Abstract
In this paper, we explore minimal surfaces and graphs in differential geometry. We derive the equation for a catenoid, a rotationally symmetric solution to the first variation of area functional for equidistant bounded discs. This analysis reveals two possible configurations for the catenoid, with an inner-radius and outer-radius catenoid that arise when the distance between the coaxial discs is below a critical threshold; we rigorously prove the stability of the outer-radius catenoid as the unique, area-minimizing surface. Additionally, we establish the rigidity and uniqueness of minimal (planar) graphs; we prove that the Dirichlet problem admits at most one minimal graph. Moreover, when the Dirichlet boundary curve lies in a plane, the corresponding minimal planar graph must reside entirely in the same plane.
Introduction
Plateau’s problem, first proposed in the late 18th century1 , asks whether a surface of minimal area exists under specific boundary constraints. Solutions to this problem, minimal surfaces, have since been studied extensively and have applications in fields such as physics, molecular biology, and architecture; for instance, minimal surfaces are used to model the apparent horizon of black holes2, describe the theoretical model of biomolecules3, and even inspire modern architecture4. As such, Differential Geometry, the broader context of minimal surfaces, remains a relevant field in mathematics, as it extends the familiar study of Euclidean geometry to higher-dimensional space to measure area, curvature, torsion, etc., using the tools of calculus, linear algebra, and topology.
This paper focuses on two specific cases of minimal surfaces: catenoids and minimal graphs. More specifically, we prove two main results: (i) that the outer-radius catenoid is stable and area-minimizing as the unique solution to Plateau’s problem, Theorem (4.2), and (ii) that the Minimal Graph Equation permits one unique solution, Theorem (5.3), implying that planar Dirichlet boundary conditions yield only the trivial planar minimal graph, in Corollary (5.1). While there exist previous proofs4 for the stability of the outer-radius catenoid, we provide a self-contained proof that avoids reliance on advanced background in Sturm-Liouville theory or Differential Geometry aside from that introduced in sections two and three, and is thus more attainable for a broader audience. Physically, regarding the stability of the catenoid, several soap ring experiments5,6 demonstrate the existence of two potential catenoid configurations bounded by coaxial rings, but that only the outer-radius catenoid is stable and persists under a critical separation distance d∗ between the rings; using the first and second variation of area functionals, we mathematically justify such observations.
In the Geometry of Surfaces section, we provide the necessary background in Differential Geometry to understand and prove the results of this paper. In section three, we investigate the context of Plateau’s problem and minimal surfaces, deriving important theorems in minimal surface theory for our main results. In section four, we present an overview of the catenoid and prove our first main result in Theorem (4.2) regarding the stability of the outer-radius catenoid. Finally, in section five, we introduce the Maximum Principle for linear elliptic equations and prove our second main result in Theorem (5.3) regarding the uniqueness of minimal graphs, concluding with Corollary (5.1).
Geometry of Surfaces
This section introduces the fundamental concepts in the geometry of surfaces to properly analyze minimal surfaces. Specifically, we need to answer the question of what defines the geometry of a surface? In its essence, a surface in
has three major properties: length, area, and curvature; the latter two will be critical for defining a minimal surface. However, to start, we need to establish a formal definition of a regular surface and its composition from a local parametrization.
