滩涂围垦区土壤重金属调查及生态风险评价——以盐城市弶港镇为例

以苏北盐城弶港镇滩涂围垦土壤为研究对象,进行了重金属Cr、Pb、As、Cd、Hg的测定及其风险评价,为我国沿海滩涂种植业的发展提供依据,并为其他国家和地区相关研究提供参考。结果表明,该区域土壤中5种重金属含量均未超过《国家土壤环境质量标准》（GB15618—1995）一级标准限制,农田土壤Cr、As、Cd含量较高,郊区菜地土壤Pb、Hg含量较高;重金属Cr、Pb、As、Cd含量在不同土地利用类型间存在显著性差异;Hg含量差异不显著。采用地积累指数法进行评估可知,土壤没有受到单项重金属污染。依据内梅罗综合指数法评估可知,潮间带沉积物、工业区土壤、滩涂围垦熟化的土壤没有受到重金属污染;郊区菜地与农田土壤的污染等级已达到警戒线,污染水平属于＂尚清洁＂。Hakanson潜在生态风险评价结果表明,区域内土壤重金属处于无风险等级,尚不具有潜在生态风险。     

滨岸排污口对潮滩沉积物中重金属的影响研究

通过对排污口附近及对照点的潮滩沉积物中重金属Zn ,Cu ,Cr和Pb的含量分析发现:各采样点沉积物中的重金属含量均高于环境背景值,平均含量约为环境背景值的2～3倍,排污口附近潮滩沉积物中重金属的含量明显高于对照点潮滩沉积物中的含量;各采样点的柱状沉积物中重金属的含量随深度的变化呈现出一定的变化规律;在垃圾填埋场附近高中低潮滩由于距离排污口的远近不同,表层沉积物中重金属的含量依次降低;对各采样点沉积物中重金属含量的相关性分析发现各点沉积物中累积的重金属的来源有所不同:在排污口附近潮滩的沉积物中重金属主要来源于排污口排放的污水,而对照点朝阳农场潮滩沉积物中重金属主要来源于自然的本底输入或海水外源输入     

秦岭神安沟矿区沟道地表水和沉积物中重金属分布形态研究

为了探讨重金属在矿山水体环境中的富集规律,以秦岭神安沟矿区沟道地表水、沉积物中的重金属为研究对象,测试了各类重金属含量,并利用Tessier五步连续萃取法分析了沉积物中重金属的5种形态,旨在为该矿区环境恢复治理提供参考。结果显示,未受采矿活动影响的对照区地表水与沉积物均未检出Zn、Pb、Cd,对照区未受污染。受开采活动影响的上、中、下游地表水、沉积物受到Pb、Cd不同程度的污染,下游地表水Pb、Cd分别超标5.3倍、43.3倍,不符合农田灌溉用水水质要求;上、中、下游沉积物中重金属污染负荷指数均达Ⅲ级,沟道沉积物已受到严重污染。沉积物中重金属形态分布特征为：Zn、Cd以有机结合态所占比例最高,Pb以铁锰氧化物结合态所占比例最高,Zn、Pb的生物有效性高。由此得出下游地表水不适于灌溉。由于矿方目前已终止尾矿库淋滤水向沟道排放,沉积物中各类重金属含量已趋于稳定,矿区神安沟地表水、沉积物重金属污染严重,亟需治理恢复。     

Heavy Metals in Freshly Deposited Stream Sediments of Rivers Associated with Urbanisation of the Ganga Plain,India

