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Seasonal Temperature Oscillations Drive Contrasting Arsenic and Antimony Mobilization in a Mining‐Impacted River System
Author(s) -
Johnston Scott G.,
Karimian Niloofar,
Burton Edward D.
Publication year - 2020
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1029/2020wr028196
Subject(s) - diel vertical migration , benthic zone , environmental chemistry , hyporheic zone , redox , sediment , respiration , environmental science , chemistry , ecology , geology , inorganic chemistry , biology , paleontology , botany
Arsenic (As) and antimony (Sb) speciation and mobility in river systems can be influenced by the redox conditions of benthic and hyporheic zone sediments. However, our understanding of how temperature fluctuations influence riverine As and Sb mobility over diel and seasonal time frames, via moderation of sediment redox conditions, is poorly constrained. Here we compare diel and seasonal water quality data from a river system contaminated with As and Sb with results from sediment‐water incubations conducted at temperatures spanning 8°C to 32°C under low‐dissolved oxygen conditions. Higher incubation temperatures caused faster microbial respiration, lower redox potential, and greater As aq concentrations, coincident with reduction of As(V), Mn (III/IV), Fe (III), and SO 4 2− . Initial rates of As 3+ aq formation increased exponentially with temperature ( Q 10 = 3.3 ± 0.5) and were positively correlated with microbial respiration ( r 2 = 0.99, P < 0.01). In contrast, Sb aq displayed an initially negative and comparatively weak overall temperature dependence during incubations. In river waters, diel mobilization of reduced species (As 3+ aq and Fe 2+ aq ) and contrasting attenuation of Sb was coincident with lower redox potential during nightly respiration cycles. Distinct seasonal oscillations in river water As aq were exponentially correlated with temperature ( r 2 = 0.68, P < 0.01), whereas Sb aq was not. These characteristics reflect the fundamental role of anaerobic metabolism (as influenced by temperature) within benthic and hyporheic zone sediments as a key driver of contrasting riverine As and Sb mobility. The findings imply that riverine As mobility may be enhanced, while Sb mobility possibly attenuated, by eutrophication or by elevated stream temperatures due to a warming climate.