Definition 2.1 (Local Parametrization).
Let
represent a subset in
. A map
is called a local parametrization of
if the following conditions are satisfied:
is
; that is,
is infinitely differentiable with respect to the codomain
.
is a homeomorphism; i.e.,
is bijective, and both
and
are continuous.
, the cross product![Rendered by QuickLaTeX.com \[\frac{\partial F}{\partial u} \times \frac{\partial F}{\partial v} \neq 0\]](https://nhsjs.com/wp-content/ql-cache/quicklatex.com-483790a6499b56d2c3aadb03daaa1084_l3.png)
Note that the third condition in Definition 2.1 is necessary to establish the linear independence of the parametrization for
; i.e., the nonzero cross product implies that, at any point on
, the surface cannot locally collapse to a single point or curve and must permit local tangent planes everywhere. This property is vital for Definition 2.3.
Definition 2.2 (Regular Surface). A subset
is called a regular surface if,
, there exists an open subset
and a corresponding open subset
containing
such that
is a local parametrization.
Importantly, we need to establish a local coordinate system on the surface
to examine its behavior in space; specifically, we need a basis to reference the curvature and geometry of
around an arbitrary point
. Conveniently, the partial derivatives of a local parametrization
are well-defined (nonzero) everywhere on
and are thus of interest for defining a local (tangent) plane.
Definition 2.3 (Tangent Plane). Let
be a regular surface and
a point. If
is a local parametrization around
, then the tangent plane
at
is defined as
![]()
Remark 2.1.
,
, since
by Definition 2.1.
With the proper local coordinates, we can now proceed with analyzing the behavior and geometry of
around a point
; namely, we can examine the properties of curvature, area and length associated with
. The latter two are defined with respect to a local inner product; let
. Then
![Rendered by QuickLaTeX.com \[\left\langle x,y \right\rangle = \begin{bmatrix} x_1 & x_2 & x_3 \end{bmatrix} \begin{bmatrix} \left\langle e_1,e_1 \right\rangle & \left\langle e_1,e_2 \right\rangle & \left\langle e_1,e_3 \right\rangle \\ \left\langle e_2,e_1 \right\rangle & \left\langle e_2,e_2 \right\rangle & \left\langle e_2,e_3 \right\rangle \\ \left\langle e_3,e_1 \right\rangle & \left\langle e_3,e_2 \right\rangle & \left\langle e_3,e_3 \right\rangle \end{bmatrix} \begin{bmatrix} y_1 \\ y_2 \\ y_3 \end{bmatrix}\]](https://nhsjs.com/wp-content/ql-cache/quicklatex.com-ac68f36a1cfa2dd6b7440fa99a552d65_l3.png)
such that
First Fundamental Form. As alluded to earlier, we can express area and length attributed to a regular surface
using a local inner product; to do so, we must define the first fundamental form and its matrix definition.
Definition 2.4 (First Fundamental Form). If
is a regular surface, the first fundamental form of
is the inner product on
for all
, denoted as
.
Remark 2.2 (Matrix Form). Let
represent a local parametrization for a regular surface
and
have tangent plane
. Then, for
, by Definition 2.4, the first fundamental form for
at
is defined in its matrix form as
![Rendered by QuickLaTeX.com \[g_p = \begin{bmatrix} \frac{\partial F}{\partial u_1}(p)\cdot\frac{\partial F}{\partial u_1}(p) & \frac{\partial F}{\partial u_1}(p)\cdot\frac{\partial F}{\partial u_2}(p) \\ \frac{\partial F}{\partial u_2}(p)\cdot\frac{\partial F}{\partial u_1}(p) & \frac{\partial F}{\partial u_2}(p)\cdot\frac{\partial F}{\partial u_2}(p) \end{bmatrix}\]](https://nhsjs.com/wp-content/ql-cache/quicklatex.com-63779e40869f074f82aa1da27c4117a2_l3.png)
Thus,
Remark 2.3 (Length). Let
represent a regular surface with local parametrization
. Consider a parametrized curve
from the interval
. In
, the length of
is
![]()
Since
![]()
![]()
![]()
Thus, we can express the length of
![]()
Remark 2.4 (Area). Let
represent a closed region in the regular surface
with local parametrization
. Then, we know the surface area of
is
![]()
However, we can further express this inner cross product in terms of the first fundamental form of

