Abstract
This paper extends, in a sharp way, the famous Efimov’s Theorem to immersed ends in \(\mathbb {R}^3\). More precisely, let M be a non-compact connected surface with compact boundary. Then there is no complete isometric immersion of M into \(\mathbb {R}^3\) satisfying that \(\int _M |K|=+\infty \) and \(K\le -\kappa <0\), where \(\kappa \) is a positive constant and K is the Gaussian curvature of M. In particular Efimov’s Theorem holds for complete Hadamard immersed surfaces, whose Gaussian curvature K is bounded away from zero outside a compact set.
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Acknowledgements
The author would like to thank Heudson Mirandola, Cristina Levina and Manolo Heredia for useful discussions during the reading of [11]. He also thanks the referee for very interesting observations.
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To my beloved wife, Cristina, whose love and sincerity inspire me.
Appendix: Proof of Lemma 3.1
Appendix: Proof of Lemma 3.1
Consider a Riemannian smooth surface (S, g) and a connected surface with piecewise smooth boundary \(D\subset S\), with internal angles at the vertices different from 0 and \(2\pi \). Denote by \(d_g(p,q)\) the distance induced by the Riemannian metric g, and \(d_{\mathrm {int}}(p,q)\) the infimum of the g-lengths of piecewise \(C^1\) curves \(\gamma :[0,1]\rightarrow D\) joining p to q satisfying that \(\gamma \bigl ((0,1)\bigr )\subset \mathrm {int}(D)\).
The purpose of this appendix is to prove Lemma 3.1 above, which asserts that \(d_\mathrm {int}\) is a distance on D, and that the distances \(d_g\) and \(d_\mathrm {int}\) induce the same topology on D.
To prove Lemma 3.1 we first assume that \(d_\mathrm {int}\) is a distance on D. To show that \(d_g\) and \(d_\mathrm {int}\) induce the same topology on D, we need to prove that, given \(q\in D\) and \(\epsilon >0\), there exists \(\delta >0\) such that if \(p\in D\) with \(d_g(p,q)<\delta \) then \(d_\mathrm {int}(p,q)<\epsilon \). If \(q\in \mathrm {int}(D)\) the proof is trivial. Thus we will assume that \(q\in \partial D\).
Fix \(q\in \partial D\) and \(\epsilon >0\). For some small \(\lambda >0\), there exists a curve \(\sigma :[-\lambda ,\lambda ]\rightarrow \partial D, \lambda >0\), parameterized by the g-arc length satisfying that \(\sigma (0)=q\) and such that \(\sigma |_{[-\lambda ,0]}\) and \(\sigma |_{[0,\lambda ]}\) are smooth curves. Since \(\partial D\) is a piecewise smooth curve and the angles at the vertices differ from 0 and \(2\pi \), there exists a unit vector \(v\in T_qS\) pointing to \(\mathrm {int}(D)\) and transversal to both \(\sigma '(0-)\) and \(\sigma '(0+)\). Let \(v_t\) be the parallel transport of v along the both directions on \(\sigma \). If \(\lambda \) is small enough, we may assume that \(v_t\) is transversal to \(\sigma '(t)\) and that \(v_t\) points to \(\mathrm {int}(D)\). Set \(\sigma _s(t)=\exp _{\sigma (t)}sv_t=\gamma _t(s)\). By smoothness of the geodesic flow there exists sufficiently small \(0<\eta <\min \left\rbrace \lambda ,\frac{\epsilon }{3}\right\lbrace \) such that:
-
(1)
for \(0<s\le \eta \) and \(-\eta \le t\le \eta \), the point \(\sigma _s(t)\in \mathrm {int}(D)\);
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(2)
\(L_g(\sigma _\eta )<\frac{\epsilon }{3}\).
