镇江市金山湖沉积物磷元素分布特征研究

以镇江市金山湖为研究区域,于2019年1月（冬季）和2019年7月（夏季）采集了10个点位的表层沉积物样品,参照欧洲标准测试测量组织建立的沉积物磷形态分析方法（SMT）测定沉积物总磷（TP）、无机磷（IP）、有机磷（OP）、铁/铝-磷（Fe/Al-P）和钙-磷（Ca-P）质量分数,研究金山湖表层沉积物磷元素及其赋存形态的季节分布特征。结果表明,金山湖表层沉积物中TP质量分数在冬、夏季分别为727.39~1 073.70 mg/kg和700.90~1 002.17 mg/kg,处于中等污染水平;金山湖表层沉积物磷以IP为主,IP在TP中的占比在冬、夏季分别为68.58%~88.86%,73.09%~87.21%;除了Fe/Al-P以外,OP作为生物有效磷源,其冬、夏季质量分数分别为69.37~190.93 mg/kg和108.45~210.42 mg/kg;其平均值分别为129.01,160.15 mg/kg。金山湖冬、夏季沉积物各形态磷质量分数所占比例均表现为Ca-P>Fe/Al-P>OP,表明该研究区域沉积物以Ca-P占优势。金山湖表层沉积物pH值呈现弱碱性,通过Ca-P直接释放到上覆水中的磷较少,故金山湖沉积物磷元素的潜在风险较小。各形态磷的相关性分析结果发现,冬季沉积物TP与Fe/Al-P、IP呈极显著正相关（P<0.01）。夏季沉积物TP与IP、Fe/Al-P之间呈极显著正相关（P<0.01）,与Ca-P呈显著正相关（P<0.05）。此外,金山湖沉积物OP、Fe/Al-P以及Ca-P的来源不一致。pH值对沉积物IP会产生一定影响,而其余磷形态则受pH值的影响程度较小。     

海河干流（市区段）表层沉积物重金属污染及变化趋势分析

根据1990—2006年监测资料,对海河干流（市区段）沉积物中重金属的现状和变化趋势进行了分析,采用地积累指数和Hakanson危害指数对海河干流（市区段）沉积物重金属富集现状和对水生生物危害进行评估。结果显示：海河干流（市区段）表层沉积物除Zn外,均呈现污染下降趋势。海河干流（市区段）沉积物中重金属对生物潜在危害顺序为Cd〉Hg〉As〉Cu〉Pb〉Cr〉Zn,各项指标对生物潜在危害性上游大于下游。     

梁子湖水体和沉积物中邻苯二甲酸酯分布特征及生态健康风险评价

对枯水期、平水期和丰水期梁子湖水体和沉积物中7种邻苯二甲酸酯（PAEs）的污染水平及分布特征进行了研究,并评价了其健康风险和生态风险。结果表明,枯水期、平水期和丰水期梁子湖水体中7种PAEs总量（∑PAEs）分别为0.10~3.56、0.16~1.78、0.57~2.16 μg/L,沉积物中∑PAEs分别为0.10~0.41、0.21~0.66、0.12~4.49 μg/g,3个水期的水体和沉积物中均以邻苯二甲酸二异丁酯（DiBP）和邻苯二甲酸二（2-乙基己基）酯（DEHP）占主要组分。与国内外其他河流/湖泊相比,梁子湖水体和沉积物中各PAE单体的含量均处于中等偏低水平。健康风险评价结果表明,梁子湖水体中PAEs的总非致癌风险值均远低于1,不会对人体产生明显的非致癌健康危害;3个水期绝大部分或全部采样点位中DEHP对人体存在潜在的致癌风险。生态风险评价结果表明,枯水期和丰水期沉积物中PAEs总量对水藻类和鱼类达到中等风险程度,对其存在较大的毒性。     

