The impact of mine dewatering on the hydrology and mercury bioeochemistry of peatlands in the Hudson / James Bay lowland: The De Beers Victor Diamond Mine

矿山脱水对哈德逊/詹姆斯湾低地泥炭地水文和汞生物化学的影响：戴比尔斯维克多钻石矿

• 批准号: 360525-2007
• 负责人: Price, Jonathan
• 金额: $ 15.54万
• 依托单位: University of Waterloo
• 依托单位国家: 加拿大
• 项目类别: Collaborative Research and Development Grants
• 财政年份: 2008
• 资助国家: 加拿大
• 起止时间: 2008-01-01 至 2009-12-31
• 项目状态: 已结题
• 来源: https://www.nserc-crsng.gc.ca/ase-oro/Details-Detailles_eng.asp?id=403778
• 关键词: impact; mine; dewatering; hydrology; mercury

Diamond mining operations near Attawapiskat, Ontario are set to begin in early 2008. Over 90% of this area is covered by peatlands (muskeg). Dewatering of the mine will pull water from the underlying permeable limestone aquifer that could cause or accelerate downward seepage of water from the surface system, and partially drain about 3000 km2 of peatland. We anticipate distinct spatial patterns of drainage related to the strength of the connection between the upper and lower hydrological systems. Relatively permeable bioherms (ancient coral reefs) that protrude to the surface from the bedrock aquifer through the layer of fine-grained sediments that directly underlie the peatland, are expected to provide "windows" of seepage. Where partial drainage of peatland occurs the ecosystem will change, notably the vegetation patterns. DeBeers has made a substantial financial contribution to a research project which aims to explore and document the hydrogeological linkages between the surface (peatland) and deep (limestone) aquifer systems. The current proposal builds on that research by 1) examining in more detail the peatland drainage systems (water table, soil moisture, flow pathways) so we can construct a water budget that includes a range of peatland types; 2) investigating the mercury dynamics in this system, since we suspect that the disturbance will cause methylization of the naturally occurring mercury, hence its liberation into surface waters; and 3) expanding the scale of disturbance-monitoring with the addition of a remote sensing component which will detect changes in water-sensitive vegetation communities and peatland surface configurations - and thus allow us to interpret the broader impacts and responses of the mining activity.

安大略Attawapiskat附近的钻石开采作业将于2008年初开始。超过90%的面积被泥炭地（沼泽）覆盖。矿井的排水将从下面的可渗透石灰岩含水层中抽水，这可能导致或加速水从地表系统向下渗透，并部分排出约3000平方公里的泥炭地。我们预计不同的空间格局的排水有关的强度之间的连接的上部和下部的水文系统。从基岩含水层穿过泥炭地正下方的细粒沉积物层突出到地表的相对渗透性生物礁（古珊瑚礁）预计将提供渗漏“窗口”。当泥炭地出现部分排水时，生态系统将发生变化，特别是植被模式。戴比尔斯公司为一个研究项目提供了大量财政捐助，该项目旨在探索和记录地表（泥炭地）和深层（石灰岩）含水层系统之间的水文地质联系。目前的建议是建立在这项研究的基础上的：1）更详细地研究泥炭地的排水系统（地下水位、土壤湿度、流动路径），从而可以构建一个包括一系列泥炭地类型的水收支; 2）调查该系统中的汞动力学，因为我们怀疑扰动会导致天然存在的汞甲基化，从而释放到地表沃茨中; 3）扩大扰动监测的规模，增加遥感部分，以探测对水敏感的植被群落和泥炭地表面形态的变化，从而使我们能够解释采矿活动的更广泛影响和反应。