摘要
以河流冲积扇、河流冲积扇与滨海平原过渡带、滨海平原3种主要地貌类型,分析了海河低平原区土壤盐分含量、盐基离子组成及电导率的变化规律。结果表明:河流冲积扇耕层虽明显脱盐,但由于底土含盐量高,仍存在土壤盐渍化的威胁,阴离子以Cl-和SO42-为主;相反,河流冲积扇与滨海平原过渡带、滨海平原表土含盐量较高,而底土含盐量较低,阴离子以Cl-为主;土壤盐分中阳离子含量以Na++K+为主,盐分组成主要的可溶性盐为NaCl,其次是Na2SO4和CaCl2。
Soil salt contents,salt composition and electrical conductivity changes of three kinds of landforms in low Haihe River,i.e.,alluvial plain,transition between alluvial and coastal plain,coastal plain were studied.The results showed that in the alluvial plain the desalinization in surface layer was noticeable,but salt content in the subsoil layer was still high,predominant salt anion in the soil were Cl-and SO42-.In transition between alluvial and coastal plain as well as coastal plain,salt content of top soil was high,predominant salt anion in the soil was Cl-.Na＋ and K＋ were predominant salt cations in the soil,which indicated that the dominant soluble salt was NaCl,followed by Na2SO4 and CaCl2.
出处
《土壤》
CAS
CSCD
北大核心
2011年第2期285-288,共4页
Soils
基金
山西省自然科学基金项目(2010011044-3)
国家重点基础研究发展计划项目(2005CB121106)资助
关键词
海河低平原
电导率
土壤盐分
离子组成
Low Haihe River plain
Electrical conductivity
Soil salt
Ion composition
作者简介
杨萍果（1974-），女，山西襄汾人，博士，副教授，主要研究土壤环境质量及其空间变异性。E-mail：lfypg@126.com
