Key Laboratory of Drinking Water Science and Technology, Research Centre for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China; Department of Civil and Environmental Engineering, Imperial College London, South Kensington Campus, London SW7 2AZ, UK.
Centre for Water Resources Research (CWRR), School of Civil, Structural and Environmental Engineering, University College Dublin, Newstead Building, Belfield, Dublin 4, Ireland.
Water Res. 2018 Oct 15;143:346-354. doi: 10.1016/j.watres.2018.06.063. Epub 2018 Jun 27.
When aluminum salts are added to water at around neutral pH, a precipitate of Al hydroxide is formed very rapidly. Initially the precipitate is in the form of nano-scale primary particles, which then aggregate to form flocs. The nature of the flocs depends greatly on the solution composition, for instance on the presence of humic acid (HA), which not only increases the size of the primary nanoparticles, but also decreases the connection points between them. The nanoparticles become smaller with aging, both with and without HA, as a result of crystallization. The aggregated amorphous nanoparticles (settled flocs) undergo a room temperature structural modification best characterized as a disorder-to-order transition, following elimination of water. During this process, the apparent Al concentration in the supernatant of water increases with age. The "dissolved Al" concentration in the supernatant becomes higher with increasing pH and, to some extent, in the presence of HA. However, it can be shown that the "dissolved Al" in the supernatant exists in the form of crystalline nano-particles or larger clusters, which are detached from the settled flocs. TEM results confirmed that HA only adsorbed on the surface of nano-particles during the coagulation process, which shows precipitate nanoparticles formed firstly during sweep coagulation before the adsorption of HA or complexed Al-HA. However, the adsorbed outer layer of HA does not change the crystallization process for the inner part of nano-particles. This laboratory study may have implications for the release of Al from sediments into lake water, following addition of coagulants to lower phosphorus concentrations.
当铝盐在接近中性 pH 值的水中添加时,会迅速形成氢氧化铝沉淀。最初沉淀的形式是纳米级的初级粒子,然后聚集成絮体。絮体的性质在很大程度上取决于溶液的组成,例如腐殖酸 (HA) 的存在,它不仅增加了初级纳米粒子的尺寸,而且还减少了它们之间的连接点。由于结晶,纳米颗粒在有或没有 HA 的情况下都会随着老化而变小。聚集的无定形纳米颗粒(沉淀絮体)经历了室温结构改性,最好被描述为无序到有序的转变,同时消除了水。在此过程中,上清液中可见的 Al 浓度随着年龄的增长而增加。上清液中的“溶解 Al”浓度随着 pH 值的升高而升高,在一定程度上,在 HA 的存在下也是如此。然而,可以表明上清液中的“溶解 Al”以结晶纳米颗粒或更大的簇的形式存在,这些颗粒从沉淀絮体中分离出来。TEM 结果证实,在混凝过程中,HA 仅吸附在纳米颗粒的表面上,这表明在 HA 吸附或形成 Al-HA 复合物之前,在扫集混凝过程中首先形成了沉淀纳米颗粒。然而,HA 的吸附外层不会改变纳米颗粒内部的结晶过程。这项实验室研究可能对在向低磷浓度的湖水中添加混凝剂后,沉积物中 Al 的释放产生影响。