean space
with coordinates
. We denote by
the compatible almost product structure on
as follows;
Example 1
Let
be a submersion defined by
Then it follows that
and
Moreover,
Hence,
and
. Also by direct computations, we obtain
where
and
denote the standard metrices on
and
, respectively. Thus
is CGS with
.
We start with the preliminary results of CGS.
Proposition 2
Let
be a CGS from a l.p.R. manifold
onto a RM
. Then
Proof
These can easily be obtained with the help of (19)–(21).
Using (4), (5), (19) and (20), we have the covariant derivative of
and
as follows;
(22)
(23)
(24)
(25)
for any
.
In view of (4)–(7), (19) and (20), we have.
Lemma 3
Let
be a CGS from a l.p.R. manifold
onto a RM
. Then
-
,
-
,
-
,
for any
and
.
We proceed now to the main results of this section where first we prove the equivalent conditions for the integrability of the distributions
and
. As vertical distribution
is integrable so far, we give the necessary and sufficient condition for the horizontal distribution
to be integrable. Also we study the geometry of foliations of all the distributions.
Theorem 2
Let
be a CGS from l.p.R. manifold
onto a RM
. Then the f.a.e;
-
The distribution
is integrable.
-
-
and
,
for any
and
.
Proof
For any
, applying (16), (17), (4) and (19), we get
Since
is a CGS, using (19) and Lemma 2, we get
(26)
We note that
, for any
as the distribution
is always integrable. Therefore,
follows. Moreover, with Lemma 2 and (1), (26) reduces to
By using (23) and Proposition 2, we obtain
.
Theorem 3
Let
be a l.p.R. manifold and
, a RM and
be a CGS. Then the f.a.e;
-
The distribution
is integrable.
-
,
-
,
for any
and
.
Proof
The distribution
to be integrable iff
, as well as
, for any
and
. As
is integrable, then we can easily get
.
Moreover, by using (16), (17), (19) and (13), we obtain
which shows
.
On the other side, applying (13), we arrive at
Hence,
.
Theorem 4
Let
be a CGS from a l.p.R manifold
to a RM
i.e.,
. Then, the distribution
is integrable iff
-
There is no component of
in
.
-
for
and
.
Proof
Since the horizontal distribution is integrable if and only if
, for any
and
, where
such that
and
. This implies that
and
.
We omit the proof as it easily follows by the use of the Eqs. (16), (17), (6), (7), (20), (13)in addition to the fact that
is a horizontal conformal submersion, using Lemma 2.
Theorem 5
Let
be a CGS from a l.p.R manifold
onto a RM
. Then,
-
The distribution
defines a totally geodesic foliation on M iff
and
-
The distribution
defines a totally geodesic foliation on M iff
and
for any
and
.
Proof
For any
and
, using (16) and (17) and Proposition (2), we have
(27)
Furthermore, using (13), we get
(28)
Taking into account that
is a CGS and using (5), (13), we obtain
(29)
Therefore, by the virtue of (28) and (29), we obtain
.
For any vector fields
and
, using (16)(17)
(30)
Moreover, for any
(31)
Therefore, with (30) and (31), we arrive at
.
In view of Theorem 5, we have;
Corollary 1
Let
be CGS from a l.p.R. manifold
to a RM
. Then, the necessary and sufficient conditions for the fibres of
to be a l.P. manifold of the form
are
-
and
,
-
) and
,
for any
and
and
are the integral manifolds of the distribution
and
, respectively.
Proofs of the following Theorem 6 and Theorem 7 can easily be obtained from Theorem 3.20 and Theorem 3.21 Akyol (Akyol, 2021), respectively.
Theorem 6
Let
be a CGS from a l.p.R manifold
onto a RM
. Then, the horizontal distribution
defines a totally geodesic foliation on
iff
-
.
-
,
for any
and
.
Theorem 7
Let
be a CGS from a l.p.R manifold
to a RM
. Then, the vertical distribution
defines a totally geodesic foliation on M iff
,for any
and
.
We recall that a horizontal conformal map
between two RMs is called horizontally homothetic if and only if
.
