Characterization of how contaminants arise in a dredged marine sediment and analysis of the effect of natural weathering

被引:26
作者
Couvidat, Julien [1 ]
Chatain, Vincent [1 ]
Bouzahzah, Hassan [3 ]
Benzaazoua, Mostafa [1 ,2 ]
机构
[1] Univ Lyon, INSA Lyon, Lab Dechets Eaux Environm Pollut DEEP, EA 7429, 7 Rue Phys, F-69621 Villeurbanne, France
[2] UQAT Polytech, IRME, 445 Boul Univ, Rouyn Noranda, PQ J9X 5E4, Canada
[3] Univ Liege ULG, Lab Genie Mineral Mat & Environm GeMMe, Allee Decouverte,13-A Bat B52-3 Sart Tilman, B-4000 Liege, Belgium
关键词
Biogeochemical reactivity; Contaminated marine sediment; Sulfides; Leaching; Oxidation; Organic matter; ACID-VOLATILE SULFIDES; HEAVY-METALS; ELEMENT MOBILITY; DIFFUSION METHOD; REMEDIATION; SPECIATION; PREDICTION; PYRITE; ZN; BIOAVAILABILITY;
D O I
10.1016/j.scitotenv.2017.12.130
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Millions of tons of contaminated sediments are dredged each year from the main harbors in France. When removed from water, these sediments are very reactive, therefore their geochemical behavior must be understood in order to avoid dispersion of contaminated lixiviates in the surrounding soils. In this objective, it is necessary to evaluate the principal physicochemical parameters, and also achieve advanced mineralogical characterization. These studied sediments are highly contaminated by metals, notably copper (1445 and 835 mg/kg, in the unweathered and naturally-weathered sediments, respectively), lead (760 and 1260 mg/kg, respectively), zinc (2085 and 2550 mg/kg, respectively), as well as by organic contaminants (PAH, PCB) and organometallics (organotins). A high concentration of sulfide minerals was also observed both in the unweathered sediment preserved under water (3.4 wt% of pyrite especially), and in the naturally weathered sediment (2 wt% pyrite), and in particular framboidal pyrite was observed in the two materials. The presence of reactive mineral species in the naturally-weathered sediment can be explained by the deposit of a protective layer, composed of sulfide and their oxidation products (sulfate and iron oxides), thus preventing oxygen from diffusing through to the sulfide minerals. Additionally, the presence of aluminosilicates aggregates coating the sulfide minerals could also explain their presence in the naturally-weathered sediment. As organic matter is one of the principal constituents of the sediments (5.8 and 6.3 wt% total organic carbon in the unweathered and weathered sediment, respectively), the aggregates are probably partially constituted of refractory humic material. It therefore appears that the natural weathering has led to a significant decrease in PAHs and organotins, but not in PCBs. The evolution of the granulometric structure and the distribution of the metallic contaminants could therefore lead us to consider a treatment by size separation, and a possible valorization of the dredged sediments in civil engineering. (C) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:323 / 332
页数:10
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