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Correction to: Mediterr. J. Math. (2022) 19:3 https://doi.org/10.1007/s00009-021-01877-4
In the previous paper [2, Section 3.2], we describe the family of titled \([\varphi ,{\vec {e}}_{3}]\)-catenary cylinders as surfaces obtained from a \([\varphi ,{\vec {e}}_{3}]\)-catenary cylinder \(\Sigma \), by rotation of angle \(\theta \in ]0,\pi /2[\) about the x-axis and dilation by scale factor \(1/\cos \theta \). The authors state that the resulting surface, \({\widetilde{\Sigma }}\), is always a \([\varphi ,{\vec {e}}_{3}]\)-minimal surface, but this is only true when the starting \([\varphi ,{\vec {e}}_{3}]\)-catenary cylinder is a grim reaper translating soliton, which follows directly from the relationship between their mean curvatures. In fact, following the same notation as in [2, Section 3.2], \( \widetilde{H} =\cos \theta \, H\), and \({\widetilde{\Sigma }}\) will be a \([\varphi ,{\vec {e}}_{3}]\)-minimal surface if and only if
that is, if and only if \(\Sigma \) is a grim reaper translating soliton. In this case, \({\widetilde{\psi }}\) will be a tilted grim reaper cylinder.
The following result updates the classification of complete flat \([\varphi ,{\vec {e}}_{3}]\)-minimal surfaces in \({\mathbb {R}}^3\) [2, Theorem 3.7]:
Let \(\varphi :{\mathbb {R}}\rightarrow {\mathbb {R}}\) be a diffeomorphism and \(\Sigma \) be a complete flat \([\varphi ,{\vec {e}}_{3}]\)-minimal surface in \({\mathbb {R}}^{3}.\) Then, one of the following statements holds
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\(\Sigma \) is a vertical plane.
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\(\Sigma \) is a grim reaper cylinder (maybe tilted).
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\(\Sigma \) is a \([\varphi ,{\vec {e}}_{3}]\)-catenary cylinder.
From basic differential geometry, \(\Sigma =\gamma \times \Pi ^\perp \) is a ruled surface and its Gauss map is constant along the rules, where \(\gamma \) is a complete regular curve in a plane \(\Pi \subset {\mathbb {R}}^3\). Thus, \(\Sigma \) can be parametrized by \(\psi (s,t)=\gamma (s)+t{\vec {v}}\), with \(\gamma (s)\) a complete regular curve contained in a plane \(\Pi \) and \({\vec {v}}\) a unit vector orthogonal to \(\Pi \). We may assume that \((s,t)\in {\mathbb {R}}^2\) and \(\vert \gamma '\vert =1\), then, the Gauss map N of \(\psi \) and its mean curvature H are given by
where \(\kappa _{\gamma }\) is the curvature of \(\gamma \). Hence, \(\Sigma \) is \([\varphi ,{\vec {e}}_{3}]\)-minimal if and only if the following relation holds
Differentiating with respect to t in the above expression, we obtain that
If \(\langle {\vec {v}},{\vec {e}}_{3}\rangle = 0\), arguing as in [2, Theorem 3.7], for any horizontal rule \({\mathcal {L}}\) of \(\Sigma \) there exists a \([\varphi ,{\vec {e}}_{3}]\)-catenary cylinder \({\mathcal {C}}\) containing \({\mathcal {L}}\) and tangent to \(\Sigma \) along \({\mathcal {L}}\). Thus, from standard theory of uniqueness of solution for an ODE, up to horizontal translation, \(\Sigma \) must coincide with \({\mathcal {C}}\).
If \(\langle {\vec {v}},{\vec {e}}_{3}\rangle \ne 0\),
and we can assume that \(\ddot{\varphi }\) does not vanish everywhere otherwise, from [1], \(\varphi \) is a linear function and \(\Sigma \) is either a vertical plane or a grim reaper cylinder (maybe tilted). Thus, we have that \(\gamma '\wedge {\vec {v}}\) is orthogonal to \({\vec {e}}_{3}\) and \(\Sigma \) must be a vertical plane. \(\square \)
Now, the Corollary 3.8 in [2] updates to
Let \(\varphi :{\mathbb {R}}\rightarrow {\mathbb {R}}\) be a increasing diffeomorphism with \(\dddot{\varphi }\le 0\) and \(\Sigma \) be a complete locally convex \([\varphi ,{\vec {e}}_{3}]\)-minimal surface in \({\mathbb {R}}^{3}\). If the Gauss curvature vanishes anywhere, then one of the following statements holds
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\(\Sigma \) is a vertical plane.
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\(\Sigma \) is a grim reaper cylinder (maybe tilted).
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\(\Sigma \) is a \([\varphi ,{\vec {e}}_{3}]\)-catenary cylinder.
Although it does not affect any of the results shown throughout the paper, the Eqs. (6) and (7) in [2, Lemma 2.1] must be change to
References
Martín, F., Savas-Halilaj, A., Smoczyk, K.: On the topology of translating solitons of the mean curvature flow. Calc. Var. 54, 2853–2882 (2015)
Martínez, A., Martínez-Triviño, A.L.: Equilibrium of surfaces in a vertical force field. Mediterr. J. Math. 19, 3 (2022). https://doi.org/10.1007/s00009-021-01877-4
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Martínez, A., Martínez-Triviño, A.L. Correction to: Equilibrium of Surfaces in a Vertical Force Field. Mediterr. J. Math. 20, 250 (2023). https://doi.org/10.1007/s00009-023-02442-x
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DOI: https://doi.org/10.1007/s00009-023-02442-x