汕头湾表层沉积物重金属污染与潜在生态风险评价

汕头湾作为华南地区重要的出海门户,汕头市主要的旅游区和水产养殖基地,其环境污染问题已成为制约当地经济发展的重要因素,为此2002年在此开展了重大科技术兴海项目,以海洋沉积物质量标准、单因子污染指数和潜在生态风险评价体系对汕头湾表层沉积物重金属污染现状和潜在生态风险进行了评价。结果表明:汕头湾表层沉积物中Cd,Cu,Pb,Zn的平均含量超过海沉积物质量标准(Ⅰ类);以单因子污染指数评价,Cd达到很强污染等级,Zn为强污染,Cu,Ni,Pb为中等污染;以单元素生态系数(E_rⁱ)评价,只有Cd的潜在生态风险达到很强等级,其它元素则只属于轻微潜在风险范畴;以多元素潜在生态风险指数(RI)评价,汕头湾的潜在生态风险水平处于中等强度;重金属含量分布特征与重金属污染及潜在生态风险的空间差异性一致,表现为由上游至下游呈波状递减趋势,其中以牛田洋和汕头港上游最为严重;这一污染特征主要是由集水区域内的产业结构特点、河流入海口及排污口的分布以及汕头湾的地理和水文特性所决定的。     

黄河水系沉积物重金属赋存形态及污染特征

2004年采集了黄河干流及西纳川等支流的水系沉积物,测定了沉积物样品中Cu、Zn、Pb、Cd、Cr、As和Hg等重金属元素的含量,并用BCR连续提取法分析研究了各元素的赋存形态,同时采用地累积指数法(Igeo)和次生相原生相分布比值法(RSP)分别对黄河流域水系沉积物中重金属的污染状况及生态风险进行了评估.结果表明:黄河水系沉积物中重金属含量特征总体符合全球页岩重金属元素丰度的基本趋势,但在部分人为污染较重的区域,表现出一定的地理差异;从浓度水平衡量,重金属的污染较轻;黄河水系沉积物中Cu、Zn、Cr和As主要以残渣态(B4)形式存在,具有较好的环境稳定性,而Pb、Hg和Cd以活性较大的弱吸附态存在,可能具有相对较大的环境影响;生态风险评价的结果显示,Pb、Cd和Hg具有相对较高的生态风险指数,尤其是Pb的潜在风险应该引起重视.     

青山水库表层沉积物重金属污染特征及生态风险评价

在位于浙江省临安市的青山水库采集了具有代表性的8个样点的表层沉积物样品,分析比较了样品中As、Cr、Cu、Ni、Mn、Pb、Zn等7种重金属总量的差异,采用BCR连续提取法对重金属不同形态(酸提取态、可还原态、可氧化态、残渣态)进行分析.采用地积累指数法(I_geo)和Hakanson潜在生态风险指数法,对青山水库不同采样点表层沉积物中重金属的污染程度和潜在毒性与生态风险进行评价.结果表明: 青山水库表层沉积物重金属污染程度存在明显的空间差异,流经城区和工业园区的青山水库支流入库河口附近的表层沉积物重金属含量明显高于其他采样点.青山水库表层沉积物7种重金属中,Mn主要以酸提取态存在;Cu和Pb主要以可还原态形式存在;As主要以残渣态形式存在.流经城区的支流入库河口附近表层沉积物还原态和酸提取态重金属比例较高,对水生生物有一定的毒性风险.8个样点的表层沉积物7种重金属中,以As污染程度最高,潜在生态风险最大,其次是Cu、Ni、Mn、Pb和Zn,均处于轻度污染状态,而Cr处于清洁水平,潜在生态风险较低.不同采样点比较发现,分别流经城区的锦溪和工业园区的横溪入库河口附近表层沉积物重金属污染程度和潜在生态风险明显高于其他采样点.     