Freshly deposited stream sediments from six urban centres of the Ganga Plain were collected and analysed for heavy metals to obtain a general scenery of sediment quality. The concentrations of heavy metals varied within a wide range for Cr (115–817), Mn (440–1 750), Fe (28 700–61 100), Co (11.7–29.0), Ni (35–538), Cu (33–1 204), Zn (90–1 974), Pb (14–856) and Cd (0.14–114.8) in mg kg^-1. Metal enrichment factors for the stream sediments were <1.5 for Mn, Fe and Co; 1.5–4.1 for Cr, Ni, Cu, Zn and Pb; and 34 for Cd. The anthropogenic source in metals concentrations contributes to 59% Cr, 49% Cu, 52% Zn, 51% Pb and 77% Cd. High positive correlation between concentrations of Cr/Ni, Cr/Cu, Cr/Zn, Ni/Zn, Ni/Cu, Cu/Zn, Cu/Cd, Cu/Pb, Fe/Co, Mn/Co, Zn/Cd, Zn/Pb and Cd/Pb indicate either their common urban origin or their common sink in the stream sediments. The binding capacity of selected metals to sediment carbon and sulphur decreases in order of Zn > Cu > Cr > Ni and Cu > Zn > Cr > Ni, respectively. Stream sediments from Lucknow, Kanpur, Delhi and Agra urban centres have been classified by the proposed Sediment Pollution Index as highly polluted to dangerous sediments. Heavy metal analysis in the <20-μm-fraction of stream sediments appears to be an adequate method for the environmental assessment of urbanisation activities on alluvial rivers. The present study reveals that urban centres act as sources of Cr, Ni, Cu, Zn, Pb and Cd and cause metallic sediment pollution in rivers of the Ganga Plain.     

Contaminated sediments as a potential source of Zn, Pb, and Cd for a river system in the historical metalliferous ore mining and smelting industry area of South Poland

Background, aim, and scope  Elevated levels of heavy metals in the aquatic and soil systems can be caused by the weathering of mineralized rocks. This enrichment is often considerably enlarged by historical and current mining and smelting activities. In Poland, the most contaminated river systems are those in the Silesia region. The metalliferous ore mining and smelting industries have been the main sources of heavy metal pollutions over the last 100–170 years. The previous and present studies have shown very high concentrations of heavy metals in the bottom sediments of the Mala Panew River, the most polluted tributary of the Oder River. The main objective of this work was to study temporary changes of selected metal (Zn, Pb, and Cd) concentrations in upper layer of bottom sediments at the measuring point near the outlet of the Mala Panew River into the Oder River, and to determine the vertical distribution of the metals in the sediment cores from the most polluted middle part of this river. The mobility of the metals and their potential bioavailability were assessed based on metal partitioning in the sediments and metal concentrations in pore waters. The presented data were compared with metal concentrations in aquatic sediments from similar historical mining and smelting sites in Poland and other countries. Methods  The upper layer of bottom sediment samples from the same Mala Panew River measuring point were collected six times in the period 1997–2005, while five sediment cores were collected once from the middle course of Mala Panew River in 2006. Abiotic parameters such as pH and Eh have been determined in situ. Metal contents were determined in the <20 and <63 μm size fractions of sediments after digestion in a microwave oven with aqua regia or concentrated nitric acid. Metal mobility was assessed in the selected sediment cores by the chemical forms of metals (sequential extraction method) and their concentrations in pore waters were investigated. Results  The concentrations of Cd, Pb, and Zn in the upper layer of sediments varied, depending on both the season and the year of sampling. Their mean concentrations (from six samplings) are [mg/kg]: Zn 1,846, Pb 229 and Cd 73. The metal concentrations in the sediment cores varied with the depth in the range of [mg/kg]: 0.18–559 for Cd, 26.2–3,309 for Pb and 126–11,153 for Zn, although the highest accumulations generally could be observed in the deeper layers. The most mobile metal fractions, i.e., exchangeable, carbonate and easily reducible fractions, are typical of Zn and Cd. Cadmium was found to be the most mobile metal and its relative contribution ranges from 84 to 96%, while in the case of Zn it ranged from 45 to 94%. Lead is mainly associated with the moderately reducible fraction (30–60%). Relative contributions of metal chemical forms slightly vary with the depth in the sediment profile. The results obtained for the pore water samples show very high concentrations of the metals studied, especially in the case of Cd (31–960 μg/dm³) and Zn (300–4,400 μg/dm³). Discussion  Accumulation of Cd, Pb, and Zn in the upper layer of the bottom sediments and in the sediment core samples from the Mala Panew River is very high, considerably exceeding the local geochemical background. High contributions of mobile Cd and Zn and the toxicity of cadmium can cause environmental risk. Our measurements also suggest that mobile metals can migrate into groundwater, whereas the groundwater itself can leach some chemicals from river sediments, because of a relatively high water table in the study area, especially during rainfall periods. Comparison of the results obtained with the literature data from the last decade shows that the concentrations of Cd and Zn in the sediments from the Mala Panew River are the highest among other submersed sediments in Poland and other regions (e.g., the Mulde River, Germany). Conclusions  The Mala Panew River is one of the most polluted rivers when compared with similar historical mining and smelting areas in Poland and elsewhere. The sediments studied are strongly polluted with the metals analyzed. In the upper layer of the bottom sediments there has been no reduction of Zn and Cd amounts over the last decade, which could suggests a long-term migration and a secondary contamination. Considerably higher accumulations of metals in overbank sediment cores and in the deeper core section could result from strong contamination in previous decades and translocation of Cd and Zn (secondary pollutants). The relatively high concentrations of the two metals in pore waters support these findings. Cadmium is crucial in the environmental risk assessment because of its high mobility and toxicity. These data are important for water/sediment management in the transboundary Oder River catchment, situated in Poland, Germany and the Czech Republic. Recommendations and perspectives  It is important to assess mobility phase and pore water in the contaminated historical aquatic sediments. Such studies may help explain the changes, which take place in the sediment layers as well as at the water–sediment interface. Obtained results should be used for the risk assessment of the historical contaminated sediments at the local river-basin scale. The treatment of contaminated sediments, e.g., dragging activity, should be considered as very important in management strategies in order to avoid remobilization of metals.     