We now imitate Theorem 4 and Theorem 6 as follows;
Theorem 8
Let
be a CGS from a l.p.R manifold
to a RM
i.e.,
and additionally
is horizontally homotheic map. Then, the distribution
is integrable iff
-
There is no component of
in
.
-
for any
and
.
Theorem 9
Let
be a CGS from a l.p.R manifold
to a RM
and
is horizontally homothetic. Then, the horizontal distribution
defines a totally geodesic foliation on
iff
-
.
-
,
for
and
.
From Theorems 6 and 7, we deduce the following:
Theorem 10
Let
be CGS from a l.p.R manifold
onto a RM
. Then, the total space M is a generic product RM
iff
and
for any
and
, where
and
are leaves of the distributions
and
, respectively.
We now conclude this section with the necessary and sufficient condition for CGS to be harmonic map.
Theorem 11
Let
be a CGS, where
is a l.p.R. manifold and
is a RM. Then,
is harmonic if and only if
Proof
For any vertical vector field
and
, using (16), (13), (19), (20) and Proposition (2), we have
In view of the Eqs. 19,20, we get
Hence, the assertion follows directly.
5
5 Curvature relations on conformal generic submersions
This section investigates the sectional curvatures of the fibres of a CGS as well as the total space and base manifold. Let
be a CGS whose total space
is a l.p.R. manifold and the base space
be a RM. We denote the Riemannian curvature tensors by
and
for any fibre
and
, respectively. The sectional curvature denoted by K, defined as follows;
(32)
where
and
are the pair of non-zero orthogonal tangent vectors on M.
Theorem 12
Let
be a CGS from a l.p.R. manifold
to a RM
. Then, for any horizontal vector field
and vertical vector fields
(33)
(34)
(35)
where
and
be the sectional curvatures of the total space
, the base space
and fibers, respectively.
Proof
Since
is a CGS and
is a l.p.R. manifold, using (19), we obtain
(37)
Using (32) and (9), we arrive at
(38)
Similarly, using (12), we arrive at
Also by direct calculations, we obtain
(39)
Similarly, using (11) we have
(40)
On using (11), we obtain
(41)
In view of (38), (39), (40), (41) and (37), we get (35).
As M is a l.p.R. manifold, for unit vector fields
and
, using (19) and (20) we have
(42)
With the help of (32) and (9), we obtain
(43)
Using (11), we have
(44)
Lastly, using (11) we get
(45)
Similarly, from (12) we have
(46)
Hence, (36) follows by (42), (44) and (43) and (46).
Since M is a l.p.R. manifold, using (17) and (19) for unit vector fields
and
, we have
(47)
Using (9), we derive
(48)
Similarly, using (12), we get
Also by direct calculations, we obtain
(49)
In a similar way, using (11) we have
(50)
Lastly, using (11) we have
(51)
Writing (48), (49), (50) and (51) in (47), we get (35).
Theorem 12 has the following direct consequences, which we state below:
Corollary 2
Let
be a CGS from a l.p.R. manifold
to a RM
. Then, for any
The equality holds iff the fibers are totally geodesic and
is integrable.
Proof
Using Corollary 1, (O’Neill, 1966), Eq. (34) can be rewritten as
which proves our claim.
Furthermore,
Corollary 3
Let
be a CGS from a l.p.R. manifold
to a RM
i.e.,
. Then,
for
. In above expression equality is satisfied iff
is a homothetic submersion.
Corollary 4
Let
be a CGS from a l.p.R. manifold
to a RM
. Then,
for
. The equality holds iff for any
and either
or
.
Proof
On using (35) we have,
which proves the assertion. The necessary and sufficient condition for the equality is
Hence, we obtain
, for any
and either
or
.
Moreover,
Corollary 5
Let
be a CGS from a l.p.R. manifold
to a RM
. Then,
for
. The equality holds iff
and
.
Corollary 6
Let
be a CGS from a l.p.R. manifold
to a RM
. Then,
for
and
. The equality holds iff
and
horizontally homothetic submersion.
Proof
On Using (36) we have,
This follows the inequality. For the equality case,
Thus, the eqality follows if and only if
and
which ensures that
is horizontally homothetic.
We now conclude this section with the following result;
Corollary 7
Let
be a CGS from a l.p.R. manifold
to a RM
. Then,
for
and
. The equality case follows iff
and
.