瓯江下游流域河流沉积物重金属污染特征、来源及潜在生态风险评价

为了解瓯江下游流域及沿岸城郊入江河流沉积物中重金属的污染特征, 对瓯江流域下游及温州城区河流43个表层沉积物中Cr、Co、Ni、Cu、Zn、As 和Pb 共7 种重金属元素的含量特征进行分析, 比较了城郊与城区、城区入江口与城区内部之间河流沉积物重金属含量的特征及差异并探讨其污染来源。结果表明: 沉积物中7 种重金属元素的含量由高到低依次为: Zn>Cr>Cu>Ni>Pb>Co>As, 与浙江省土壤背景值相比, 7 种重金属的平均含量超标1.5-4.9 倍,各种重金属的污染程度依次为: Co>Ni>Cr>Zn>As>Cu>Pb, 综合污染程度已达到警戒线等级。来源分析表明, 重金属元素Cu、Zn、Pb 和Cr 主要来自于工业污水排放及船舶交通等人类活动, Co 和As 主要来自于工业及农业生产活动, Ni主要来自于以工业为主的排污污染。潜在生态风险系数Eri 评价结果显示, 7 种重金属潜在生态风险大小为:Co>As>Cu>Ni>Pb>Cr>Zn, Co 元素处于较强生态风险等级; 潜在生态风险指数RI 介于72.05-107.80 之间, 其中55.5%的样点处于较强生态风险水平, 44.4%为中等生态风险水平, 研究区整体处于较强生态风险水平。     

厦门杏林湾表层沉积物重金属污染特征及潜在生态风险评价

论文对杏林湾表层沉积物重金属、有机碳和硫化物含量进行了检测,对数据作了相关性分析和因子分析,并应用潜在生态危害指数法对重金属的潜在生态风险进行了评价。结果表明:重金属之间有显著的相关性,Cu与Ni、Pb与Ni、Pb与Cr以及Cr与Hg之间的相关系数分别为0.786(P﹤0.05)、0.783(P﹤0.05)、0.937(P﹤0.01)和0.770(P﹤0.05)。重金属与有机碳及硫化物的相关性较差,表明该地区重金属污染来源与硫化物和有机碳并不相同。既有人为输入,又有自然的沉积过程。因子分析进一步解释了该水域重金属污染的主要来源。根据E_rⁱ均值大小,Hg的危害风险最大,Cr最小。6种重金属潜在生物毒性风险大小依次为:Hg > Pb > Cu > Cd > Ni > Cr。重金属的生态危害程度均较小,尚属轻微生态危害。     

珠江(广州河段)表层沉积物中重金属的生态风险研究

随着广州市截污工程的实施,珠江（广州河段）外源污染得到有效控制后,沉积物内源污染将成为影响河流水质的重要因素。我们测定了珠江（广州河段）沉积物中Cu、Pb、Zn、Cr、Cd、Hg和As 7种重金属的浓度,研究了它们的分布特征和潜在生态风险。结果表明：在主干流河道的顺流断面中,各种重金属元素整体上表现出明显的倒“W”型分布。在各内河涌的各监测断面中,花地涌沉积物中重金属浓度最高,乌涌最低,其余各河涌居中。各种重金属元素的空间分布特征基本相似,除了Hg与Cd、Cr、As之外,其他各元素之间均呈现较明显的正相关关系,尤其是Cr和Cd、Cu和Cd、Cr和Cu之间的相关性显著,表明这些重金属元素在沉积物中的浓度具有共同变化的趋势。潜在生态危害指数法的评价结果显示,7种重金属元素的生态危害系数的大小顺序为：Hg>Cd>Cu>As>Pb>Zn>Cr,其中Hg是最主要的生态风险因子。对单个重金属的潜在生态危害系数（ ）和多个重金属的潜在生态危害指数（RI）的分析,生态风险最大的断面是5#（黄歧）、6#（黄沙）、16#（花地涌北出口）、7#（横滘）和14#（增埗桥）。     

乐安江沉积物中金属污染的潜在生态风险评价

选择污染严重的乐安江河流沉积物为对象,利用风险因子Ｅ和风险指数ＲＩ等定量诊断工具开展沉积物中重金属污染的潜在生态风险评价。根据风险指标体系和空间分异规律,将流域划分居不同特征的４种生态风险功能区。对比评价效果。潜在生态风险评价与地积累 情况大同小异,可以相互补充和借鉴。     

