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Tracer Approaches

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Demonstrate process on short time scale. Perturbation of system ... Atom Percent Excess = APE, A%E = Measured ratio natural abundance. 15NH4. 14NH4. PO15N ... – PowerPoint PPT presentation

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Title: Tracer Approaches


1
Tracer 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

2
N 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

3
Tracer Terminology
  • Atom Percent Excess APE, AE
  • Measured ratio natural abundance

4
Two Fundamental Approaches
Direct Tracer uptake of NH4
Isotope Dilution (NH4 regeneration)
Spike
15NH4 14NH4
PO15N
PON (0.366 atm )
Enriched (5-25)
5
Calculations 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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N 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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Isotope 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)

13
2 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
14
Nitrification
15
Methods
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Spike
Direct Tracer uptake of NO3
Isotope Dilution (Nitrification NH4 ox)
15NO3 14NO3
PO15N
NH4 (0.366 atm )
Enriched (5-25)
17
Nitrification Rates
Oceanic nitrification should roughly balance new
production based on NO3- Range 500 (Eppley)-
2500 (Falkowski) Tg
18
Nitrification (cont)
19
Denitrification, Nitrate Reduction (dissimilatory)
20
Denitrification (cont)
21
Methods
  • 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

22
Rates of Denitrification
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Nitrification-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
24
Calculations
  • 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

25
MIMS- N2/Ar ratios
  • Changes in N2 relative to Ar
  • Traditionally w/ GC
  • High precision with mass spec
  • Quadrupole or isotope ratio mass spec
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