ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
亚高山不同植被类型区的雨季岩溶溶蚀速率研究
  
关键词:karst  vegetation  corrosional ratio  Jinfo Mountain in Chongqing
基金项目:国家科技支持计划课题(编号:2006BAC01A16); 中国博士后科学基金(编号:2005038473); 国家自然科学基金重点项目“多重胁迫下西南岩溶生态系统脆弱性和生态恢复能力研究”(编号:90202016); 重庆市科委研究项目(编号:2004-8258)
作者单位E-mail
王冬银 西南大学地理科学学院,重庆400715  
章程 西南大学地理科学学院,重庆400715
中国地质科学院岩溶地质研究所,国土资源部岩溶动力学重点实验室,广西桂林541004 
 
谢世友 西南大学地理科学学院,重庆400715
西南大学三峡库区生态环境教育部重点实验室,重庆400715 
xiesy@swu.edu.cn 
杨平恒 西南大学地理科学学院,重庆400715  
张文晖 西南大学地理科学学院,重庆400715  
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摘要:
Karst Dissolution Rates of Areas with Different Vegetation Types in the Sub-mountain Region
      Previous studies of karst processes were mainly focused on summarizing the driving effect of CO2 density change on the karst process in a certain karst area.Nevertheless,the direction and intensity of the karst process could be deeply affected by soil physical and chemical variations resulting from land cover.Using the method of standard limestone tablets,the authors detected the corrosional ratios and average corrosional rates of four different vegetation types on the basis of the observation of karst districts of Bitan and Shuifang springs in the Jinfo Mountain in the summer of 2006.Almost all the vegetation types occurred in a small study area,so the present study was typical and representative.The results show that the corrosional ratios of different vegetation types at different elevations are quite different.In general,the corrosional ratios increase gradually from the forest land of Shuifang spring,through the bamboo forest land of Shuifang,the meadow of Shuifang and the forest of Bitan spring,to the shrub of Bitan spring.On the basis of rainfall and temperature differences in the two springs,it is concluded that,besides soil CO2,soil organism is one of the major factors controlling the karst dissolution rate in these districts.
WANG Dong-yin,ZHANG Cheng,XIE Shi-you,YANG Ping-heng,ZHANG Wen-hui.2007.Karst Dissolution Rates of Areas with Different Vegetation Types in the Sub-mountain Region[J].Acta Geoscientica Sinica,28(5):488-495.
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