鸭绿江口湿地滩涂表层沉积物重金属空间分布特征及生态风险评价

利用GIS软件空间内插值法分析鸭绿江河口近海湿地滩涂表层沉积物重金属的空间分布特征,并采用环境风险指数法和潜在生态危害指数法进行重金属元素的生态风险评价.结果表明: 研究区表层沉积物中的重金属含量与国内典型河口湿地相比处于较高水平.从空间分布上看,重金属含量东部高于西部,在人类活动密集区存在明显的累积性.环境风险指数法分析结果表明,Cu对该区域环境污染的影响最大,而Hakanson潜在生态危害指数法分析结果表明,Hg和Cd的潜在生态危害最大,重金属的综合潜在生态危害指数介于93.65～507.20,平均值为189.30,属于中等生态危害,并以东部潜在危害程度最大,应作为今后重金属污染防治的重点区域.     

海河流域西部地区水库沉积物重金属潜在生态风险评价

海河流域西部地区水库是下游平原区重要的水源地,水库沉积物重金属的潜在生态风险受到关注.运用Hakanson潜在生态风险评价方法对海河流域西部10座水库沉积物重金属的潜在生态风险进行评价,并采集水库上下游河流沉积物与水库作对比分析.结果表明:海河流域西部水库沉积物中Cd超标严重,平均含量是背景值的1.67倍,最高达2.77倍;超过半数水库的Pb超出背景值.结合毒性系数,计算了沉积物重金属的潜在生态风险,依次为Cd＞As＞Pb＞Ni＞Cu＞Cr＞Zn.多数水库的Cd生态风险危害等级均在中等危害及以上,承担保定市和北京市供水功能的西大洋水库Cd生态风险等级为“强”.水库上、下游河流沉积物重金属中Cd的生态风险显著高于水库自身,水库上游河流沉积物Pb、Cu、Ni的生态风险也高于水库,Zn和Cr的生态风险在水库上下游差异不显著.     

珠江口桂山岛表层沉积物中重金属的分布特征及潜在生态危害评价

于2011年8月采集了珠江口桂山岛海域12个站点的表层沉积物, 对沉积物中重金属的含量进行了测定。结果表明, 桂山岛沉积物中重金属含量与国内外港湾相比属于中等水平, Pb、Cr、Ni、Cu、Zn、Mn平均含量分别为40.06、31.29、14.17、30.67、100.18、599.76 mg/kg。富集系数法和 Hakanson潜在生态风险指数法评价表明:桂山岛沉积物各重金属元素的富集顺序为Cu﹥Pb﹥Zn﹥Mn﹥Cr﹥Ni, 其中Cu、Pb、Zn和Mn富集系数大于1;该海域重金属潜在生态风险总体上处于低水平, 从空间上看, S11危害最为严重。进一步通过主成分分析研究沉积物中重金属的来源, 发现前2个主成分贡献率分别为44.38%、42.61%, 表明重金属主要有2个来源:工业和生活污水排放、岩石的自然风化与侵蚀过程。     

Total concentrations and fractionation of heavy metals in road-deposited sediments collected from different land use zones in a large city (Nanjing), China

Abstract

In order to investigate heavy metal contamination in an urban environment during urbanization and economic development, 35 road-deposited sediment samples were collected from seven different land-use zones (commercial, residential, traffic, scenic park, educational, industrial and peri-urban) in Nanjing, a large city in P.R. China. The ranges of total metal concentrations found were: 28.7–272 mg kg^?1 for Cu; 24.8–268 mg kg^?1 for Ni; 37.3–204 mg kg^?1 for Pb; 140–798 mg kg^?1 for Zn; 0.44–2.19mg kg^?1 for Cd; and 60.6–250 mg kg^?1 for Cr. Metal fractionation was carried out using a modified three-step European Bureau of References (BCR) sequential extraction procedure. Cadmium and Zn were found predominantly associated with the acid extractable fractions; Ni and Cr were dominant in the residual fraction; Pb was predominantly associated with the residual and reducible fractions; Cu was dominant in the oxidizable and residual metal fractions. Based on the sum of the acid-extractable, reducible, and oxidizable fractions, Cd, Zn and Pb are potentially the most toxic metals in the road-deposited sediment in Nanjing. No significant differences, except for Zn, were found in the metal fractionation pattern for Cu, Ni, Pb, Cd, and Cr in different land use zones.     

