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Diane McKnight, Matt Miller, Rose Cory and Mark Williams
Coupling of carbon and nitrogen cycles through humic redox reactions in an alpine stream Diane McKnight, Matt Miller, Rose Cory and Mark Williams Depart. Civil, Environmental & Architectural Engineering, University of Colorado
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NWTLTER: C & N transport and reactivity in Green Lakes Valley
Response of pristine, cold regions to climate change and N enrichment
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Hyporheic Zone: “hotspot” of biogeochemical reactions driven by mixing across redox gradient
Stream h2o mixes with groundwater and returns to the stream
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Redox Couples Oxidizing Conditions O2 H2O NO3- N2, NH4+ Mn(IV) Mn(II)
Fe(III) Fe(II) Oxidized Humics Reduced Humics SO H2S Reducing Conditions
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DOM reducing microorganism
CO2 Acetate Oxidized DOM DOM reducing microorganism Reduced DOM Photoreduction of Ferric to Ferrous Iron e- e- Humics act as electron shuttle Fe3+ Fe2+ NO2- + DOM DOM-N Ferrous Wheel Hypothesis NO3-
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Tracer experiment: Navajo Meadow Stream *formed by snowmelt
*elevation~3,750m *formed by snowmelt and glacial runoff *surrounded by alpine wetland *~150m in length
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Approach: Tracer injection experiment and modeling with OTIS
Main Channel: Lateral inflow Advection Dispersion Transient storage Storage Zone: Transient storage s
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Humic Peaks: (quinone moieties) Protein Peak
Approach: Fluorescence index 370 nm Ex, and EEM’s (Excitation and emission over a range of wavelengths) Excitation (nm) Emission (nm) Humic Peaks: (quinone moieties) Protein Peak
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PARAFAC Excitation-emission matrix (EEM) Comp Comp Comp. 3
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“HQ” “Q” Quinones found in enzymes, e.g ubiquinone, and formed by lignin oxidation. Forms of this complex are found throughout cells Important in electron transfer reactions, such as the oxidation of NADH Also known as coenzyme Q Ubiquinone
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Quinone fluorescence AQDS/AHDS useful as models for humic fluorescence
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Stream Br- Addition, July 10
Background [Br-] = 0 mg/L Reach 1 Reach 2 Reach 3
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Storage Zone Br- Simulation
Reach 1 Reach2 Reach 3 0.1 mg/L 0.1 mg/L
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Connectivity of wells Br, Ca, del 18O & D on July 10
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Stream Chemistry July 10th July 17th July 24th DOC LF FI SR SUVA
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Stream-Well Comparisons
B A A A A,B B A,B A B B A A A FI Well 1 = No and Low Br, Well 2 = High Br
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Stream Site EEMs S1 S2 S3 July 10th (tracer) July 17th July 24th
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Well Site EEMs Characteristic Humic Peaks Protein Peaks July 10th, V13
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PARAFAC Components Red-shifted: C2 (HQ1), C3 (HQ2)
Blue-shifted: C5 (Q) Protein: C9 2 5
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Ex, Em spectra for HQ1 and HQ2
Note: similar excitation spectra
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Comparison of HQ1 and AHDS
Em and Ex spectra: Same ex. max and shape. Emission max are different, probably related to H bonding, solvent, excited state rxns
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Comparison of Q and AQDS
Very similar ex and em max (ex 260 nm; em max at 418 nm). Similar features of spectra, Q has broader peaks as typical for humics
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Stream-Well Comparisons
B C A A Well 1 = No and Low Br Well 2 = High Br F = (Σ HQ1, HQ2) / (Q)
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Two Components Explain Fluorescence Index
Matt’s data appears on click!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!
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DOM reducing microorganism
CO2 Acetate Oxidized DOM DOM reducing microorganism Reduced DOM Photoreduction of Ferric to Ferrous Iron e- e- Humics act as electron shuttle Fe3+ Fe2+ NO2- + DOM DOM-N Ferrous Wheel Hypothesis NO3-
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Ferrous Wheel: Addition of Ferric Nitrate to reduced DOM samples with high ferrous iron concentrations, causes decrease in ferrous due to nitrate reduction. NOTE: Addition of Ferric Citrate causes ferrous iron to INCREASE.
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Hyporheic zone interactions, e. g. humic redox
Hyporheic zone interactions, e.g. humic redox!!, hotspot of C & N interactions, influencing N transport in alpine systems. Fluorescence index = HQ1/HQ2 FI increases with microbial sources (primary and secondary) Nitrogen and Carbon cycling coupled by biotic and chemical processes
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Questions?
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Ferrous Wheel Results: Added Ferric Nitrate to Samples with high ferrous iron concentrations.. NOTE: get different results when ferric citrate added, in that case ferrous iron INCREASES.
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