Thus, we find the area of
![]()
Second Fundamental Form. Now that we have explored the length and area of regular surfaces, we can investigate the nature of curvature, defining the second fundamental form in order to so. It is important to note that the typical, inherent idea of curvature only exists in space curves in
as a measure of the rate at which a curve
changes direction; clearly, such a measure is well defined, as
only has one tangent vector
at any point along its trace.
However, in a regular surface
, there is no sole, unique tangent vector—only planes (
). Thus, different curves along
will often have varying curvatures, and so we must define curvature in the context of each “direction” along
(in a similar manner to a “directional derivative”).
To start, by Definition 2.3, we know that the (linearly independent) partial derivatives of a local parametrization form the tangent plane for the corresponding regular surface; this composition implies that the cross product between them defines a form of normal vector.
More concretely, let
represent a regular surface with local parametrization
around a point
. Then, at
, we can express the ‘‘normal vectors’’
as

Importantly, there exist two normal vectors (
Definition 2.5 (Gauss Map). Let
be a regular, orientable surface. Then, the Gauss map
is a smooth map such that
,
is the globally defined unit normal vector of
at
. We typically have
. See equation (2.1).
Definition 2.6 (Normal Curvature). Let
be a regular surface with Gauss map
. For each
and any unit vector
such that
, we denote
to be the plane in
that contains
and is spanned by
and
. If
is the curve that is formed by the intersection of
and
, then the normal curvature at
along
, denoted by
, is the signed curvature of
at
with respect to
such that
![]()
Theorem 2.1. Let
be a regular surface with local parametrization
and Gauss map
. For a point
and unit vector
, express
![Rendered by QuickLaTeX.com \[e = \sum_{i=1}^2 x_i \frac{\partial F}{\partial u_i}\]](https://nhsjs.com/wp-content/ql-cache/quicklatex.com-464e583352c246e7456d637820c8ddd9_l3.png)
Then, the normal curvature

Proof. Let
represent the arc-length parametrized curve of the intersection of
and
for
, such that
and
.
Since
, we can express
![]()
![Rendered by QuickLaTeX.com \[\gamma'(s) = u_1'(s)\frac{\partial F}{\partial u_1} + u_2'(s)\frac{\partial F}{\partial u_2} = \sum_{i=1}^2 u_i'(s)\frac{\partial F}{\partial u_i}\]](https://nhsjs.com/wp-content/ql-cache/quicklatex.com-46208ebe3d6dc7aae077f7f6906429dd_l3.png)
![Rendered by QuickLaTeX.com \[\Rightarrow \gamma'(0) = e = \sum_{i=1}^2 u_i'(0)\frac{\partial F}{\partial u_i}\]](https://nhsjs.com/wp-content/ql-cache/quicklatex.com-dbac7d5a823f0d890c1cabecac140a66_l3.png)
![]()
Thus, we find the second derivative of


