Historical accumulation of potentially toxic trace elements resulting from mining activities in estuarine salt marshes sediments of the Asturias coastline (northern Spain)

被引:24
作者
Garcia-Ordiales, Efren [1 ]
Cienfuegos, Pablo [1 ]
Roqueni, Nieves [1 ]
Covelli, Stefano [2 ,3 ]
Flor-Blanco, German [4 ]
Fontolan, Giorgio [2 ,3 ]
Loredo, Jorge [1 ]
机构
[1] Univ Oviedo, Min Energy & Mat Engn Sch, ISYMA Res Grp, Oviedo, Spain
[2] Univ Trieste, Dept Math & Geosci, Trieste, Italy
[3] CoNISMa Consorzio Nazl Interuniv Sci Mare, Piazzale Flaminio 9, I-00196 Rome, Italy
[4] Univ Oviedo, Dept Geol, GeoQUO Res Grp, Oviedo, Spain
关键词
Geochronology; Salt marshes; Sediments; Mining; Mercury; Arsenic; METAL CONTAMINATION; GRADO LAGOON; HEAVY-METALS; DEPOSITION; EVOLUTION; DISTRICT; ALMADEN; PB-210; BAY; ENVIRONMENTS;
D O I
10.1007/s11356-017-0449-5
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The extensive extraction activity of mercury ores in Asturias (northwest Spain), also rich in As and Sb, has impacted the Nalon river estuary. The objective of this research was to assess the historical evolution of As-Hg-Sb accumulation in the salt marsh sediments of this area. For this purpose, sediment cores were collected from two different salt marshes (eastern and western river banks) in the estuarine environment to evaluate the degree of anthropogenic enrichment and the geochronology of As-Hg-Sb accumulation. Core subsampling was performed by cutting 2-cm-thick slices of sediments. The subsamples were then analysed for several physical and chemical parameters. Sedimentation rate was assessed by measuring short-lived radionuclides (excess Pb-210 and Cs-137). Pre-mining levels of As-Hg-Sb were observed at core depths below 50cm. In the less extended salt marsh (eastern river bank), maximum As-Hg-Sb concentrations of 87.48, 3.66, and 5.75gg(-1), respectively, were found at the core top as a consequence of long-term mining activity in the area. The vertical distribution of As-Hg-Sb was influenced by the single-point contamination sources, whereas grain-size variability and diagenetic remobilisation did not seem affected. Geochronological measurements showed that the depositional fluxes of As-Hg-Sb were influenced by anthropogenic input after 1900, when mining activity in the area was most intense. Hg mining ceased in 1969; however, the corresponding core profiles did not show a drastic decreasing trend in element fluxes, implying that the river drainage basin retains some memory of contamination which affects riverine sediments. A preliminary gross estimation of total As-Hg-Sb trapped in the Nalon river salt marsh sediments amounted to approximately 18.7, 1.0, and 0.7t, respectively. These morphological structures suffer erosive processes, thus representing a potential source of these elements associated with sediments; consequently, management conservation and monitoring of salt marshes should be taken into consideration from this environmental point of view.
引用
收藏
页码:3115 / 3128
页数:14
相关论文
共 49 条
[1]   VERTICAL SALT-MARSH ACCRETION SINCE THE ROMAN PERIOD IN THE SEVERN ESTUARY, SOUTHWEST BRITAIN [J].
ALLEN, JRL ;
RAE, JE .
MARINE GEOLOGY, 1988, 83 (1-4) :225-235
[3]  
Andersen TJ, 2017, DEV PALEOENVIRON RES, V20, P121, DOI 10.1007/978-94-024-0990-1_6
[4]  
[Anonymous], 2001, Canadian Sediment Quality Guidelines for the Protection of Aquatic Life
[5]  
[Anonymous], 1998, ATLAS CAESIUM DEPOSI
[6]  
[Anonymous], 2012, GEOCHEMICAL ATLAS SP
[7]   THE ASSESSMENT OF PB-210 DATA FROM SITES WITH VARYING SEDIMENT ACCUMULATION RATES [J].
APPLEBY, PG ;
OLDFIELD, F .
HYDROBIOLOGIA, 1983, 103 (JUL) :29-35
[8]   The impact of sulphide oxidation on dissolved metal (Cd, Zn, Cu, Cr, Co, Ni, U) inputs into the Lot-Garonne fluvial system (France) [J].
Audry, S ;
Blanc, G ;
Schäfer, J .
APPLIED GEOCHEMISTRY, 2005, 20 (05) :919-931
[9]   Determination of sediment metal background concentrations and enrichment in marine environments - A critical review [J].
Birch, G. F. .
SCIENCE OF THE TOTAL ENVIRONMENT, 2017, 580 :813-831
[10]  
Bricker SB, 1996, SCI TOTAL ENVIRON, V179, P27, DOI 10.1016/0048-9697(96)90047-9