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Using Ca-Fe layered double hydroxide transformation to optimise phosphate removal from waste waters

机译:使用Ca-Fe分层双氢氧化物转化来优化废水中的磷酸盐去除

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Single phase Ca-Fe layered double hydroxide (LDH) minerals containing Cl- species in the interlayer was synthesized by coprecipitation with a Ca-II: Fe-III ratio of 2: 1. In both phosphate (PO4) free water and at low aqueous PO4 concentration, the LDH was fully transformed into a mixture of a "ferrihydrite-like" material, calcite and soluble calcium species. Mossbauer spectroscopy and transmission electron microscopy showed that phosphate was removed by the "ferrihydrite like" phase that contained a significant quantity of Ca. At high phosphate concentration the Ca species released from the LDH precipitated to form hydroxyapatite leading to a maximal removal capacity of similar to 130 mg P-PO4 g(-1). The Ca-Fe LDH was deposited onto a pozzolana volcanic rock in order to perform a column experiment under hydrodynamic conditions for 70 days. A high removal capacity was observed, a q(B) of similar to 4 mg P-PO4 g(-1) was measured at the breakthrough of the column, however the pH in the outflow was measured to be higher than 11. Such an increase was due to the very high solubility of the Ca-Fe LDH.
机译:通过共沉淀以2:1的Ca-II:Fe-III比例共沉淀法合成夹层中含有Cl-的单相Ca-Fe层状双氢氧化物(LDH)矿物。在无磷酸盐(PO4)的水中和低水在PO4浓度下,LDH被完全转化为“类铁水合物”材料,方解石和可溶性钙物质的混合物。 Mossbauer光谱法和透射电子显微镜显示,磷酸盐被“铁水合物样”相除去,其中含有大量的Ca。在高磷酸盐浓度下,从LDH释放的Ca物质沉淀形成羟基磷灰石,从而导致最大去除能力类似于130 mg P-PO4 g(-1)。为了在水动力条件下进行70天的柱实验,将Ca-Fe LDH沉积到火山灰火山岩上。观察到较高的去除能力,在色谱柱的穿刺点处测得的aq(B)与4 mg P-PO4 g(-1)相似,但是流出的pH值被测量为高于11。这是由于Ca-Fe LDH的溶解度很高。

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