Premium
Activities of 223 Ra and 226 Ra in Fluids From the Lost City Hydrothermal Field Require Short Fluid Residence Times
Author(s) -
Moore W. S.,
Frankle J. D.,
BenitezNelson C. R.,
FrühGreen G. L.,
Lang S. Q.
Publication year - 2021
Publication title -
journal of geophysical research: oceans
Language(s) - English
Resource type - Journals
eISSN - 2169-9291
pISSN - 2169-9275
DOI - 10.1029/2021jc017886
Subject(s) - hydrothermal circulation , basalt , seawater , geology , geochemistry , mantle (geology) , radium , mineralogy , residence time (fluid dynamics) , chemistry , radiochemistry , oceanography , seismology , geotechnical engineering
The residence time of fluids circulating through deep‐sea hydrothermal systems influences the extent of water‐rock reactions and the flux of major and minor elements to the ocean. While the fluid residence times in numerous basaltic and gabbroic systems have been determined, those of the less studied ultramafic systems are currently unknown. Fluids that interact with mantle rocks have fundamentally different chemistries and therefore have unique influences on seawater chemistry. In this first investigation of radium isotopes in a serpentinite‐hosted system, vent fluids were discovered to contain 10–100 times greater activities of 223 Ra (half‐life = 11.4 days) than observed in high‐temperature basalt‐hosted systems. The 223 Ra activities of 10–109 dpm L −1 produce 223 Ra/ 226 Ra activity ratios ranging from 9 to 109. These extremely high 223 Ra activities, which are accompanied by low activities of 226 Ra, place significant constraints on fluid residence times and the adsorption coefficient of radium between fluid and rock. Our data constrain the nondimensional retardation factor ( R ) to very low values between 1 and 4, reflecting the extent to which Ra is transported more slowly than fluids due to adsorption and other processes. These results suggest that the residence time of fluids in contact with serpentinite is less than 2 y and perhaps as low as 0.5 y. They are surprisingly similar to those of basalt‐hosted systems. Thus, fluids in hydrothermal systems share similar hydrogeological characteristics despite differences in rock types, underlying porosity, and heat sources, enabling larger‐scale models of hydrothermal biogeochemistry to be developed across systems.