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Serreze et al, 2000 Climatic Change

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Soil Organic Matter. C:N 15:1. Nitrogen inputs. Nitrogen outputs. Plants. C:N 30:1. NPP. Soil Respiration ... Major means of N removal from soil to atmosphere ... – PowerPoint PPT presentation

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Title: Serreze et al, 2000 Climatic Change


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Serreze et al, 2000 Climatic Change
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Arctic tundra C/N model
Shaver et al, 1992 Bioscience
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Denitrification
  • Microbial-mediated, anaerobic N reduction from
    NO3- to N2O and N2
  • Major means of N removal from soil to atmosphere
  • Once thought unimportant in arctic ecosystems,
    but with effects of climate change could be a
    significant N loss pathway

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How does this N loss pathway contribute to
the amount of missing N? Do
denitrification rates differ between site and
with experimental fertilization?
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Denitrification Assays
  • Two measurements using acetylene block
  • Denitrification enzyme activity (DEA) - NO3-,
    Dextrose
  • Unamended denitrification rates - DI

Make systems anoxic Add acetylene (C2H2)
Incubate at room temperature on a shaker table
in the dark Collect air samples at 30, 60 and
90 minute time points N2O analysis on GC
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An Upper Bound Estimate
Assume - A denitrification rate of 0.1 µg Ng
soil-1h-1 in fertilized plots Unamended CT,
Moist Acidic Tundra - Bulk density 0.06 g/cm3,
depth of denitrification activity 10cm - 100
day growing season ? This represents a
loss of 1.44 g Nm-2y-1 The annual vegetation N
uptake requirement is lt1 g
Nm-2y-1 ? Denitrification may have
considerable effects on N availability in
these systems.
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