Milton Javier Cardenas Mendez
Instituto de Matemática e Estatística
Universidade Federal de Goiás, 74001-970 Goiânia, GO, Brazil
miltonjcardenas@ufg.br
Armardo Mauro Vasquez Corro
Instituto de Matemática e Estatística
Universidade Federal de Goiás, 74001-970 Goiânia, GO, Brazil
corro@ufg.br
(August 10, 2025)
Abstract
In this work we define the Ribaucour-type surfaces (in short, RT-surfaces). These surfaces satisfy a relationship similar to the Ribaucour surfaces that are related to the Élie Cartan problem. This class furnishes what seems to be the first examples of pairs of noncongruent
surfaces in Euclidean space such that, under a diffeomorphism, lines of curvatures
are preserved and principal curvatures are switched. We show that every compact and connected RT-surface is a sphere with center at the origin.
We obtain present a Weierstrass type representation for RT-surfaces with prescribed Gauss map which depends on two holomorphic functions. We give explicit examples of RT-surfaces. Also, we use this representation to classify the RT-surfaces of rotation.
Keywords.
Ribaucour surfaces, generalized Weingarten surfaces, prescribed normal Gauss map, Weierstrass type representation.
Introduction: An oriented surface is called a Weingarten surface if it exists
a differentiable relation between the mean curvatures and Gaussian curvatures of , such that
, when function is linear, that is, for and
constants, the surfaces are called linear Weingarten surfaces.
Examples of linear Weingarten surfaces are constant Gaussian curvature surfaces ( and ) and constant mean curvature surfaces ( and ). Several authors have studied these classes of surfaces, see [1], [6] and [2], among others.
Let be an oriented surface with normal Gauss map , functions given by and , , where denotes the Euclidean scalar product in , are called support function
and quadratic distance function, respectively. Geometrically, measures the signed distance from the origin to and measures the squared distance from the origin to . Let , a sphere with center and radius is called the middle sphere.
In 1888, Appell [5] studied a class of surfaces oriented in associated with area-preserving sphere transformations. Later, Ferreira and Roitman [3] showed that these surfaces satisfy the Weingarten relation, .
In 1907, Tzitzeica [8] studied hyperbolic surfaces oriented so that there is a nonzero constant for which .
In [1], the authors motivated by the works [5] and [8] defined generalized Weingarten surfaces as surfaces that satisfy a relation of the form , where are differentiable functions that do not depend on the parameterization of .
In particular, they studied the class of surfaces that satisfy the relation . Called Special Generalized Weingartem Surfaces depending on the support function and the distance function (in short, EDSGW-surfaces), these surfaces have the geometric property that all medium spheres pass through the origin. The authors obtained a Weierstrass-like representation of EDSGW-surfaces depending on two homomorphic functions. In [6], the authors classified isothermic EDSGW-surfaces in relation to the third fundamental shape parameterized by plane curvature lines. Also in [4], it is shown that EDSGW-surfaces are in correspondence with the surface class in where the Gaussian curvature and the extrinsic curvature satisfy .
Martínez and Roitman, in [2] showed what appears to be the first example found for the second case of the problem posed by Élie Cartan in his classic book about external differential systems and their applications to Differential Geometry. Such examples are given by a class of Weingarten surfaces that satisfy the relation , Ribaucour surface calls, these surfaces have the geometric property that all the medial spheres intercept a fixed sphere along a large circle.
In [9], the authors define a surface class called Ribaucour surface of harmonic type (in short, HR-surface) if it satisfies
, where is a nonzero real constant, a harmonic function with respect to the third
fundamental form. These surfaces generalize Ribaucour surfaces studied in [2].
Motivated by [1],[6], [2] and [3], we define Ribaucour-type surfaces (RT-surfaces) which have the geometric property for every a sphere of center e radius passes through the origin, in this case is satisfied.
We obtain a Weierstrass-type representation for RT-surfaces with prescribed normal Gaussian application depending on two holomorphic functions. Using this representation we classify rotating RT-surfaces. Furthermore, we show that a compact and connected RT-surface is a sphere.
1 Preliminaries
In this section we fix the notation used in this work, a surface on , its normal Gaussian map, and an open subset of .
Let , a parameterization of a surface and , normal Gaussian map. Considering as a base of , where , further we can write vector , , as
The coefficients are called Christoffel symbols.
Definition 1.1.
Let be a local parameterization of with map of Gauss , matrix , such that
is called the Weingarten matrix of .
Lemma 1.2.
Let be the normal Gaussian map given by (4) such that the metric is Euclidean conformal. Christoffel’s symbols for metric are given by
For e different.
The next result was obtained by Roitman and Ferreira [3].
Theorem 1.3.
Let be an orientable hypersurface and normal Gauss application with non-zero Gauss-kroncker curvature in every point. Let be a neighborhood of such that invertible and , then
Remark.
Using the above equation we have functions
(1)
(2)
called quadratic distance function and support function, respectively.
Remark.