as desired.
From Theorem (2.1), we are inspired to define a map in a similar fashion as Definition (2.4) to measure the normal curvature on a regular surface. This directly leads us to define the second fundamental form.
Definition 2.7 (Second Fundamental Form). Let
be a regular surface with Gauss map
and local parametrization
. Then, for
, the second fundamental form of
is a map
such that
![Rendered by QuickLaTeX.com \[h(x,y) = \sum_{i,j=1}^2 x_i y_j \left\langle \frac{\partial^2 F}{\partial u_i \partial u_j}, N \right\rangle\]](https://nhsjs.com/wp-content/ql-cache/quicklatex.com-0201ae871eca7fea9a729aab76c2d3a2_l3.png)
evaluated at a given
Remark 2.5 (Matrix Form). Often, we express
in terms of a matrix:
![Rendered by QuickLaTeX.com \[h_p = \begin{bmatrix} \left\langle \frac{\partial^2 F}{\partial u_1 \partial u_1}(p), N(p) \right\rangle & \left\langle \frac{\partial^2 F}{\partial u_1 \partial u_2}(p), N(p) \right\rangle \\ \left\langle \frac{\partial^2 F}{\partial u_2 \partial u_1}(p), N(p) \right\rangle & \left\langle \frac{\partial^2 F}{\partial u_2 \partial u_2}(p), N(p) \right\rangle \end{bmatrix}\]](https://nhsjs.com/wp-content/ql-cache/quicklatex.com-7956a56f4f5119fd745e4ad5fe15980a_l3.png)
such that
Remark 2.6 (Normal Curvature). For
, the normal curvature in the direction
is given by
![]()
However, while we can now find the normal curvature along any vector in
relative to a point
, several questions still arise: namely, which directions minimize/maximize the normal curvature and the respective implications. As such, we desire to optimize
given that
for some
.
To do so, define
![Rendered by QuickLaTeX.com \[e = \sum_{i=1}^2 x_i \frac{\partial F}{\partial u_i}\]](https://nhsjs.com/wp-content/ql-cache/quicklatex.com-464e583352c246e7456d637820c8ddd9_l3.png)
for a fixed point
![]()
![]()
Thus, we desire to optimize
![]()
![]()
Expanding equation (2.2), we are left with the system
![]()
![]()
Furthermore, noting the symmetry of
![]()
![]()
To solve equation (2.6), we note that
![]()
We therefore conclude from equation 2.7 that the extrema
Definition 2.8 (Shape Operator). For a regular surface
, the shape operator of
is a map
such that ![]()
Furthermore, we define the eigenvalues of
as the principal curvatures, which are the critical values of
given that
. Note that this fact follows briefly as
![]()
Finally, since
Definition 2.9 (Mean Curvature & Gauss Curvature). For a point
on a regular surface
with first fundamental form
and second fundamental form
, the mean curvature of
, denoted by
, is given by
![]()
and the Gauss curvature, denoted by
![]()
where
Here, for both the mean and Gauss curvature, we calculate them under the gauss map with the normal vector that (globally, under the orientability assumption) points outward from the enclosed volume of the surface; as such, the sign for the mean curvature is positive for all convex regions.
Minimal Surfaces
This section will introduce the notion of and context for minimal surfaces, providing the necessary background for the main results of this paper in regard to catenoids and minimal graphs. However, we must first explore the motivating problem that introduced minimal surfaces.
Plateau’s Problem. Given a closed curve
of class
, find a regular surface
such that
and
, where
is the set of all regular surfaces in
that span
.
To solve Plateau’s Problem, we must employ the first variation of area functional; however, we require context. For a fixed closed and smooth curve
, let
be a regular surface that spans
with local parametrization
and Gauss map
. Consider a family of variational surfaces
that span
for
with
. Then, let the local parametrization
of
be of the form
![]()
for smooth
We restrict our examination to fixed boundary conditions, so
is sufficient, and no additional-order boundary conditions arise. Note that since
by Definition 2.1.
. In fact, for all orientable surfaces,
must be differentiable; see7 for more detailed explanation. As such,
is differentiable.
Let
such that
![]()
![]()
Now, if
solves Plateau’s Problem, then
![]()
by Remark (2.4).
Lemma 3.1. Let
be a family of symmetric, invertible
matrices. Then,
![]()
Proof. Let
be eigenvalues for
.
![Rendered by QuickLaTeX.com \begin{align*} \frac{d}{ds}\ln(\det(g(s))) &= \frac{d}{ds}\ln(\lambda_1(s)\lambda_2(s)\dots\lambda_n(s)) \\ &= \frac{d}{ds}(\ln(\lambda_1(s)) + \ln(\lambda_2(s)) + \dots + \ln(\lambda_n(s))) \\ &= \frac{\lambda_1'(s)}{\lambda_1(s)} + \frac{\lambda_2'(s)}{\lambda_2(s)} + \dots + \frac{\lambda_n'(s)}{\lambda_n(s)} \\ &= \text{tr} \left( \left[ \begin{smallmatrix} \lambda_1^{-1}(s) & \dots & 0 \ \vdots & \ddots & \vdots \\ 0 & \dots & \lambda_n^{-1}(s) \end{smallmatrix} \right] \left[ \begin{smallmatrix} \lambda_1'(s) & \dots & 0 \ \vdots & \ddots & \vdots \\ 0 & \dots & \lambda_n'(s) \end{smallmatrix} \right] \right) \\ &= \text{tr} \left( g(s)^{-1}\frac{d}{ds}g(s) \right) \end{align*}](https://nhsjs.com/wp-content/ql-cache/quicklatex.com-2caedbf204ead09e854ebfc628bf0b2f_l3.png)
Applying Lemma (3.1), we have

Furthermore, since
, we know



Now we substitute equation (3.6) into equation (3.4).
![]()
Finally, we plug equation (3.7) into (
Theorem 3.1 (Minimal Surface Equation). The First Variation of Area of a regular surface
is given as
![]()
![]()
for all choices of variation
![]()
everywhere on
Definition 3.1 (Minimal Surface). A regular surface
is a minimal surface if it is a solution to the Minimal Surface Equation; namely, if
everywhere on
.
Remark 3.1. While we call regular surfaces that have a zero mean curvature everywhere “minimal surfaces,” they do not necessarily solve Plateau’s Problem; often, when solving for generalized minimal surfaces given boundaries, multiple solutions satisfying the Minimal Surface Equation arise, while some may not be truly “area-minimizing.” Put simply, satisfying the Minimal Surface Equation is not enough to warrant a surface a solution to Plateau’s Problem; refer to Theorem (4.1).
Catenoids
This section will introduce the catenoid and its properties as a minimal surface, providing the background for and proving the main result of the outer-radius catenoid’s stability. However, we must first define what a catenoid is; in order to do so, we pose a question: what is the solution to Plateau’s Problem for two separated, equiradial rings? Or more succinctly, what surface that connects two rings has the smallest possible surface area?
Formally, we can answer this question using the Minimal Surface Equation. Fix two unit circles and at and , respectively, as seen in Figure 1.

