Masson Matthieu, Schäfer Jörg, Blanc Gérard, Pierre Anschutz
Université Bordeaux 1, UMR CNRS 5805 EPOC, TGM (Traceurs Géochimiques et Minéralogiques), Av. des Facultés, 33405 Talence Cedex, France.
Sci Total Environ. 2007 Feb 1;373(1):196-207. doi: 10.1016/j.scitotenv.2006.10.039. Epub 2006 Dec 13.
Daily measurements of water discharges and suspended particulate matter (SPM) concentrations and monthly analyses for arsenic were conducted from 1999 to 2005 on the Garonne, Dordogne and Isle Rivers, the three main tributaries of the Gironde Estuary, France. Despite the known historical polymetallic pollution affecting the Lot-Garonne River system, the highest As concentration level was observed in the Isle River. This was explained by the geological context and various Au/As deposits in this watershed. In the three studied rivers, dissolved As concentrations showed important seasonal variations with maximum values in summer. The dissolved As concentrations were closely related to water temperature and their increase in spring/summer appeared to be induced by water temperatures above approximately 15 degrees C, independently from discharge. The reduction of As(V) to more soluble As(III) and/or destruction of solid As carrier phases by micro-organisms could explain this observation, suggesting that temperature-dependent biogeochemical processes play an important role in controlling As partition and speciation in fluvial systems. Water and SPM fluxes in the Garonne River mainly control arsenic inputs into the Gironde Estuary and the downstream coastal zones. Based on the present data, we propose an empirical model to roughly estimate the annual dissolved and particulate As fluxes in the Garonne, Dordogne and Isle Rivers from annual water and SPM fluxes. The comparison of observed As fluxes and those estimated from the empirical model suggests that resuspension of historical, polluted reservoir sediments during a major flood accounted for approximately 50% of the annual As fluxes in 2003.
1999年至2005年期间,对法国吉伦特河口的三条主要支流加龙河、多尔多涅河和 Isle 河进行了每日水流量和悬浮颗粒物(SPM)浓度测量以及每月砷含量分析。尽管已知历史上多金属污染影响了洛特 - 加龙河水系,但在 Isle 河中观察到了最高的砷浓度水平。这是由该流域的地质背景和各种金/砷矿床所解释的。在这三条研究河流中,溶解态砷浓度呈现出重要的季节性变化,夏季达到最大值。溶解态砷浓度与水温密切相关,其在春季/夏季的增加似乎是由水温高于约15摄氏度引起的,与流量无关。微生物将五价砷还原为更易溶的三价砷和/或破坏固体砷载体相可以解释这一现象,表明温度依赖性生物地球化学过程在控制河流系统中砷的分配和形态方面起着重要作用。加龙河的水和SPM通量主要控制着进入吉伦特河口和下游沿海地区的砷输入。基于目前的数据,我们提出了一个经验模型,以根据年水流量和SPM通量大致估算加龙河、多尔多涅河和 Isle 河的年溶解态和颗粒态砷通量。观察到的砷通量与根据经验模型估算的通量之间的比较表明,2003年一次大洪水期间历史污染水库沉积物的再悬浮占年砷通量的约50%。