Temporal-spatial variability of soil fertility in karst region: a case study of Xiaojiang watershed Yunnan

被引:6
|
作者
Jiang, Yongjun [1 ,2 ]
Li, Linli [1 ,2 ]
Wu, Yuexia [1 ,2 ]
Jia, Yanan [1 ,2 ]
Yuan, Daoxian [1 ,2 ]
机构
[1] Southwest Univ, Inst Karst Environm & Rock Desertificat Rehabil, Chongqing 400715, Peoples R China
[2] Southwest Univ, Sch Geog Sci, Chongqing 400715, Peoples R China
来源
ENVIRONMENTAL GEOLOGY | 2008年 / 55卷 / 04期
基金
中国国家自然科学基金;
关键词
geo-statistics; soil fertility; temporal-spatial variability; karst watershed;
D O I
10.1007/s00254-007-1039-5
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
By sampling in the field and analyzing the soil samples in the laboratory in 1982 and 2005 the soil fertility data were obtained. Through application of geo-statistics combined with GIS, the temporal-spatial variability of the pH, organic matter, total nitrogen, total phosphorus and total potassium in soil of Xiaojiang watershed from 1982 to 2005 were analyzed. Results showed that: (1) the pH value and total potassium in soil showed an increasing trend, but the organic matter, total nitrogen and the total phosphorus in soil declined in the past 20 years in Xiaojiang watershed, (2) the parameters fitted by semivariogram models for fertility indices changed significantly in the past 20 years and (3) the result estimated by ordinary Kriging indicated the spatial pattern of the soil fertility indices changed significantly in the past 20 years. The soil pH increased in the east and southeast, but decreased in the middle of the watershed. The organic content of the soil matter decreased in the east, southeast and southwest, but increased in the northeast and middle of the watershed. The total nitrogen content of the soil decreased in the east, but increased in the middle of watershed. The total phosphorus content of the soil decreased in the whole watershed. The total potassium content of the soil increased in the southwest and southeast, but decreased in the middle of the watershed and (4) the change of land use and soil management measures was the main driving force of variability of soil properties.
引用
收藏
页码:875 / 887
页数:13
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