Free Boundary Flat Y-Cone Model
- The free boundary flat Y-cone is a singular Plateau model consisting of three planar half-unit disks that meet along a common diameter at 120° angles with free-boundary conditions on the unit sphere.
- Its configuration is rigidly maintained through conformal minimal immersion, balanced junction conditions, and orthogonal free-boundary constraints that enforce planarity on each face.
- The model is characterized by a Morse index of two and a five-dimensional nullity, highlighting its stability and serving as a key reference in free-boundary minimal surface theory.
The free boundary flat -cone is the standard singular Plateau model in which three planar half-unit disks meet along a common diameter at equal angles of , while the outer boundary lies on the unit sphere and is orthogonal to it. In current arXiv usage, this object is most precisely the compact model denoted in the study of free-boundary minimal -surfaces in , where rigidity, index, and classification results are now available (Matinpour, 29 Sep 2025). It must be distinguished from several different “free boundary cone” problems on arXiv—especially one-phase Bernoulli problems on singular ambient cones and capillary hypersurface cones—which concern cone-tip interaction or codimension-one capillary geometry rather than triple-junction -surfaces (Allen, 2017).
1. Geometric model and terminology
The ambient space for the classical flat -cone problem is the unit ball
A free boundary minimal surface in is a minimal surface whose boundary lies on 0 and which meets 1 orthogonally along 2 (Matinpour, 29 Sep 2025).
In the singular setting, the surface is a triple junction surface
3
where each 4 is a smooth two-sided surface, the identified boundary components 5 are glued together along a common smooth curve 6, and the remaining components 7 form the outer boundary
8
A minimal 9-surface in 0 means that each face 1 is minimally immersed, the singular set is the common junction curve 2, and at each 3 the three outward conormals 4 satisfy
5
This is the standard balancing law for a 6-junction (Matinpour, 29 Sep 2025).
The standard compact flat 7-cone is built from the half-disk
8
with boundary decomposition
9
where
0
The model domain is
1
where 2 denotes rotation of 3 by angle 4 about the 5-axis. Geometrically, 6 is the union of three planar half-unit disks meeting along their diameters at equal 7 angles. It is “flat” because each face is planar, so
8
The singular set is the common diameter, hence in the compact model a line segment with endpoints on 9 (Matinpour, 29 Sep 2025).
Along the junction, the paper also imposes the metric compatibility condition
0
where
1
This is the intrinsic counterpart of the 2 balancing relation (Matinpour, 29 Sep 2025).
2. Conformal minimal immersion and free-boundary structure
A map
3
is conformal when each restriction 4 is conformal on its face and the three maps agree along the common edge: 5 On each face, conformality and minimality are expressed by
6
In polar coordinates 7 on 8, these become
9
The free-boundary condition along the outer semicircle 0 is that 1 and the surface meets the sphere orthogonally. Analytically,
2
for some scalar function 3, and differentiation yields
4
This identity is one of the main inputs in the rigidity argument (Matinpour, 29 Sep 2025).
Along the singular diameter 5, the triple-junction conditions are encoded by
6
7
and
8
Using harmonicity, the paper further derives
9
These formulas place the flat 0-cone in a highly rigid class: the conformal structure is sectorwise classical, but the singular geometry is carried by the matching, balancing, and free-boundary orthogonality constraints. A plausible implication is that the object is best understood as a Plateau singularity model with analytic control on each face rather than as a weak multi-phase interface.
3. Rigidity theorem and planarity of the faces
The core rigidity statement is that any conformal and minimal immersion of the standard compact flat 1-cone into 2 meeting 3 orthogonally is again a flat 4-cone (Matinpour, 29 Sep 2025). A later paper restates the earlier theorem in the broader form that any conformal minimal immersion of the flat 5-cone into 6 that meets the boundary sphere orthogonally must coincide with the flat 7-cone itself, up to orthogonal transformation (Matinpour, 26 May 2026).
