Geological Survey of Canada, Natural Resources Canada, Québec, QC G1K 9A9, Canada.
INRS, Centre Eau Terre Environnement, Québec, QC G1K 9A9, Canada.
Sci Total Environ. 2018 Dec 1;643:392-399. doi: 10.1016/j.scitotenv.2018.06.159. Epub 2018 Jun 22.
Potential seepage of naphthenic acids (NAs) from tailings ponds into surface water and groundwater is one of the main environmental concerns associated with the Canadian Athabasca oil sands mining operations. Here we report the application of C-labelled NA surrogate compounds to evaluate intrinsic biodegradation along groundwater flow-paths originating from oil sands tailings ponds at two different sites: a glacio-fluvial aquifer (Site 1) and a low-lying wetland (Site 2). Microcosms containing the carboxyl group labelled (99%) NA surrogates (cyclohexanecarboxylic acid, CHCA; 1,2-cyclohexanedicarboxylic acid, CHDCA; 1-adamantanecarboxylic acid, ACA) were lowered into monitoring wells for several months to allow sufficient time for substrate degradation and formation of a biofilm in conditions characteristic of the local aquifer. Phospholipid fatty acids (PLFAs), biomarkers for the active microbial population, were extracted from the biofilms for stable carbon isotope (δC) analysis. At Site 1, highly C-enriched δC values (up to ~+7100‰) confirmed the in situ microbial breakdown of CHCA and CHDCA. At Site 2, δC-PLFA values from -60.6 to -24.5‰ indicated uptake of a C-depleted substrate such as biogenic methane and not C-labelled ACA. Determination of the microbial community using 16s RNA sequencing confirmed the presence of methane-oxidizing bacteria in the subsurface at Site 2. The in situ biodegradation of NAs at Site 1 demonstrates that the indigenous microbial population in the shallow subsurface near tailings ponds can readily break down some of these compounds prior to surface water discharge. The lack of evidence for microbial uptake of C-labelled ACA at Site 2 demonstrates that other NAs, in particular tricyclic diamondoid acids, may persist in the environment following seepage from tailings ponds or natural sources.
从尾矿池渗漏到地表水和地下水中的环烷酸(NAs)是与加拿大艾伯塔省油砂矿开采作业相关的主要环境问题之一。在这里,我们报告了使用 C 标记的 NA 替代物来评估源自两个不同地点的油砂尾矿池的地下水流动路径的固有生物降解:一个冰川河流含水层(地点 1)和一个低洼湿地(地点 2)。含有羧基标记(99%)NA 替代物(环己烷羧酸,CHCA;1,2-环己烷二羧酸,CHDCA;1-金刚烷羧酸,ACA)的微宇宙被降低到监测井中几个月,以允许足够的时间用于在当地含水层条件下进行基质降解和生物膜形成。从生物膜中提取磷脂脂肪酸(PLFA),作为活性微生物种群的生物标志物,用于稳定碳同位素(δC)分析。在地点 1,高度 C 富集的 δC 值(高达约+7100‰)证实了 CHCA 和 CHDCA 的原位微生物降解。在地点 2,从-60.6 到-24.5‰的δC-PLFA 值表明吸收了一种 C 耗尽的底物,如生物甲烷,而不是 C 标记的 ACA。使用 16s RNA 测序确定微生物群落证实了地点 2 地下水中甲烷氧化菌的存在。地点 1 的 NA 原位生物降解表明,尾矿池附近浅层地下水中的土著微生物种群可以在地表水排放之前很容易地分解其中一些化合物。在地点 2 没有发现微生物摄取 C 标记的 ACA 的证据,这表明其他 NAs,特别是三环倍半萜酸,可能会在尾矿池或自然来源渗漏后在环境中持续存在。