水酸化マグネシウム共沈法における廃水中のホウ素除去機構の考察

  • 井澤 彩
    早稲田大学大学院 創造理工学研究科
  • 前田 素生
    早稲田大学大学院 創造理工学研究科
  • 所 千晴
    早稲田大学理工学術院 創造理工学部 環境資源工学科
  • 笹木 圭子
    九州大学工学研究院 地球資源システム工学部門

書誌事項

タイトル別名
  • Sorption Mechanism of Boron to Magnesium Hydroxide using Co-precipitation Process in Aqueous Solution
  • スイサンカ マグネシウム キョウチンホウ ニ オケル ハイスイ チュウ ノ ホウソ ジョキョ キコウ ノ コウサツ

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抄録

We investigated co-precipitation using magnesium (Mg) salt as a cost efficient method of removing B from wastewater. To clarify the mechanism of co-precipitation and the effect of precipitation rate against B sorption mechanism, we conducted co-precipitation experiments changing reaction time at different temperatures. For these experiments, we carried out sorption isotherm formation and XRD analysis to clarify how co-precipitation of B with magnesium hydroxide (Mg (OH) 2) occurred. The sorption isotherm of co-precipitation was a BET type, while the XRD peak shift occurred as the initial B/Mg molar ratio increased. These results suggested that the mechanism of B uptake was a combination of surface precipitation and surface complexation, and the later mechanism became more apparent as the initial B/Mg molar ratio increased. XRD spectrum of co-precipitated residues was relatively similar to that of hydromagnesite, which indicated that structure of surface precipitation is similar to that of hydromagnesite. Co-precipitation experiments for 6 hours revealed that Mg precipitation rate was faster at the higher temperature, while sorption density became worse as the temperature increased. At 40<tt>℃</tt> and 60<tt>℃</tt>, XRD peak shift did not occur when the initial B/Mg molar ratio was0.063, which suggests that fast precipitation rate disturbed production of surface precipitation. In addition, the initial B/Mg molar ratio in which B sorption mechanism changed from formation of surface compexation to production of surface precipitation became larger as Mg precipitation rate increased.

収録刊行物

  • 資源と素材

    資源と素材 130 (5), 155-161, 2014

    一般社団法人 資源・素材学会

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