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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Mercury in the Lot-Garonne River system (France): Sources, fluxes and anthropogenic component
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Mercury in the Lot-Garonne River system (France): Sources, fluxes and anthropogenic component

机译:Lot-Garonne河系中的汞(法国):来源,通量和人为成分

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Dissolved and particulate Hg fluxes in the Lot-Garonne-Gironde fluvial-estuarine system were obtained from observation of daily discharge and suspended particulate matter (SPM) concentrations. In addition to the measurements of the total dissolved (< 0.45 gm) and particulate Hg (> 0.45 gm), called HgTD and HgTp respectively, the dissolved inorganic Hg species (HgRD) were determined monthly. Geochemical background values for HgTp in sediments and SPM were similar to crustal values and to typical concentrations in SPM of non-contaminated river systems, respectively. The Riou Mort watershed already known as the origin of important historical polymetallic (e.g., Cd, Zn) pollution was identified as an important Hg point source. In the downstream Lot River, Hg concentrations were clearly higher than those in other moderately contaminated systems. The mean relative contribution of HgRD to HgTD in the Lot River and in the Garonne River was close to 25% and 50%, respectively, and showed no correlation with water discharge or SPM concentration. Depending on the origin and nature of SPM, HgTp concentrations were correlated or not with particulate organic C (POC). Maximum HgTp concentrations were measured in samples containing low POC concentrations and were attributed to sediment resuspension. In contrast, high POC concentrations (6-17%) during algal blooms were associated with low/moderate HgTp concentrations (< 0.5 mg kg(-1)) at different sites, suggesting that Hg concentrations in fluvial phytoplankton may be limited by bioavailability of dissolved Hg and/or physiologically controlled Hg accumulation. Mercury was mostly (up to 98%) transported in the particulate phase with estimated annual Hg fluxes at the outlet of the Lot River system ranging from 35 to 530 kg a(-1) for the past decade. The minimum anthropogenic component (58-84% of total Hg fluxes) could not be explained by present Riou Mort point source contributions, suggesting important Hg release from contaminated sediment as a major source and from downstream point sources (e.g., coal-fired power plants and/or metal processing industries). HgTp concentrations and fluxes were strongly related to hydrologic variations and were clearly increased by riverbed dredging during lock construction. Therefore, the estimated Hg stocks in the Lot River sediment (5-13 tons) represent an important potential Hg source for the downstream fluvial-estuarine system. (c) 2006 Elsevier Ltd. All rights reserved.
机译:通过观察每日排放量和悬浮颗粒物(SPM)的浓度,获得了Lot-Garonne-Gironde河口系统中的溶解汞和颗粒汞通量。除了测量分别称为HgTD和HgTp的总溶解(<0.45 gm)和颗粒Hg(> 0.45 gm)之外,还每月测定溶解的无机Hg种类(HgRD)。沉积物和SPM中HgTp的地球化学背景值分别类似于无污染河系的地壳值和SPM中的典型浓度。已被称为重要的历史多金属(例如Cd,Zn)污染起源的Riou Mort流域被确定为重要的Hg点源。在下游的洛特河,汞浓度明显高于其他中等污染系统中的汞浓度。洛特河和加龙河中HgRD对HgTD的平均相对贡献分别接近25%和50%,并且与水排放或SPM浓度无关。根据SPM的来源和性质,HgTp的浓度与有机碳(POC)是否相关。在低POC浓度的样品中测量了最大HgTp浓度,这归因于沉积物的重悬。相比之下,藻华期间的高POC浓度(6-17%)与不同位置的低/中等HgTp浓度(<0.5 mg kg(-1))相关,表明河流浮游植物中Hg的浓度可能受到生物利用度的限制。溶解的汞和/或生理控制的汞积累。在过去十年中,汞主要以颗粒形式(达98%)运输,估计在洛特河系统出口处的年汞通量为35至530 kg a(-1)。最小的人为成分(占总汞通量的58-84%)无法由Riou Mort点源的当前贡献来解释,这表明从污染的沉积物(作为主要来源)和下游点源(例如,燃煤电厂)中释放出大量的Hg和/或金属加工行业)。 HgTp的浓度和通量与水文变化密切相关,并且在闸门施工期间因河床疏ging而明显增加。因此,估计的罗特河底泥中的汞储量(5-13吨)是下游河口系统的重要潜在汞来源。 (c)2006 Elsevier Ltd.保留所有权利。

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