松辽平原土壤盐渍化现状及盐分特征分析  

The Actuality of Soil Salinization and Characteristics Analysis of Salt in Songliao Plain

作　　者：王耿明[1] 姜琦刚[1] 高永志 邢宇[1] 

机构地区：[1]吉林大学地球探测科学与技术学院遥感应用研究所 [2]黑龙江省地质调查院,哈尔滨150036

出　　处：《水土保持研究》2008年第3期105-107,111,共4页Research of Soil and Water Conservation

基　　金：中国地质调查局项目(1212010510613)

摘　　要：在野外调查采样和土样化学分析基础上,给出了松辽平原土壤盐渍化现状及特征;利用统计分析方法,对研究区盐分特征进行分析表明:松辽平原盐渍土土壤含盐量较高,盐渍化程度较重且差异较大。建立的研究区土壤电导率预测土壤离子含量和含盐量的模型,有助于实现野外土壤离子含量和含盐量的快速经济测定。Soil salinization is one of primary environmental problems,which faces the sustainable development in Songliao Plain. On the basis of field investigation,soil sampling and chemical analysis, soil salinization actuality and characteristics are investigated. Statistical analysis was applied to explore the characters of salt in Songliao Plain. The results show that the salt content is high,soil salinization levels is serious and distinction is great. The advantage of this model of predict hydronium and salt contents by electrical conductivity is less expensive and less time consuming.

关 键 词：松辽平原 土壤盐渍化 盐分 

分 类 号：S156.41[农业科学—土壤学]