Metal Contamination of River Waters and Sediments from Effluents of Kaolin Processing in Brazil

In order to evaluate the metal contamination from kaolin industry discharges into rivers in the State of Minas Gerais, Brazil, samples of river water and fluvial sediment were collected up- and down-river from the industries and analysed todetect metal inputs. The metal examined included zinc, iron, andaluminium among others, being selected due to their toxicity andoccurence in waste waters. Metal inputs in the samples analysed appeared to be related to effluent discharges into the rivers. The river water showed high concentrations (in μg mL^-1) of Zn (355), Fe (354) and Al (303). Sediment investigations indicated heavy enrichment (SEF = 9.4) for Zn. The Geoaccumulation Index for this element accounted for 3 (moderately to heavy polluted). River water pH of the sample collected near the effluent discharge site reached 3.7, suggesting inadequate treatment.     

Schwermetallanreicherung und Schwermetallverfügbarkeit im Einsickerungsbereich von Stammablaufwasser in Buchenwäldern (Fagus sylvatica) des Wienerwaldes

Heavy metal enrichment and mobility in the infiltration zone of stemflow from beech (Fagus sylvatica) in the Vienna woods Filtering action of beech crowns in a polluted atmosphere produces acidic stemflow enriched with heavy metals. Series of soil profiles through the infiltration zone of stemflow waters were analyzed in three old growth beech stands on pseudogley (aqualf) soils of the northeastern Vienna Woods to study soil acidification and heavy metal accumulation and mobility: + In the infiltration zone of stemflow soil pH can be less than pH 3 and thus more than 2 pH units lower than in profiles more distant from the stem base. + Heavy metal contents of the soil peaked near the stembase. Maximum values for lead were 500 to 1.200 mg·kg^?1 soil, for copper 70 to 150 mg·kg^?1 soil and for zinc 250 to 500 mg·kg^?1 soil. + Manganese was not enriched but leached out from the soil profile. + The proportion of AED-complexable lead and copper to total lead and copper decreased under stemflow influence in the topsoil but increased in the subsoil. These results indicate that significant amounts of heavy metals are deposited with stemflow in beech stands of the Vienna Woods. Strong soil acidification enhances heavy metal solubility and thus promotes leaching into deeper soil strata.     

Verteilungsmuster lithogener,pedogener und anthropogener Schwermetalle in Böden

Distribution of lithogeneous, pedogeneous and anthropogeneous heavy metals in soils The study in hand shows relations between lithogeneously, pedogeneously and anthropogeneously enriched heavy metals and their concentration grades. Conclusions can be drawn from the vertical and horizontal distribution pattern of heavy metals on the nature and origin of their enrichment which is determined decisively by their mobility. Heavy metals enriched lithogeneously show relatively uniform as well as stratified concentration grades in the profile. A diminution of the heavy metal contents in all surface directions takes place starting from the centre of the lithogeneous enrichment. Pedogenetic processes lead to an increase of all element concentrations in certain soil horizons. Lateral transport causes an increase of heavy metal contents in the soils of low grounds compared with summits. Heavy metals enriched anthropogeneously are mostly accumulated in topsoils. Heavy metals concentrations due to dust immissions are characterized by a remarkable diminution of the concentration within the main wind direction. Heavy metal enrichments due to direct anthropogeneous charges are following the ground borders.     

