焦化厂污染场地表层土壤有机-矿质复合体中多环芳烃的分布

采用湿法物理分级方法将湖南省某焦化厂遗留场地表层土壤分成4种粒级的有机-矿质复合体组分,即粘粒(<2μm)、粉粒(2—20μm)、细砂(20—200μm)和粗砂(>200μm),并研究了美国EPA优先控制的16种多环芳烃(PAHs)在其中的分布特征及土壤不同有机-矿质复合体组分中有机质和矿物质组成的差异对PAHs赋存分布的影响.研究结果表明,不同粒级有机-矿质复合体中PAHs的含量顺序为粗砂>粉粒>细砂>粘粒,低环PAHs(环数≤3)在粘粒中的含量较高,达到56.3%,而高环PAHs(环数≥4)在粉粒、细砂和粗砂中的分布较高含量分别是79.37%、72.7%和71.63%,各粒级矿质复合体中PAHs含量与土壤有机碳有较好的相关性.通过对有机-矿质复合体进行X射线衍射分析发现,场地土壤粘粒和粉粒中粘土矿物含量较高,这也在一定程度上影响了污染物质在其中的分布.     

Sediment preferences and oil contamination in the Pacific sand lance Ammodytes hexapterus

Sand lance, Ammodytes hexapterus Pallas, forage for zooplankton in the water column and are under heavy predation from fish, marine birds and marine mammals. To avoid predation, these fish bury themselves in soft bottom sediments when not foraging and during overwintering. We collected sand lance in Sequim Bay, Washington State, USA, in 1982. In three experiments we presented the fish with: (1) four different sediment types (fine sand, coarse sand, gravel, silt) to determine their sediment preferences; (2) clean and oil-contaminated preferred sediment to determine whether the fish would avoid the contamination; and (3) clean unpreferred and oil-contaminated preferred sediment to determine whether the contamination would alter their sediment preferences. In the first experiment, sand lance preferred to bury in fine and coarse sands and avoided gravel and silt. In the second experiment, sand lance avoided sand contaminated with Prudhoe Bay crude oil (116 and 1050 ppm). In the third experiment, sand lance avoided the oiled sand (131 and 1041 ppm) and buried in clean gravel, and also avoided both oiled sand (113 and 1004 ppm) and clean silt, and chose to remain in the water column. The sediment particle size and the way it affects water flow through the sediment seemed to be responsible for the preferences. We suggest that the sediment type, the sediment distribution, the nutritional state of the fish, and the predation pressure influence how sand lance use the sediment as a refuge and how they respond to contamination of that refuge.Contribution No. 1392 of the School of Oceanography, University of Washington     

退耕还湖后安庆沿江湿地土壤颗粒分形特征

以安庆沿江不同退耕还湖方式(白荡湖区,低坝高网式养鱼;菜子湖区,自然恢复湿地)和不同历史利用方式(水耕和旱耕)的湿地土壤为研究对象,分析退耕还湖后湿地土壤的颗粒分形特征变化。结果表明,退耕还湖后白荡湖区湿地土壤颗粒分形维数和<0.01 mm粒径颗粒含量降低,且历史水耕湿地土壤颗粒分形维数降幅小于历史旱耕湿地;菜子湖区湿地土壤颗粒分形维数和<0.01 mm粒径颗粒含量升高,且历史水耕湿地土壤颗粒分形维数增幅大于历史旱耕湿地。2个湖区湿地土壤颗粒分形维数与土壤细黏粒、粗黏粒和细粉粒含量呈显著正相关(P<0.01),与粗粉粒、细砂粒和粗砂粒含量呈显著负相关(P<0.01),与土壤有机质、全磷和有效氮含量呈显著正相关(P<0.05),土壤颗粒分形维数和土壤养分含量的聚类分析结果总体相似。土壤颗粒分形维数可作为评价退耕还湖后湿地生态恢复过程中土壤演变状况的重要参考指标。     

Assessment of Trace Metals in the Sediments From the Coastal Zone of Alexandria, Egypt

Freshly deposited surface sediments from the Alexandria coastal zone were collected and analysed in 1995 for their trace metal concentrations. Metal concentrations in the sediments vary between sites within a wide range for copper, zinc, iron, lead, chromium and cadmium. the statistical analysis between the metal concentrations and the different constituents (organic carbon, total nitrogen, silt, clay and total iron) showed significant correlations. the enrichment factors for the sediments ranged between 3 and 4-fold for copper, chromium and zinc and reached up to 9-fold for lead and 113-fold for cadmium. the highest index for cadmium and lead may be attributed to the anthropogenic inputs from the surrounding area, where they are highest in lower discharge areas.     

