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CaO2不同投加方式对黑臭河道底泥内源磷释放抑制作用
摘要点击 2699  全文点击 901  投稿时间:2016-12-29  修订日期:2017-02-28
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中文关键词  过氧化钙  富营养化  底泥  磷形态
英文关键词  calcuim peroxide  eutrophication  sediment  phosphorus fractions
作者单位E-mail
徐垚 苏州科技大学环境科学与工程学院, 苏州 215009 sustxuyao@163.com 
李大鹏 苏州科技大学环境科学与工程学院, 苏州 215009 ustsldp@163.com 
韩菲尔 苏州科技大学环境科学与工程学院, 苏州 215009  
宋小君 苏州科技大学环境科学与工程学院, 苏州 215009  
李鑫 苏州科技大学环境科学与工程学院, 苏州 215009  
周婧 苏州科技大学环境科学与工程学院, 苏州 215009  
黄勇 苏州科技大学环境科学与工程学院, 苏州 215009  
中文摘要
      以S市某黑臭河道底泥和上覆水为研究材料,研究了CaO2在3种不同投加方式下对内源磷释放的抑制效果.结果表明CaO2在3种投加方式下,均导致上覆水中pH和DO有所增加.注射条件下,上覆水DO浓度明显低于覆盖,说明注射确实延缓了CaO2的氧化速度,有利于创造底泥微氧化环境.CaO2覆盖和注射条件下,上覆水中TP和DIP浓度以及变化趋势基本一致,均明显低于混匀条件.但是,覆盖条件下,间隙水中DIP浓度最高,达到注射条件下的120.33~142.18倍.相反,注射条件下,间隙水中DIP浓度最低,并且上覆水中DIP浓度也较低,说明注射条件下CaO2对内源磷的释放确有抑制作用,这与其创造的微氧化环境密切相关.底泥中不同形态磷数量分布也证实了这一点.投加CaO2加快了有机磷的矿化速度,铁铝结合态磷和钙结合态磷也明显增加,使得内源磷持留能力增强.
英文摘要
      The inhibition of sedimentary phosphorus(P) was investigated under the CaO2 with 3 addition ways. The overlying water and sediments came from a black-odor channel in S City. The results showed that the value of pH and DO in the overlying water increased under the 3 addition ways of CaO2. Under the condition of injection, the DO concentration of the overlying water was lower than that of the covering condition, which indicated that the injection could delay the oxidation of CaO2 and be favor of creating the micro-oxidation environment in the sediment. The concentrations and the trend of TP and DIP in the overlying water were similar under the injection and covering, which were lower than that in the mixing condition. However, under the covering condition, the DIP concentration in the pore water was the highest, reaching up to 120.33-142.18 times, compared with the injection condition. Noticeably, the DIP in the pore water and the overlying water was lower, indicating that the addition of CaO2 could inhibit the release of sedimentary P. This was attributed to the micro-oxidation environment. The sedimentary P fractions also confirmed this. The explanation may be that the addition of CaO2 accelerated the mineralization of organophosphate and the formation of Fe-Al/P and Ca-P, which enhanced the retention of sedimentary P.

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