The proof adapts Nitsche’s complex-analytic method from the disk case. For each face one defines
8
and then
9
Because each 0 is harmonic and conformal,
1
is holomorphic. The free-boundary identity 2 shows that 3 is real on 4, while the matching and balancing conditions imply that 5 on 6. Hence 7 is holomorphic and real on the whole boundary, so it is constant; since it vanishes at the origin,
8
From this one obtains along 9
0
The vanishing of the quartic differential forces the boundary curves 1 to be arcs of great circles on 2. If 3 is the plane containing 4, with unit normal 5, then 6 is harmonic and vanishes on 7. By the free-boundary condition,
8
and Calderón unique continuation yields
9
Therefore each face lies in a plane, and the image is the planar 0-configuration (Matinpour, 29 Sep 2025).
The later 1-cone rigidity paper describes this as the prototype singular rigidity mechanism: conformal parametrization on each sector, harmonicity and conformality, free-boundary orthogonality, junction balance, a holomorphic quadratic differential with real boundary values, vanishing of that differential, and planarity of the faces (Matinpour, 26 May 2026).
4. Morse index, nullity, and the index-two characterization
The flat 2-cone is not only rigid under conformal free-boundary minimal immersion; it also occupies a distinguished place in the Morse-index landscape. The paper proves:
The Morse index of the free boundary flat 3-cone in the unit ball is two, and its nullity is five. Moreover, if 4 is a free boundary minimal 5-surface in the unit ball with Morse index two, then 6 is a 7-cone (Matinpour, 29 Sep 2025).
Normal variations are written as
8
with admissible space
9
The compatibility condition
00
preserves the 01-junction under variation (Matinpour, 29 Sep 2025).
The second variation quadratic form is
02
Since each face is flat,
03
and because the junction is straight in the flat model,
04
Along the outer free boundary on 05,
06
Thus the spectral problem reduces to harmonic functions on the half-disk with Steklov boundary conditions (Matinpour, 29 Sep 2025).
The relevant Steklov spectrum on each face is
07
and for 08,
09
For compatible triples with coefficients 10 satisfying
11
the 12 eigenspace contributes a 13-dimensional negative space, giving index 14, while the 15 eigenspace yields a 16-dimensional kernel, giving nullity 17 (Matinpour, 29 Sep 2025).
The index-two classification uses ambient translations. If 18 are parallel vector fields in 19, their normal components are Jacobi fields on each face. The paper shows that whenever such a normal component is nontrivial,
20
Since there are three independent ambient translation directions but the index is only 21, one direction must have vanishing normal component everywhere. That forces an ambient direction tangent to all three faces, hence tangent to the junction curve 22, which must therefore be a straight line segment. From this the paper concludes that the surface is a flat 23-cone (Matinpour, 29 Sep 2025).
5. Position within the Plateau-model rigidity theory
The flat 24-cone now appears as one of the three canonical free-boundary Plateau model surfaces in the unit ball: the planar disk, the flat 25-cone, and the flat 26-cone (Matinpour, 26 May 2026). In the language of Plateau singularities, a surface is locally modeled on one of
27
where
28
This is the local model for 29-junctions, and tangent cones at 30-points are required to be 31 up to orthogonal transformation (Matinpour, 26 May 2026).
The unifying rigidity statement is:
Let 32 be a free-boundary minimal Plateau surface in 33 arising as the image of a conformal minimal immersion of one of the classical model domains: a planar disk, the flat 34-cone, or the flat 35-cone. Then 36 is congruent, via an orthogonal transformation of 37, to the corresponding flat model (Matinpour, 26 May 2026).
Within this trichotomy, the flat 38-cone is the intermediate singular model between the smooth disk and the tetrahedral 39-cone. The later 40-cone paper explicitly states that its proof “follows the same strategy as the uniqueness proof for the flat 41-cone,” adapted to tetrahedral combinatorics. This places the 42-cone theorem in a structural role: it is both a classification result and a methodological prototype for singular free-boundary Plateau rigidity (Matinpour, 26 May 2026).
