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方解石/氯磷灰石混合物添加对水体内源磷迁移转化的调控效应和机制
摘要点击 1653  全文点击 521  投稿时间:2019-08-15  修订日期:2019-12-01
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中文关键词  方解石  氯磷灰石  混合物  底泥  内源磷  释放控制  改良
英文关键词  calcite  chlorapatite  mixture  sediment  internal phosphorus loading  release control  amendment
作者单位E-mail
柏晓云 上海海洋大学海洋生态与环境学院, 上海 201306 1399241599@qq.com 
林建伟 上海海洋大学海洋生态与环境学院, 上海 201306 jwlin@shou.edu.cn 
詹艳慧 上海海洋大学海洋生态与环境学院, 上海 201306  
常明玥 上海海洋大学海洋生态与环境学院, 上海 201306  
吴俊麟 上海海洋大学海洋生态与环境学院, 上海 201306  
辛慧敏 上海海洋大学海洋生态与环境学院, 上海 201306  
黄良君 八帆仪器设备(上海)有限公司, 上海 201114  
中文摘要
      阐明方解石/氯磷灰石混合物添加对内源磷迁移转化的调控效应与机制,对于其实际应用至关重要.为此,本文采用氯化钙和磷酸钠制备得到氯磷灰石,再与天然方解石进行混合,形成氯磷灰石和方解石的混合物,然后通过批量吸附实验考察了该混合物对水中磷酸盐的去除作用,再通过底泥培养实验考察了该混合物添加对底泥中磷迁移转化的影响.结果表明,该混合物对水中磷酸盐的去除能力明显强于单纯的方解石和氯磷灰石;该混合物对水中磷酸盐的去除动力学过程较好地符合准二级和Elovich动力学模型;增加方解石和氯磷灰石的投加量均有利于该混合物对水中磷酸盐的去除;溶液共存钙离子促进了该混合物对水中磷酸盐的去除.该混合物的添加可以有效控制底泥中磷向上覆水体的释放,导致上覆水中的溶解性活性磷(SRP)浓度处于相对较低的水平.此外,该混合物添加还可以降低间隙水中SRP的浓度,其对间隙水中SRP的削减作用对其调控底泥中磷向上覆水体的迁移转化起到重要的作用.该混合物添加虽然会增加底泥中磷的含量,但所增加的磷主要是以稳定的钙磷形式存在,发生二次污染的风险低.结果显示,方解石/氯磷灰石混合物可以作为底泥改良材料用于水体内源磷释放的控制.
英文摘要
      Understanding the effect of calcite and chlorapatite mixture (CA/ClAP) addition on the mobilization of phosphorus (P) in sediments is crucial to the application of CA/ClAP as an amendment material to control the release of P from sediments. To address this issue, batch experiments were conducted to investigate the removal performance of phosphate by CA/ClAP, and sediment incubation experiments were carried out to study the effect of CA/ClAP addition on the mobilization of P in sediments. The results showed that the removal ability of phosphate by CA/ClAP was much higher than those by calcite and chlorapatite, and the kinetics data of phosphate removal by CA/ClAP followed a pseudo-second-order kinetics model. Increasing calcite and chlorapatite dosages would be favorable for the removal of phosphate by CA/ClAP, and coexisting Ca2+ enhanced the phosphate removal. CA/ClAP addition not only reduced the concentration of soluble reactive P (SRP) in the overlying water, but also decreased the concentration of SRP in the pore water. The addition of CA/ClAP in sediments caused an increase in the content of P in the sediments, but the increased P mainly existed in the form of calcium-bound P (HCl-P), which was difficult to be re-released into the water column under anoxic and common pH (5-9) conditions. The reduction of SRP in the pore water after the addition of CA/ClAP played an important role in the prevention of sedimentary P liberation into the overlying water by the CA/ClAP amendment. The results of this work indicate that CA/ClAP can be used as an amendment material for interception of the release of P from sediments into overlying water.

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