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Effects of climate change on decomposition in Arctic Tussock Tundra: A modeling synthesis

Conference · · Bulletin of the Ecological Society of America; (United States)
OSTI ID:6043468
 [1];  [2]
  1. Texas Tech Univ., Lubbock (United States)
  2. Duke Univ., Durham, NC (United States)
A model of litter decomposition was used to examine the potential effects of climate change on the decay of dead organic matter in a tussock tundra soil of northern Alaska, USA. Under current conditions (714% mean soil water content, 4.5[degrees]C mean soil temperature, 93-d season length), the model estimated a net release of 5.28g N[times]m[sup [minus]2][times]yr[sup [minus]1] and 79.5g CO[sub 2]-C[times]m[sup [minus]2][times]yr[sup [minus]1] from soil organic matter, respectively. These values are consistent with observations from field and laboratory studies of decomposition and plant growth. With changing climate, the greatest increase in net N release from dead organic matter (199% of current value), occurred at 600% soil moisture, 140-d season and 8.5[degrees]C mean summer temperature. The least amount of N was immobilized (46% of current value) at the present temperature, 70-d season and 1000% soil moisture content. Season length had little affect on the size of the mineral N pool, although pool size does respond to temperature and soil moisture content; ranging from 12-25 mg N[times]m[sup [minus]2]. Model results also indicate that patterns of net C and N mineralization need not be similar. Net C mineralization, estimated as cumulative CO[sub 2] efflux, is roughly proportional to total C transfer through the decomposer community. However, net N mineralization is not as closely related to mineral N pool size because of the high immobilization potential of tussock tundra soils.
OSTI ID:
6043468
Report Number(s):
CONF-930798--
Conference Information:
Journal Name: Bulletin of the Ecological Society of America; (United States) Journal Volume: 74:2
Country of Publication:
United States
Language:
English

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