A series of laboratory experiments were conducted to examine how partitioning of Fe among solid reaction products and rates of H sub(2) generation vary as a function of temperature during ...serpentinization of olivine. Individual experiments were conducted at temperatures ranging from 200 to 320 degree C, with reaction times spanning a few days to over a year. The extent of reaction ranged from <1% to similar to 23%. Inferred rates for serpentinization of olivine during the experiments were 50-80 times slower than older studies had reported but are consistent with more recent results, indicating that serpentinization may proceed more slowly than previously thought. Reaction products were dominated by chrysotile, brucite, and magnetite, with minor amounts of magnesite, dolomite, and iowaite. The chrysotile contained only small amounts of Fe (X sub(Fe) = 0.03-0.05, with similar to 25% present as ferric Fe in octahedral sites), and displayed little variation in composition with reaction temperature. Conversely, the Fe contents of brucite (X sub(Fe) = 0.01-0.09) increased steadily with decreasing reaction temperature. Analysis of the reaction products indicated that the stoichiometry of the serpentinization reactions varied with temperature, but remained constant with increasing reaction progress at a given temperature. The observed distribution of Fe among the reaction products does not appear to be entirely consistent with existing equilibrium models of Fe partitioning during serpentinization, suggesting improved models that include kinetic factors or multiple reaction steps need to be developed. Rates of H sub(2) generation increased steeply from 200 to 300 degree C, but dropped off at higher temperatures. This trend in H sub(2) generation rates is attributable to a combination of the overall rate of serpentinization reactions and increased partitioning of Fe into brucite rather than magnetite at lower temperatures. The results suggest that millimolal concentration of H sub(2) could be attained in moderately hot hydrothermal systems like Lost City during fluid circulation on timescales of a few years.
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