The biogeochemical processes controlling the speciation
and transport of manganese in a Colorado mountain streamwere studied using a conservative tracer approachcombined with laboratory experiments. The study stream,Lake Fork Creek, receives manganese-rich inflows froma wetl
and contaminated by acid mine drainage. A conservativetracer experiment was conducted on a 1300-m reach ofthe stream. Results indicate that manganese was progressivelyremoved from the stream, resulting in a loss of 64 ± 17
![](/images/entities/mgr.gif)
mol day
-1 m
-1. Laboratory experiments using streamwater,mine effluent,
and rocks from the stream showed theimportance of surface-catalyzed oxidation
and photoreductionon the speciation of manganese. The field
and modelingresults indicate that light generally promotes oxidation
andremoval of manganese from the stream, presumablythrough a photosynthetically enhanced oxidation process.Differences in Mn speciation within the stream suggestthat reductive processes affect Mn speciation within thewater column. These results identify the rapid oxidation
andprecipitation of MnO
x as a dominant process within thisfreshwater stream.