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。     

江苏省沿海脊尾白虾养殖池塘重金属污染及潜在生态危害评价

于2020年对江苏省沿海脊尾白虾养殖区池塘的海水、沉积物和脊尾白虾肌肉组织中的重金属进行分析,同时采用单因子污染指数法和潜在生态风险指数法对其沉积物重金属进行评价。结果显示,养殖池塘水体中铜（Cu）、铅（Pb）、镉（Cd）和锌（Zn）的平均质量浓度分别为3.13,1.02,0.094和28.02 μg/L;沉积物中的平均质量分数分别为22.88,19.93,0.18和140.69 mg/kg;虾肌肉组织中的平均质量分数分别为12.49,0.50,0.18和28.65 mg/kg。生态环境质量评价结果表明,参照《海水水质标准》（GB 3097—1997）,水体中Cu、Pb和Cd的质量浓度达到一类标准,Zn的质量浓度达到二类标准,属于清洁水平;沉积物中重金属的质量分数均达到《海洋沉积物质量标准》（GB 18668—2002）一类标准,属于较清洁水平,潜在生态风险为Cd>Zn>Cu>Pb,整体为轻微生态风险等级,Cd为主要污染元素;虾肌肉组织中重金属Pb和Cd的质量分数均达到《无公害食品 海水虾》（NY 5058—2006）标准。     

洪泽湖湖滨带表层沉积物氮、磷、有机质分布及污染评价

洪泽湖作为中国第四大淡水湖泊,是江苏北部地区重要的水源地,同时也是南水北调东线工程的重要调蓄湖泊之一,研究其湖滨带表层沉积物氮、磷、有机质的污染情况对维持洪泽湖水安全和生物多样性具有重要现实意义。基于2020年8月于洪泽湖湖滨带采集的43个表层（0~10 cm）沉积物样品,分析了总氮（TN）、总磷（TP）和有机质（OM）含量的空间分布特征及相关性,并运用综合污染指数法和有机污染指数法评价其污染程度。结果表明,洪泽湖湖滨带表层沉积物TN、TP、OM含量范围分别为232~2 152 ,123~439,0.91~18.65 mg/kg,均值分别为985,276,10.93 mg/kg;空间分布上均表现为东部大堤、成子湖和西部区域的TN、TP、OM含量高于过水通道;Pearson相关性分析显示,表层沉积物中ω(OM)与ω(TN)（r=0.705,P<0.01）、ω(TN)与ω(TP)（r=0.504,P<0.01）呈显著正相关;洪泽湖湖滨带表层沉积物综合污染指数范围为0.45~1.88,平均值为0.93,有机污染指数范围为0.001~0.221,平均值为0.067,2种评价方法均显示洪泽湖湖滨带表层沉积物中TN、TP、OM整体处于清洁—轻度污染状态。     

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。     

千岛湖沉积物中碳、氮、磷的分布特征及污染评价

通过测定千岛湖柱状沉积物中有机质（OM）、总氮（TN）和总磷（TP）含量,分析其污染分布特征,并评价污染水平。结果表明,千岛湖沉积物中OM、TN、TP平均值分别为1.44%、1.86mg/g、0.89mg/g。空间分布差异明显,城区库湾、新安江干流沿线污染相对较重;垂直分布,OM、TN、TP整体上均从湖底由下而上呈逐步上升变化过程。相关性分析表明,该湖沉积物中OM、TN、TP具有较高的同源性,氮、磷多以有机形式存在。C/N值表明,该湖沉积物中有机质主要来自内源的水生生物分解。评价结果显示,综合污染指数范围为1.1～4.2,该湖整体上处于重度污染水平,TP污染重于TN;有机指数范围为0.04～0.52,整体上属于轻度污染水平。     

TOA—苯体系萃取分离—原子吸收法测定环境水样中铬（Ⅲ）和铬（Ⅵ）

研究了三正辛胺（ＴＯＡ）－茉体系对Ｃｒ（Ⅲ）和Ｃｒ（Ⅵ）的选择性萃取作用,在硫酸介质中可将水相中的Ｃｒ（Ⅵ）萃取到有机相里,而Ｃｒ（Ⅲ）仍留在留在水相中,用原子吸收法（ＡＡＳ）测定可求得Ｃｒ（Ⅲ）和Ｃｒ（Ⅵ）的含量,回收率分别为９４％￣１０５％和９４％￣１０４％。方法简单、快速、准确。     

湖泊沉积物中有机磷酸酯阻燃剂污染特征及生态风险评价

利用气质联用仪（GC-MS）检测广州15个城市湖泊表层沉积物中16种有机磷酸酯阻燃剂（OPFRs）含量,分析其分布特征及来源,并评价其生态风险。结果表明,广州15个城市湖泊沉积物中16种 OPFRs总质量比（∑16OPFRs）范围为138ng/g～306ng/g,平均值为203ng/g,污染属于中等水平。TBEP、TCEP、TBP、TDCP为主要OPFRs,其中TBEP值最高。相关性研究表明,大部分OPFRs单体与总有机碳无显著相关性,OPFRs来源具有点源性特征。主成分分析表明,沉积物中 OPFRs 来源并不单一,游客产生的废弃塑料、大气沉降、污水排放、路面径流及污泥再利用等都可能成为其来源。生态风险评价表明,沉积物中OPFRs存在一定的生态风险。     

