秦皇岛石河口海域沉积物重金属污染及生态风险评价

为了研究石河口海域的沉积物环境,于2009年9月对石河口海域表层沉积物的Cu、Pd、Zn、Cd、Hg、As含量进行了测定,探讨了重金属含量的分布特征和相关关系,采用地累积指数法和潜在生态风险指数法对重金属的富集程度和潜在生态风险进行了评价。结果表明:Cu和Pd、Cu和Cd、Pd和Cd之间存在显著正相关性。重金属富集程度排序为CdHgCuZnPdAs。石河口海域多种重金属潜在生态风险指数属于轻微风险状态。重金属潜在生态风险指数排序为CdHgPdCuAsZn,Cd的生态风险指数属中度风险状态,研究区域在一定程度上受到了Cd的污染。     

渭河干流(宝鸡段)表层沉积物Cu、Zn、Pb污染特征与评价

对渭河干流（宝鸡段）表层沉积物中重金属Cu、Zn、Pb含量进行了调查，用潜在生态危害系数法对其污染水平进行了评价，并与松花江（吉林市段）、淮河（江苏段）、长江（下游）、苏州河、珠江（广州段）5条河流表层沉积物中Cu、Zn、Pb的含量做了对比研究。结果表明，3种重金属元素平均含量均超出相应的土壤背景值，出现了一定程度上的富集；生态危害系数均〈40，属轻微生态危害。重金属含量水平在国内诸河中处于中间位置。     

花溪水库表层沉积物重金属污染及潜在生态风险评价

以现代工业化前正常颗粒沉积物中重金属含量的最高背景值为参比值,结合潜在生态风险指数法对花溪沉积物中重金属的生态危害进行了评价。结果表明,花溪水库沉积物中重金属的富集顺序为Cu>Zn>Pb>Cr>As>Cd>Hg,污染水平顺序为Hg>Cd>Cu>As>Pb>Cr>Zn;重金属的潜在生态风险系数(Eir)表明,除个别样点外,大多属于轻微生态危害范畴;多种重金属的生态系统的潜在生态风险指数(IR)表明,花溪水库沉积物重金属污染属于轻微生态危害。     

贵州某流域城市河段沉积物及悬浮物重金属污染研究

通过在丰水期对贵州省某流域城市河段悬浮物和沉积物中的重金属含量进行测定，运用单因子指数法、生态风险评价法、因子分析法，初步探讨了该河段Cu、Zn、Pb、Hg、Cd、Cr、Ni及As等8种重金属元素的含量分布、污染特征、潜在生态风险及主要来源。检测结果显示，沉积物和悬浮物中Hg、Cd、Zn、Pb、As的平均含量较高，是贵州省土壤背景值的1.02～16.97倍。单因子指数评价结果表明：在沉积物中，Zn、Pb、As为轻度污染，Hg和Cd为重度污染；在悬浮物中，Cu、Pb、As为轻度污染，Zn为中度污染，Hg和Cd为重度污染。潜在生态风险指数评价结果显示，Hg和Cd的生态风险最大，为主要污染元素。研究区沉积物样品综合生态风险指数(RI)介于183.27～1 393.96,平均值为912.06,总体处于严重生态风险等级；悬浮物样品RI值介于341.53～612.38,平均值为436.85,总体处于重度生态风险等级。其中，沉积物样品重金属平均生态风险等级高于悬浮物样品，支流样品重金属生态风险等级总体上低于干流下游样品。根据因子分析法分析结果，初步推测沉积物及悬浮物Hg、Cd、Cr、Ni含量主要受工...     

鄱阳湖沉积物重金属空间分布及潜在生态风险评价

通过分析鄱阳湖沉积物重金属空间分布特征,评价其潜在生态风险,并探讨了主要重金属污染来源。结果表明:鄱阳湖沉积物7种重金属元素Cd、Hg、As、Cu、Pb、Cr、Zn含量平均值分别为0.67、0.078、17、51、72、42.9、117 mg/kg,除Cd外,其余6种元素均明显高于相应的背景值。从空间分布来看,Cd、Cr含量总体呈现东南、西北部偏高的现象,而Hg、Cu、Pb含量总体呈现东南部偏高的现象,As、Zn的含量分布相对平均。Hg、Cu、Pb、Zn 4种金属元素之间存在极显著相关性,表明这些元素污染具有同源性。潜在生态风险评价结果显示,单个重金属潜在生态风险顺序为CuHgPbCdAsCrZn;从综合潜在生态风险分析来看,整个湖区的RI值为46.4~476.3,平均值为165.4,属于中等潜在生态危害,其中湖区东南部综合潜在生态风险最高。Cu、Hg、Pb等重金属主要来自乐安河流域工业排放。     