Mikrosondenuntersuchungen an unterschiedlich stark mit Schwermetallen belasteten Böden. 2. Gehalte an Schwermetallen und anderen Elementen in Huminstoffaggregationen,Streustoffen und Holzkohlepartikeln

Electron microprobe studies on soil samples with varying heavy metal contamination. 2. Contents of heavy metals and other elements in aggregations of humic substances, litter residues and charcoal particles EMA point analysis show that the organic matter constituents of heavy metal contaminated soils are highly enriched with heavy metals. The maximal trace element accumulation were for Cu up to 13,000 mg/kg, for Zn up to 48,000 mg/kg, for Cd up to 2,100 mg/kg and for Pb up to 193,000 mg/kg. The affinity for the accumulation of the different heavy metals in aggregations of humic substances can be described by the sequence Cu > Pb ? Cd > Zn ? Ni > Co. In very strongly acidified humic top soil horizons the Pb and Cd accumulation in the organic matter constituents is in competition with the accumulation in Fe and Mn oxides. The heavy metal contents (especially of Cu) of the organic matter are often correlated with the content of organically bound calcium. The EMA results also show that high heavy metal amounts occur in combination with Ca-accumulations in the epidermis and the outer bark parenchym of decayed roots. EMA point analysis of the interior of fungus sclerotias show that sclerotias can contain high amounts of heavy metals, in particular lead (up to 49,700 mg Pb/kg). From statistical results of EMA point analysis follows that lead and other heavy metals attached to humic substances are not only bound as metal organic complexes but also as organic metal phosphate complexes. Also charcoal particles of polluted soils contain high amounts of heay metals. The accumulation affinity is quite similar to that of humic substances.     

南通市城市边缘带土壤重金属污染现状及评价

通过对不同土地利用方式下的7个样区进行系统的采样测定,对南通城市边缘带土壤重金属富集与污染状况进行了分析与评价。结果显示,研究区土壤未发生明显的重金属污染。但3个样区的土壤有轻度的重金属污染现象,Zn是发生富集最普遍的元素,约76%的样点土壤Zn富集指数>1,18%的样点土壤出现Zn的轻度污染。Cu、Pb等重金属元素导致的污染也在零星样点被发现。方差分析表明,土地利用方式不是导致研究区土壤重金属含量空间差异的主要因素,而土壤类型、样区空间环境与土壤重金属含量及富集、污染有相对密切的关系。     

Effect of Solid/Liquid Ratio on the Remobilization of Cu,Pb, Cd and Zn from Polluted River Sediment

The incidence of the solid/liquid ratio on thesolubilization of heavy metals from a polluted riversediment was assessed by batch experiments. Thepercentage of solubilized metal increases stronglywhen the concentration of the sediment-watersuspension decreases from 50 to 0.1 g L^-1. Thissolubilization behavior is described by a simpleequilibrium desorption model on the association of themetals and sediment. The association constantscalculated with this model indicate the affinitybetween the metals and the sediment (Pb > Cu > Zn> Cd). If polluted river sediments are in situresuspended, the decrease of the solid/liquid ratioassociated to this natural event could provoke theremobilization of metals trapped in sediments.     

Mercury Accumulation in Sediments of a Mangrove Ecosystem in SE Brazil

The Hg accumulation in sedimentary environments of a mangrove ecosystem in Sepetiba Bay, SE Brazil, was investigated. These environments include sediments of a mangrove forest, the main tidal creek that drains the forest, and the bare seaward-edge mud flat adjacent to forest and tidal creek. Maximum Hg concentration peaks in sediments from the mud flat (184 ng g^-1), tidal creek (98 ng g^-1), and mangrove forest (60 ng g^-1) correspond to enrichment factors of 6.1, 3.3, and 2.0 above the estimated average background level, respectively. Average inventories of Hg excess (background-corrected) concentrations were substantiallydifferent between environments, decreasing from mud flat sediments (5.2 mg m^-2) to creek sediments (3.3 mg m^-2)to mangrove forest sediments (0.9 mg m^-2). Mercury concentration profiles indicated a consistently higher accumulation of Hg in surface layers of mud flat and tidal creeksediments, whereas mangrove forest sediments showed a higher Hgaccumulation in root-rich subsurface layers, in agreement with an enrichment of Fe and organic matter contents. While Hg distribution in mud flat and tidal creek sediments appears to belargely affected by contamination, its distribution in mangrove forest substrate appears to be greatly affected by root-sedimentinteractions. Mercury levels in the study site were comparable tothose observed in coastal sediments under moderate Hg contamination at local and regional scales. Results indicate thatsedimentary environments surrounding the mangrove forest retain most of the anthropogenic Hg reaching the ecosystem. Since tidal waters have been previously demonstrated as the main source of metals to the site, it is suggested that the Hg retention in mudflat sediments precede and may avoid a higher Hg accumulation inlandward environments.     

