Simulated soil organic matter dynamics in forests of the Leningrad administrative area, northwestern Russia

Abstract The assessment of carbon balance in forest soils of the Leningrad administrative area (south boreal sub-zone of east European plain) has been carried out using: (1) previous data on carbon pools of forest soils without considering mires area as initial data (organic layer plus 50 cm soil); (2) inventory data on forest stands that has been converted into biomass and data on litter input; (3) meteorological data concerning the mean monthly air temperature and precipitation. The most recent model version of soil organic matter (SOMM) dynamics was applied for a 100-year simulation of carbon dynamics in the 3.22×106 ha of forest soils of the Leningrad area considering a constant forest-age structure and climate. The results demonstrate unique carbon dynamics in various soils, and an 8% increase of the total carbon pool of the area’s forest soils during the 100-year simulation (from 266 to 286 million tons of carbon). The total carbon input to the soil, in the form of litter carbon, was 8.3 million tons annually, and the carbon emission, in the form of carbon dioxide released from the soils, was 8.1 million tons annually at the end of simulation.

[1]  S. Nilsson,et al.  Soil Carbon Estimates and Soil Carbon Map for Russia , 1996 .

[2]  A. Mäkelä,et al.  Model analysis of the effects of soil age, fires and harvesting on the carbon storage of boreal forest soils , 1998 .

[3]  D. Howard,et al.  Carbon storage in forest soils , 1995 .

[4]  H. N. Chappell,et al.  Soil organic carbon in a mountainous, forested region : relation to site characteristics , 1995 .

[5]  Anthony W. King,et al.  Soil Organic Matter Models and Global Estimates of Soil Organic Carbon , 1996 .

[6]  H. Bossel,et al.  Simulation of forest stand dynamics, using real-structure process models , 1991 .

[7]  M. Cannell,et al.  Carbon pools and sequestration in forest ecosystems in Britain , 1995 .

[8]  O. Chertov,et al.  The simulation of soil organic matter and nitrogen accumulation in Scots pine plantations on bare parent material using the combined forest model EFIMOD , 1999, Plant and Soil.

[9]  Raisa Mäkipää,et al.  Scenarios for the carbon balance of Finnish forests and wood products , 1999 .

[10]  R. Lal Soil Management and Greenhouse Effect , 1995 .

[11]  Andrew D. Friend,et al.  A process-based, terrestrial biosphere model of ecosystem dynamics (Hybrid v3.0) , 1997 .

[12]  P. Duchaufour Précis de pédologie , 1960 .

[13]  G. Nabuurs,et al.  Carbon sequestration in the forest sector under climate change: upscaling from the plot level to the European forests level , 1997 .

[14]  David S. Powlson,et al.  Evaluation of Soil Organic Matter Models , 1996 .

[15]  B. A. Stewart,et al.  Advances in Soil Science , 1986, Advances in Soil Science.

[16]  T. Karjalainen Model Computations on Sequestration of Carbon in Managed Forests and Wood Products under Changing Climatic Conditions in Finland , 1996 .

[17]  O. G. Čertov Ecology of forest lands. , 1981 .

[18]  O. Chertov,et al.  SOMM: A model of soil organic matter dynamics , 1997 .

[19]  R. Birdsey,et al.  Carbon storage in forests and peatlands of Russia , 1998 .

[20]  Naohiro Goto,et al.  Modelling of soil carbon dynamics as a part of carbon cycle in terrestrial ecosystems , 1994 .

[21]  P. Grace,et al.  Simulating trends of soil organic carbon in seven long-term experiments using the SOMM model of the humus types , 1997 .

[22]  Leif T. Jensen,et al.  A comparison of the performance of nine soil organic matter models using datasets from seven long-term experiments , 1997 .

[23]  W. Parton Ecosystem model comparisons: science or fantasy world? , 1996 .