Atwood effects on nonlocality of the scalar transport closure in three-dimensional Rayleigh-Taylor mixing
Dana Lynn Ona-Lansigan Lavacot, Ali Mani, Brandon E. Morgan
TL;DR
This work analyzes nonlocality in mean scalar transport for turbulent three-dimensional Rayleigh–Taylor mixing across Atwood numbers by extending the Macroscopic Forcing Method to variable-density flows and measuring eddy-diffusivity moments $D^{mn}$. It demonstrates that higher Atwood numbers amplify nonlocality, with higher-order and temporal moments growing in magnitude and memory effects lengthening in time, especially near layer edges. Using Matched Moment Inverse, the study tests how spatial, temporal, and spatio-temporal moments influence flux predictions $F$, revealing that temporal moments significantly improve accuracy at low $A$ and that robustness constraints emerge for higher $A$. The authors propose an Atwood-dependent analytic model for the inverse operator coefficients, enabling improved closures in self-similar space and highlighting the need to incorporate Atwood-driven nonlocality into RANS-like RT closures. Overall, the results support incorporating nonlocal, temporally extended eddy-diffusivity effects into variable-density RT models, with a practical path forward via Atwood-aware inverse operators and reduced-order moment constructions.
Abstract
The importance of nonlocality is assessed in modeling mean scalar transport for turbulent Rayleigh-Taylor (RT) mixing at different Atwood numbers. Building on the two-dimensional incompressible work of Lavacot et al. (2024, JFM), the present work extends the Macroscopic Forcing Method (MFM) to variable density problems in three-dimensional space to measure moments of the generalized eddy diffusivity kernel in RT mixing for increasing Atwood numbers (A=0.05, 0.3, 0.5, 0.8). It is found that as A increases: 1) the eddy diffusivity moments become asymmetric, and 2) the higher-order eddy diffusivity moments become larger relative to the leading-order diffusivity, indicating that nonlocality becomes more important at higher A. There is a particularly strong temporal nonlocality at higher $A$, suggesting stronger history effects. The implications of these findings for closure modeling for finite-Atwood RT are discussed.