RECOVERY: A Contaminated Sediment-Water Interaction Model

This paper describes the U.S. Army Corps of Engineers screening-level water quality model (RECOVERY version 3.0) for assessing long-term impacts of contaminated bottom sediments on surface waters. The model couples contaminant interaction between the water column and the bottom sediment, as well as between contaminated and clean bottom sediments. The analysis is intended primarily for organic contaminants with the assumption that the overlying water column is well mixed vertically. The contaminant is assumed to follow linear, reversible, equilibrium sorption and first-order decay kinetics. The system is physically represented as a well-mixed water column (i.e., zero-dimensional) underlain by a vertically-stratified sediment column (i.e., one-dimensional). The sediment is well-mixed horizontally but segmented vertically into a well-mixed surface (active) layer and deep sediment. The deep sediment is segmented into variably contaminated and clean sediment regions. Processes incorporated in the model are sorption, decay, volatilization, burial, resuspension, settling, bioturbation, and pore-water diffusion. The solution couples contaminant mass balance in the water column and in the mixed sediment layer along with diffusion in the deep sediment layers. The model was verified against laboratory and field data, as well as against an analytical solution for the water and mixed sediment layers. These comparisons indicate that the model can be used as an assessment tool for evaluating remediation alternatives for contaminated bottom sediments.     

Observation of saltwater intrusion and ETM dynamics in a stably stratified estuary: the Yangtze Estuary,China

Spatial and temporal measurement data describing spring–neap variations of velocity, salinity, and suspended sediment concentration (SSC) in the North Passage Deepwater Navigational Channel (DNC) of the Yangtze Estuary, China, were obtained in the wet season of 2012. These data were collected in the middle of the DNC and apparently document the formation of a rather stable density stratification interface and salt wedge, especially during neap tides and slack waters. The convergent zone of residual currents, salinity transport, and sediment transport during neap and spring tides oscillates in the middle and lower reach of the DNC. It encourages the formation of a near-bed high-SSC layer, which favours siltation in the dredged channel. Both the near-bed gradient Richardson number and the bulk/layer Richardson number vary dramatically from around zero to several hundred from spring to neap tides. Stratification and turbulence damping effects near the estuarine turbidity maximum (ETM) area induce the upper half (near water surface) of the water body to be ebb-dominant and the lower part (near-bed) to be flood-dominant, which is a previously undocumented phenomenon in this region. These data reveal that the residual pattern of currents, salt flux and sediment flux are of critical differences in a stratified estuary, and that the salinity-induced baroclinic pressure gradient is a major factor controlling the vertical velocity structure. In addition, field observations indicate that the salinity and sediment transport of residuals generated by internal tidal asymmetry plays a dominant role in maintaining a stable density stratification interface near the estuarine front.     

An HPLC method development for the assessment of degradation products of anthraquinone dye

The behavior of metsulfuron-methyl and its residues in an artificial pond was studied using a ¹⁴C isotopic tracer technique. Throughout the experimental period, the majority of metsulfuron-methyl residues were sustained in the pond water. Furthermore, the metsulfuron-methyl residues were just found in the surface layer of the sediment, and the transfer distance of these residues had only reached 9?C12 cm by the end of the experiment. The extract residues of metsulfuron-methyl in sediment were slightly higher than those of the bound residues (BR) during the initial experiment stage, while the BR dominated the surface sediment after 45 days. Finally, the metsulfuron-methyl residues could be combined with humus in the surface sediment, and the distribution of metsulfuron-methyl residues in fulvic acid was significantly higher than that in humic acid.     