We want to find a minimal surface such that . Let us also assume that M is rotationally symmetric. A simple argument can be made that M must be rotationally symmetric because the boundary conditions are symmetric; if a solution for M were not rotationally symmetric, then there must exist an infinite number of solutions identical to M (but rotated slightly) that are also area-minimizing. However, this violates uniqueness; see8,9 for more. Thus, we may locally parametrize M as
Thus, we may locally parametrize M as
![]()
for some strictly positive
with
and
. Therefore, our objective is to solve for
.
First, we compute the first fundamental form
of
.
![]()
![]()
Thus, by Definition (2.4), the first fundamental form is given as
![]()
Further, we can also compute the Gauss map and second fundamental form for M.

So, by Definition (2.5), we have

where the global (due to assumed orientability) direction of
is of the form
in equation (2.1). Furthermore, by Definition (2.7), we also find
![]()
Thus, by Definition (2.8), we compute S as

As such, by Definition (2.9), the mean curvature of M is

Therefore, by Theorem (3.1), the Minimal Surface Equation for M is given by
(
) ![]()
where
. To find a solution
for (
), let
![]()
Then, we have

by (
). However, equation (4.7) implies that
, for some constant
. Thus, we can solve for
.

for some integration constant
. However, since M is symmetric about
, we note that
. This fact follows directly from the boundary conditions,
, so
by the symmetry of the hyperbolic cosine function. Thus, we simplify equation (4.8) and conclude
![]()
Finally, we must find the value of C in equation (4.9) given that
. Furthermore, according to equation (4.9), C must be the minimum value of
, attained at
. This fact is because
for all
. Accordingly, we are brought to the definition of a catenoid.
Definition 4.1 (Catenoid). A catenoid is the unique, non-planar minimal surface of revolution in
given by the local parametrization
![]()
for some real
. This is equivalent to the initial conditions of two equiradial disks in Plateau’s Problem at the start of this section.
Note that in Definition (4.1),
, where
, according to the boundary conditions. As such, define
![]()
Thus, a connected solution
only exists if
has a positive root. Observe, however, that as
, we have
. Furthermore, as
, we also have
. Thus, we know
attains a global minimum when
.
cannot have any local extrema because the hyperbolic cosine function is strictly concave everywhere; that is, since
everywhere, no local extrema (maxima) can occur, and so the only extrema is the global minimum.
This fact leads us to suspect that for certain separation distances between
and
,
, and there will consequently be no solutions for
. To demonstrate this fact, we must first find the minimum of
.
![]()
![]()
![]()
![]()
where
. Implicitly solving equation (4.11) for
, we arrive at one unique solution
. Thus, for a given
, we have that
attains its minimum when
.
However, also observe that when
, then
. This is once again because
. However, because
is strictly positive, we have
, so
. This fact, of course, conforms with our intuition, as
is the minimal radius from
to the
-axis, and as such must be strictly less than the boundary disk radius.
Now that we have
, we substitute into equation (4.10) to find the minimum value of
as
![]()
Thus, for connected solutions for M to exist, we want
. Rearranging equation (4.12) to satisfy this inequality, we are left with
![]()
Consequently, when
becomes too large (
), there are no solutions for the equation
and thus no connected solutions for
, as we expect. As alluded to in the introduction, this can be seen with real experiments; soap ring bubbles form a catenoid until their separation distance exceeds a certain value, at which point the connecting bubble abruptly pops. See10,11 for more.
When
, one unique solution
exists. However, in the case when
, it is clear that multiple solutions for
exist; Figure 2 displays plots of
for different values of
. For
, there are two solutions:
and
, where
. Since
, we call
and
the inner and outer-radius catenoid, respectively. Figure 3 displays both catenoids,
and
, corresponding to
and
, respectively.
By inspection, we intuitively suspect that
has a smaller surface area than
; however, this result must be proven rigorously. As such, we will prove Theorem (4.2), one of the main results of this paper; namely, that when
the outer-radius catenoid
is the solution to Plateau’s Problem for the Dirichlet boundary conditions depicted in Figure 1, while the inner-radius catenoid
is not.
Second Variation of Area.
Lemma 4.1. It should be stated that this Lemma is known as Weingarten’s Formula. For additional proof, see7. Let
be a regular surface with local parametrization
, first fundamental form
, second fundamental form
, shape operator
, and Gauss map
. Then,
![Rendered by QuickLaTeX.com \[\frac{\partial N}{\partial u_i} = -\sum_{j=1}^2 S_{ij}\frac{\partial F}{\partial u_j}\]](https://nhsjs.com/wp-content/ql-cache/quicklatex.com-ab983a838186f3460c795126993449a0_l3.png)
Proof. Since
, it follows that
. Thus, we can write

for some coefficients
. Furthermore, we differentiate
with respect to
to find
![]()
However, since
by Definition (2.7), we simplify equation (4.15) and have
![]()
But using equation (4.14), we also have

because
, by Definition (2.4). Thus, we compare
in equations (4.16) and (4.17) and conclude

