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

亚热带岩溶山区植被演替和夏季土壤CO2浓度动态关系
引用本文:吴威,况明生,魏秉铎,孙艳丽,张远瞩.亚热带岩溶山区植被演替和夏季土壤CO2浓度动态关系[J].西南师范大学学报(自然科学版),2004,29(2):289-293.
作者姓名:吴威  况明生  魏秉铎  孙艳丽  张远瞩
作者单位:西南师范大学资源环境科学学院,重庆 400715
基金项目:教育部重点资助项目 (教技司 [2 0 0 0 ] 15 6) .
摘    要:对南川市金佛山西坡相近的环境条件下不同植被类型土壤CO2 浓度及其主要环境因子进行连续观测的基础上 ,采用空间换时间的方法对植被演替对夏季土壤CO2 浓度的动态影响作了详细的研究 ,认为 :土壤CO2 随气温的变化有明显的日变化 ,降水对其浓度也有较大的影响 ,其变化过程及CO2 浓度剖面动态与植被类型有关 ;不同植被条件下土壤CO2 浓度月动态受环境因素影响显示出的差异不大 ,但浓度值水平有很大差别 ;植被演替是岩溶和土壤吸收CO2 作用的重要促进因素 .

关 键 词:CO2浓度动态  植被演替  空间换时间  岩溶作用
文章编号:1000-5471(2004)02-0289-05
修稿时间:2003年9月24日

The Research of the Relationship Between Vegetation Succession and Soil CO2 Concentration Dynamics in Subtropic Karst Area in Summer
WU Wei,KUANG Ming-sheng,WEI Bing-duo,SUN Yan-li,ZHANG Yuan-zhu School of Resources and Environmental Science,Southwest China Normal University Chongqing ,China.The Research of the Relationship Between Vegetation Succession and Soil CO2 Concentration Dynamics in Subtropic Karst Area in Summer[J].Journal of Southwest China Normal University(Natural Science),2004,29(2):289-293.
Authors:WU Wei  KUANG Ming-sheng  WEI Bing-duo  SUN Yan-li  ZHANG Yuan-zhu School of Resources and Environmental Science  Southwest China Normal University Chongqing  China
Institution:WU Wei,KUANG Ming-sheng,WEI Bing-duo,SUN Yan-li,ZHANG Yuan-zhu School of Resources and Environmental Science,Southwest China Normal University Chongqing 400715,China
Abstract:Based on the continuous investigation on soil CO_2 concentration and main environment factor of different vegetation types in similar environment conditions in west district of Mount Jinfo of Nanchuan city, chongqing municipality, with the method of conversion from space to time, the relationship between vegetation succession and soil CO_2 concentration dynamics in summer are researched. Some preliminary conclusions are drawn as follows: soil CO_2 concentration has distinct change in a day with temperature change, and is effected by precipitation, its change process and the profile dynamics of CO_2 concentration in soil have close relationship with vegetation types; soil CO_2 concentration dynamics in a month effected by environment factors shows little difference, but concentration level varies greatly; based on the measuration of dissolution rate of standard limestone tables and hydrochemical analysis of water in different soil, vegetation succession is an important promotive factor to karstification and soil absorbency of CO_2.
Keywords:CO_2 concentration dynamics  vegetation succession  conversion from space to time  karstification
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《西南师范大学学报(自然科学版)》浏览原始摘要信息
点击此处可从《西南师范大学学报(自然科学版)》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