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Historical mass balance of cadmium decontamination trends in a major European continent-ocean transition system: Case study of the Gironde Estuary

机译:欧洲主要大陆-海洋过渡系统中镉去污趋势的历史质量平衡:以吉伦特河口为例

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摘要

Despite the effective remediation efforts following the end of the metallurgic activity thirty years ago upstream the Lot River watershed, the levels of cadmium (Cd) accumulated in wild oysters from the downstream Gironde Estuary still exceed nowadays the admissible human consumption limit (5 mg/kg, d.w.). The main goal of this work is to quantify the role of sediments as long-term intra-estuarine sources or sinks of Cd and the transport of this contaminant towards the estuary mouth taking as case study the example of the highly turbid Gironde Estuary. The original estimation for the annual net fluxes of the suspended particulate matter (F-netSPM(year ) ) and particulate Cd (F-netCd(pyear) ) presented in this work between 1990 and 2020 indicates that 80 of the Cd discharged into the ocean is in dissolved form (Cd-d). The values of F(net)(Cdp)( yea)r vary proportionally to those of F-netSPM(year) and ranged between 0.1 and 1.4 t/y, with a ten-year average decreasing from 0.8 to 0.6 t/y for the past 30 years. The differences between ten-year total (Cdp + Cdd) gross and net fluxes show that Cd has effectively been stored in estuarine sediments. This Cd storage was of about 43, 22 and 13 t for the 1990s, 2000s and 2010s, respectively. However, during years of low gross fluxes, estuarine sediments act as additional, secondary sources of bioavailable/dissolved Cd into the water column, potentially relating to the continued observations of high Cd concentrations in wild oysters at the estuary mouth. In addition to the natural solubility of Cd-p along the salinity and turbidity gradients of the estuary, natural and anthropogenic remobilization of bottom sediment particles further contribute to its mobilization from the particle phase, along with other numerous inorganic/organic pollutants. The mass balances presented in this work could support a new sediment management policy potentially more beneficial to the estuarine ecosystem.
机译:尽管在30年前洛特河流域上游的冶金活动结束后进行了有效的补救工作,但下游吉伦特河口野生牡蛎中积累的镉(Cd)含量仍然超过目前允许的人类消费限度(5毫克/千克,分重比)。这项工作的主要目标是以高度浑浊的吉伦特河口为例,量化沉积物作为长期河口内镉源或汇的作用,以及这种污染物向河口的迁移。本文对1990年至2020年间悬浮颗粒物(F-netSPM(年))和颗粒镉(F-netCd(pyear))的年净通量的原始估计表明,80%的镉排放到海洋中是溶解形式(Cd-d)。F(net)(Cdp)(yes)r的值与F-netSPM(year)的值成正比变化,范围在0.1至1.4吨/年之间,过去30年的十年平均值从0.8吨/年下降到0.6吨/年。10年总通量(Cdp+Cdd)总通量和净通量之间的差异表明,Cd已有效地储存在河口沉积物中。1990年代、2000年代和2010年代的镉储量分别约为43、22和13吨。然而,在总通量较低的年份,河口沉积物是进入水体的生物可利用/溶解镉的额外次要来源,这可能与在河口野生牡蛎中持续观察到高镉浓度有关。除了Cd-p沿河口盐度和浊度梯度的天然溶解性外,底部沉积物颗粒的自然和人为再动员进一步有助于其从颗粒相以及其他众多无机/有机污染物中迁移。这项工作中提出的质量平衡可以支持新的沉积物管理政策,可能对河口生态系统更有利。

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