Constrained Isometric Co-extension Theory
- Constrained isometric co-extension is a boundary-value formulation where prescribed isometric data on a hypersurface is extended to a neighborhood while preserving both trace and metric constraints.
- The construction utilizes convex integration techniques and adapted short maps to correct metric defects by decomposing them into primitive metrics and employing localized corrugation profiles.
- The approach differentiates equidimensional rigidity from one-sided flexibility, highlighting the role of curvature, second fundamental forms, and regularity thresholds in isometric embedding.
“Constrained isometric co-extension” (Editor's term) denotes a boundary-value form of the isometric immersion problem in which isometric data prescribed on a hypersurface or submanifold are extended to a neighborhood, or to one side of that submanifold, while preserving both the trace data and the metric constraint. In its basic equidimensional form one fixes a smooth -manifold , a hypersurface , and a smooth isometric immersion , and asks for a map on a neighborhood such that
or, in low regularity, almost everywhere. The modern theory is stratified by codimension, sidedness, and regularity: equidimensional extensions are highly rigid above the Lipschitz threshold, one-sided codimension-one problems admit convex-integration flexibility, and smooth submanifold-based formulations are governed by curvature and second-fundamental-form compatibility (Wasem, 2015, Hungerbühler et al., 2014, Yu, 2019).
1. Boundary-value formulation and geometric setup
In the equidimensional setting studied by Wasem, the target has the same dimension as the source, so the problem is codimension zero. The prescribed datum is an isometric immersion
with carrying the Euclidean metric 0, and the extension problem is local near a point of 1. The paper distinguishes full neighborhoods from one-sided neighborhoods, and the constructive theory is one-sided: in local coordinates one works on an 2-polytope 3, sets
4
and treats 5 and 6 as the relevant one-sided domains (Wasem, 2015).
A parallel codimension-one formulation appears in the one-sided isometric extension literature. There the prescribed datum is a smooth isometric immersion or embedding 7, 8, or 9, and the extension is sought on a one-sided neighborhood of 0 constructed from the exponential map. In Cao and Inauen’s global formulation, if 1 is the unit normal respecting the orientation, then
2
defines
3
and one asks for an isometric embedding 4 satisfying 5 (Cao et al., 2020).
Regularity is intrinsic to the formulation. In codimension zero, the exact equation is often relaxed from 6 pointwise to
7
because the available flexible constructions are Lipschitz and generally non-8. In codimension one, by contrast, one-sided 9 and 0 extensions exist under suitable positivity hypotheses, and in that regime the output can be chosen as an embedding if the seed short map is an embedding (Wasem, 2015, Hungerbühler et al., 2014, Cao et al., 2018).
2. Equidimensional rigidity and obstruction
The equidimensional problem is fundamentally different from the classical Nash–Kuiper regime. Wasem emphasizes that in codimension zero there is no positive-dimensional sphere of normal oscillatory directions, and the classical Liouville theorem implies that images of 1 equidimensional Euclidean isometric immersions are congruent. This is sharpened by a local nonexistence theorem: an 2-dimensional Riemannian manifold 3 can be locally isometrically embedded by a differentiable map into 4 if and only if 5 is flat, and in that case the map is in fact 6 (Wasem, 2015). Thus any differentiable equidimensional constrained co-extension forces flatness.
For hypersurface data there is a more refined obstruction based on second fundamental forms. Let 7 be the second fundamental form of 8, with scalar form
9
and let 0 be the second fundamental form of 1, with scalar form
2
If there exists a unit vector 3 such that
4
then no isometric Lipschitz extension 5 can exist (Wasem, 2015). The proof is a length-comparison argument: along a geodesic 6, any Lipschitz isometric extension would imply
7
while the asymptotic expansions of these distances are controlled by the scalar second fundamental forms.
An analogous obstruction survives in higher codimension for two-sided local extension. In Hungerbühler–Wasem’s one-sided theory, if there exists a unit vector 8 such that
9
then no isometric extension 0 can exist on a full neighborhood 1 of 2 (Hungerbühler et al., 2014). The point is not that all low-regularity extension is obstructed, but that full local extension is more rigid than one-sided extension.
