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

滇黔桂地区土壤有机碳储量与影响因素研究
引用本文:张勇,史学正,赵永存,于东升,王洪杰,孙维侠.滇黔桂地区土壤有机碳储量与影响因素研究[J].环境科学,2008,29(8):2314-2319.
作者姓名:张勇  史学正  赵永存  于东升  王洪杰  孙维侠
作者单位:1. 中国科学院南京土壤研究所土壤与农业可持续发展国家重点实验室,南京,210008;中国科学院研究生院,北京,100049
2. 中国科学院南京土壤研究所土壤与农业可持续发展国家重点实验室,南京,210008
基金项目:国家自然科学基金,国家重点基础研究发展规划(973)项日,科技部科技基础条件平台建设计划
摘    要:土壤有机碳(SOC)库在陆地生态系统中具有重要作用.由于土壤剖面数量和采用的土壤图比例尺等的限制,目前土壤有机碳库估箅尚存在很大不确定性.为了提高SOC库估算的精确性,利用798个土壤剖面及1:50万土壤图估算了滇黔桂地区(云南省、贵州省和广西壮族自治区)的SOC储量,并采用逐步回归分析和通径分析方法分析了影响SOC密度的主要因子.结果表明,滇黔桂地区表土层(0-20 cm)和土壤剖面(0-100 cm)的SOC储量分别为4.39 Pg和10.91 Pg;SOC密度分别为56.2Mg·hm-2和139.8 Mg·hm-2.高于全国平均水平.环境因子(海拔、经度、纬度、气温和降雨)、成土母质和土地利用方式对表土层和土壤剖面SOC密度变异性的解释度分别为37.9%和30.7%;环境因子为影响SOC密度的主要因子.环境因子中.气温对SOC密度的影响大干降雨,其中气温和降雨的变化分别主要由海拔和纬度的变化引起的.除气温和降雨外,还有其它随海拔或经纬度而变化的因子也对SOC密度产生显著影响,这种影响要大于降雨的影响.

关 键 词:土壤有机碳  碳储量  碳密度分布图  影响因子
修稿时间:2007/10/16 0:00:00

Estimates and Affecting Factors of Soil Organic Carbon Storages in Yunnan-Guizhou-Guangxi Region of China
Zhang Yong,Shi Xue-zheng,Zhao Yong-cun,Yu Dong-sheng,Wang Hong-jie,Sun Wei-xia.Estimates and Affecting Factors of Soil Organic Carbon Storages in Yunnan-Guizhou-Guangxi Region of China[J].Chinese Journal of Environmental Science,2008,29(8):2314-2319.
Authors:Zhang Yong  Shi Xue-zheng  Zhao Yong-cun  Yu Dong-sheng  Wang Hong-jie  Sun Wei-xia
Institution:State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China. zhangyongjeff@163.com
Abstract:Soil organic carbon (SOC) plays a key role in the terrestrial eco-systems. However, there is a large variation in SOC estimates at regional and global scales. In order to improve the accuracy of SOC estimates, the SOC storage in Yunnan-Guizhou-Guangxi Region of China (include Yunnan Province, Guizhou Province and Guangxi Zhuang Municipality) was estimated using 798 soil profiles and 1:500 000 digitized soil map, and the dominant affecting factors on SOC density were also discussed employing stepwise regression and path analysis. Results showed that the SOC storages estimated in the 0-20 cm and 0-100 cm layers are 4.39 Pg and 10.91 Pg, respectively; and the corresponding SOC density are 56.2 Mg x hm(-2) and 139.8 Mg x hm(-2), respectively. The mean SOC density of Yunnan-Guizhou-Guangxi Region is higher than that of China. The environmental factors (including altitude, longitude, latitude, annual mean precipitation and annual mean temperature), soil parent materials and land use could explain 37.9% and 30.7% of the variability of SOC density to the upper 20 cm and 100 cm, respectively. The environmental factors are the dominant affecting factors of SOC density. The effect of temperature is more important than that of precipitation, and the temperature and precipitation mainly vary with altitude and latitude, respectively. Except for temperature and precipitation, there are also other factors varying with altitude, longitude and latitude significantly affect SOC density. And the effects of other factors are more important than that of precipitation.
Keywords:Key words: soil organic carbon (SOC)  carbon storage  map of carbon density  affecting factors
本文献已被 维普 万方数据 PubMed 等数据库收录!
点击此处可从《环境科学》浏览原始摘要信息
点击此处可从《环境科学》下载免费的PDF全文
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