磁性锆铁改性膨润土添加对河道底泥磷迁移与形态转化的影响
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  • 英文篇名:Effect of Magnetic Zirconium/Iron-Modified Bentonite Addition on Phosphorus Mobilization and Species Transformation in River Sediments
  • 作者:王艳 ; 林建伟 ; 詹艳慧 ; 张宏华 ; 张志斌 ; 何思琪 ; 赵钰颖 ; 吴小龙 ; 俞阳
  • 英文作者:WANG Yan;LIN Jian-wei;ZHAN Yan-hui;ZHANG Hong-hua;ZHANG Zhi-bin;HE Si-qi;ZHAO Yu-ying;WU Xiao-long;YU Yang;College of Marine Ecology and Environment,Shanghai Ocean University;College of Environment,Zhejiang University of Technology;College of Municipal and Environmental Engineering,Shandong Jianzhu University;
  • 关键词:磁性锆铁改性膨润土 ; 河道底泥 ; ; 钝化 ; 改良
  • 英文关键词:magnetic zirconium/iron-modified bentonite;;river sediment;;phosphorus;;immobilization;;amendment
  • 中文刊名:HJKZ
  • 英文刊名:Environmental Science
  • 机构:上海海洋大学海洋生态与环境学院;浙江工业大学环境学院;山东建筑大学市政与环境工程学院;
  • 出版日期:2018-09-12 13:26
  • 出版单位:环境科学
  • 年:2019
  • 期:v.40
  • 基金:国家自然科学基金项目(51408354,50908142);; 上海市自然科学基金项目(15ZR1420700);; 上海海洋大学优秀本科生进实验室项目;上海海洋大学本研一体化教学团队项目
  • 语种:中文;
  • 页:HJKZ201902017
  • 页数:9
  • CN:02
  • ISSN:11-1895/X
  • 分类号:139-147
摘要
首先采用Fe~(3+)、Fe~(2+)、溶解性锆盐、膨润土和碱液作为原料制备得到了一种磁性锆铁改性膨润土,再通过底泥培养实验考察了磁性锆铁改性膨润土添加对底泥中磷迁移与形态转化的影响.结果表明,在缺氧条件下,河道底泥中磷会被释放进入间隙水中,继而会被释放进入上覆水中,而磁性锆铁改性膨润土添加可以极大地降低底泥中磷向间隙水的迁移通量,最终导致了上覆水中磷数量的显著下降.此外,添加磁性锆铁改性膨润土不仅促使底泥中弱吸附态磷(Liable-P)和氧化还原敏感态磷(BD-P)这2种容易释放态磷向较为稳定的金属氧化物结合态磷(NaOH-rP)和非常稳定的残渣态磷(Res-P)转变,而且降低了底泥中水溶性磷(WSP)、易解吸磷(RDP)、NaHCO_3可提取磷(Olsen-P)、藻类可利用磷(AAP)和铁氧化物-滤纸提取磷(FeO-P)这5种不同类型生物有效态磷(BAP)含量,从而降低了底泥中磷的释放风险.从底泥中分离出来的磁性锆铁改性膨润土中潜在活性磷(NH4Cl-P+BD-P)占总磷的26%左右,且含一定数量的FeO-P和Olsen-P(含量分别为161 mg·kg~(-1)和127mg·kg~(-1)).因此,及时采用磁分离的方式从底泥中将吸附磷后的磁性锆铁改性膨润土回收是非常必要的.磁性锆铁改性膨润土添加控制河道底泥中磷释放的机制是:改良剂通过对底泥中潜在活性磷和生物有效态磷的钝化作用,以及通过对间隙水中磷的吸附作用,降低了底泥中磷向间隙水的释放风险,导致间隙水中磷浓度的下降,进而降低了底泥-上覆水界面磷的扩散通量,最终导致上覆水中磷浓度的下降.以上结果说明,磁性锆铁改性膨润土是一种非常有希望的用于控制河道底泥中磷释放的改良剂.
        A magnetic zirconium/iron-modified bentonite( ZrFeBT) was prepared,and the effect of ZrFeBT addition on the mobilization and species transformation of P in river sediments was investigated using incubation sediment core experiments. The results showed that,under anoxic conditions,P could be released from river sediments into the pore water,and then P in the pore water could be released into the overlying water. The addition of ZrFeBT into river sediments could greatly suppress the release of P from river sediments into the pore water under anoxic conditions. Therefore,the release of P from the pore water into the overlying water could be significantly suppressed by the addition of ZrFeBT. After the addition of ZrFeBT into river sediments,the transformation of loosely sorbed P( Labile-P) and BD extractable P( BD-P) to Na OH extractable P( Na OH-rP) and residual P( Res-P) in the sediments was observed. The decrease of bioavailable P( BAP) including water soluble P( WSP),readily desorbable P( RDP),NaHCO_3 extractable P( Olsen-P),algal available P( AAP),and Fe oxide-paper extractable P( Fe O-P) in the sediments was also observed. A certain amount of P in the ZrFeBT after the incubation experiment was present in the form of mobile P( Labile-P and BD-P),Olsen-P,and Fe O-P,which could be re-released into the pore water and overlying water when the environmental conditions change in the future.The control of P release from river sediment into the overlying water by the addition of ZrFeBT could be mainly attributed to the reduction of P in the pore water as well as the reduction of mobile P and BAP in the sediments after ZrFeBT amendment. The results of this study inidcated that ZrFeBT is a promising amendment for the regulation of P release from river sediments into the overlying water.
引文
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