However, with respect to the coordinate basis
, equation (4.18) expands to the matrix equation
![]()
![]()
for
. By definition, equation (4.20) implies
![]()
Thus, plugging equation (4.21) into equation (4.14), we get our desired result.
Lemma 4.2. Let
be a family of regular surfaces with local parametrizations in the form of equation (3.1), first fundamental form
, and shape operator
, such that
. Then,
(a) ![]()
(b) ![]()
where
is the surface gradient of
for smooth
.
Proof. Since
from equation (3.6), the result for (a) trivially follows. As for (b), first consider
. By equation (3.5), we have
![Rendered by QuickLaTeX.com \[g'(s)_{ij} = \left\langle \frac{\partial V}{\partial u_i},\frac{\partial \stackrel{\sim}F}{\partial u_j} \right\rangle + \left\langle \frac{\partial \stackrel{\sim}F}{\partial u_i},\frac{\partial V}{\partial u_j} \right\rangle\]](https://nhsjs.com/wp-content/ql-cache/quicklatex.com-751c79bbf83ba60cb9139d953c79eb31_l3.png)
for
. Therefore, we compute
as

Thus, from equation (4.22), we conclude

as desired. Note that sign conventions depending on metric signature might flip
trace sign in some contexts, but follows derivation above.
For a minimal surface M to be the solution to Plateau’s Problem, we must confirm that M is indeed area-minimizing while satisfying the Minimal Surface Equation; this implies that the area of M would satisfy the “second derivative test.” As such, we are brought to the definition of the Second Variation of Area.
Theorem 4.1 (Second Variation of Area). Let
be a family of regular surfaces with local parametrizations in the form of equation (3.1), first fundamental form
, and shape operator
, such that
, where
is a minimal surface. Then, the Second Variation of Area of
is given as
![]()
for all smooth
such that
on
.
Remark 4.1. A minimal surface
is locally minimizing if
![]()
Proof. From (
), we find
![]()
Thus, we must find
. Recall from equation (3.4) that we have
![]()

This result comes simply from
.
![]()
because
since
is a minimal surface. Finally, we substitute Lemmas (4.2, a) and (4.2, b) into equation 4.25 and obtain our desired result.
Now, we will prove the main result of this section, Theorem (4.2).
Outer-Radius Catenoid Stability
Theorem 4.2 (Outer-Radius Catenoid Stability). Consider Plateau’s Problem for the boundary curves
consisting of two coaxial unit discs in
, as seen in Figure 1, such that
for
, where
is defined in equation (4.13). Consequently, there exist two catenoids
and
such that
, and
. Then,
is stable, while
is unstable; i.e.
is the unique solution to Plateau’s Problem.
Proof. We present a self-contained proof of Theorem (4.2). However, for a more concise proof using Sturm-Liouville theory, see12. We will start by proving that Area(
) < Area(
) and then prove that
is indeed the unique solution to Plateau’s Problem by using Theorem (4.1).
First, note that
is parametrized by equation (4.1), where
![]()
from equation (4.9). Further, by equation (4.2), the first fundamental form for
is given by

and its inverse as

Therefore, we also have
![]()
and

by equation (4.5). Thus, we compute
![]()
Now, by Remark (2.4), we calculate Area(
) as

Define
and function
such that
![]()
According to equation (4.10, we must have that
![]()
and consequently
![]()
These two equalities are because
in equation (4.10). Therefore, we simplify
as

by equations (4.34) and (4.35). Define a function
such that
![]()
where
![]()
according to equation (4.35). Also note that equation (4.38) implies that
![]()
Thus, we find
as

