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Sequential Reduction and Oxidation of Inorganic Nitrogen, Manganese, and Iron in Flooded Soil
Author(s) -
Patrick W. H.,
Jugsujinda A.
Publication year - 1992
Publication title -
soil science society of america journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.836
H-Index - 168
eISSN - 1435-0661
pISSN - 0361-5995
DOI - 10.2136/sssaj1992.03615995005600040011x
Subject(s) - redox , manganese , chemistry , nitrogen , reduction potential , electron acceptor , inorganic chemistry , photochemistry , organic chemistry
When a soil is flooded, the curtailment of O 2 diffusion into the soil causes the microorganisms decomposing organic matter to switch from O 2 to alternate electron acceptors. Three alternates utilized by facultative microorganisms when O 2 becomes depleted are NO ‐ 3 , Mn 4+ compounds, and Fe 3+ compounds. We studied the sequence of reduction of these three redox systems under controlled redox potential conditions. The redox potential of soil suspensions was changed stepwise in 50‐mV increments from oxidized to reduced conditions and from reduced to oxidized conditions and maintained at each new potential for 15 d, at which time NO ‐ 3 , NH + 4 , Mn 2+ , and Fe 2+ concentrations in the soil solution were analyzed. The results of this study showed that the oxidation and reduction of the three electron acceptors were sequential, with no overlap in the oxidation or reduction of the NO ‐ 3 and Mn systems and little overlap in oxidation and reduction of the Mn and Fe systems. In the oxidized‐to‐reduced experiment, the critical redox potential at which all of the NO ‐ 3 was reduced and Mn 2+ first appeared in the soil solution was approximately 200 mV. The critical redox potential at which Fe 2+ appeared was 100 mV. For all three redox systems, the critical redox potentials for the oxidized‐to‐reduced transition were approximately 50 mV lower than for the reduced‐to‐oxidized transition.