Class Central is learner-supported. When you buy through links on our site, we may earn an affiliate commission.

YouTube

Solutal Convection in Porous Media

Society for Industrial and Applied Mathematics via YouTube

Overview

Save Big on Coursera Plus. 7,000+ courses at $160 off. Limited Time Only!
Explore solutal convection in porous media through this comprehensive lecture by Marc Hesse from the University of Texas at Austin. Delve into the intricacies of molecular and dispersive Rayleigh numbers, examining their impact on mass flux and finger spacing in convective patterns. Discover how bead size in porous media affects these parameters and learn about the limitations of flux at large bead sizes due to mechanical dispersion anisotropy. Analyze numerical simulations at the Darcy scale and their correlation with pore-scale results, focusing on the role of mechanical dispersion anisotropy. Investigate the transition between diffusion and dispersion-dominated regimes, and understand the implications of convective up- and downwellings in individual pores. Gain insights into buoyancy-driven pore-scale mixing and its unique characteristics compared to pressure-driven flows, highlighting the need for new approaches in upscaling to the Darcy scale. The lecture covers various aspects including time scales, fluid mechanics, numerical simulations, analog fluid systems, experiments, dispersion properties, and density profiles, concluding with a summary and Q&A session.

Syllabus

Intro
Housekeeping
Presentation
Time scales
Fluid mechanics
Numerical simulations
Analog fluid system
Experiments
Experiment Data
Properties of Dispersion
Standard Dispersion
Scatter
Numerical Comparison
Summary
Questions
Density Profiles
Simulations

Taught by

Society for Industrial and Applied Mathematics

Reviews

Start your review of Solutal Convection in Porous Media

Never Stop Learning.

Get personalized course recommendations, track subjects and courses with reminders, and more.

Someone learning on their laptop while sitting on the floor.