OS43A-2008
Coupled Porosity and Chemical Evolution of Hydrothermal Circulation: Implications for the Morphology of Vents and Recharge Zones at Mid-Ocean Ridges

Thursday, 17 December 2015
Poster Hall (Moscone South)
Laurent Montesi1, Yang Liao2, Hailong Bai1, Zhitu Ma3, Renbiao Tao4, Drew D Syverson5, Robert P Lowell6 and Tobias P Fischer7, (1)University of Maryland College Park, College Park, MD, United States, (2)Yale University, New Haven, CT, United States, (3)University of California San Diego, IGPP, La Jolla, CA, United States, (4)Peking University, Beijing, China, (5)University of Minnesota Twin Cities, Minneapolis, MN, United States, (6)Virginia Polytechnic Institute and State University, Geosciences, Blacksburg, VA, United States, (7)University of New Mexico, Department of Earth and Planetary Sciences, Albuquerque, NM, United States
Abstract:
While the clearest evidence for hydrothermal circulation resides in focused upwellings at high-temperature vents, which form chimneys, circulation also features less-understood low-temperature diffuse flow and recharge zones. Flow focusing depends on the subsurface porosity and permeability structure, which, in the reactive environment of hydrothermal circulation, is likely influenced by mineral dissolution and precipitation from hydrothermal fluids. We developed two-dimensional Finite Element models of coupled reactive flow and porosity evolution and discuss how reactions may influence flow focusing and the morphology of upwellings and downwellings. This work can also address the chemical and thermal flux provided to the ocean, and the grade and volume of metal sulfide deposition.

Our coupled system (See image) considers 1) Darcy flow driven by fluid buoyancy; 2) Heat transport in a porous medium; 3) Evolution of dissolved mineral concentration; 4) Evolution of porosity and permeability in response to mineral precipitation or dissolution. We also include an “ocean” layer, which allows hot fluid to escape the system without being forced to cool dramatically as they approach the seafloor.

Absent porosity evolution, hydrothermal circulation forms flame-like upwellings that bend to avoid downdrafts. The circulation varies at the time scale of decades. Assuming thermodynamic equilibrium is maintained, precipitation of amorphous silica takes place in the upwellings as they rise and cool down. When coupled with porosity and permeability evolution, silicate precipitation forces the upwellings to flatten and become diffuse. Localized recharge zones stabilize and develop an armor of low porosity rocks where high temperature fluids cooled rapidly and deposited silica as they approach the recharge zone. This morphology of localized, armored recharge zone and diffuse upwellings does not match observations at natural vent fields, which implies that a critical element of the hydrothermal system is missing from our models. Future models will also consider anhydrite which precipitates as seawater is heated and hence may counteract the effects of silica and may form localized upwellings and diffuse downwellings.

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