Power Spectra of Velocity Fluctuations in Granular Heap Flow

Abstract

This study used Speckle Visibility Spectroscopy to examine velocity fluctuations in a three-dimensional granular heap flow, where the mean velocity profile consists of a fast-flow surface layer and a creep layer beneath. The velocity spectra follow power-law scalings, $E(f) \propto f^{\alpha}$, with $\alpha \approx -0.85$ in the surface flow layer -- matching the Self-Organized Criticality (SOC) model with open boundaries ($\alpha \approx -0.95$). In the creep layer, $\alpha$ decreases with depth, reaching $\alpha \approx -1.5$ at approximately 55 mean particle diameters, consistent with the SOC model with closed boundaries ($\alpha \approx -1.58$). Analysis of the fluctuation velocity distributions offers additional insights into the microscopic origins of the spectrum's characteristics. These findings help resolve the long-standing puzzle of flow localization in gravity-driven granular flows despite a constant shear stress-to-pressure ratio throughout the material.