Sensitivity analysis of predicted change in soil carbon following afforestation

被引:57
作者
Paul, KI
Polglase, PJ
Richards, GP
机构
[1] CSIRO, Forestry & Forest Prod, Kingston, ACT 2604, Australia
[2] Australian Greenhouse Off, Natl Carbon Accounting Syst, Canberra, ACT 2601, Australia
关键词
afforestation; reforestation; sequestration; 3PG; GENDEC; RothC; FullCAM;
D O I
10.1016/S0304-3800(03)00027-9
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
A credible and cost-effective methodology is needed to support the use of new tree plantations to offset greenhouse gas emissions, and ultimately to form part of an emissions trading scheme. A number of validated models of forest growth are available. However, there has been relatively little validation of models to predict changes in pools of C in litter and soil, and thus suitable for C accounting. A modelling approach is needed to track changes in soil C because direct measurements are currently cost-prohibitive. Modelling approaches also allow for scenario analyses that can be useful for planning purposes. We used a complete C accounting model for forests, GRC3, to simulate patterns of change in soil C following afforestation under four test cases representing typical conditions in Australia. Soil C was predicted to initially decrease (usually during the first 10 years) before a gradual recovery and accumulation of soil C occurred. Sensitivity analyses were used to determine which parameters and inputs potentially. cause the greatest uncertainty in calculated change in soil C using GRC3. Taking into account the uncertainties in the values of parameters and inputs, initial (0-10 years) decrease in soil C was predicted to be 0.96-2.35% per year (or 4.16-14.8 t C ha(-1)) with a standard deviation between 0.10 and 0.43% per year among case studies, whereas the predicted increase in soil C (10-40 years) was predicted to be between 0.49 and 1.80% per year (or 7.57-24.4 t C ha(-1)) with a standard deviation between 0.18 and 0.69% per year. Results indicated that uncertainty could be greatly reduced by calibration of the fraction of above-ground litter transferred to soil C (i.e. humification), fraction of C lost by respiration during decomposition of litter, dead roots and soil C, and decomposition rates of the soil C pools. It was also important to obtain accurate input data for initial soil C content (including inert soil C), climatic conditions and allocation of net primary production to various tree components. (C) 2003 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:137 / 152
页数:16
相关论文
共 25 条
[1]  
[Anonymous], 1990, PHILOS T R SOC B, DOI DOI 10.1098/rstb.1990.0177
[2]  
[Anonymous], 22 NCAS AUSTR GREENH
[3]  
Bashkin MA, 1998, ECOLOGY, V79, P828, DOI 10.1890/0012-9658(1998)079[0828:CISCFA]2.0.CO
[4]  
2
[5]   Carbon accounting model for forests in Australia [J].
Brack, CL ;
Richards, GP .
ENVIRONMENTAL POLLUTION, 2002, 116 :S187-S194
[6]   Assessing forest productivity in Australia and New Zealand using a physiologically-based model driven with averaged monthly weather data and satellite-derived estimates of canopy photosynthetic capacity [J].
Coops, NC ;
Waring, RH ;
Landsberg, JJ .
FOREST ECOLOGY AND MANAGEMENT, 1998, 104 (1-3) :113-127
[7]  
GIFFORD R, 2000, 7 NCAS AUSTR GREENH
[8]  
HEATH LS, 2000, ENVIRON SCI POLICY, V3, P73, DOI DOI 10.1016/S1462-9011(00)00075-7
[9]  
HENDERSON GS, 1995, CARBON FORMS AND FUNCTIONS IN FOREST SOILS, P419
[10]  
Jenkinson DS., 1987, INTECOL Bull, V15, P1