首页  |  本刊简介  |  编委会  |  投稿须知  |  订阅与联系  |  微信  |  出版道德声明  |  Ei收录本刊数据  |  封面
城市重污染河道底泥对外源磷的吸附和固定机制
摘要点击 2743  全文点击 2004  投稿时间:2010-01-09  修订日期:2010-03-25
查看HTML全文 查看全文  查看/发表评论  下载PDF阅读器
中文关键词  底泥  吸附  磷形态  磷平衡浓度
英文关键词  sediment  adsorption  phosphorus fraction  zero equilibrium phosphorus concentration
作者单位
李大鹏 中国科学院南京地理与湖泊研究所湖泊与环境国家重点实验室南京210008 苏州科技学院环境科学与工程学院苏州215011 
黄勇 苏州科技学院环境科学与工程学院苏州215011 
袁砚 苏州科技学院环境科学与工程学院苏州215011 
范成新 中国科学院南京地理与湖泊研究所湖泊与环境国家重点实验室南京210008 
中文摘要
      以重污染河道底泥和上覆水为材料,研究了周期性加入外源磷条件下,间歇扰动对底泥吸附和固定外源磷的作用机制.结果表明,扰动状态下,39d内底泥对外源磷的累积吸附量达到363.4 mg·kg-1,远高于静态试验(213.2 mg·kg-1).内源磷形态分析表明,扰动状态下底泥吸附的外源磷中超过61%被结合到铁铝结合态磷(Fe/Al-P)中,而静态试验则上升为83%.考虑到Fe/Al-P的生物有效性,结合到非闭蓄态铁铝结合态磷中的外源磷分别占40.6%(扰动试验)和59.5%(静态试验).另外,扰动状态下,超过23%的底泥吸附的外源磷结合到钙结合态磷(HCl-P),而静态试验中HCl-P基本保持不变.底泥吸附外源磷后,2种底泥磷最大吸附容量(Smax)均有所降低,而扰动后底泥的磷平衡浓度(EPC0)、磷饱和度p(%)的增加幅度明显低于静态试验底泥.因此推测,底泥扰动不仅可以加快底泥对磷的吸附,而且提高了内源磷持留能力.
英文摘要
      The mechanisms of phosphorus (P) adsorption and immobility were investigated in laboratory experiments. The sediments and waters used were taken from an inner-city heavily polluted canal. Addition of KH2PO4 into the operated experimental units,with and without (i.e.,static) intermittent sediment resuspension,were made similar to the external P input and carried out periodically. The results show that the amount of the accumulative P adsorption onto the sediments was up to 363.4 mg·kg-1 under the conditions of sediment disturbance over a 39-day period,and it was evidently higher than that (213.2 mg·kg-1) under static conditions. Sequential fractionation indicated that most of the incorporated P was accounted for in the Fe/Al-P. There were over 61% in the case of intermittent sediment disturbance and up to 83% in the case of static conditions. Based on the bioavailability of Fe/Al-P,40.6% of the incorporated P was accounted for in non-occluded Fe/Al-P of the sediments under intermittent sediment disturbance conditions. This value increased to 59.5% under static conditions. In addition,more than 23% of the incorporated P was accounted for in HCl-P of the sediments under intermittent sediment disturbance conditions,on the other hand,the concentration of HCl-P kept relatively constant under static conditions. After 39 d of P adsorption by the both sediments,the values of the maximum sorption capacity (Smax) decreased,while zero equilibrium P concentration (EPC0) and P saturation p(%) increased. However,the extent of EPC0 and P% under intermittent sediment disturbance conditions was obviously lower than that under static conditions. It was hopefully suggested that intermittent sediment disturbance can not only accelerate the P adsorption but also enhance the P retention by sediments.

您是第53198782位访客
主办单位:中国科学院生态环境研究中心 单位地址:北京市海淀区双清路18号
电话:010-62941102 邮编:100085 E-mail: hjkx@rcees.ac.cn
本系统由北京勤云科技发展有限公司设计  京ICP备05002858号-2