Effect of land use on organic carbon storage in soils in eastern China

被引:36
作者
Cai, ZC
机构
[1] Institute of Soil Science, Chinese Academy of Sciences
关键词
organic carbon; land use; eastern China;
D O I
10.1007/BF00666272
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The change of land from natural vegetation to agricultural use causes the loss of organic carbon stored in soils and is considered as an important contributor of CO2 to the atmosphere. Four types of land use were defined in the study as: 1) natural vegetation fields (NF); 2) fuel forest, fruit tree orchards and wasteland near residential areas (FF); 3) upland crop fields (UF) and 4) paddy fields (PF). For a large area in eastern China, 416 soil species cited in the book ''Soil Species of China-Volume One'' were placed in one of the four use categories. Statistical results showed that organic carbon density in soil profiles 0 to 62.3 cm ranged from 3.87 to 14.25 kg m(-2). Relative to NF, the loss of organic carbon in soils was correlated with human impact but varied with the type of human use. The total loss in the studied area was estimated to be 1.646 GtC. Although organic carbon in paddy soils was also significantly less than that in NE the mean carbon density in the profile 0 to 62.3 cm was 68.1% higher than that in UF and 23.6% higher than that in FF. Therefore, flooded rice is the preferred land use type with respect to the storage of organic carbon in heavily impacted soils. On the other hand, other ecological values, e.g., biodiversity, are also affected by land use type and any change in land use should be preceded by a comprehensive review of objectives and ecological impacts.
引用
收藏
页码:383 / 393
页数:11
相关论文
共 21 条
[1]   AGGREGATE-PROTECTED AND UNPROTECTED ORGANIC-MATTER POOLS IN CONVENTIONAL-TILLAGE AND NO-TILLAGE SOILS [J].
BEARE, MH ;
CABRERA, ML ;
HENDRIX, PF ;
COLEMAN, DC .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1994, 58 (03) :787-795
[2]  
BOUWMAN AF, 1990, SOILS AND THE GREENHOUSE EFFECT, P61
[3]   CHANGES IN SOIL PROPERTIES IN A CENTRAL PLAINS RANGELAND SOIL AFTER 3, 20, AND 60 YEARS OF CULTIVATION [J].
BOWMAN, RA ;
REEDER, JD ;
LOBER, RW .
SOIL SCIENCE, 1990, 150 (06) :851-857
[4]  
Commission of Agricultural Chemistry Soil Science Society of China, 1983, ROUT AN METH SOILS A, P67
[5]  
*DIV AGR HUN PROV, 1989, SOILS HUN PROV CHIN, P280
[6]  
*DIV LAND MAN JIAG, 1991, RED SOILS JIANGX PRO
[7]  
DONG YH, 1991, J NANJING FORESTRY U, V15, P33
[8]   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
[9]   CROP-ROTATION AND TILLAGE EFFECTS ON SOIL ORGANIC-CARBON AND NITROGEN [J].
HAVLIN, JL ;
KISSEL, DE ;
MADDUX, LD ;
CLAASSEN, MM ;
LONG, JH .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1990, 54 (02) :448-452
[10]  
*IPCC, 1992, CLIM CHANG S REP IPC