湘江(衡阳段)河流沉积物中重金属潜在生态风险评价

对湘江（衡阳段）10个断面18个采样点的表层沉积物重金属（Cd、Hg、Pb、As、Cr、Zn、Cu）进行监测和分析，采用Lars Hanson潜在生态危害指数法对各种重金属的生态风险进行评价。结果表明，湘江（衡阳段）表层沉积物中各重金属潜在生态危害系数大小排序为：Cd〉Hg〉Pb〉As〉Cu〉Zn〉Cr。多种重金属的综合潜在生态风险指数RI为913．4，表明湘江（衡阳段）沉积物重金属污染属于很强的生态危害。     

南沙河水体重金属污染特征及潜在生态危险评价

通过测定南沙河水体中重金属的含量,探讨重金属的分布特征,并采用地累积指数法和潜在生态危害指数法对沉积物中重金属污染程度和潜在生态危害进行了评价。结果表明,南沙河水体重金属的污染较轻,沉积物的重金属地累积指数分级在0～3之间,属于无污染至中度污染水平,各重金属的污染程度为Zn>As>Pb>Cu>Cr>Cd。沉积物重金属呈现由较轻到中等的生态风险,以Cd的生态风险为主。     

长江南京段近岸沉积物和土壤中重金属分布特征分析

通过测定沉积物和土壤中Cd、Pb、Cr、Zn、Cu、Ni 6种重金属元素的平均含量,计算其富集因子,分析长江南京段近岸沉积物和土壤中重金属的空间分布特征,结果表明,几种重金属在沉积物中的富集次序为:CdPbCr1NiCuZn,在土壤中为:CdZnCu1CrPbNi,除Zn和Cu外,其他几种金属在沉积物中的富集程度高于土壤,同时Cd的含量超过土壤环境质量三级标准。以Cd和Pb为例分析了重金属含量与沉积物粒级之间的关系,回归分析显示,Cd、Pb的含量与颗粒物的粒级呈显著的相关性,与细颗粒物的含量有密切关系,细颗粒携带的重金属,在长江水力分选作用下到达下游,成为沉积物中重金属的主要来源。     

镇江内江底泥重金属分布特征及潜在生态危害评价

对镇江内江的底泥进行采集,测定底泥中的Cu、As、Hg、Cr、Pb、Cd、Zn、总磷、总氮、有机质的含量,采用潜在生态风险评价和相关性分析的方法,研究了底泥中重金属的污染水平、生态危害、分布特征和溯源。结果表明,(1)内江底泥中的重金属污染主要为Hg、Cd、As。各重金属单项潜在生态危害指数大小关系为Hg>Cd>As>Pb>Cu>Cr>Zn。(2)内江的整体生态环境受重金属的危害程度处在中等水平,重金属的生态威胁主要来自Hg,建议在达到强生态威胁程度的3#、8#、20#、21#采样点附近清理淤泥。(3)由重金属分布特征可知,湿地生态系统对重金属具有较好的吸附去除作用;在内江流速慢、死水多的地方易造成重金属富集;入江河口重金属富集也较明显;污染企业与重金属含量有直接关系。(4)由相关性探源可知,Cu、Zn、Cr主要来自于自然界,Hg、Cd、Pb主要来自于企业污水排放,As则来自于自然界和人为排放。     

湘江长沙段沉积物重金属污染状况及潜在生态风险评价

根据重金属环境化学行为的特点，应用沉积学原理，对湘江长沙段5个代表性断面10个采样点的表层沉积物中重金属（Hg、CA、As、Pb、Cu、Cr、Zn）进行监测和分析，采用Lars Hakanson潜在生态危害指数法对各种重金属的生态风险进行了评价。结果表明：按当地最高背景值为参比值计算，湘江长沙段表层沉积物中各种重金属潜在生态危害系数大小排序为Cd〉Hg〉As〉Pb〉Cu〉Cr〉Zn，多种重金属的潜在生态风险综合指数为560．8，表明湘江长沙段沉积物重金属污染属于强生态危害。     