Hence, from equations (4.36) and (4.40), we have that
. This implies that
![]()
since
, where
. However, equation (4.41) implies that the difference between
and
, denoted as
, is strictly decreasing as
increases. As such, we bound this difference by considering the endpoints in the interval
. Note that in equation (4.38), the maximum value of
occurs when
and thus when
. Therefore, at
, we have that
and hence
. However, in our interval for
, we have
, and so
by equation (4.41). As
increases,
decreases, so by the converse, as
decreases,
increases. Thus, we conclude that
. However, by equation (4.32), we also note
![]()
By equation (4.42), it therefore suffices to show that if
is area-minimizing, it then must be the unique solution to Plateau’s Problem.
Let
and
. Now consider the Second Variation of Area for
. Let
be a variational function such that
and
. That is, we only consider axisymmetric variations and not rotational ones; this restriction is necessary, as rotational variations will not distinguish stability between the catenoids. We define a
instead of
since M is rotationally symmetrical and surface perturbations will therefore be independent of
. Furthermore, non-axisymmetrical perturbations will result in apparent stability for both catenoids, which is unfavorable for our proof13.
By Theorem (4.1), we therefore have

where
is defined as
![]()
In a similar manner to earlier, define
. Now, consider the function
![]()
Then we find the derivatives of
as
![]()

Observe now that equation (4.47) implies that
. Furthermore, on the interval
, the function
is strictly positive. This is because
for all
, and thus
at the unique solution
. However, since
, we have
, so
for all
(since
). This implies that
. Thus, for some continuous function
such that
, define
![]()
Then, by equation (4.44), consider

Now we substitute equation (4.49) into equation (4.43).

Here we used integration by parts on
. Therefore, by equation (4.50), we conclude that
![]()
and thus, by Remark (4.1), it follows that M is a solution to Plateau’s Problem. Furthermore, as we have proven in equation (4.42),
, while satisfying the Minimal Surface Equation, cannot be a solution. A similar argument made in equation (4.50) cannot be made for
; since
, the function
has a root and thus
is not a continuous function. Therefore,
is the unique solution; the outer-radius catenoid is stable and area-minimizing while the inner-radius catenoid is not.
Minimal Graphs
This section will introduce the necessary background into minimal graphs, a specific class of minimal surfaces; furthermore, we will prove the main result of the uniqueness of minimal (planar) graphs. However, we must first introduce the definition of minimal graphs.
Definition 5.1 (Minimal Graph). Let
be a bounded domain. Then, a regular surface
is called a minimal graph if
![]()
is a minimal surface, where
.
In a similar manner to the Minimal Surface Equation, we desire to find a generalized equation to determine if a regular surface M is a minimal graph; to do so, we must solve the Minimal Surface Equation for M. Let
be a regular surface in the form of Definition (5.1). Then, the local parametrization of M is
![]()
Thus, according to Definition (2.4), the first fundamental form of M is given as
![]()
and we also have
![]()
Therefore, we compute the inverse of g as
![]()
By Definition (2.5), find the Gauss map N as

and by Definition (2.7), the second fundamental form is then
![]()
Therefore, by Definition (2.8), we compute the shape operator as

Finally, by Definition (2.9), the mean curvature is then

Now, by Theorem (3.1), we are motivated to define the Minimal Graph Equation.
Theorem 5.1. For a bounded domain
, a regular surface
in the form of
is a minimal graph if
for a function
.
Now that we have the Minimal Graph Equation defined, we will prove the main result of this section; specifically, we will conclude the uniqueness of minimal graphs, in Theorem (5.3), and the uniqueness of planar graphs for boundaries confined in a plane in
, in Corollary (5.1).
First, consider Plateau’s Problem for the following:
Let
be a bounded domain with smooth curve
above
such that ![]()
Consider then a regular surface
such that ![]()
where
. Then, we will prove in Theorem (5.3) that
is unique. However, we will need to first explore the Maximum Principle for linear elliptic equations.
Maximum Principle. Let
be a bounded domain. Define the function
and the linear operator
such that

where
are smooth functions. Then,
is called elliptic if the symmetric matrix
![]()
for all
.
is positive definite; i.e.,
. When we have
, we have an elliptic equation, and thus we can apply the Maximum Principle.
Theorem 5.2 (Maximum Principle). Note here that Theorem (5.2) is actually the weak Maximum Principle; for a proof of the strong version with a generalization to
, see14. Let
be a bounded domain with the smooth function
and operator
as defined in equation (5.11). Then, if
, we have
![]()
Proof. The following proof is adapted from Colding and Minicozzi15. We prove this by contradiction. Suppose a function
reaches a global maximum inside
; i.e., there exists a
such that
attains a maximum. Then, by the first derivative test, we have
. Furthermore, by the second derivative text, we also have
![]()
where
denotes the Hessian matrix. Therefore, we find

where
is defined in equation (5.12). In general, if we have an
symmetric positive definite matrix A and negative semidefinite matrix B, we have that tr(AB)
0. The proof for this comes simply when we define a matrix
and consider the definiteness of C, where
for all
. Thus, from equation (5.11), we have

