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

典型岩溶农业区土地利用变化对土壤性质的影响——以云南小江流域为例
引用本文:蒋勇军.典型岩溶农业区土地利用变化对土壤性质的影响——以云南小江流域为例[J].地理学报(英文版),2006,16(1):69-77.
作者姓名:蒋勇军
作者单位:School of Resources & Environmental Sciences, Southwest University, Chongqing 400715, China
基金项目:The open foundation of physical geography of Southwest University, No.250-411109; Foundation of Science and Technology Committee of Chongqing, No.20027534; No.20048258; Project of Ministry of Land and Resources, No.200310400024
摘    要:1 Introduction Because of modifying land-cover (Turner et al., 1991) and management measures of soil (Dalal, 1986), land use changes can cause significant modifications in soil properties (Islam, 2000; Mcalister, 1998; Braimoh, 2004; Lal, 1996; Shepherd, …

关 键 词:云南  小江流域  典型岩溶农业区  土地利用变化  土壤性质
收稿时间:9/7/2005 12:00:00 AM
修稿时间:2005-09-072005-12-05

The impact of land use on soil properties in a karst agricultural region of Southwest China: a case study of Xiaojiang watershed, Yunnan
Yongjun Jiang Ph.D..The impact of land use on soil properties in a karst agricultural region of Southwest China: a case study of Xiaojiang watershed, Yunnan[J].Journal of Geographical Sciences,2006,16(1):69-77.
Authors:Yongjun Jiang PhD
Abstract:Supported by RS and GIS, the land use change from 1982 to 2003 were analyzed and the impacts of land use changes on pH value, organic matter, total N, total P, total K, available N, available P, and available K in soil of Xiaojiang watershed, a typical karst agricultural region of Yunnan Province, Southwest China were assessed. The following aspects are concluded. (1) The total land use converted during the past 20 years in Xiaojiang watershed covers an area of 610.12 km2, of which 134.29 km2 of forestland was converted into cultivated land, and 210 km2 of unused land was converted into cultivated land. (2) The rapid growth of population and the economic development were the main driving forces of land use change. (3) With the change in land use, the soil properties have been changed significantly. The pH, organic matter, total N, total P, total K, available N, available P and available K in soil in 1982 were 6.3, 38.02 g kg-1, 1.86 g kg-1, 1.63 g kg-1, 10.94 g kg-1, 114.42 g kg-1, 11.65 mg kg-1 and 64.69 mg kg-1g, respectively; and those in 2003 were 6.73, 25.26 g kg-1, 1.41 g kg-1, 0.99 g kg-1, 12.6 g kg-1, 113.43 mg kg-1, 11.11 mg kg-1 and 151.59 mg kg-1, respectively. Pared samples t-test of the tested indices of soil properties indicate that those indices have changed significantly during the last 20 years. But the soil properties changed differently, due to the differences in land use change. (4) Also, with the change in land use and management measures of soil, the modifications in soil properties which developed from carbonate rocks were more sensitive than those in the soil developed from sandstone.
Keywords:karst agricultural region  land use change  soil properties  Xiaojiang watershed  Yunnan Province
本文献已被 维普 万方数据 SpringerLink 等数据库收录!
点击此处可从《地理学报(英文版)》浏览原始摘要信息
点击此处可从《地理学报(英文版)》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