A higher-regularity codimension-one rigidity phenomenon appears in 3. Cao and Inauen prove that if 4, 5, and 6 is an isometric extension of prescribed smooth codimension-one data, then
7
for every tangent field 8 (Cao et al., 2020). Equivalently, along 9, the tangential connection induced by the extension must agree with the Levi-Civita connection. This is a first-order compatibility law forced by regularity above the Hölder threshold 0.
3. Weak convex integration in codimension zero
The positive equidimensional theory begins with an adapted short map. For a one-sided neighborhood 1 of 2, a map
3
is a short map adapted to 4 if 5 and
6
as quadratic forms, with equality on 7 only; equivalently, 8 is positive definite on 9 and zero on 0 (Wasem, 2015). Such a seed exists if there are choices of normals 1 for which
2
is positive definite.
From an adapted short map, Wasem constructs a one-sided Lipschitz a.e.-isometric extension. The main theorem states that for every 3 there exists a Lipschitz map 4 whose singular set has Hausdorff dimension 5, such that
6
(Wasem, 2015). The metric defect is not eliminated pointwise by classical Nash spirals or codimension-one corrugations. Instead, the defect is decomposed into primitive metrics
7
and corrected one rank-one term at a time by a degenerate corrugation ansatz adapted to codimension zero.
The crucial geometric obstruction to classical convex integration is that in codimension zero the “sphere” of oscillatory directions degenerates to two points. Accordingly, the exact circle equation is replaced by inequalities and average identities. In the regular case, the corrugation profile 8 is chosen so that
9
0
1
thereby producing only an averaged correction to the metric defect (Wasem, 2015). This is why the scheme is described as weak convex integration.
Iteration proceeds by steps and stages. After correcting all primitive metrics in a stage, the map is approximated again by an adapted piecewise affine short map. The key stage estimate is that for any 2 one obtains 3 with
4
and
5
Derivative control is obtained from the 6 estimate
7
which yields 8-Cauchy convergence of the gradients and finally
9
(Wasem, 2015).
The singular set is explicit: 0 so
1
unless no new simplices are introduced. The paper also proves a density statement: if
2
is the 3-closure of adapted short maps and
4
then the zero set of 5 is dense in 6 (Wasem, 2015).
4. One-sided flexibility in codimension one
In codimension one, the one-sided theory of Hungerbühler–Wasem gives a 7 analogue of the adapted-short-map paradigm. A smooth immersion 8 is adapted to 9 if
00
with equality only on 01. If there exists a unit normal field 02 such that
03
is positive definite on 04, then near every 05 there exists an adapted short map, even an adapted short embedding (Hungerbühler et al., 2014). The main existence theorem states that every such adapted short map can be approximated arbitrarily well in 06 by a 07-isometric one-sided immersion 08 satisfying
09
and that the construction satisfies a 10-dense parametric 11-principle (Hungerbühler et al., 2014).
Codimension-one 12 extensions sharpen this picture. Given a smooth isometric immersion 13, if there exists a unit normal field 14 along 15 such that
16
as a quadratic form on 17, then there is a one-sided neighborhood 18 of 19 and, for every
20
a 21 isometric immersion
22
with
23
(Cao et al., 2018). The initial seed is an adapted short immersion with defect of the form
24
where 25 near 26, and the iteration is localized away from 27 so that every perturbation vanishes near the prescribed hypersurface.
The codimension-one convex integration mechanism is stronger than the equidimensional one because there is still a genuine normal direction. Primitive metrics are corrected by corrugations satisfying the exact identity
28
and the resulting 29 regularity threshold
30
comes from balancing defect decay, frequency growth, and the 31-cost of each stage (Cao et al., 2018). This is a low-codimension Nash–Kuiper regime with an explicit boundary-preserving localization.
5. Critical regularity at 32
Cao and Inauen identify 33 as the critical Hölder exponent for constrained codimension-one 34 extensions. Their theorem has a rigidity/flexibility dichotomy. If 35, 36, and 37 is a 38 isometric extension of 39, then
40
If 41, 42 with
43
then there exists 44 and 45 such that
46
at all points where 47 (Cao et al., 2020).