Let the inner product be defined by , where and are holomorphic functions. If are holomorphic functions, then
(3)
where
2 RT-surfaces
Motivated by the works [1],[6], [2] and [3], we will begin the study of Ribaucour-type surfaces and will call them RT-surfaces. In addition to presenting some examples, will provide a Weierstrass representation depending on two holomorphic functions for surfaces in this class and characterize the case where such surfaces are of rotation.
Theorem 2.1.
Let , an orientable surface with non-zero Gauss-Kronecker curvature. Then there is a differentiable function and a holomorphic function such that normal Gauss map is given by
(4)
the coefficients of the fundamental form are
(5)
is locally parameterized by
(6)
In this case is the support function. Furthermore, the Weingarten matrix is given by
where
(7)
where are Christoffel’s symbols of and the fundamental forms and of , in local coordinates, are given by
Proof.
In theorem (1.3) we can choose a local parameterization of the sphere given by (4) with a metric given by (5) and is locally parameterized by (6), calculating their derivatives we get
Considering matrix , given by , therefore
(8)
In search of the Weingarten matrix we have to , by definition 1.1 we have to . To obtain the coefficients of the fundamental forms, we use (8), therefore
Definition 2.2.
A surface is called Ribaucour-type surfaces (RT-surface) such that for each the center sphere and radius go through the origin, in this case satisfies the following generalized Weingarten relation
for all .
Lemma 2.3.
Let be a Riemann surface and an immersion such that the Gauss-kronecker curvature is non-zero, under the conditions of the theorem 2.1 then is a SS-surface if and only if
(9)
Proof.
By theorem (2.1), we have , let be the eigenvalues of and the eigenvalues of , then . Using this fact and the expressions in lemma 1.2, (5), (6) and (7), we get
For RT-surfaces with Gaussian curvature we will present a complete characterization through pairs of holomorphic functions. This representation will allow to classify all RT-surfaces of rotation. Before that, we will need the following lemma.
Lemma 2.4.
Consider holomorphic functions , with . Taking local parameters and . So elements of the matrix given by (7) in terms of and are given by
Let be a Riemann surface and an immersion such that the Gauss-kronecker curvature is non-zero.
Then is a SS-surface if and only if there are holomorphic functions , where is a simply connected open and , such that is locally parameterized by
(13)
With normal application of Gauss N given by (4), the regularity condition is given by
The coefficients of the first and second fundamental forms of have the following expressions
Where , e
Proof.
Using (9 ), we can assume without loss of generality where is a differentiable function, in this case,
Now satisfies (9), if and only if , where is a holomorphic function. As is given by (4), deriving we have
using these expressions and (5) in (6),we have (13).
Therefore, using (3),(8) and (10) we obtain the coefficients of the first and second fundamental forms given in the statement of the theorem.
Example 2.6.
A sphere of center at the origin and radius is RT-surface, in fact, using theorem 2.5 and taking , by equations (6) and (9) the result follows.
Theorem 2.7.
Let be a compact, connected SS-surface, then is a sphere with center at the origin.
Proof.
Let be a compact then there is a sphere with center at the origin of radius , such that is contained in the closed ball with center at the origin and radius , and a point , such that .
Let , where function support of . We know that , for every , then
is a RT-surface and by theorem 2.5 and (6), there is a parameterized locally around such that
support function ,
given by , with harmonic then
Since is harmonic, by the maximum principle, in , later in , for an argument of compactness and connectedness of , we conclude for all , therefore is a sphere with center at the origin.
For some holomorphic functions and we show some examples of (13).
Figure 1:
Figure 2:
Figure 3:
The following theorem characterizes the rotating RT-surfaces.
Theorem 2.8.
Let be a connected RT-surface. Since is of rotation if and only if there are constants , such that can be locally parameterized by
(14)
where
(15)
Proof.
Let be locally parameterized by (13) with normal application of Gauss given by (4) and where are holomorphic functions. As is of rotation if and only if and , , for some differentiable function. Changing parameters , we have and .
Consequently, , remembering that and , then , so
Thereby, is regular if and only if . If , the expression from above vanishes for
In figures (4), (5) and (6) we present examples of RT-surfaces of rotation. We consider only the case where .
Figure 4:
Figure 5:
Figure 6:
Bibliografía
[1]A.V. Corro, D.G. Dias,
Classes of generalized Weingarten surfaces in the Euclidean 3-space,Adv.Geom. 2016;16(1)45–55
[2]A. Martinez, P. Roitman,
A class of surfaces related to a problem posed by Élie Cartan, Ann.Mat. Pura Appl,195,513–527
[3]W. Ferreira, P. Roitman,
Area preserving transformations in twodimensional space forms and classical differential geometry, Israel J.Mat,190,325–348
[4]A.V. Corro, R. Pina, M. Souza,
Classes of Weingarten surfaces in , HOUSTON JOURNAL OF MATHEMATICS, v. 46, p. 651-664, 2020.
[5]P. Appell,,
Surfaces telles que lórigine se projette sur chaque normale au milieu des centres de courbure principaux.,
Amer. J. Math. 10(1888),175–186. MR1505475 JFM 19.0825.01
[6]A.V. Corro, C.M. Riveros, D.G. Dias,
A class of generalized special Weingarten surfaces,
International Journal of Mathematics Vol. 30, No. 14 (2019) 1950075