典型设施栽培土壤盐分变化规律及潜在的环境效应研究
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*国家自然科学基金重点项目(30230250);中国科学院知识创新方向性项目(KZCW3-SW-439);土壤与农业可持续发展国家重点实验室开放基金(055124);四川省科技厅应用基础项目(03JY029-0301);四川省教育厅重点项目(2003A022)资助


SALT IN TYPICAL GREENHOUSE SOIL PROFILES AND ITS POTENTIAL ENVIRONMENTAL EFFECTS
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    摘要:

    研究了山东寿光设施土壤盐分的变化规律.结果表明:(1)设施土壤的盐分含量高,变化幅度大.耕层盐分含量为2.69gkg-1(CV=58%),而相应的露地仅为0.61gkg-1(CV=14%).(2)设施土壤连续种植到4a左右,其耕层的盐分含量则可达到限制作物正常生长的临界点,此后盐分含量随采取的各种管理措施而有所降低.土壤次生盐渍化是造成温室可持续利用周期较短的主要原因.(3)除HCO3-外,NO3-、SO42-、Cl-、Ca2+、Mg2+、K+、Na+在剖面的累积明显高于露地,且以NO3-和Ca2+的相对富集为主要特征,两者可占耕层盐分离子总量的47.4%和19.3%.(4)与露地相比,盐分离子在设施土壤剖面存在着明显的累积和向下迁移现象,同时在剖面的分布还具有明显的表聚特征,其中NO3-的大量累积和向下层迁移已严重影响到当地地下水水质.

    Abstract:

    Salt in greenhouse soils was studied in Shouguang,Shandong Province.The results indicate that 1) the salt content in greenhouse soils was much higher than that in open field soils,with an average value being 2.69 g kg-1(CV=58%) and only 0.61 g kg-1(CV=14%),respectively,in 0~20 cm soil layer;2) the salt content in greenhouse soils might reach the threshold value for normal growth of crops after 4 years of cultivation,and secondary salinization of the soil is a main limiting factor for sustainable development of greenhouse cropping;3) apart from HCO3-,the contents of NO3-,SO42-,Cl-,Ca2+,Mg2+,K+,Na+ increased significantly in greenhouse soils,and Ca2+and NO3- were the majorions in the soils,accounting for 47.4% and 19.3% of the total salt in the topsoil,respectively;and 4) compared with neighboring open field soils,greenhouse soils displayed apparent phenomena of salts leaching downwards to the bottom of the soil(80~100 cm) and salts accumulating in the topsoil(0~20 cm),especially NO3- that has seriously affected quality of the groundwater in the area.

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余海英,李廷轩,周健民.典型设施栽培土壤盐分变化规律及潜在的环境效应研究[J].土壤学报,2006,43(4):571-576. DOI:10.11766/200505300406 Yu Haiying, Li Tingxuan, Zhou Jianmin. SALT IN TYPICAL GREENHOUSE SOIL PROFILES AND ITS POTENTIAL ENVIRONMENTAL EFFECTS[J]. Acta Pedologica Sinica,2006,43(4):571-576.

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  • 收稿日期:2005-05-30
  • 最后修改日期:2005-10-18
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  • 在线发布日期: 2013-02-25
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