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<p>The Young–Dupré equation is a cornerstone of the theory of capillary and wetting phenomena, which governs the shape of droplets adsorbed on surfaces in equilibrium. However, many living and synthetic materials, such as swarming bacteria and active colloids, are composed of self-propelled particles that are inherently out of thermal equilibrium. The description of the wetting of surfaces by such active fluids thus requires a new framework. Here we develop an analogue to the Young–Dupré equation for systems made of self-propelled particles. A key step is to define the liquid–gas surface tension of active fluids as the force exerted along the interface, which we show from first principles to be negative, even when active materials separate into stable liquid and gas phases. Our active Young–Dupré equation explains why partial wetting appears in simulations where the surface tensions do not balance and reveals the underlying feedback mechanism: the interface is stable only because of steady flows, which are themselves generated by the parity symmetry-breaking interface. Unlike in passive fluids, where the droplets are scale-free, this feedback loop selects the sizes and shapes of adsorbed droplets in active materials. Our results outline a framework for understanding how active matter wets surfaces.</p>

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Wetting by active fluids

  • 期刊论文

  • 发表日期：

    2026年4月3日

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  • Yongfeng Zhao,
  • Ruben Zakine,
  • Adrian Daerr,
  • Yariv Kafri,
  • Julien Tailleur,
  • Frédéric van Wijland

摘要

The Young–Dupré equation is a cornerstone of the theory of capillary and wetting phenomena, which governs the shape of droplets adsorbed on surfaces in equilibrium. However, many living and synthetic materials, such as swarming bacteria and active colloids, are composed of self-propelled particles that are inherently out of thermal equilibrium. The description of the wetting of surfaces by such active fluids thus requires a new framework. Here we develop an analogue to the Young–Dupré equation for systems made of self-propelled particles. A key step is to define the liquid–gas surface tension of active fluids as the force exerted along the interface, which we show from first principles to be negative, even when active materials separate into stable liquid and gas phases. Our active Young–Dupré equation explains why partial wetting appears in simulations where the surface tensions do not balance and reveals the underlying feedback mechanism: the interface is stable only because of steady flows, which are themselves generated by the parity symmetry-breaking interface. Unlike in passive fluids, where the droplets are scale-free, this feedback loop selects the sizes and shapes of adsorbed droplets in active materials. Our results outline a framework for understanding how active matter wets surfaces.