Assessment of Trace Metals in the Sediments From the Coastal Zone of Alexandria,Egypt

Freshly deposited surface sediments from the Alexandria coastal zone were collected and analysed in 1995 for their trace metal concentrations. Metal concentrations in the sediments vary between sites within a wide range for copper, zinc, iron, lead, chromium and cadmium. the statistical analysis between the metal concentrations and the different constituents (organic carbon, total nitrogen, silt, clay and total iron) showed significant correlations. the enrichment factors for the sediments ranged between 3 and 4-fold for copper, chromium and zinc and reached up to 9-fold for lead and 113-fold for cadmium. the highest index for cadmium and lead may be attributed to the anthropogenic inputs from the surrounding area, where they are highest in lower discharge areas.     

入田泥沙对黄河三角洲地区土壤物理性状的影响——以小开河引黄灌区为例

为研究人田泥沙对小开河灌区自然土壤的影响,用分析化验和工程测试等方法,分析了引黄泥沙和输沙人田后土壤颗粒组成、容重、孔隙状况等物理性状。结果表明：引黄泥沙中0．02～0．002mm的细粉粒比例最高,平均39-31％。小开河自然土壤中0．05-0．02mm的粗粉粒比例最高,为53．41％,泥沙中细粉粒和粘粒含量明显高于当地土壤。输沙人田使灌区土壤中0．02—0．002mm的细粉粒和〈0．002mm的粘粒比例明显增加,〉0．02mm的颗粒比例下降,虽有效避免了因渠首集中沉沙造成的土壤沙化和生态环境恶化,但增加了土壤的粘重程度。农田耕作在一定程度上增加土壤通气孔隙比例、降低土壤容重,但土壤毛管孔隙度依旧稳定在40％左右,毛管作用旺盛,使土壤通气状况不能满足作物需求。在黄河三角洲地区输沙入田的泥沙处理,应结合当地土壤的基本性质和水盐运动规律配置泥沙,以免增强当地土壤紧实、通透性差的性状。     

入田泥沙对黄河三角洲地区土壤物理性状的影响——以小开河引黄灌区为例

为研究入田泥沙对小开河灌区自然土壤的影响,用分析化验和工程测试等方法,分析了引黄泥沙和输沙入田后土壤颗粒组成、容重、孔隙状况等物理性状。结果表明:引黄泥沙中0.02～0.002mm的细粉粒比例最高,平均39.31%。小开河自然土壤中0.05～0.02mm的粗粉粒比例最高,为53.41%,泥沙中细粉粒和粘粒含量明显高于当地土壤。输沙入田使灌区土壤中0.02～0.002mm的细粉粒和﹤0.002mm的粘粒比例明显增加,0.02mm的颗粒比例下降,虽有效避免了因渠首集中沉沙造成的土壤沙化和生态环境恶化,但增加了土壤的粘重程度。农田耕作在一定程度上增加土壤通气孔隙比例、降低土壤容重,但土壤毛管孔隙度依旧稳定在40%左右,毛管作用旺盛,使土壤通气状况不能满足作物需求。在黄河三角洲地区输沙入田的泥沙处理,应结合当地土壤的基本性质和水盐运动规律配置泥沙,以免增强当地土壤紧实、通透性差的性状。     

现代黄河三角洲土壤特性对多氯联苯分布的影响规律

对现代黄河三角洲22个表层土壤样品中类二噁英类多氯联苯(PCBs)进行双毛细管柱GC-ECD结合MS测试,并使用相关数学统计学分析方法-相关性研究方法研究了现代黄河三角洲地区土壤特性对PCBs分布的影响,结果表明:土壤有机质量分数与其类二噁英类PCBs的总质量浓度呈弱的正相关关系。土壤粒径组成中粘粒质量分数与其类二噁英类PCBs的总质量浓度呈相关性关系,且达到极显著的水平;粉砂粒的质量分数与类二噁英类PCBs的总质量浓度无相关关系;砂粒质量分数与类二噁英类PCBs的质量浓度呈负相关关系,达到显著相关的水平。土壤溶解盐质量分数及pH值与类二噁英类PCBs的总量没有明显的相关性。可见,土壤中有机质、土壤颗粒组成中粘粒和砂粒质量分数是影响现代黄河三角洲地区土壤中PCBs分布的主要因素。     