辽宁绥中海域海水和表层沉积物中重金属污染评价

根据2009年10月的调查数据对辽宁绥中海域海水和表层沉积物中的重金属(砷、汞、铜、铅、锌和镉)进行了研究。用单因子指数评价法对海水中的重金属进行了评价,结果表明,海水中的Zn、Hg含量均超过《海水水质标准》(GB3097-1997)中Ⅰ类海水水质标准。采用《海洋沉积物质量》(GB 18668-2002)Ⅰ类海洋沉积物质量标准评价,表层沉积物中的As超标一倍以上。采用瑞典科学家Hkanson的潜在生态危害指数法进行评价,生态危害程度As>Hg>Cd>Cu>Zn>Pb。     

贵州煤矿区表层水-沉积物重金属分布特征及来源分析——以新寨河为例

为探索贵州煤矿区表层水-沉积物中重金属的分布特征及来源,科学制定环境保护与污染治理措施,以新寨河为研究对象,在11个样点共采集66个表层水体和沉积物样品,通过对Cd、Pb、Cr、Zn、Cu、As、Hg、Fe、Mn等9种重金属元素进行分析,揭示其在新寨河的空间分布特征。同时,利用多指数法开展了有毒重金属元素污染状况评价,通过相关性分析和主成分分析解析了重金属的来源。结果表明,新寨河流域表层水体中,Fe、Mn点位超标率达100%。表层水中重金属元素的平均含量排序为Fe＞Mn＞Zn＞Cu＞Cr＞As＞Cd＞Pb＞Hg,而沉积物中重金属元素的平均含量排序则是Fe＞Mn＞Zn＞Cr＞Cu＞As＞Pb＞Cd＞Hg,表明新寨河表层水体和沉积物中重金属元素的空间分布存在一定差异。各重金属元素的内梅罗综合污染指数介于0.59~1.13之间,表明新寨河表层水体中重金属的污染程度达到轻微污染水平。单种重金属元素的潜在生态危害系数计算结果显示,90.91%和9.09%的沉积物样点分别被归类为轻微风险和中等风险。所有样点沉积物的潜在生态危害指数介于14.57~120.55之间(均值为72.08),表明新寨河沉积物的潜在生态风险较低。Cu、As在多个样点存在污染现象,需予以重点监控管理。新寨河流域重金属的来源可分为三大类:Cd、Pb、Cr、Zn、Cu为第一类,对应地表径流源;As、Fe、Mn为第二类,对应煤矿开采源;Hg为第三类,对应复合源。     

Metal Fractionation Studies in Surfacial and Core Sediments in the Achankovil River Basin in India

The Fractionation of Fe, Zn, Cu, Pb, Mn and Cd in the sediments of the Achankovil River, Western Ghats, India using a sequential extraction method was carried out to understand the metal availability in the basin for biotic and abiotic activities. Spatial distribution of heavy metals has been studied. Sediment grain size has significant control over the heavy metal distribution. The fluctuations in their concentration partly depend upon the lithology of the river basin and partly the anthropogenic activities. The sediments are dominated by sand and are moderately to strongly positively skewed and are very leptokurtotic in nature. The quartzite and feldspars are abundant minerals along with significant amount of mica with low clay content. The core sediments show increasing trend of heavy metal concentration with depth due to the recent addition of anthropogenic sources and post-diagenic activities. Significant amount of Cd (18%) was found in carbonate fraction, which may pose environmental problems due to its toxic nature. Small concentrations of metals, except Cd and Cu, are in exchangeable fraction, which indicate low bio-availability. Enrichment Factor (EF) for individual metals shows the contribution from terrregious and in part from anthropogenic sources. Selective Sequential Extraction (SSE) study shows the variation in specific metal distribution pattern, their distribution in different phases and their bio-availability. Maximum amount of the metals were bound to the non-residual fractions (mainly Fe-oxides). Overall, bio-availability of these micronutrients from sediments seems to be very less. Non-residual phase is the most important phase for majority of heavy metals studied. Among the non-residual fraction, maximum amount of the heavy metals bound to Fe-oxides. The study high lights the need for in-depth study of heavy metals distribution and fractionation in the smaller river basins to get precise information on the behavior and transport of heavy metals in the fluvial environment and their contribution to the world ocean.     

