首页 | 本学科首页   官方微博 | 高级检索  
     检索      

Soil Organic Carbon Loss under Different Slope Gradients in Loess Hilly Region
作者姓名:JIA  Songwei  HE  Xiubin  WEI  Fangqiang
作者单位:[1]Key Laboratory of Mountain Hazards and Surface Process, Chinese Academy of Sciences/Institute of Mountain Hazards and Environment, Chengdu 610041, Sichuan, China [2]Graduate University of Chinese Academy of Sciences, Beijing 100049, China
基金项目:Supported by the National Natural Science Foundation of China (90502007) and the National Basic Research Program of China (973 Program 2007CB407206)
摘    要:Based on field runoff plots observation and sample analysis, the effect of slope gradient on soil organic carbon loss was studied under natural rainfall conditions in loess hilly region. The results showed that with slope gradient increasing (from10° to 30°), the changing trend of soil erosion intensity (A) was A20°〉A30°〉A15°〉A10°〉A25°, suggesting that slope gradient between 20° and 25° was a critical degree ranger to exist. Soil organic carbon loss was mainly influenced by soil erosion intensity, appearing the same trend as did soil erosion intensity with increasing slope gradient. Soil erosion results in organic carbon enrichment in sediment. Average enrichment ratios of five runoff plots varied from 2.27 to 3.74, and decreased with increasing erosion intensity and slope gradient. The decrease of surface runoff and soil erosion is the key to reduce soil organic carbon loss.

关 键 词:土壤侵蚀  土壤有机碳流失  碳循环  坡度
文章编号:1007-1202(2007)04-0695-04
收稿时间:2 September 2006
修稿时间:2006-09-02

Soil organic carbon loss under different slope gradients in loess hilly region
JIA Songwei HE Xiubin WEI Fangqiang.Soil Organic Carbon Loss under Different Slope Gradients in Loess Hilly Region[J].Wuhan University Journal of Natural Sciences,2007,12(4):695-698.
Authors:Jia Songwei  He Xiubin  Wei Fangqiang
Institution:(1) Key Laboratory of Mountain Hazards and Surface Process, Chinese Academy of Sciences, Chengdu, 610041, Sichuan, China;(2) Graduate University of Chinese Academy of Sciences, Beijing, 100049, China;(3) Institute of Mountain Hazards and Environment, Chengdu, 610041, Sichuan, China
Abstract:Based on field runoff plots observation and sample analysis, the effect of slope gradient on soil organic carbon loss was studied under natural rainfall conditions in loess hilly region. The results showed that with slope gradient increasing (from 10° to 30°), the changing trend of soil erosion intensity (A) was A 20°>A 30°>A 15°>A 10°>A 25°, suggesting that slope gradient between 20° and 25° was a critical degree ranger to exist. Soil organic carbon loss was mainly influenced by soil erosion intensity, appearing the same trend as did soil erosion intensity with increasing slope gradient. Soil erosion results in organic carbon enrichment in sediment. Average enrichment ratios of five runoff plots varied from 2.27 to 3.74, and decreased with increasing erosion intensity and slope gradient. The decrease of surface runoff and soil erosion is the key to reduce soil organic carbon loss. Biography: JIA Songwei (1979–), male, Ph. D. candidate, research direction: soil erosion and soil organic carbon loss.
Keywords:soil erosion  soil organic carbon loss  slope gradient  carbon cycle
本文献已被 CNKI 维普 SpringerLink 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号