Neue Aspekte in der Behandlung von Siedlungsabflüssen

The surface runoff from urban areas is one of the most important sources of pollutants emitted into surface waters. Suspended solids which act as a transport vehicle for many anthropogenic pollutants (e.?g. heavy metals, PAH) are a key factor in this regard. The development of efficient measures of storm water runoff treatment thus requires a further differentiation of suspended solids in a fine (clay and silt) and coarse (sand and gravel) fraction. Both fractions show distinctly different characteristics in pollutant loading, transport and retention on urban surfaces and sewer systems. The primary aim of storm water runoff treatment is the reduction of the fine particles which are always highly loaded with anthropogenic pollutants. In contrast the coarse particles are almost unpolluted especially if they have a low organic share. The widespread sedimentation tanks with surface loadings between 10 and 2?m/h are very inefficient. A significant, save and lasting reduction of the emitted load of fine particles requires a considerable reduction of the surface loads. That can be achieved with the installation of lamellar settler or the utilization of the very large volumes of flood management tanks frequently present in urban areas. Filtration plants are highly efficient but there application in urban areas is limited due to their high space demands.     

藏北高寒草原样带土壤有机碳分布及其影响因素

沿藏北高寒草原冈底斯山-申扎-双湖样带（30°25′N至33°6′N）,在37个样点采集土壤和植物样品,分析藏北高寒草原土壤有机碳含量及其影响因素。结果表明：藏北高寒草原土壤0~15、15~30和0~30 cm有机碳含量分别为2.27、2.17和4.44 kg.m-2。土壤有机碳含量沿样带呈随着纬度的增加而减少的趋势。藏北高寒草原土壤质地总体偏粗,不同质地土壤之间有机碳含量大小关系为砂土〈壤质砂土〈粉壤土〈砂质壤土〈壤土。不同深度土壤有机碳含量与土壤颗粒含量相关性存在显著差异,0~15 cm土壤有机碳与粉粒、黏粒含量呈显著性正相关,与砂粒含量呈显著性负相关,而15~30 cm土壤有机碳含量与土壤颗粒组成相关性不显著。0~15 cm土壤有机碳含量与草地盖度、地下生物量和总生物量呈显著或极显著正相关,与优势种高度呈极显著负相关;15~30 cm土壤有机碳含量与优势种高度呈显著负相关。     

Physico-chemical characteristics of the peloid mud from Morinje Bay (eastern Adriatic coast, Croatia): suitability for use in balneotherapy

The study conducted in the Morinje Bay (Central Dalmatia, Croatia) included the investigation of the sedimentological, physico-chemical and geochemical properties of the Morinje Bay sediments in order to assess the suitability of the material for wellness-related purposes including medicinal use. The sedimentological characteristics of the Morinje mud are in accordance with the geological origin of the material; the sediment is fine grained, composed mostly of carbonates, quartz and clay minerals. The composition of the sediment determines the physico-chemical properties of the mud. The high content of carbonate minerals diminishes adsorbing the characteristics of the mud to some extent; however, they are still comparable to some commercial mud already successfully used for medicinal purposes. Geochemical analyses have shown that trace metals concentrations in the Morinje Bay samples were mostly in the range with similar material from unpolluted Adriatic environments. Only the concentrations of Cu, Pb, Zn and As were slightly higher than in the reference material, but still within acceptable limits.     

Sediment characterisation of the 26 December 2004 Indian ocean tsunami in Andaman group of islands, bay of Bengal, India

The large tsunami, which was generated by an earthquake on 26 December 2004, affected most of the countries around the Indian Ocean. A total of 48 tsunamigenic surface sediments have been collected from various coastal geomorphological features such as beaches, estuaries/creeks and mangrove areas in the Andaman group of islands. These samples were analysed for sediment characteristics such as sediment texture, granulometric studies. The studied tsunamigenic sediments, deposited by the 26 December 2004 tsunami in the Andaman group of islands consist of poorly sorted, coarse sand to medium sands, and are similar to depositional effects of previously reported earthquake-generated tsunami waves. The tsunamigenic sediment consists of a coarse sand layer with abundant reworked shell and other carbonate fragments. The tsunami sediments were mainly composed of boulders of corals and sand which determines the high-energy environment throughout the study area. The variation in Ф mean size, therefore, reveals the differential energy conditions that lead to the deposition of these kinds of sediments in different locations. The tsunamigenic sediments were mainly poorly sorted, moderately well sorted and well sorted during the post-tsunami (2005) and whereas they were mainly moderately well sorted to well sorted during the post-monsoon (2008). The symmetry of the samples varies from strongly fine skewed to strongly very coarse skewed in the post-tsunami (2005) and post-monsoon (2008). The Kurtosis of the tsunami sediments were mainly Platykurtic, Mesokurtic and Lepokurtic during the post-tsunami (2005) and mainly Mesokurtic and Lepokurtic in post-monsoon (2008).     

