Regional patterns of soil organic carbon stocks in China

被引:167
作者
Yu, D. S. [1 ]
Shi, X. Z.
Wang, Ht
Sun, W. X.
Chen, J. M.
Liu, Q. H.
Zhao, Y. C.
机构
[1] Chinese Acad Sci, Inst Soil Sci, State Key Lab Soil & Sustainable Agr, Nanjing 210008, Peoples R China
[2] Univ Toronto, Dept Geog, Toronto, ON M5S 3G3, Canada
关键词
soil organic carbon stock; 1 : 1,000,000 soil database of China;
D O I
10.1016/j.jenvman.2006.09.020
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Soil organic carbon (SOC) is of great importance in the global carbon cycle. Distribution patterns of SOC in various regions of China constitute a nation-wide baseline for studies on soil carbon changes. This paper presents an integrated and multi-level study on SOC stock patterns of China, and presents baseline SOC stock estimates by great administrative regions, river watersheds, soil type regions and ecosystem. The assignment is done by means of a recently completed 1: 1,000,000 scale soil database of China, which is the most detailed and reliable one in China at the present time. SOC densities of 7292 soil profiles collected across China in the middle of the 1980s were calculated and then linked to corresponding polygons in a digital soil map, resulting in a SOC Density Map of China on a 1: 1,000,000 scale, and a 1 km x 1 km grid map. Corresponding maps of administrative regions, river watersheds, soil types (ST), and ecosystems in China were also prepared with an identical resolution and coordinate control points, allowing GIS analyses. Results show that soils in China cover an area of 9.281 x 10(6) km(2) in total, with a total SOC stock of 89.14 Pg (1 Pg = 10(15) g) and a mean SOC density of 96.0 t C/ha. Confidence limits of the SOC stock and density in China are estimated as [89.23 Pg, 89.08 Pg] and [96.143 t C/ha, 95.981 t C/ha] at 95% probability, respectively. The largest total SOC stock (23.60 Pg) is found in South-west China while the highest mean SOC density (181.9 t C/ha) is found in north-east China. The total SOC stock and the mean SOC density in the Yangtze river watershed are 21.05 Pg and 120.0 t C/ha, respectively, while the corresponding figures in theYellow river watershed are 8.46 Pg and 104.3 t C/ha, respectively. The highest total SOC stocks are found in Inceptisols (34.39 Pg) with SOC density of 102.8 t C/ha. The lowest and highest mean SOC densities are found on Entisols (28.1 t C/ha), and on Histosols (994.728.1 t C/ha), repectively. Finally, the total SOC stock in shrub and forest ecosystem classes are 25.55 and 21.50 Pg, respectively; the highest mean SOC density (209.9 t C/ha) was recorded in the wetland ecosystem class and the lowest (29.0 t C/ha) in the desert ecosystem class. Among five forest ecosystem types, Evergreen conifer forest stores the highest SOC stock (6.81 Pg), and Deciduous conifer forest shows the highest SOC density (225.9 t C/ha). Figures of SOC stocks stratified by Administrative regions, river watersheds, soil types and ecosystem types presented in the study may constitute national-wide baseline for studies of SOC stock changes in various regions in the future. (C) 2006 Elsevier Ltd. All rights reserved.
引用
收藏
页码:680 / 689
页数:10
相关论文
共 40 条
[1]  
[Anonymous], GEOGR RES, DOI [10.11821/yj1999040003, DOI 10.3321/J.ISSN:1000-0585.1999.04.003]
[2]   The carbon content of topsoil and its geographical distribution in France [J].
Arrouays, D ;
Deslais, W ;
Badeau, V .
SOIL USE AND MANAGEMENT, 2001, 17 (01) :7-11
[3]   Carbon and nitrogen stocks in the soils of Central and Eastern Europe [J].
Batjes, NH .
SOIL USE AND MANAGEMENT, 2002, 18 (04) :324-329
[4]  
Batjes NH, 1996, EUR J SOIL SCI, V47, P151, DOI [10.1111/j.1365-2389.1996.tb01386.x, 10.1111/ejss.12114_2]
[5]   ESTIMATE OF ORGANIC-CARBON IN WORLD SOILS .2. [J].
BOHN, HL .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1982, 46 (05) :1118-1119
[6]  
Bolin B., 2000, Land use, land-use change and forestry eds, P23
[7]  
Buringh P, 1984, ROLE TERRESTRIAL VEG, V3, P91
[8]  
Cheng XF, 2004, PEDOSPHERE, V14, P425
[9]   ORGANIC-CARBON IN SOILS OF THE WORLD [J].
ESWARAN, H ;
VANDENBERG, E ;
REICH, P .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1993, 57 (01) :192-194
[10]  
Fang J, 1996, STUDY KEY ISSUES MOD, P251