Heavy Metal Partitioning in Bottom Sediments of the Matanza-Riachuelo River and Main Tributary Streams

This study provides geochemical partitioning, potential bioavailability, and enrichment of Cd, Cu, Pb, and Zn in bottom sediments collected from the Matanza-Riachuelo River and its main tributary streams. A modified Tessier sequential extraction procedure, complemented with acid volatile sulfide (AVS) and simultaneous extracted metals (SEM) measurements, was applied to determine the partitioning of metals into four fractions (metals bound to amorphous sulfide, carbonate, and exchangeable), bound to Fe/Mn oxides (reducible), bound to organic matter/sulfide (oxidizable) and residual. Spatial and vertical distributions of metals were studied. The core sediments show a decreasing concentration of metals with depth. In top sediments, non-residual Cu was mainly associated with oxidizable phase, whereas Pb, Cd, and Zn were mainly associated with amorphous sulfide. Pb exhibited the highest enrichment in all sites. The ratio AVS/SEM was greater than one at sediment sections close to the water column, indicating that metals extracted with hydrochloric acid were mainly associated with the amorphous sulfide. The strong influence of amorphous sulfide in the retention of Cd, Pb, and Zn in anoxic sediments of Matanza-Riachuelo river system suggests that dredging and aeration could lead to the remobilization of metals from sediments to the water column, hence making the metals more available to the biota.     

Cumulative Title Index

Abstract

Metal fractionation is a powerful tool for studying the mobility, bioavailability and toxicity of metals in sediments and soils. A seven-step sequential extraction technique was used to determine the potential mobility of selected heavy metals (Fe, Mn, Zn, Cu, Pb, Cd and Ni) in the sediments of Lake Naivasha. Results indicate that residual fraction was the most important phase for the elements Fe, Mn, Cu and Zn. However, Pb and Cd are highly enriched in the non-residual phases. Nickel on the other hand was distributed evenly between the non-residual and the residual fractions.

The total concentrations of the heavy metals suggested a decreasing order of iron ?> manganese ? zinc > nickel > copper ? lead > cadmium. However, the detailed sequential extraction data indicated an order of release or mobility of cadmium > lead ? nickel ? zinc > manganese > copper > iron. The high percentage of Cd and Pb in the mobile fractions suggests high bioavailability of these two elements in the study area and maybe a pointer to anthropogenic input of the two elements in the study area.     

Evaluation of Heavy Metals Pollution Loadings in the Sediments of the Ave River Basin (Portugal)

Sediment samples from the Ave river basin were collected with the aim of determining metal total pollution contents. Cr, Cu, Fe, Mn, Pb, Zn and VM at 550 °C were determined. Some physico-chemical parameters were also quantified in water samples collected in the water column just above the sediments.

Metal contamination factors (CF) indicated that sediments were not contaminated with Cu and Pb, slightly with Zn and moderately with Cr.

For sediments with high metal pollution loadings, the original BCR (Community Bureau of Reference) metal speciation protocol was also applied. Speciation studies showed that chromium was mainly associated with the oxidisable plus residual fractions (>85%). These results suggest that changes in the physico-chemical properties of the river water (e.g. pH, Eh) should not be accompanied by a significative release of chromium from sediments.

The relationships between chromium speciation fractions, physic-chemical parameters of the sediments and water samples were studied by Principal Component Analysis, and allowed to reduce the dimensionality of the data matrix from 14 to 3 significant components accounting for 89% of the variance. It was found that hydrous Fe/Mn oxides and organic matter are the “carriers” of chromium associated to fractions exchangeable and oxidable.     

