CSIRO Land and Water, Private Bag 5, Wembley, WA 6913, Australia.
Water Res. 2012 Mar 15;46(4):1260-72. doi: 10.1016/j.watres.2011.12.032. Epub 2011 Dec 23.
Laboratory and field experiments were undertaken to assess the fate of N-nitrosodimethylamine (NDMA) in aerobic recycled water that was recharged into a deep anaerobic pyritic aquifer, as part of a managed aquifer recharge (MAR) strategy. Laboratory studies demonstrated a high mobility of NDMA in the Leederville aquifer system with a retardation coefficient of 1.1. Anaerobic degradation column and (14)C-NDMA microcosm studies showed that anaerobic conditions of the aquifer provided a suitable environment for the biodegradation of NDMA with first-order kinetics. At microgram per litre concentrations, inhibition of biodegradation was observed with degradation half-lives (260±20 days) up to an order of magnitude greater than at nanogram per litre concentrations (25-150 days), which are more typical of environmental concentrations. No threshold effects were observed at the lower ng L(-1) concentrations with NDMA concentrations reduced from 560 ng L(-1) to <6 ng L(-1) over a 42 day 14C-NDMA aerobic microcosm experiment. Aerobic (14)C-NDMA microcosm studies were also undertaken to assess potential aerobic degradation, likely to occur close to the recharge bore. These microcosm experiments showed a faster degradation rate than anaerobic microcosms, with a degradation half-life of 8±2 days, after a lag period of approximately 10 days. Results from a MAR field trial recharging the Leederville aquifer with aerobic recycled water showed that NDMA concentrations reduced from 2.5±1.0 ng L(-1) to 1.3±0.4 ng L(-1) between the recharge bore and a monitoring location 20 m down gradient (an estimated aquifer residence time of 10 days), consistent with data from the aerobic microcosm experiment. Further down gradient, in the anaerobic zone of the aquifer, NDMA degradation could not be assessed, as NDMA concentrations were too close to their analytical detection limit (<1 ng L(-1)).
实验室和现场实验评估了在充入深部厌氧硫质含水层的好氧再生水中 N-亚硝基二甲胺(NDMA)的归宿,这是管理型含水层补给(MAR)策略的一部分。实验室研究表明,NDMA 在利德维尔含水层系统中具有很高的迁移性,阻滞系数为 1.1。厌氧降解柱和(14)C-NDMA 微宇宙研究表明,含水层的厌氧条件为 NDMA 的生物降解提供了适宜的环境,符合一级动力学。在微克/升浓度下,观察到生物降解受到抑制,降解半衰期(260±20 天)比纳克/升浓度(25-150 天)长一个数量级,这更符合环境浓度。在较低的 ng/L 浓度下没有观察到阈值效应,在 42 天的(14)C-NDMA 好氧微宇宙实验中,NDMA 浓度从 560ng/L 降低到<6ng/L。还进行了好氧(14)C-NDMA 微宇宙研究,以评估可能发生在补给井附近的好氧降解。这些微宇宙实验表明,在一个约 10 天的滞后期后,降解半衰期为 8±2 天,比厌氧微宇宙的降解速度更快。用好氧再生水对利德维尔含水层进行 MAR 现场试验的结果表明,NDMA 浓度从补给井到 20 米下游的监测点(估计含水层停留时间为 10 天)从 2.5±1.0ng/L 降低到 1.3±0.4ng/L,与好氧微宇宙实验的数据一致。在更远的下游,在含水层的厌氧区,由于 NDMA 浓度接近其分析检测限(<1ng/L),无法评估 NDMA 的降解情况。