Department of Chemical Engineering, BarcelonaTECH-UPC, Barcelona, Spain; Department of Chemistry, Universidad Técnica Particular de Loja, Loja, Ecuador.
Department of Chemical Engineering, BarcelonaTECH-UPC, Barcelona, Spain.
Sci Total Environ. 2018 Jan 15;612:728-738. doi: 10.1016/j.scitotenv.2017.08.248. Epub 2017 Sep 1.
The removal of nutrients (nitrogen (N), phosphorous (P)) from waste water has become a resource recovery option in recent regulations worldwide, as observed in the European Union. Although both of these nutrients could be recovered from the sludge line, >70-75% of the N and P is discharged into the water line. Efforts to improve the nutrient recovery ratios have focused on developing low-cost technologies that use sorption processes. In this study, a natural zeolite (clinoptilolite type) in its potassium (K) form was impregnated with hydrated metal oxides and used to prepare natural hybrid reactive sorbents (HRS) for the simultaneous recovery of ammonium (NH) and phosphate (PO) from treated urban waste water. Three unfertile soils (e.g., one acidic and two basic) amended with N-P-K charged HRS were leached with deionized water (e.g. to simulate infiltration in the field) at two- and three-day time intervals over 15 different leaching cycles (equivalent to 15 bed volumes). The N-P-K leaching profiles for the three charged hybrid sorbents exhibited continuous nutrient release, with their values dependent on the composition of minerals in the soils. In the basic soil that is rich in illite and calcite, the release of potassium (K) and ammonium (NH) is favoured by-ion exchange with calcium (Ca) and accordingly diminishes the release of phosphate (PO) due to its limited solubility in saturated calcite solutions (pH8 to 9). The opposite is true for sandy soils that are rich in albite (both acidic and basic), whereas the release of NH and K was limited and the values of both ions measured in the leaching solutions were below 1mg/L. Their leaching solutions were poor in Ca, and the release of PO was higher (up to 12mgP-PO/L). The nutrient releases necessary for plant growth were provided continuously and were controlled primarily by the soil mineral dissolution rates fixing the soil aqueous solution composition (e.g. pH and ionic composition; in particular, the presence of calcite is a determinant for nutrient release, especially in alkaline soils). The N-P-K charged HRS sorbents that were used for soil amendment may be an alternative for avoiding nutrient leaching and reaching the goals of soil sustainability in agriculture and reducing the nutrient overloading of surface waters.
从废水去除营养物(氮(N)、磷(P))已成为最近全球法规中的一种资源回收选择,在欧盟已经观察到这一点。尽管这两种营养物都可以从污泥线中回收,但超过 70-75%的 N 和 P 被排放到水线中。为提高营养物回收比例而进行的努力集中于开发使用吸附过程的低成本技术。在这项研究中,用浸渍水合金属氧化物的方式对钾(K)形式的天然沸石(斜发沸石型)进行处理,以制备天然混合反应性吸附剂(HRS),从处理后的城市废水中同时回收铵(NH)和磷酸盐(PO)。用去离子水(例如模拟田间渗透)以两天和三天的时间间隔对 3 种未施肥土壤(例如,一种酸性土壤和两种碱性土壤)进行淋洗,在 15 个不同的淋洗周期(相当于 15 个床体积)中进行。三种带电荷的混合吸附剂的 N-P-K 淋洗曲线显示出连续的养分释放,其值取决于土壤中矿物质的组成。在富含伊利石和方解石的碱性土壤中,钾(K)和铵(NH)的释放通过与钙(Ca)的离子交换而得到促进,因此由于其在饱和方解石溶液中的有限溶解度(pH8 至 9),磷酸盐(PO)的释放减少。对于富含钠长石(酸性和碱性)的沙土则相反,NH 和 K 的释放受到限制,测量的淋洗溶液中两种离子的值均低于 1mg/L。它们的淋洗溶液中 Ca 含量较低,PO 的释放量较高(高达 12mgP-PO/L)。植物生长所需的养分持续释放,并主要由固定土壤水溶液组成的土壤矿物溶解速率控制(例如 pH 和离子组成;特别是方解石的存在是养分释放的决定因素,特别是在碱性土壤中)。用于土壤改良的带 N-P-K 的 HRS 吸附剂可能是避免养分淋失和实现农业土壤可持续性目标以及减少地表水中养分过负荷的一种替代方法。