Jessen Gerdhard L, Chen Lin-Xing, Mori Jiro F, Nelson Tara E Colenbrander, Slater Gregory F, Lindsay Matthew B J, Banfield Jillian F, Warren Lesley A
Instituto de Ciencias Marinas y Limnológicas, Universidad Austral de Chile, Valdivia 5090000, Chile.
Department of Civil and Mineral Engineering, University of Toronto, Toronto, ON M5S 1A4, Canada.
Microorganisms. 2022 Feb 26;10(3):510. doi: 10.3390/microorganisms10030510.
Here, we examine the geobiological response to a whole-lake alum (aluminum sulfate) treatment (2016) of Base Mine Lake (BML), the first pilot-scale pit lake established in the Alberta oil sands region. The rationale for trialing this management amendment was based on its successful use to reduce internal phosphorus loading to eutrophying lakes. Modest increases in water cap epilimnetic oxygen concentrations, associated with increased Secchi depths and chlorophyll-a concentrations, were co-incident with anoxic waters immediately above the fluid fine tailings (FFT) layer post alum. Decreased water cap nitrate and detectable sulfide concentrations, as well as increased hypolimnetic phospholipid fatty acid abundances, signaled greater anaerobic heterotrophic activity. Shifts in microbial community to groups associated with greater organic carbon degradation (i.e., SAR11-LD12 subclade) and the SRB group Desulfuromonodales emerged post alum and the loss of specialist groups associated with carbon-limited, ammonia-rich restricted niches (i.e., MBAE14) also occurred. Alum treatment resulted in additional oxygen consumption associated with increased autochthonous carbon production, watercap anoxia and sulfide generation, which further exacerbate oxygen consumption associated with on-going FFT mobilized reductants. The results illustrate the importance of understanding the broader biogeochemical implications of adaptive management interventions to avoid unanticipated outcomes that pose greater risks and improve tailings reclamation for oil sands operations and, more broadly, the global mining sector.
在此,我们研究了对基础矿湖(BML)进行全湖明矾(硫酸铝)处理(2016年)后的地球生物学响应,基础矿湖是阿尔伯塔省油砂地区建立的首个中试规模的矿坑湖。试验这种管理改良措施的基本原理是基于其成功用于减少富营养化湖泊的内部磷负荷。与塞氏深度和叶绿素-a浓度增加相关的水表上层水体氧气浓度适度增加,与明矾处理后流体细尾矿(FFT)层上方立即出现的缺氧水体同时出现。水表硝酸盐和可检测硫化物浓度降低,以及下层水体磷脂脂肪酸丰度增加,表明厌氧异养活性增强。明矾处理后微生物群落向与更高有机碳降解相关的类群(即SAR11-LD12亚分支)和脱硫单胞菌目SRB类群转变,并且与碳限制、氨丰富的受限生态位相关的特化类群(即MBAE14)也消失了。明矾处理导致与自生性碳产量增加、水表缺氧和硫化物生成相关的额外氧气消耗,这进一步加剧了与持续的FFT动员还原剂相关的氧气消耗。结果表明,了解适应性管理干预措施更广泛的生物地球化学影响对于避免产生带来更大风险的意外结果以及改善油砂作业尾矿复垦以及更广泛的全球采矿业的尾矿复垦具有重要意义。