焉耆盆地土壤盐渍化状况的主成分分析  

Principal component analysis of soil salinization in Yanqi Basin

作　　者：刘延锋[1] 靳孟贵[1] 金英春[2] 

机构地区：[1]中国地质大学工程学院,湖北武汉430074 [2]新疆水利水电勘测设计研究院地质勘察研究所,新疆乌鲁木齐830000

出　　处：《干旱地区农业研究》2004年第1期165-171,共7页Agricultural Research in the Arid Areas

基　　金：高等学校博士学科点专项科研基金资助课题(20020491011)

摘　　要：利用主成分分析法分析了焉耆盆地内荒地和耕地的土壤盐分特征,结果表明,荒地内土壤盐分表聚强烈,基本无自然淋洗过程;而耕地内土壤盐分存在多次积盐和脱盐过程,培面中盐分分布比较均匀。第一主成分综合反映了区内土壤盐渍化程度,第二和第三主成分联合反映了土壤的碱性特征。Based on the principal component analysis (PCA) of soil salinization fectors in Yanqi Basin, it is discovered that soil salinity in the wasteland cumulates strongly toward to the surface and there is hardly natural eluviation in it. But there are the phenomena of salinity cumulation and eluviation in the arable land, and the soil salinity is relatively even in the profile. The first principal component can denote the degree of soil salinity, and the second and third principal component can denote the degree of soil alkalinity.

关 键 词：主成分分析 土壤盐渍化 焉耆盆地 土壤盐分 

分 类 号：S153[农业科学—土壤学]