Distribution,risk assessment,and source analysis of heavy metals in sediment of rivers located in the hilly area of southern China

Purpose

River sediment, the important sink and source of heavy metals, can provide critical information for aquatic ecosystem health. Heavy metal pollution has been a serious problem facing river systems worldwide and can adversely affect human beings via the food chain. However, no comprehensive study has been conducted on heavy metal pollution in sediments of river systems in the hilly area of southern China, which plays a key role in water supply and ecosystem balance. This study is aimed at comprehensively studying the pollution status of heavy metals in river sediments in the hilly area of southern China and apportioning sources.

Materials and methods

A total of 39 superficial sediment samples were collected from the upstream, midstream, and downstream of 13 rivers (Xiangjiang River, Zishui River, Yuanjiang River, and Lishui River located in Hunan Province; Ganjiang River, Xinjiang River, Fuhe River, Raohe River), and Xiushui River located in Jiangxi Province; Qiantangjiang River and Oujiang River located in Zhejiang Province; Minjiang River and Jiulongjiang River located in Fujian Province) in the hilly area of southern China. The total concentrations of metals of Mn, Zn, Cr, Co, Ni, Cu, As, Cd, Sb, Pb, and V were analyzed using the inductively coupled plasma-mass spectrometry method. The pollution status and potential ecological risk were assessed with the geoaccumulation index (I_geo), sediment quality guidelines (SQGs), and potential ecological risk index (RI). The source apportionment of heavy metals was performed by correlation analysis and principle component analysis (PCA).

Results and discussion

Results indicated that Mn, Zn, and Pb concentrations were significantly higher than other metals, especially in the upstream of the Jiulong River and midstream and downstream of the Xiangjiang River. Pollution assessment indicated that Cd pollution of sediments was most serious and that more than 50% of sampling sites were significantly polluted, with a very high potential ecological risk. The rivers in Hunan provinces (HN) were identified as the priority controlled rivers because of the high I_geo and RI index values. Correlation and PCA analysis indicated that Mn, Pb, and Zn originated from natural and mineral exploitation activities; As, V, Ni, and Sb originated from industrial wastewater and mineral-smelting activities; Cu and Co originated from agricultural activities; Cr and Ni originated from natural sources. While the most polluted Cd came from a combination of multiple sources described above.

Conclusions

Results indicated that Cd was the most common heavy metal pollutant, especially in river sediments of Hunan Province. Anthropogenic activities have become the main source of heavy metals in the river sediments of the hilly area of southern China. Special attention should be paid to Cd, and measures must be taken to prevent from further anthropogenic influence on heavy metal pollution.

     

Zeitschrift für Pflanzenernährung und Bodenkunde: Schwermetallgehalt von Wurzel und Sproßorganen der Rebe (Vitis vinifera L.) nach Düngung mit Müll-Klärschlammkompost

Heavy metal content of roots and shoots of vines (Vitis vinifera L.) after fertilization with garbage-sewage-sludge-compost The enrichment of Zn, Cu, Pb, Cd, Co, Ni and Cr from garbage-sewage-sludge-compost in vineyard soils, vines and must was studied in field-and pot-experiments. The following results were obtained: 1. In a field experiment, in which garbage-sewage-sludge-compost was applied, a marked soil enrichment of Zn, Cu, Pb, Cd and Cr was found. It was most evident at the 0–20 cm depth but also obvious at the 40–60 cm depth thus indicating downward migration. The soil was not enriched with Co and Ni. The heavy metal content of leaves, berries and must of riesling vines did not increase on the plots treated with garbage-sewage-sludge-compost. 2. In a pot trial, using an acid and an alkaline soil each mixed with garbage-sewage-sludge-compost, it was observed that only the uptake of Zn and Cu increased into the leaves, tendrils and wood of the riesling cuttings. In relation to the content of the substrate, the heavy metals were detected in the roots percentually in the following order: Cu, Cd > Zn > > Pb, Co, Ni, Cr The root contents were mostly substantially higher than those of the shoot. The migration from root to shoot decreased in the following percentual order: Zn > Cu > Cd, Pb 3. The heavy metal content decreased considerably from the roots to the upper plant organs. This was reflected in low concentrations of heavy metals in the vine must.     

