University of Auckland, Civil and Environmental Department, Private Bag 92019, Auckland Mail Centre, Auckland 1142, New Zealand.
Water Res. 2014 Jan 1;48:430-42. doi: 10.1016/j.watres.2013.09.056. Epub 2013 Oct 12.
A field trial comparing the fate of metals in two parallel stormwater retention ponds, one of which was retrofitted with a Floating Treatment Wetland (FTW), was carried out near Auckland, New Zealand. Results suggest that the FTW increased metal accumulation in the pond sediment especially in summer due to lower sediment Eh, more anoxic water column, neutral pH and greater source of organic matter (OM) induced by the FTW. These factors combined with higher temperature enhanced metal sorption onto OM, flocculation of particulate pollutants, metal sulphide formation and reduced OM degradation and thus limited release of metals. Unlike Zn, Cu speciation in the pond sediment was relatively unchanged under various sediment Eh conditions due to its strong binding property with sulphide and OM. Occasional moderate metal release was detected from the FTW pond sediment likely due to aerobic OM degradation at the beginning of spring and/or hydroxides reduction when sediments became reduced later in the season. No release was noticed from the conventional pond sediment likely due to biosorption and/or uptake by algae which developed in the conventional pond and settled on the bottom sediment. Direct uptake by the plants of the FTW and sorption onto root plaques are not thought to be significant removal pathways. Nevertheless roots play a major role in trapping particulate pollutants, eventually sloughing off to settle on the bottom of the pond, and provide an adequate substrate for bacterial development due to release of organic compounds which are both essential for dissolved metal sorption and metal sulphide formation.
一项在新西兰奥克兰附近进行的现场试验比较了两个平行雨水滞留池中的金属命运,其中一个被浮式处理湿地(FTW)改造。结果表明,由于 FTW 降低了沉积物 Eh 值、增加了缺氧水层、中性 pH 值和更多的有机物(OM)来源,FTW 增加了池塘沉积物中的金属积累,特别是在夏季。这些因素与较高的温度一起增强了金属对 OM 的吸附、颗粒物污染物的絮凝、金属硫化物的形成以及 OM 降解的减少,从而限制了金属的释放。与 Zn 不同,由于 Cu 与硫化物和 OM 具有很强的结合特性,因此在各种沉积物 Eh 条件下,Cu 的形态在池塘沉积物中相对不变。FTW 池塘沉积物中偶尔会检测到中等程度的金属释放,可能是由于春季初有氧 OM 降解,或者在季节后期沉积物还原时,氢氧化物还原。由于常规池塘中藻类的生物吸附和/或吸收,常规池塘沉积物中没有发现金属释放,藻类在常规池塘中生长并沉降在底部沉积物上。FTW 的植物直接吸收和/或根斑块上的吸附被认为不是重要的去除途径。然而,由于释放了对溶解金属吸附和金属硫化物形成都必不可少的有机化合物,根系在捕获颗粒物污染物方面起着重要作用,最终脱落并沉降在池塘底部,并为细菌的生长提供了充足的基质。