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Some geometric relations for equipotential curves

Yajun Zhou

TL;DR

This work analyzes how the curvature of equipotential curves and the gradient magnitude of a harmonic function are statistically correlated in a 2D exterior Dirichlet problem. It introduces four level-set functionals $\mathscr H(\varphi)$, $\mathscr E(\varphi)$, $\mathscr F(\varphi)$, and $\mathscr L(\varphi)$ and proves their convexity in the level parameter $\varphi$, from which sharp covariance-type inequalities between $\kappa$ and $E$ on each level set follow; a conservation law $\mathscr E(\varphi)\equiv \frac{4\pi^2}{\Phi}$ further ties curvature and gradient statistics. The approach is entropy-monotonicity driven, aligning with ideas of Colding and Colding–Minicozzi to provide monotone isoperimetric-type trends and supporting heuristics for dendritic patterns in Hele-Shaw flow and diffusion-limited aggregation; a complementary 2-inD analysis using Green's functions yields reversed-sign inequalities. The paper also discusses extensions to higher dimensions, highlighting challenges like potential critical points and the absence of a global mapping tool, and outlines avenues for conditional generalizations and future work. Overall, it provides a rigorous geometric-entropic framework to quantify how level-set geometry constrains or correlates with field intensities in harmonic exterior problems, with potential implications for electrostatics, fluid dynamics, and pattern formation.

Abstract

Let $U(\boldsymbol r),\boldsymbol r\inΩ\subset \mathbb R^2$ be a harmonic function that solves an exterior Dirichlet problem. If all the level sets of $U(\boldsymbol r),\boldsymbol r\inΩ$ are smooth Jordan curves, then there are several geometric inequalities that correlate the curvature $κ(\boldsymbol r) $ with the magnitude of gradient $ |\nabla U(\boldsymbol r)|$ on each level set ("equipotential curve"). One of such inequalities is $ \langle [κ(\boldsymbol r)-\langleκ(\boldsymbol r)\rangle][|\nabla U(\boldsymbol r)|-\langle |\nabla U(\boldsymbol r)|\rangle]\rangle\geq0$, where $ \langle \cdot\rangle$ denotes average over a level set, weighted by the arc length of the Jordan curve. We prove such a geometric inequality by constructing an entropy for each level set $U(\boldsymbol r)=\varphi $, and showing that such an entropy is convex in $\varphi$. The geometric inequality for $κ(\boldsymbol r) $ and $ |\nabla U(\boldsymbol r)|$ then follows from the convexity and monotonicity of our entropy formula. A few other geometric relations for equipotential curves are also built on a convexity argument.

Some geometric relations for equipotential curves

TL;DR

This work analyzes how the curvature of equipotential curves and the gradient magnitude of a harmonic function are statistically correlated in a 2D exterior Dirichlet problem. It introduces four level-set functionals , , , and and proves their convexity in the level parameter , from which sharp covariance-type inequalities between and on each level set follow; a conservation law further ties curvature and gradient statistics. The approach is entropy-monotonicity driven, aligning with ideas of Colding and Colding–Minicozzi to provide monotone isoperimetric-type trends and supporting heuristics for dendritic patterns in Hele-Shaw flow and diffusion-limited aggregation; a complementary 2-inD analysis using Green's functions yields reversed-sign inequalities. The paper also discusses extensions to higher dimensions, highlighting challenges like potential critical points and the absence of a global mapping tool, and outlines avenues for conditional generalizations and future work. Overall, it provides a rigorous geometric-entropic framework to quantify how level-set geometry constrains or correlates with field intensities in harmonic exterior problems, with potential implications for electrostatics, fluid dynamics, and pattern formation.

Abstract

Let be a harmonic function that solves an exterior Dirichlet problem. If all the level sets of are smooth Jordan curves, then there are several geometric inequalities that correlate the curvature with the magnitude of gradient on each level set ("equipotential curve"). One of such inequalities is , where denotes average over a level set, weighted by the arc length of the Jordan curve. We prove such a geometric inequality by constructing an entropy for each level set , and showing that such an entropy is convex in . The geometric inequality for and then follows from the convexity and monotonicity of our entropy formula. A few other geometric relations for equipotential curves are also built on a convexity argument.

Paper Structure

This paper contains 11 sections, 14 theorems, 62 equations, 1 figure, 1 table.

Key Result

Theorem 1.1

We have the following inequalities that correlate $\kappa(\bm r)$ with $E(\bm r)$ on each level set $\Sigma$ in 2-exD problems: where $\bm n\times\nabla f(\bm r)$ denotes tangential gradient of a scalar $f(\bm r)$ (up to a 90$^\circ$ rotation). Furthermore, these inequalities are strict, unless $\partial\Omega$ is a circle.

Figures (1)

  • Figure 1: An illustration of electricians' folklore. Some level sets of a 2-dimensional harmonic function $U(\bm r),\bm r\in\Omega$ are displayed as gray curves. The boundary $\partial \Omega$, drawn in black, is also a level set ("equipotential curve"). Graphically speaking, the values of $|\nabla U(\bm r)|$ around the sharp tips (which "stick out") of level sets are larger (with much denser spacing between level sets) than those around the depressed pits (which "cave in").

Theorems & Definitions (25)

  • Theorem 1.1: Sharp geometric inequalities for 2-exD
  • Theorem 1.2: Sharp geometric inequalities for 2-inD
  • Proposition 2.1: Convexity of $\mathscr H(\varphi)$
  • proof
  • Corollary 2.2
  • Proposition 2.3: Sharp inequality for $\mathscr H'(\varphi)$
  • proof
  • Corollary 2.4: Sharp inequalities related to isoperimetric deficit
  • proof
  • Proposition 2.5: Non-negative correlation between curvature and field intensity
  • ...and 15 more