copper,lead and zinc distribution in soils and sediments of the south-western coast of the río de la plata estuary

Background, Aim and Scope.  The compositional study of suspended matter in water from rivers of different latitudes and climates has revealed that the fine fraction reflects both substrate lithology from source areas or topsoil composition along the course. Metal distribution patterns are also strongly related to the clay mineral fate in fluvial aquatic systems. For the particular case of the coastal area of the Río de la Plata estuary in South America, previous studies have, on the one hand, focused on the analysis of distribution patterns of heavy metals in bottom river sediments and, on the other hand, on the assessment of metal contents in topsoils. The present study was conducted to evaluate the Cu, Pb and Zn distribution in soils and sediments from four drainage basins crossing two differentiated geomorphologic units composed of unconsolidated materials and to understand the metal behaviour. Methods  Data used included the existent, self-produced soil and sediment data sets (grain size, organic matter and Cu, Pb and Zn contents from 124 samples). Analyses were performed by using standardised methods: grain size analysis by sieving and settling; organic matter content based on the reduction of dichromate ion followed by titration; metal content by atomic absorption spectrophotometry following acid digestion. Results and Discussion. The average (% w/w) clay and organic matter content were 45.9 ± 17.1 and 1.5 ± 1.7 for sediments and 32.0 ± 19.8, and 7.5 ± 7.6 for soils, respectively. The raw mean metal concentrations (mg-kg^-1 dry weight) for sediments and soils were: Cu: 28.02 ± 27.28, 32.08 ± 21.64; Pb: 32.08 ± 46.94, 68.44 ± 69.25 and Zn: 83.09 ± 150.33, 118.22 ± 74.20, respectively. A good correlation for each clay-normalised metal concentration was found between soil and sediments using regression analysis considering average data for each basin sampling site (r > 0.89, p < 0.05). A comparison between metal concentration levels taking into account geomorphologic units by a t independent sample test showed significant differences for the normalised soil-sediment metal data (p < 0.001), responding to differences in grain size, clay mineralogy, organic matter and neoformed Fe-Mn oxide composition. Conclusion, Recommendation and Outlook  A clear parenthood between the topsoils and the bottom sediments in the study area was found. The Argiudolls from the inner zone are frequently affected by rainwater erosion, which washes the fine materials with sorbed metals and carries them to the streams. These watercourses reach the flat coastal plain, where soil flooding and bottom sediment depositional processes predominate. Here, both soils and bottom sediments are enriched in clay, organic matter and metals. The topography and lithology, under the environmental conditions of a temperate and humid climate control the fate of metals within these small basins. The influence of the physical media on the distribution and fate of pollutants should not be minimised in the understanding of the governing processes from natural systems.     

Contribution of Oil Industry Activities to Environmental Loads of Heavy Metals in the Tabasco Lowlands, Mexico

In Tabasco the petroleum industry pollutes soil recurrently by oil spills. We analysed Pb, V, Ni and Cr concentrations in water samples, and total metal contents and metal fractions in soil samples of contaminated and non-contaminated soils and in sediments. Besides, we determined Eh, pH, DOC and major ions in water and Eh, pH, C_org in soils and sediments. Sediments contained considerably larger heavy metal (HM) concentrations than soils. Local background concentrations of V, Ni and Cr in soils are larger than global means and oil spillages have not added these metals in quantities that exceed the natural variation. Spillage of formation water increases Pb concentrations in soils, particularly in mobile fractions. The contribution of the oil industry to HM loads is diluted by large fluvial water and sediment discharges and difficult to assess by comparison of total metal contents. Therefore, easily mobile metal fractions are much better indicators.     

