Cruse Anna M.

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Cruse
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Anna M.
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  • Preprint
    Geochemistry of low-molecular weight hydrocarbons in hydrothermal fluids from Middle Valley, northern Juan de Fuca Ridge
    ( 2006-01-10) Cruse, Anna M. ; Seewald, Jeffrey S.
    Hydrothermal vent fluids from Middle Valley, a sediment-covered mid-ocean ridge on the northern Juan de Fuca Ridge, were sampled in July, 2000. Eight different vents with exit temperatures of 186 to 281°C were sampled from two areas of venting: the Dead Dog and ODP Mound fields. Fluids from the Dead Dog field are characterized by higher concentrations of ΣNH3 and organic compounds (C1-C4 alkanes, ethene, propene, benzene and toluene) compared with fluids from the ODP Mound field. The ODP Mound fluids, however, are characterized by higher C1/(C2+C3) and benzene:toluene ratios than those from the Dead Dog field. The aqueous organic compounds in these fluids have been derived from both bacterial processes (methanogenesis in low-temperature regions during recharge) as well as from thermogenic processes in higher-temperature portions of the subsurface reaction zone. As the sediments undergo hydrothermal alteration, carbon dioxide and hydrocarbons are released to solution as organic matter degrades via a stepwise oxidation process. Compositional and isotopic differences in the aqueous hydrocarbons indicate that maximum subsurface temperatures at the ODP Mound are greater than those at the Dead Dog field. Maximum subsurface temperatures were calculated assuming that thermodynamic equilibrium is attained between alkenes and alkanes, benzene and toluene, and carbon dioxide and methane. The calculated temperatures for alkene-alkane equilibrium are consistent with differences in the dissolved Cl concentrations in fluids from the two fields, and indicate that subsurface temperatures at the ODP Mound are hotter than those at the Dead Dog field. Temperatures calculated assuming benzene-toluene equilibrium and carbon dioxide-methane equilibrium are similar to observed exit temperatures, and do not record the hottest subsurface conditions. The difference in subsurface temperatures estimated using organic geochemical thermometers reflects subsurface cooling processes via mixing of a hot, low-salinity vapor with a cooler, seawater salinity fluid. Because of the disparate temperature dependence of alkene-alkane and benzene-toluene equilibria, the mixed fluid records both the high and low temperature equilibrium conditions. These calculations indicate that vapor-rich fluids are presently being formed in the crust beneath the ODP Mound, yet do not reach the surface due to mixing with the lower-temperature fluids.
  • Thesis
    Geochemistry of hydrothermal vent fluids from the northern Juan de Fuca Ridge
    (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 2003-02) Cruse, Anna M.
    The presence of aqueous organic compounds derived from sedimentary organic matter has the potential to influence a range of chemical processes in hydrothermal vent environments. For example, hydrothermal alteration experiments indicate that alteration of organic-rich sediments leads to up to an order of magnitude more metals in solution than alteration of organic-poor basalt. This result is in contrast to traditional models for the evolution of vent fluids at sediment-covered mid-ocean ridge axis environments, and indicates the fundamental importance of including the effects of organic compounds in models of crustal alteration processes. However, in order to rigorously constrain their role in crustal alteration processes, quantitative information on the abundances and distributions of organic compounds in hydrothermal vent fluids is required. This thesis was undertaken to provide quantitative information on the distributions and stable carbon isotopic compositions of several low-molecular weight organic compounds (C1-C4 alkanes, C2-C3 alkenes, benzene and toluene) in fluids collected in July, 2000, at three sites on the northern Juan de Fuca Ridge: the Dead Dog and ODP Mound fields, which are located at Middle Valley, and the Main Endeavour Field, located on the Endeavour segment. At Middle Valley, the ridge axis is covered by up to 1.5 km of hemipelagic sediment containing up to 0.5 wt.% organic carbon. The Main Endeavour Field (MEF) is located approximately 70 km south of Middle Valley in a sediment-free ridge-crest environment, but previously measured high concentrations of NH3 and isotopically light CH4 relative to other bare-rock sites suggest that the chemical composition of these fluids is affected by sub-seafloor alteration of sedimentary material (LILLEY et al., 1993). Differences in the absolute and relative concentrations of NH3 and organic compounds and the stable carbon isotopic compositions of the C1-C3 organic compounds suggest that the three fields represent a continuum in terms of the extent of secondary alteration of the aqueous organic compounds, with the Dead Dog fluids the least altered, the MEF fluids the most altered and ODP Mound fluids in an intermediate state. At the two Middle Valley sites, the greater extent of alteration in the ODP Mound fluids as compared to the Dead Dog fluids is due either to higher temperatures in the subsurface reaction zone, or a greater residence time of the fluids at high temperatures. Higher reaction zone temperatures at the ODP Mound field than at the Dead Dog field are consistent with differences in endmember C1 concentrations between the two fields. The greater extent of alteration in the MEF fluids is caused by relatively oxidizing conditions in the subsurface reaction zone that promote faster reaction kinetics. Temperatures in the subsurface reaction zones calculated by assuming equilibrium among aqueous alkanes, alkenes and hydrogen are consistent with other inorganic indicators (C1 and Si concentrations) of temperature, indicating that metastable equilibrium among these compounds may be attained in natural systems. Isotopic equilibration among CH4 and CO2 appears to have been attained in ODP Mound fluids due to the high temperatures in the subsurface reaction zone and the approach to chemical equilibrium from excess methane. However, isotopic equilibrium between CH4 and CO2 was not attained in the MEF fluids, due to a short residence time of the fluids in the crust following late-stage addition of magmatic-derived CO2 to the fluids. Time series analysis indicate that Middle Valley fluid compositions are generally characterized by stable concentrations over the last decade. However, decreases in Br concentrations in Dead Dog fluids from 1990 to 2000 suggest that either a greater proportion of the fluids interact with basalt rather than sediments or that the sediment with which hydrothermal fluids interact is becoming exhausted. In contrast, the concentrations of H2 and H2S and the δ34S of H2S are quite different in fluids sampled from vents of differing ages at the ODP Mound field, despite their close spatial proximity. The observed variations are caused by the reaction of hydrogen-rich fluids within the ODP Mound massive sulfide to reduce pyrite to pyrrhotite during upflow. The replacement of pyrite by pyrrhotite is opposite to the reaction predicted during the weathering of sulfide minerals weather on the seafloor and reflects the real-time equilibration of the reduced fluids with mound mineralogy due to the very young age (<2 years) venting from Spire vent. The presence of aqueous organic compounds therefore affects not only the inorganic chemical speciation in vent fluids, but can also control the mineralogy of associated sulfide deposits. These results also indicate that vent fluid compositions do not necessarily reflect conditions in the deep subsurface, but can be altered by reactions occurring in the shallow subsurface.