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中国农学通报 ›› 2016, Vol. 32 ›› Issue (17): 91-97.doi: 10.11924/j.issn.1000-6850.casb16030083

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

不同吹填年限围海吹填土的障碍特征分析

赵秀芳,王振宇,张振,刘祥宏,张清   

  1. 天津泰达绿化集团有限公司,天津泰达绿化集团有限公司,天津泰达绿化集团有限公司,天津泰达绿化集团有限公司,天津泰达绿化集团有限公司
  • 收稿日期:2016-03-10 修回日期:2016-03-24 接受日期:2016-03-24 出版日期:2016-06-20 发布日期:2016-06-20
  • 通讯作者: 赵秀芳
  • 基金资助:
    天津市自然科学基金青年项目“吹填陆域原土改良绿地生态系统盐渍胁迫机理与防控技术”(13JCQNJC08100);天津市滨海新区“十大战役”重大科技支撑项目“滨海旅游区盐土与吹填土绿化关键技术集成与示范”(2010-Bk140003);天津市建交委科技项目“南港工业区围海吹填土原土改良绿化技术研究与示范应用”(NG-CW-QT-11-0010)。

Constraining Characteristics of Coastal Dredger Fill in Different Dredged Years

王振宇,张振,刘祥宏 and 张清   

  • Received:2016-03-10 Revised:2016-03-24 Accepted:2016-03-24 Online:2016-06-20 Published:2016-06-20

摘要: 为确定不同吹填年限围海吹填土的障碍特征,通过田间调查对不同吹填年限围海吹填土的植被与土壤质量进行了全面研究。结果表明:吹填土植被生长量与吹填时间正关联,吹填初期,地表裸露,鲜有碱蓬,3~5 年后,地肤、滨藜入侵,碱蓬生长量显著增加,6 年以后,碱蓬成片生长,有芦苇着生;吹填土容重轻,田间持水量大,有机质含量低,氮素匮乏,速效磷、速效钾含量丰富;吹填初期,土壤含盐量高,均大于30 g/kg,碱性强,8.4<pH<8.8,ESP>30%,为NaCl 型盐渍土;吹填前5 年,盐分离子仅在表层和亚表层间进行迁移、再分配;6 年后,1 m土体才开始脱盐。土质粘紧,含盐量高、碱性强,有机质和氮素贫乏是不同吹填年限围海吹填土的障碍特征。

关键词: 粪肠球菌, 粪肠球菌, fsr群体感应系统, 毒力基因, 抑制剂

Abstract: A comprehensive study on vegetation and soil quality of coastal dredger fill in different dredged years was conducted through a field investigation, to determine the constraining characteristics of the coastal dredger fill in different dredged years. The results showed that: biomass was positively correlated with the dredged time of the coastal dredger fill, the soil surface was basically bare and Suaeda salsa was little in the early time of the dredger fill; after the deposition of 3 to 5 years, the dredger fill was initially invaded by the plants of Kochiascoparia and Atriplex and the biomass of Suaeda salsa significantly increased; after 6 deposition years, the Suaeda salsa on the ground of the dredger fill increased to a large amount; the bulk density of the dredger fill in different dredged years was light and had large field capacity; soil organic matter content was low and nitrogen was lacking, while the contents of available phosphorus and available potassium were rich in different dredged years; the average soil salt content whose determined ions were Na and Cl- was above 30 g/kg; the soil pH was between 8.4 and 8.8 and ESP was all more than 30%, which showed that the dredger fill was strong alkaline soil; the migrations and redistributions of soil salt ions were limited to be between the surface and the subsurface within the first 5 years; the soil at 1 m depth began to desalination 6 years later. Tight clay soil, high salt content, strong alkaline, poor organic matter and nitrogen were the constraining characteristics of the coastal dredger fill in different dredged years.