A plausible implication is that the flat 43-cone should be regarded as the first singular analogue of Nitsche’s equatorial disk: the singularity is permitted, but conformality, minimality, and the free-boundary condition still force the model to be planar.
6. Distinct cone problems and common misidentifications
The phrase “free boundary cone” has several incompatible meanings in current literature. The flat 44-cone belongs to the Plateau/minimal-surface setting, not to the one-phase Bernoulli or capillarity settings. The distinction is substantive rather than terminological.
| Setting | Model object | Relation to the flat 45-cone |
|---|---|---|
| Free-boundary minimal 46-surface | Three planar half-disks meeting at 47 in 48 | Genuine flat 49-cone (Matinpour, 29 Sep 2025) |
| One-phase Bernoulli on a right circular cone | Rotationally symmetric 50-homogeneous free boundary on a singular ambient cone | Not a 51-junction (Allen, 2017) |
| Capillary or wedge free-boundary hypersurfaces | Codimension-one hypersurface with contact-angle condition | Generally excludes triple-junction 52-cones (Pacati et al., 11 Feb 2025) |
In the one-phase Bernoulli problem on the three-dimensional right circular cone
53
the governing system is
54
and the relevant homogeneous solution is a rotationally symmetric cone
55
The authors state explicitly that this problem is “not about classical triple-junctions or soap-film 56-cones,” and that the resulting cone-tip blow-up is a single conical sheet rather than a 57-shape. In dimension three, stable homogeneous solutions are, up to rotation, exactly the symmetric solution 58, and the structural lemmas force the zero set to be a single connected convex cone in a half-space, which is incompatible with a genuine 59-junction (Allen, 2017). The later computational refinement proves that for
60
the distinguished homogeneous cone solution is the unique minimizer for its boundary data, while the stability threshold is numerically
61
again in a setting unrelated to flat 62-cones (Allen et al., 2021).
A different but related dictionary appears in the correspondence between free boundary minimal surfaces in 63 and homogeneous one-phase free boundary cones in 64. There the cone problem is
65
with 66 homogeneous of degree 67. The paper proves that if 68 is diffeomorphic to a disk, then 69 is a half-space; if 70 is diffeomorphic to an annulus, then 71 is a circular cone formed by lines with aperture
72
This again classifies smooth one-phase cone geometries but does not address triple-junction 73-cones (Nadirashvili et al., 2018).
Capillarity and wedge problems impose yet another framework. For minimizing capillary cones in the half-space, one studies
74
with stability inequality
75
In this class, the paper proves that in dimension 76 any minimizing capillary cone with non-sign-changing 77 is flat, and that axially symmetric minimizing capillary cones are flat for 78. But it also emphasizes that a classical 79-cone is generally outside the framework because the objects are boundaries of a single set of finite perimeter rather than multi-sheet triple-junction surfaces (Pacati et al., 11 Feb 2025).
The same exclusionary pattern appears in wedge free-boundary minimal hypersurfaces. In a 80-dimensional wedge 81, 82, any stable 83-to-edge properly embedded free boundary minimal hypersurface 84 is flat: 85 for some hyperplane 86. This is a strong flatness theorem, but its admissible class is properly embedded hypersurfaces, not 87-junction cones (Yan, 2024).
The most precise conclusion is therefore terminological and geometric at once: the free boundary flat 88-cone is a singular Plateau model surface with three planar faces meeting at 89, rigid under conformal free-boundary minimal immersion and characterized by Morse index 90 in 91 (Matinpour, 29 Sep 2025). Many nearby arXiv literatures discuss “free boundary cones,” but these are usually rotational Bernoulli cones, capillary hypersurface cones, or wedge-hyperplane sections rather than genuine 92-junction configurations (Matinpour, 26 May 2026).