Buoyant plumes in cross flows
Diffuse 
        venting and background contributions to chemical anomalies in a neutrally 
        buoyant ocean hydrothermal plume (Abstract)
        
Problem 
        Description: 
        High-temperature, 
        focused venting leads to significant vertical mixing and redistribution 
        of tracers in the benthic ocean. Vent discharge and background benthic 
        water entrained into a plume lead to altered geochemical and microbial 
        payloads found well above the seafloor. Take the case of aluminum. Observations 
        in the Atlantic show Al profiles naturally enhanced near bottom. That 
        is caused by Al rich particles settling to the sea floor and the subsequent 
        remobilization of elemental AL. But diffuse hydrothermal flows also introduce 
        Al to the near-bottom waters surrounding high temperature vents. A question 
        to be answered is how focused, diffuse, and background sources of Al all 
        contribute to Al levels in neutrally buoyant plumes. This study looks at 
        Al distributions at the TransAtlantic Geotraverse (TAG) site in the Atlantic 
        using one- and three- dimensional models of convective plumes. Contributions 
        of the background and diffuse Al fields dominante. 
|  | Vertical (x-z) sections along the flow direction and though the TAG mound for each source component species: a) 
              Al from focused sources,  click for larger view FLI 
              Animation (1.1 mb)  | 
| Related 
        Papers:  Chronic 
        focused-source plumes Lavelle, J.W. (1997): Buoyancy-driven plumes in rotating, stratified cross flows: Plume dependence on rotation, turbulent mixing, and cross-flow strength. Journal of Geophysical Research, 102(C2), 3405-3420. Geochemical Transport 
 | ||
| Modeling focuses: Chronic focused-source | Event Plumes | Axial Valley transport | Ridge Flow | Geochemical Transport | Hydrographic-Tracer Relationships | ||