滇池污染底泥环保疏浚一期工程实施后环境效益评估

通过对滇池草海污染底泥环保疏浚一期工程实施前后水质、底质及水生生物的监测和分析,评价工程实施后对改善草海水质,减轻内源负荷及对水生态恢复的环境效益。结果表明,疏浚工程直接去除了草海污染底泥层,随污染层分别去除TN、TP20 538 t和1 716 t。疏浚后草海水体透明度由0.37 m提高到0.80 m,水体中的TN和TP由疏挖前的8.91 mg/L和1.07 mg/L降低到疏挖后的8.15 mg/L和0.69 mg/L。疏浚后新生界面层促使形成新的水—沉积物的平衡,水质与底质条件改善以及水下光照条件超过沉水植物恢复的需求,是疏浚后水生态呈现恢复趋势的机理。     

Distribution and contamination assessment of heavy metals in sediment of the Second Songhua River, China

The Second Songhua River was subjected to a large amount of raw or primary effluent from chemical industries in Jilin city in 1960s to 1970s, resulting in serious mercury pollution. However, an understanding of other trace metal pollution has remained unclear. The objective of this study was to investigate trace metal contamination in the sediment of the river. Bottom sediment samples were taken in the river between Jilin city and Haerbin city in 2005. An uncontaminated sediment profile was taken in the Nen River at the same time. Total concentrations of Al, Fe, Mg, Ca, K, Na, Ti, Mn, V, Sc, Co, Cu, Cr, Ni, Pb and Zn in the sediment samples were measured by ICP-MS or ICP-OES, following digestion with various acids. Concentrations of Co, Cu, Cr, Ni, Pb and Zn in the surface sediments were 5.1–14.7, 18.5–78.9, 2.4–75.4, 7.2–29.0, 13.5–124.4, and 21.8–403.1 mg/kg, respectively, generally decreasing along the course of the river from Jilin city to Haerbin city. Background concentrations of trace metals were reconstructed by geochemical normalization to a conservative element scandium. Results showed that concentrations of Co, Cr, and Ni in the sediment were generally only slightly higher than or equal to their background values, while concentrations of Cu, Pb, and Zn in the some sediment samples were significantly higher than their background values. In detail, the sediment at Jilin city was moderately contaminated by Cu, and the sediment of the Second Songhua River was moderately contaminated by Pb and Zn. The top layer (0–10 cm depth) and bottom layers (30–46 cm depth) of one sediment profile at Wukeshu town were generally moderately polluted by Pb and Zn. Synthetically, the surface sediment in the studied river section was classified as natural sediment without ecological risk by the sediment pollution index (SPI) of Cu, Cr, Ni, Pb and Zn. Only the 30–45 cm depth of the sediment profile at Wukeshu town was classified as low polluted sediment by the SPI of these metals, recording a historical contamination of the river in the 1960s to 1970s. This buried contamination of trace metals might pose a potential risk to water column under disturbance of sediment. Foundation item: The National Basic Research Priorities Program of China (2004CB418502)     

Sedimentation and remobilization of radiocesium in the coastal area of Ibaraki, 70 km south of the Fukushima Dai-ichi Nuclear Power Plant

Sedimentation and remobilization processes of radiocesium were investigated from time-series observations at nine stations in the coastal area of Ibaraki, 70–110 km south of the Fukushima Dai-ichi Nuclear Power Plant (1FNPP). Sediment samples were collected four times between June 2011 and January 2012, and concentrations of radiocesium as well as sediment properties such as grain size and elemental compositions were analyzed. Cumulative inventory of ¹³⁷Cs in sediment (0–10 cm) ranged between 4?×?10³ and 3?×?10⁴ Bq/m² as of January 2012. This amount was generally higher at stations nearer 1FNPP and has remained at the same level since August 2011. From these results, it can be inferred that dissolved radiocesium advected southward from the region adjacent to the 1FNPP and was deposited to the sediment of the study area in the early stage after the accident. The incorporation of radiocesium into sediments was almost irreversible, and higher concentrations of ¹³⁷Cs were obtained from the finer-grained fraction of sediments. In the northern offshore stations, resuspension of the fine-grained sediments formed a high-turbidity layer 10–20 m above the seabed. These results indicate that radiocesium-enriched fine particles were transported from the coast to offshore regions through the bottom high-turbidity layer.     