Bioavailability and mobility of heavy metals in soil in vicinity of a coal mine from Huaibei,China

This study investigated the concentrations of Co, Cr, Cu, Mn, Ni, Pb and Zn in surface soil and corn cob samples collected from agricultural fields near a coal mine from Huaibei, China. Meanwhile, the mobility and availability of heavy metals in soil samples were evaluated by a modified three-step The European Community Bureau of Reference (BCR) sequential extraction procedure. The total concentrations of metals in soil pose no ecological threats to the local plants. Transfer factors of essential metals, Cu and Zn, as well as those of non-essential metal Pb, were higher than those of the remained metals. The results of BCR fractionation analysis revealed that the acid soluble, reducible and oxidizable fractions of the Mn, Pb and Zn were higher than those of the residual fraction, suggesting that these elements may be more bioavailable. The pH and organic matter contents of soil were significant parameters affecting speciation of metals in soil samples. Hierarchical cluster analysis indicated significant correlations between metal levels in corn grains and more available (acid soluble and reducible) fractions in soil, indicating that heavy metals in the first two fractions were more available for corn crops. The elevated mobility and bioavailability of Pb in soil are of great concern in the study area.     

Characterization of Heavy Metal Fractions in Agricultural Soils by Sequential Extraction Procedure: The Relationship Between Soil Properties and Heavy Metal Fractions

The present research was conducted to determine heavy metals in agricultural soils from Çanakkale, Turkey, using a sequential extraction procedure (acid soluble, reducible, oxidizable, and residual) as proposed by the Community Bureau of Reference (BCR) of the European Commission. Soil samples were taken from 12 different cultivated sites and analyzed for Cd, Co, Cr, Cu, Mn, Ni, Pb, and Zn concentrations. The results revealed an order of Mn > Cd > Pb > Co > Ni > Cu > Zn > Cr for the heavy metals based on the sum of the first three fractions (acid soluble + reducible + oxidizable). The relationships between soil properties and each metal fraction were identified through Pearsons's correlation analysis. Hierarchical cluster analysis was performed to determine the behaviors and similarities of metals in each fraction. While Mn, Pb, and Zn exhibited subjective behaviors in the acid-soluble fraction, Cd, Co, Cu, Cr, and Ni exhibited similar behaviors with each other.     

Sludge-Derived Cu and Zn in a Humic-Gley Soil: Effect of Dissolved Metal-Organic Matter Complexes on Sorption and Partitioning

A sequential extraction scheme was combined with sorption isotherm analysis in order to investigate sorption of sewage sludge-derived Cu and Zn to the A-horizon of a humic-gley soil as a whole, and to the operationally defined exchangeable (1?M MgCl₂), carbonate (1?M NaOAc), Fe/Mn oxide (0.04?M NH₂OH.HCl), and organic (0.02?M HNO₃+30% H₂O₂) soil fractions. Sorption parameters were compared for a sample of sludge leachate (with 97.4% of Cu and 63.2% of Zn present as dissolved metal-organic matter complexes, as calculated by geochemical modeling involving MINTEQA2 and verified using an ion exchange resin method) with that of a reference solution exhibiting the same chemical characteristics as the leachate, except for the presence of dissolved organic material. Dissolved metal-organic matter complexes were found to significantly (P<0.05) depress sorption to the bulk soil and each fraction. The greatest depression of Cu and Zn sorption was observed for the exchangeable, carbonate, and Fe/Mn oxide fractions, while the organic fraction of the soil was the least affected. This reflects a greater affinity for the exchangeable, carbonate, and Fe/Mn oxide fractions by the free divalent metal (Cu²⁺, Zn²⁺), with sorption by these fractions attributed to cation exchange, chemisorption, and co-precipitation processes. The sorption characteristics of the organic fraction indicated that Cu and Zn sorption by soil organic matter mostly involved dissolved metal-organic matter complexes. This may be attributed to hydrophobic interactions between nonpolar regions of the dissolved metal-organic matter complexes and solid-phase soil organic matter.