Given \(s_0\in [0,\eta ]\) and \(t_0\in [-\eta ,\eta ]\), we have that \(2\eta +|t_0|-s_0> \eta +|t_0|-s_0\ge 0\). We will construct a piecewise smooth curve \(\xi =\xi _{s_0t_0}:[0,2\eta +|t_0|-s_0]\rightarrow D\) from q to \(\sigma _{s_0}(t_0)\) satisfying \(\xi \bigl ((0,2\eta +|t_0|-s_0)\bigr )\subset \mathrm {int}(D)\) and \(L_g(\xi )<\epsilon \). From q to \(\sigma _{\eta }(0)=\gamma _0(\eta )\), let \(\xi |_{[0,\eta ]}\) coincide with the geodesic \(\gamma _0:[0,\eta ]\rightarrow D\). From \(\sigma _{\eta }(0)\) to \(\sigma _{\eta }(t_0)\) the curve \(\xi \) follows the curve \(\sigma _\eta \) in the direction that t is increasing if \(t_0\ge 0\), or in the other direction if \(t_0<0\). More precisely, for \(0\le t\le |t_0|\), we define \(\xi (\eta +t)=\sigma _\eta (t)\), if \(t_0\ge 0\), and \(\xi (\eta +t)=\sigma _\eta (-t)\), if \(t_0<0\). Finally, from \(\sigma _{\eta }(t_0)\) to \(\sigma _{s_0}(t_0)\) the curve \(\xi \) follows the geodesic \(s\longmapsto \gamma _{t_0}(\eta -s)\). Namely, for \(0\le s\le \eta -s_0\) we define \(\xi (\eta +|t_0|+s)=\gamma _{t_0}(\eta -s)=\sigma _{(\eta -s)}(t_0)\). In particular we have that \(\xi (2\eta +|t_0|-s_0)= \xi (\eta +|t_0|+(\eta -s_0))=\gamma _{t_0}(s_0)=\sigma _{s_0}(t_0)\). By construction we have that \(L_g(\xi )\le \eta + L_g(\sigma _{\eta })+(\eta -s_0)<\epsilon \).
Given \(s_1\in [0,\eta ]\) and \(t_1\in [-\eta ,\eta ]\), a similar construction as above shows that \(\sigma _{s_0}(t_0)\) may be connected to \(\sigma _{s_1}(t_1)\) by a piecewise smooth curve \(\psi :[0,1]\rightarrow D\) with \(\psi ((0,1))\subset \mathrm {int}(D)\) and \(L_g(\psi ) <\epsilon \).
Set \(X=\{\sigma _s(t)\bigm |0\le s\le \eta ,\, -\eta \le t\le \eta \}\). Since X is a compact neighborhood of q in D, we have that \(\delta =d_g(q,D-X)>0\). Now we take \(p\in D\) with \(d_g(p,q)<\delta \). We have that \(p\in X\), hence \(p=\sigma _{s_0}(t_0)\) for some \(s_0\in [0,\eta ]\) and \(t_0\in [-\eta ,\eta ]\). As a consequence we have that \(d_{\mathrm {int}}(p,q)\le L_g(\xi _{s_0t_0})<\epsilon \).
Now we consider points \(p,q,r\in D\) and we will show that \(d_\mathrm {int}(p,q)+d_\mathrm {int}(q,r) \ge d_\mathrm {int}(p,r)\). We will just consider the case that \(q\in \partial D\), since the other case is easier. Fix \(\epsilon >0\) and consider piecewise smooth curves \(\gamma :[0,1]\rightarrow D\) from p to q with \(\gamma ((0,1))\subset \mathrm {int}(D)\) and \(L_g(\gamma )<d_\mathrm {int}(p,q)+\epsilon \), and \(\sigma :[0,1]\rightarrow D\) from q to r with \(\sigma ((0,1))\subset \mathrm {int}(D)\) and \(L_g(\sigma )<d_\mathrm {int}(q,r)+\epsilon \). By using a neighborhood X of q as above, it is easy to obtain a piecewise smooth curve \(\varphi :[0,1]\rightarrow D\) from p to r with \(\varphi ((0,1))\subset \mathrm {int}(D)\) and \(L_g(\varphi )<L_g(\gamma )+L_g(\sigma )+\epsilon \). In fact, take \(0<s_1<1\) such that \(\gamma (s_1)\in X-\{q\}\) and \(0<s_2<1\) such that \(\sigma (s_2)\in X-\{q\}\). We define a curve \(\varphi \) which follows \(\gamma \) from \(t=0\) to \(t=s_1\) then follows a curve \(\psi \) in \(X\cap \mathrm {int}(D)\) with \(L_g(\psi )<\epsilon \), and then follows \(\sigma \) from \(t=s_2\) to \(t=1\). Thus we obtain that \(d_{\mathrm {int}}(p,r)\le L_g(\varphi )< L_g(\gamma )+L_g(\sigma )+\epsilon < d_\mathrm {int}(p,q)+d_\mathrm {int}(q,r)+3\epsilon \). By making \(\epsilon \rightarrow 0\) we conclude the proof of Lemma 3.1.
Remark 2
It is not difficult to see that Lemma 3.1 may be improved to assume that internal angles are just different from 0.
Remark 3
We inform that the paper [GMT] proves Theorem A, with another proof, simultaneously and independently.
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Mendonça, S. Complete negatively curved immersed ends in \(\mathbb {R}^3\) . Geom Dedicata 195, 319–337 (2018). https://doi.org/10.1007/s10711-017-0292-3
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DOI: https://doi.org/10.1007/s10711-017-0292-3