Coynel Alexandra, Schäfer Jörg, Dabrin Aymeric, Girardot Naïg, Blanc Gérard
Université Bordeaux 1, UMR CNRS 5805 EPOC Avenue des Facultés, 33405 Talence Cedex, France.
Water Res. 2007 Aug;41(15):3420-8. doi: 10.1016/j.watres.2007.04.019. Epub 2007 May 1.
The Riou Mort watershed, strongly affected by former coal mining and Zn ore treatment, has been the major source of the historical polymetallic pollution of the Lot-Garonne-Gironde fluvial-estuarine system. Two decades after the end of ore treatment, the former industrial area still contributes important amounts of metals/metalloids from various, partly unidentified, sources to the downstream river system. This study presents the high spatial variability of metal/metalloid (Cd, Zn, As, Sb, U, V) concentrations in water and suspended particulate matter (SPM) from eight observation sites during a short, intense flood event. Despite important dilution effects, the observed concentration levels at the different sites suggested additional Cd and Zn inputs, probably from polluted groundwater. This formerly unknown metal source was then localized and characterized by sampling water and SPM along two longitudinal profiles during different hydrological situations. Groundwater inputs of "truly dissolved" (<0.02 microm) Cd and Zn occurred along approximately 200 m, contributing 43% and 28% to the total annual (2004) Cd and Zn fluxes in the Riou Mort River. The estimated groundwater concentrations of Cd and Zn (2500-6700 and 83,000-170,000 microg l(-1), respectively) in the source zone were consistent with values measured in samples from the near aquifer (5400-13,000 and 200,000-400,000 microg l(-1)). The present work induced concrete remediation actions (pumping and treatment of the polluted groundwater), that are expected to strongly reduce dissolved Cd and Zn emissions into the Riou Mort River.
里奥莫尔特流域曾受到以往煤矿开采和锌矿处理的严重影响,一直是洛特-加龙河-吉伦特河河口系统历史多金属污染的主要来源。在矿石处理结束二十年后,这片 former industrial area 仍从各种(部分未明确的)来源向河流下游系统输送大量金属/类金属。本研究展示了在一次短暂而强烈的洪水事件中,八个观测点的水和悬浮颗粒物(SPM)中金属/类金属(镉、锌、砷、锑、铀、钒)浓度的高空间变异性。尽管有重要的稀释作用,但不同观测点的实测浓度水平表明可能有额外的镉和锌输入,可能来自受污染的地下水。然后通过在不同水文情况下沿两条纵向剖面采集水和 SPM 样本,对这个此前未知的金属来源进行了定位和特征描述。“真正溶解的”(<0.02 微米)镉和锌的地下水输入沿约 200 米的范围发生,分别占里奥莫尔特河 2004 年全年镉和锌通量的 43%和 28%。源区镉和锌的估计地下水浓度(分别为 2500 - 6700 和 83000 - 170000 微克/升)与附近含水层样本的测量值(5400 - 13000 和 200000 - 400000 微克/升)一致。目前的工作引发了具体的修复行动(抽取和处理受污染的地下水),预计这将大幅减少溶解态镉和锌向里奥莫尔特河的排放。