Mixing density-driven

Hydrological Gravitational water flows Water and atmosphere circulation Sedimentation, suspensions Thermal water and gas flows Evaporation, condensation, precipitation Chemical, density-driven currents Chemical stratification of waters Evaporative mixing Chemical potential-driven flows, diffusion... 

The coupling between the hydrological forces and chemical processes —H->C—is responsible for transport of solutes, and this coupling is also to some extent reflected in the water-flow-rate dependence of some mineral dissolution reactions. The reverse coupling between chemical forces and hydrological processes—C- H—is seen in such phenomena as chemical density stratification in lakes, evaporative mixing caused by solute concentration increase in a surface water layer, and chemical density-driven water currents. 

Fig. 7. Model for mixing of fluids by density-driven overturning. As the interface rotates through time, its progress can be represented by the parameter Ixjh.

The model for density-driven fluid overturning discussed above (Fig. 7), and described in equation (10), is strictly designed to represent overturn and mixing of miscible fluids, such as oils of different density. However, reservoir... 

Spatial Heterogeneity and Imperfect Mixing in Chemical Reactions Visualization of Density-Driven Pattern... 

---