Influence of ambient temperature on cavitation bubble dynamics
Shaocong Pei, A-Man Zhang, Chang Liu, Tianyuan Zhang, Rui Han, Shuai Li
TL;DR
This work investigates how ambient temperature shapes the dynamics of spark-generated cavitation bubbles, spanning 23–$90\circ\mathrm{C}$. By combining hundreds of experiments with Keller-equation–based pressure estimation and compressible boundary-integral insights, it shows that higher $T$ raises internal vapour pressure and enlarges the maximum bubble radius while systematically weakening collapse and jetting. A novel secondary cavitation mechanism emerges above $70\circ\mathrm{C}$, driven by Blake-threshold–related nucleation that promotes Rayleigh–Taylor instabilities and bubble fission; near-wall dynamics further reveal reduced erosion potential at elevated temperatures, modulated by discharge energy. These findings advance the thermally mediated understanding of cavitation and offer practical guidance for erosion mitigation in high-temperature fluids.
Abstract
We investigate the influence of ambient temperature on the dynamics of spark-generated cavitation bubbles over a broad temperature range of 23 to 90$^\circ \text{C}$. Increasing temperature, the attenuation of collapse intensity of a bubble in a free field is quantitatively characterised through the Rayleigh factor, minimum bubble volume, and maximum collapse velocity. In scenarios where the bubble is initiated near a rigid boundary, this temperature-dependent weakening effect manifests further as a reduction in jet velocity and bubble migration. Additionally, our findings demonstrate that when ambient temperature exceeds 70$^\circ \text{C}$, secondary cavitation forms near the bubble surface around the moment of maximum bubble expansion, followed by coalescence-induced surface wrinkles. These perturbations trigger Rayleigh-Taylor instability and enhance bubble fission. We determine the internal gas pressure of the bubble at its maximum expansion via the Rayleigh-Plesset equation with the input of bubble radius from experimental measurements. It reveals that the secondary cavitation is derived from the gas pressure descending below the saturated vapor pressure, which provides nucleation-favorable conditions. This study sheds light on the physics behind erosion mitigation in high-temperature fluids from the perspective of cavitation bubble dynamics.
