431-8 Enigma of Assessing Redox Properties of Humic Substances.

See more from this Division: SSSA Division: Soil Chemistry
See more from this Session: Symposium--Organic Molecule Interactions with Mineral Surfaces As Key Regulators of Soil Processes: I
Wednesday, November 5, 2014: 10:15 AM
Long Beach Convention Center, Room 203C
Share |

Sudipta Rakshit, 3500 John A. Merritt Blvd, Tennessee State University, Nashville, TN and Garrison Sposito, University of California-Berkeley, Berkeley, CA
Redox properties of humic substances (HS) are known to be linked with important biogeochemical processes in the environment which control nutrient cycling and contaminant fate.  Therefore, accurate measurement of redox properties of HS is important.  However, a consensus based on the available measurements methods of the redox properties of HS has not yet been reached.  In this study, we compared common redox property measurement methods of HS using anthraquinone-2,6-disulfonate (AQDS) as a model compound and standard Elliot soil humic acid (1S102H, ESHA), reference Pahokee peat (1R103H, PPHA), and Suwannee River natural organic matter (1R101N, SRNOM) as HS.  We found, among commonly used methods, that H2/Pd reduction method followed by incubation with ferric citrate (FeCit) reagent was incomplete, H2/Pd reduction method followed by incubation with potassium ferricyanide (K3Fe(CN)6) was insensitive, and reduction of either AQDS or HS by stannous chloride (SnCl2) followed by titration of excess stannous (Sn2+) by potassium dichromate (K2Cr2O7) was most accurate.  Our research will pave the way for future investigations on detailed characterizations of functional groups of HS responsible for oxidation/reduction reactions.

See more from this Division: SSSA Division: Soil Chemistry
See more from this Session: Symposium--Organic Molecule Interactions with Mineral Surfaces As Key Regulators of Soil Processes: I