Check dam sediments: an important indicator of the effects of environmental changes on soil erosion in the Loess Plateau in China

Check dam sediments document the process of soil erosion for a watershed. The main objectives of this research are as follows: first, to determine whether the sediments trapped in check dams can provide useful information about local erosion and the environment, and second, to obtain the extent to which they can be stratigraphically interpreted and correlated to the land use history of an area controlled by check dams. Particle size and the concentration of ¹³⁷Cs in sediments are the indicators used to study the effects of environmental changes on soil erosion in the Loess Plateau, China. A total of 216 soil samples were collected from four sediment profile cores at the Yangjuangou watershed check dam constructed in 1955 and fully silted with sediments by 1965. The results indicated that ¹³⁷Cs dating and sediment particle size can characterize the sediment deposition process. Silt makes up more than 50 % of the sediment; both the clay and silt sediment fractions decrease gradually in the upstream direction. The sediment profiles are characterized by three depositional layers. These layers suggest changes in the land use. The top layer showed tillage disturbance, with moderate sediments and new soil mixed from 0 to 20 cm. A transition stage from wetlands (characterized by vegetation such as bulrush) to cropland is inferred from sediments at depths of 20–85 cm. Below 85 cm, sedimentary layering is obvious and there is no tillage disturbance. At the downstream site, A0, the average rate of sediment deposition from 1958 to 1963 was approximately 6,125.4 t year^?1 km^?2. Because of their high time resolution, check dam sediments indicate the effects of environmental changes on soil erosion, and they can provide a multiyear record of the soil erosion evolution at the local scale in the middle reaches of the Yellow River.     

微波萃取技术在分析土壤中有机污染物的应用

介绍了微波萃取技术及其使用的试剂、设备和条件,对微波萃取在分析土壤中有机污染物的应用予以综述,阐述了微波萃取技术是分析土壤中有机污染物的好方法。     

Biological responses to sediment remediation based on thin layer placement near a former pulp mill in Ward Cove, AK (USA)

In 2001, 28 acres of the bottom of Ward Cove, AK (USA) were remediated using thin layer placement, to enhance the natural recovery of contaminated sediments. The remediated areas were part of an 80-acre area of concern identified offshore from the site of a former sulfite pulp mill. The primary chemicals of concern were those commonly associated with organic enrichment near pulp mills: ammonia and 4-methylphenol. The primary remedial objectives were to reduce the toxicity of the contaminated sediments and to stimulate colonization of the remediated areas by benthic macroinvertebrates. In 2004, the initial monitoring event for the remediated areas was conducted, and included evaluations of physical/chemical sediment variables (i.e., total organic carbon, grain size distribution, ammonia, and 4-methylphenol), sediment toxicity (i.e., using the 10-day amphipod survival test with Eohaustorius estuarius), and in situ benthic macroinvertebrate communities. Results of the monitoring event showed that conditions in the remediated areas had improved considerably in the 3 years since thin layer placement had occurred. At most stations, concentrations of both ammonia and 4-methylphenol were very low, and amphipod survival was >or=90%. In addition, benthic macroinvertebrates appeared to be rapidly colonizing the remediated areas, based on evaluations of several community metrics (i.e., taxa richness, diversity, and dominance), as well as key indicator species of organic enrichment and associated transitional areas (i.e., primarily the polychaetes Capitella capitata and Nephtys cornuta, and the bivalve molluscs Axinopsida serricata and Parvilucina tenuisculpta). In general, colonization was consistent with the patterns identified for areas recovering from organic enrichment on the continental shelf of southern California and elsewhere. Based on these results, thin layer placement was considered successful in enhancing the natural recovery of the remediated sediments in Ward Cove.     

Fugacity approach to evaluate the sediment-water diffusion of polycyclic aromatic hydrocarbons

Diffusion is an important process for sediment-water exchange and plays a vital role in controlling water quality. Fugacity fraction (ff) was used to estimate the sediment-water diffusion of polycyclic aromatic hydrocarbons (PAHs) between seawater and surficial sediment. A total of 33 surface sediment and sea water samples were collected concurrently from the northeast coastal area in China and 25 PAHs were analyzed including the alkylated and chlorated PAHs. Fugacity fraction was calculated based on the PAH concentrations in water and sediment, octanol-water partition coefficient of PAHs, organic matter content in sediment, and density of sediment. The calculated results showed that ff increased with decreasing molecular weight of PAHs. The low molecular weight PAHs (2-3 rings) transferred from sediment to water and the sediment acted as a secondary source to the water. The medium molecular weight PAHs (4-5 rings) were close to the sediment-water equilibrium and the transfer tendency shifted between sediment and water. The high molecular weight PAHs (5-6 rings) transferred from water into sediment and the sediment acted as a sink. Soot carbon and the difference of PAH concentrations between sediment and water were found to be important factors affecting the sediment-water diffusion. This study provided new insight into the process of sediment-water diffusion, which has a great influence on the quality of water, especially in severely-polluted sediment areas.