Title: Tracer Approaches
1Tracer Approaches
- Natural Abundance
- Integrative over large time and space scales
- Requires much inference creative minds
- Tracer-
- Direct approach
- Demonstrate process on short time scale
- Perturbation of system potential artifact
- e.g. bottle effects, enzyme kinetics
2N Tracers
- Radioisotopes
- 13N - positron decay, high specific activity
- 10 min half-life
- Proton bombardment of H20 cyclotron
- Limited use
- Stable isotopes
- 15N available in enriched (and depleted)
forms - Emission or mass spectrometry
- Used widely in ecology, oceanography
3Tracer Terminology
- Atom Percent Excess APE, AE
- Measured ratio natural abundance
4Two Fundamental Approaches
Direct Tracer uptake of NH4
Isotope Dilution (NH4 regeneration)
Spike
15NH4 14NH4
PO15N
PON (0.366 atm )
Enriched (5-25)
5Calculations direct uptake
- v (t-1) (atomexcessproduct)tn
-
atomexsubstrate tn - fractional uptake/ unit time
- ? (umol N(L h)-1 v PN (umol NL-1)
- volume-normalized rate of mass uptake
N uptake (umol/t) AEproduct x
PNsample(umol) AEsubstrate
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10N Regeneration
- Ammonification DON/PON -gt NH4
- hydrolytic deamination
- Amino Acid oxidation aa -gt NH4
- recent, cell surface enzymes
- Protein, peptide hydrolysis -gt aas
- Redfield Model
- Stoichiometry of regeneration
- CN demand vs. CN of regeneration availability
- Bacterial/ Algal CN demand lt 101
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12Isotope Dilution Model
- 1. Measure change in concentration
- dNH4 NH4t NH40 P- I
Production - Incorp - dt t (Net flux)
- or
- NH4t NH40 (P-I)t
Slope (P-I)
132 Measure change in isotopic ratio of
pool Where R 15N ratio _at_ t0 ( 0.1), 15n
0.00366 d15NH4 P(15n) IR dt d14NH4
P(1-15n) I(1-R) dt dR (15n-R)P dt
NH40 ln (Rt 15n) ln (Ro 15n)
P/(P-I) ln NH4_at_t Slope
P/(P-I) NH4_at_0
14Nitrification
15Methods
16Spike
Direct Tracer uptake of NO3
Isotope Dilution (Nitrification NH4 ox)
15NO3 14NO3
PO15N
NH4 (0.366 atm )
Enriched (5-25)
17Nitrification Rates
Oceanic nitrification should roughly balance new
production based on NO3- Range 500 (Eppley)-
2500 (Falkowski) Tg
18Nitrification (cont)
19Denitrification, Nitrate Reduction (dissimilatory)
20Denitrification (cont)
21Methods
- Direct N2 gas flux - (difficult,N2 contamination)
- C2H2 blockage method
- C2H2
- NO3 -gt NO2 -gt NO -gt N2O --gt N2
- Direct tracer 15NO3 or 15NO2 --gt 15N2
- Natural abundance ?15N of residual NO3 increased
- N2/ Ar ratios
- Immunofluorescence
- Gene probes
22Rates of Denitrification
23Nitrification-Denitrification Coupling
- Sediment denitrification- two sources
- NO3 diffusion in
- In situ nitrification (i.e. NO3 production)
- NH4 ---gt NO3 -gt -gt N2
- Isotope Pairing (Nielsen et al.,
- Spike with 15NO3, measure 28N, 29N, 30N
Exogenous
24Calculations
- D15 (14N15N) 2(15N15N)
- D14 (14N15N) D15
- 2(15N15N)
- Dt D14 D15
- Dw D15/ e where e 15N labelled fraction
of effluent NO3 - Dn (D14 D15) - Dw
25MIMS- N2/Ar ratios
- Changes in N2 relative to Ar
- Traditionally w/ GC
- High precision with mass spec
- Quadrupole or isotope ratio mass spec