SOCRATES - A simple model for predicting long-term changes in soil organic carbon in terrestrial ecosystems

被引:56
作者
Grace, Peter R. [1 ]
Ladd, Jeffrey N.
Robertson, G. Philip
Gage, Stuart H.
机构
[1] Queensland Univ Technol, Sch Nat Resources Sci, Brisbane, Qld 4060, Australia
[2] Michigan State Univ, Wk Kellogg Biol Stn, Hickory Corners, MI 49060 USA
[3] Michigan State Univ, Dept Crop & Soil Sci, E Lansing, MI 48824 USA
[4] Michigan State Univ, Dept Entomol & Computat Ecol, E Lansing, MI 48824 USA
[5] Michigan State Univ, Visualizat Lab, E Lansing, MI 48824 USA
关键词
soil organic carbon; simulation; SOCRATES;
D O I
10.1016/j.soilbio.2005.09.013
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The maintenance of soil organic carbon (SOC) in terrestrial ecosystems is critical for long-term productivity. Simulation models of SOC dynamics are valuable tools in predicting the impacts of climate on carbon storage and developing management strategies for the mitigation of Greenhouse gas emissions, however, their utility is Generally reduced due to need for specific data. The SOCRATES model is a simple process based representation of soil SOC dynamics in terrestrial ecosystems, which requires minimal data inputs and specifically designed to examine the impact of land use and land use change on soil carbon storage. SOCRATES was successful in predicting SOC change at eighteen long-term crop, pasture and forestry trials from North America, Europe and Australasia. These trials ranged from 8 to 86 years in duration, over a wide range of climates and soil types with annual changes in SOC ranging from -3.0 to 4.2%. (c) 2005 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1172 / 1176
页数:5
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