渤海湾各形态重金属的地球化学特征及其环境意义

根据2008年对渤海湾的调查,重点研究了渤海湾湾内和湾口柱状沉积物重金属的生物地球化学特征,通过剖析不同形态重金属的特征,结合渤海湾生态环境信息的综合分析,系统探讨了渤海湾沉积物重金属的演变趋势、影响控制因素以及潜在生态风险。结果表明,湾内海河口附近沉积柱重金属含量有几次突变,20～22cm段极小值可对应1939年海河北系的洪水,10～12cm段极小值可对应1963年海河南系的洪水,1963年至今重金属含量有逐渐增加的趋势。不同形态重金属百分含量从大到小为：残渣态〉铁锰氧化物结合态〉碳酸盐结合态〉有机结合态〉可交换态,且重金属在海河口附近都表现出较高的可浸取态百分含量。风险评价结果表明,重金属总量富集因子由大到小为：Pb〉Cd〉Zn〉Cr〉V〉Co〉Cu〉Ni,其中Pb、Cd和Zn的富集因子均大于1,说明其有污染,但渤海湾沉积物总体质量良好,潜在生态风险较低。从重金属形态角度评价,V和Cr无污染,Zn、Co、Cu、Ni和Pb在湾内及湾外均有不同程度的污染,而Pb的污染最为严重。     

Schwermetallgehalte im Kultursubstrat und Erntegut des Champignons,Agaricus bisporus (Lange) Singer,beim Einsatz von Müllklärschlammkompost

Heavy metal contents in the culture substrate and in the mushroom, Agaricus bisporus, grown in composts mixed with municipal waste and sewage The addition of increasing quantities of municipal waste compost to conventional horse manure compost resulted in a proportional increase in the heavy metal content of the mixture. The increases ranged between 250% (zinc) and 900% (mercury). Ninety-four to ninety-nine percent of the heavy metals in municipal waste compost are bound in compounds from which they can not be extracted using CaCl₂ solution. The amounts extractable from horse manure compost with CaCl2₂ solution are from 1.5 (zinc)- to 33 (mercury)-times higher. The influences of the increasing quantities of heavy metals in municipal waste — horse manure composts are demonstrable in the content of these metals in harvested mushroom. This, in turn, corresponds to the availability of the metals. The relative enrichment is greatest with mercury, and least with cadmium. The quantities found in mushrooms, with the exception of mercury, fall within the normal range detected in vegetable crops.     

广州市流花湖沉积物重金属污染特征及潜在生态风险评估

近年来重金属污染日益加重,对人类及水生态系统健康产生较大危害。本研究选择广州市典型城市湖泊——流花湖,利用地累积指数(Igeo)、潜在生态风险指数(RI)对沉积物中12种重金属的污染水平、垂向分布特征及其潜在生态风险进行评价,并通过多元统计分析对金属元素的来源进行解析。结果表明:①湖泊沉积物重金属含量(Mn、V除外)均显著高于区域土壤背景值,自下而上呈现先增加后减少的趋势;②地累积指数评价结果显示Cd、Zn、Sb、Cu、Pb和As这6种重金属污染较严重,其中Cd偏重度污染的状态(Igeo=3.89);③不同重金属元素污染水平有较大差异,Cd、Cu、Zn、Sb、Pb、As、Ni、Cr、Tl、Co的单个重金属污染指数(Cif)均为中等污染水平以上,而生态风险系数(Eif)表现为Cd(Eif=818.6)极严重等级,Sb(Eif=82.64)重度风险等级,其他10种重金属Eif均为轻度风险等级;④该湖RI指数变化幅度剧烈(105.85相似文献   

Zur Ermittlung der Schwermetallverfügbarkeit lithogen und anthropogen belasteter Standorte. 1. Cd und Cu

Investigations about the availability of heavy metals in soils with lithogen and anthropogen enrichment. 1. Cd and Cu First results obtained from field experiments on two locations with high natural content of heavy metals (Cd and Cu) are described. It became evident that an anthropogen enrichment by addition of Cd oxides had a stronger effect on the Cd contents of plants (oats) than the higher lithogen soil content. In respect of the Cu it is indicated that contrary to the prevailing knowledge of high lithogen contents it seems that it leads to increased contents of the plants (barley). The CaCl₂-extraction of the soil has proved to be suitable to identify the plant available Cu contents, but it is restricted to determine the available Cd fraction. The DTPA-extractable fractions showed poorer relations to the metal contents of the plants.