Now consider a function
such that
. Define
![]()
where
and
are arbitrary real numbers. Then, suppose that
attains a maximum at
. Then, by equation (5.15), we find
![]()
However, we want to show that
to arise at a contradiction; also consider

However, we also have
![]()
for some
, since A is positive definite. Therefore, we use equation (5.19) and rewrite equation (5.18) as
![]()
Now, choose
such that
![]()
so equation (5.20) becomes
![]()
However, we compare equations (5.22) and (5.17) and arise at a contradiction! As such, we conclude
![]()
However, also note that as
in equation (5.23), we arrive at
![]()
as desired. To prove the same argument for the minimum, we instead choose
. Also, then, note that
, so we have
. However, we then have
, which must then be strictly negative according to equation (5.22). Thus, we arrive at a contradiction and the result follows. For a more detailed proof, see16,17.
Uniqueness of Minimal Graphs
Lemma 5.1. Let the functions
and
satisfy the Minimal Graph Equation, with the function
. Then,
![]()
for some symmetric matrix
in the form of equation (5.12).
Proof. Define a map
such that
![]()
Then, since
and
are both minimal surfaces, we therefore have that
. Now, consider

where A is defined as the matrix
![]()
Therefore, according to equations (5.26) and (5.27), we have
![]()
Now it suffices to show that
is positive definite. To do so, we will prove that
is positive definite. Let
where
![]()
Then, we compute
as
Therefore, by equation (5.30), we calculate
as
![]()
However, from equation (5.31), we have
![]()
and
![]()
By equations (5.32) and (5.33), it therefore follows that
is positive definite. However, by equation (5.27), it also implies that A is positive definite. The integral in a strictly positive region of a positive definite matrix is also a positive definite matrix; for a brief proof, consider
. Thus, our desired result immediately follows from equation (5.28).
With Lemma (5.1) proven, we can move on to the proof for the uniqueness of minimal graphs, the main result of this section.
Theorem 5.3 (Uniqueness of Minimal Graphs). Let
be a bounded domain and curve
in the form of equation (5.9). If
is a minimal graph in the form of equation (5.10), then
is unique.
Proof. Let
and
be minimal graphs with corresponding functions
and
, respectively. Then, define a function
. By Lemma (5.1), we have
![]()
for some positive definite matrix
. Expanding equation (5.34), we find

where
and
. However, observe now from equation (5.35) that
, where
is in the form of equation (5.11). Note here that the maximum principle invoked actually requires uniform ellipticity, a property which the minimal graph equation satisfies. On the compact domain in consideration, the gradient is bounded, ensuring uniform ellipticity. See18 for more.
Thus, according to Theorem (5.2), we have
![]()
But
, so
for all
. Therefore, according to equation (5.36), we find
![]()
Hence, by equation (5.37), it follows that
, so
, and thus
.
Note, however, that Theorem (5.3) only proves the uniqueness of minimal graphs and not the existence. For proof of existence in
, see19. Nevertheless, for minimal planar graphs, we have that uniqueness and existence hold, according to Corollary (5.1).
Corollary 5.1 (Uniqueness of Minimal Planar Graphs). If
is a planar curve bounding a convex domain, then the associated minimal graph M lies in the same plane; i.e., only the trivial, planar solution for M exists.
Proof. Suppose
lies entirely in plane
, such that P is of the form
![]()
for arbitrary coefficients
, and
. Then, we have that a function
lies entirely in
for certain
, and
. Let
correspond to the minimal surface
given in the form of equation (5.10). Then we test if
satisfies the Minimal Graph Equation:

Thus, by equation (5.38), M is a minimal graph. However, by Theorem (5.3), it follows that M is unique. Therefore, the only minimal planar graph is the trivial solution where
.
Acknowledgments
The author would like to express sincere appreciation to his mentor Dr. Tz-Kiu Aaron Chow for presenting this research topic and motivation behind the proofs, guiding the overall research process, and settling any confusion in the abundance of questions regarding the subject.
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