The rigidity mechanism above 48 is analytic. A result of De Lellis–Inauen implies that for 49, 50, the weak tangential connection is well defined distributionally, so Gauss-type identities survive at the regularity level needed to compare the induced tangential connection with the Levi-Civita connection along 51. Since 52 on 53 and 54 is smooth, the distributional identity becomes a pointwise compatibility law there (Cao et al., 2020).
Below 55, the iteration preserves not only the trace but also the differential on 56. The short initial extension is built in the form
57
and already satisfies
58
Because the convex integration step is arranged so that
59
the final exact isometric extension inherits the same strict inequality (Cao et al., 2020). The same machinery also yields a global existence theorem: if 60 is a compact 61-manifold with 62 metric and 63, then there exist infinitely many 64 isometric embeddings
65
6. Canonical constructions and applications
The most vivid equidimensional example is Wasem’s “isometric collapse” of the sphere. There exist infinitely many Lipschitz maps
66
such that
67
where 68 is the equator and 69 is the standard inclusion (Wasem, 2015). The construction extends the equatorial data separately to the upper and lower hemispheres by one-sided adapted short maps and then glues the resulting Lipschitz a.e.-isometric maps because the iteration leaves a neighborhood of the equator unchanged.
This sphere-collapse example sharply illustrates the regularity barrier. Because 70 has Gaussian curvature 71, the map cannot be 72 or even merely differentiable by the differentiable flatness theorem. The resulting map is Lipschitz, its singular set is dense in this curved example, and it cannot be locally 73 or locally injective (Wasem, 2015). Extrinsic dimension is collapsed, but metric preservation survives almost everywhere in the weak sense.
The codimension-one literature contains a conceptually similar boundary-value example. Hungerbühler–Wasem exhibit flexible 74 extensions of the equatorial inclusion
75
to maps 76, in sharp contrast with Borisov-type rigidity at 77, 78 (Hungerbühler et al., 2014). This contrast between equidimensional collapse and codimension-one wrinkling is central to the subject: the prescribed trace datum is the same type of object, but the available extension mechanisms depend decisively on codimension and regularity.
7. Related smooth and metric formulations
A smooth counterpart is provided by the submanifold-based Cartan–Ambrose–Hicks theory of Mencattini, Mendonça, and Vlachos. In the equal-dimensional case, given isometric immersions 79 and 80, a metric- and connection-preserving bundle map
81
and curvature transport relation
82
they construct a local isometry 83 such that
84
In positive codimension they prescribe, in addition, a Riemannian vector bundle 85 and a symmetric tensor
86
together with the compatibility law
87
and prove an extension theorem under the Gauss, Codazzi, and Ricci equations (Yu, 2019). This is a smooth constrained co-extension theory in which prescribed boundary data include normal bundle and second-fundamental-form information.
A variational boundary analogue arises in thin-sheet theory. Guven, Hanna, and Müller show that for isometric bending of an unstretchable sheet with free edge, the bulk metric constraint does not by itself determine admissible free-edge deformations. To make the problem mechanically well posed, one must constrain not only the local boundary arc-length but also the local boundary geodesic curvature; otherwise the naive free-edge theory implies unphysical conditions such as local planarity at the boundary (Guven et al., 2019). This does not produce an extension theorem in the convex-integration sense, but it identifies the extra edge invariants required for consistent boundary-value formulations of isometric bending.
There is also a distinct equidimensional low-regularity theory based on Gromov’s length-preserving notion of isometry rather than the pullback equation. In that setting a Lipschitz map is isometric if it preserves the length of every rectifiable curve, and a Baire-category argument shows that the typical 88-Lipschitz extension of fixed short data on a compact set 89 is isometric on 90, while the typical short map on 91 is the restriction of a global isometric map of 92 (Kirchheim et al., 2014). This suggests a broader landscape in which constrained isometric co-extension encompasses smooth curvature-driven extension, one-sided convex-integration flexibility, and metric length-preserving extension, each with its own notion of admissible boundary data and its own rigidity threshold.