滇池宝丰湾疏浚区底泥污染程度评价及环保疏浚深度的确定

根据滇池外海主要入湖河口及重点区域底泥疏浚工程,宝丰湾疏浚区设计阶段勘察结果,采用内梅罗污染指数法及Lars Hakanson的重金属潜在生态风险指数法对疏浚区底泥进行了污染程度评价。针对底泥污染空间分布特征,确定疏浚深度,为环保施工提供依据。     

珠江口黄茅海表层海水和沉积物中重金属的分布及评价

根据2014年4月对珠江口黄茅海海域表层海水和沉积物中重金属分布的调查监测,采用单因子指数法、内梅罗指数法和生态危害指数法对其重金属污染水平进行评价。结果显示:该海域表层海水中部分站位的Pb、Cu、Zn和Hg超出第一类海水水质标准,内梅罗指数评价表明其整体处于轻污染水平。表层沉积物中部分站位的Hg、As和Cu超出第一类海洋沉积物质量标准,内梅罗指数评价表明其整体处于重污染水平,生态危害指数评价表明其整体可能面临中度风险,Hg为主要风险因子。表层海水中Pb、Cu、Zn具有同源性,表层沉积物中Pb、As、Zn和Cu具有同源性。     

徐州市地表水体底泥重金属污染特征研究

文章对徐州市地表水体底泥重金属的污染特征进行了研究。对流经徐州市的四条主要河流和云龙湖的55个底泥采样点的重金属含量进行了测试,并采用单因子污染指数法进行了评价。结果表明,徐州市地表水体除云龙湖之外均不同程度地受到了重金属元素的污染。荆马河污染最为严重,其次是奎河、故黄河、京杭大运河。云龙湖的第五个采样点也受到了Hg的污染。污染元素的种类及污染程度与徐州市的产业结构密切相关。     

Assessment of trace metal contamination in a historical freshwater canal (Buckingham Canal), Chennai, India

The present study was done to assess the sources and the major processes controlling the trace metal distribution in sediments of Buckingham Canal. Based on the observed geochemical variations, the sediments are grouped as South Buckingham Canal and North Buckingham Canal sediments (SBC and NBC, respectively). SBC sediments show enrichment in Fe, Ti, Mn, Cr, V, Mo, and As concentrations, while NBC sediments show enrichment in Sn, Cu, Pb, Zn, Ni, and Hg. The calculated Chemical Index of Alteration and Chemical Index of Weathering values for all the sediments are relatively higher than the North American Shale Composite and Upper Continental Crust but similar to Post-Archaean Average Shale, and suggest a source area with moderate weathering. Overall, SBC sediments are highly enriched in Mo, Zn, Cu, and Hg (geoaccumulation index (I_geo) class 4–6), whereas NBC sediments are enriched in Sn, Cu, Zn, and Hg (I_geo class 4–6). Cu, Ni, and Cr show higher than Effects-Range Median values and hence the biological adverse effect of these metals is 20%; Zn, which accounts for 50%, in the NBC sediments, has a more biological adverse effect than other metals found in these sediments. The calculated I_geo, Enrichment Factor, and Contamination Factor values indicate that Mo, Hg, Sn, Cu, and Zn are highly enriched in the Buckingham Canal sediments, suggesting the rapid urban and industrial development of Chennai Metropolitan City have negatively influenced on the surrounding aquatic ecosystem.     

Fractionation and ecological risk of metals in urban river sediments in Zhongshan City, Pearl River Delta

Surface sediments collected from nine urban rivers located in Zhongshan City, Pearl River Delta, were analyzed for total concentration of metals with digestion and chemical fractionation adopting the modified European Community Bureau of Reference (BCR) sequential extraction procedure. The results showed that concentration and fractionation of metals varied significantly among the rivers. The total concentration of eight metals in most rivers did not exceed the China Environmental Quality Standard for Soil, Grade III. The potential ecological risk of metals to rivers were related to the land use patterns, in the order of manufacturing areas > residential areas > agriculture areas. The concentration of Pb in the reducible fraction was relatively high (60.0-84.3%). The dominant proportions of Cd, Zn and Cu were primary in the non-residual fraction (67.0%, 71.8% and 81.4% on average respectively), while the percentages of the residual fractions of Cr and Ni varied over a wide range (43-85% and 24-71% respectively). The approaches of the H?kanson ecological risk index and Secondary Phase Enrichment Factor were applied for ecological risk assessment and metal enrichment calculation. The results indicated Hg and Cd had posed high potential ecological risk to urban rivers in this region. Meanwhile, there was widespread pollution and high enrichment of Cu in river sediments in this region. Multiple regression analysis showed that five water quality parameters (pH, DO, COD(Mn), NH(4)(+)-N, TP) had little influence on the distribution of metal fractionation. This result revealed that the ecological risk of metals was not eliminated along with the improvement in water quality. Correlation studies showed that among the metals, Group A (Cd, As, Pb, Zn Hg, r = 0.730-0.924) and Group B (Cr, Cu, Ni, r = 0.815-0.948) were obtained, and the metal contaminations were from industrial activities rather than residential.