Carbon storage in China's forest ecosystems: estimation by different integrative methods

被引:25
|
作者
Peng, Shunlei [1 ,2 ]
Wen, Ding [1 ]
He, Nianpeng [1 ]
Yu, Guirui [1 ]
Ma, Anna [1 ]
Wang, Qiufeng [1 ]
机构
[1] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Beijing 100101, Peoples R China
[2] Pingdingshan Univ, Key Lab Ecol Restorat Hilly Area, Pingdingshan 467000, Henan Province, Peoples R China
来源
ECOLOGY AND EVOLUTION | 2016年 / 6卷 / 10期
基金
中国国家自然科学基金;
关键词
Carbon storage; coefficient variation; forest type classification; multimethodology; spatial interpolation; uncertain; SOIL ORGANIC-CARBON; TERRESTRIAL ECOSYSTEMS; ABOVEGROUND BIOMASS; GREEN PROGRAM; PATTERNS; STOCKS; SEQUESTRATION; GEOSTATISTICS; VEGETATION; CLIMATE;
D O I
10.1002/ece3.2114
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Carbon (C) storage for all the components, especially dead mass and soil organic carbon, was rarely reported and remained uncertainty in China's forest ecosystems. This study used field-measured data published between 2004 and 2014 to estimate C storage by three forest type classifications and three spatial interpolations and assessed the uncertainty in C storage resulting from different integrative methods in China's forest ecosystems. The results showed that C storage in China's forest ecosystems ranged from 30.99 to 34.96 Pg C by the six integrative methods. We detected 5.0% variation (coefficient of variation, CV, %) among the six methods, which was influenced mainly by soil C estimates. Soil C density and storage in the 0-100 cm soil layer were estimated to be 136.11-153.16 Mg C.ha(-1) and 20.63-23.21 Pg C, respectively. Dead mass C density and storage were estimated to be 3.66-5.41 Mg C.ha(-1) and 0.68-0.82 Pg C, respectively. Mean C storage in China's forest ecosystems estimated by the six integrative methods was 8.557 Pg C (25.8%) for aboveground biomass, 1.950 Pg C (5.9%) for belowground biomass, 0.697 Pg C (2.1%) for dead mass, and 21.958 Pg C (66.2%) for soil organic C in the 0-100 cm soil layer. The R:S ratio was 0.23, and C storage in the soil was 2.1 times greater than in the vegetation. Carbon storage estimates with respect to forest type classification (38 forest subtypes) were closer to the average value than those calculated using the spatial interpolation methods. Variance among different methods and data sources may partially explain the high uncertainty of C storage detected by different studies. This study demonstrates the importance of using multimethodological approaches to estimate C storage accurately in the large-scale forest ecosystems.
引用
收藏
页码:3129 / 3145
页数:17
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