Pier scour within long contraction in cohesive sediment bed

In the present study, an attempt has been made to study the bridge pier scour embedded long contraction for the bed sediment prepared by a mixture of clay and fine sand with varying proportions having a specific range of antecedent moisture content. Results particularly focused on the clay–sand mixed cohesive bed at varying clay fractions of the sediment bed, approach flow velocity, contraction ratio and different pier shapes, on maximum equilibrium scour depth for pier scour within long contraction. Further, regression based equations for the estimation of non-dimensional maximum scour depth for piers within long contraction in clay–sand mixed cohesive bed embedded were proposed.     

Spatial Variations of Heavy Metals in the East China Sea Continental Shelf Surface Sediments

Surface sediments collected from continental shelf of the East China Sea were analyzed for heavy metals (iron, manganese, copper, zinc, lead, cadmium), carbonate, organic carbon contents, and grain sizes. the range of concentrations observed were iron: 0.3-1.3 wt%, manganese: 2.3-14 μmole/g, copper: 7.1-184 μmole/g, zinc: 0.16-0.77μmiole/g, lead: 15-98 μmole/g, cadmium: 0.17-3.9 μmole/g, carbonate: 3.6-87 wt%, sand: 10-100%, silt: 0-70% and clay: 0-50%.

A zonal distribution pattern of the heavy metals was found in the East China Sea Continental shelf sediments. High concentrations of most heavy metals, organic carbon and fine-grained sediments were observed in the inner shelf zone, especially those near the discharge of the Yangtze River. Concentrations of these heavy metals decreased from the inner shelf to the shelf break region. High concentrations of metals were also found in sediments near Taiwan. Iron concentrations decreased north-east of the central shelf region. High concentrations of cadmium were found in the shelf break region where biogenic carbonate is predominant. This study showed that biogenic carbonate in the East China Sea shelf break region and the terrigenous sediments from the Yangtze River and island of Taiwan were the major sources of heavy metals. Heavy metal concentrations were strongly influenced by the content of the coarse-grained quartz sand present in the sediments.     

The relationship between epilithic periphyton (biofilm) bound metals and metals bound to sediments in freshwater systems

Surficial sediments and epilithic periphyton (biofilm) were sampled from six sites on the River Churnet and five sites on the River Manifold in Staffordshire and analysed for cadmium (Cd), copper (Cu), lead (Pb) and zinc (Zn). The sites demonstrated a wide range of sediment trace metal concentrations determined by inductively coupled plasma optical emission spectrometry (ICP-OES) and atomic absorbtion spectroscopy (AAS). Biofilm was removed from the substrate using physical abrasion and 0.005 M ethylenediaminoethanetetra-acetic acid (EDTA) extractant. The European Standards, Measurements and Testing Programmes (BCR) operationally defined geochemical speciation scheme was used to determine the exchangeable, acid soluble fraction of the sediments. Significant positive correlations were determined between the EDTA extractable biofilm and the exchangeable sediment fraction for Cd, Cu and Zn but not for Pb. Natural epilithic periphyton may be a potential metal biomonitor particularly of Cu, Cd and Zn in aquatic systems and provide supporting information in relation to potential sediment toxicity.     

Study on particulate and metallic elements variation at daytime and nighttime period in urban atmosphere

Daily PM_2.5, PM_2.5–10 and TSP have been collected by Universal and PS‐1 sampler simultaneously at a site within Taichung between February and March 1999. The filters were analyzed by atomic absorption spectrophotometry for the elemental analysis of Ca, Fe, Mn, Pb, Cu, Zn and Cr. In general, the concentration of these metallic elements are higher in fine particles than in coarse particles. On average, PM₁₀ accounted for 67% of the TSP at daytime, while at nighttime PM₁₀ accounted for only 44% of the TSP. For PM_2.5, PM₂._5–10 and TSP concentrations, there were no significant differences between day and night period. The averaged concentrations of metallic elements in PM_2.5 at daytime were all higher than that at nighttime. Ca, Fe and Zn have large and variable PM_2.5 concentrations at both daytime and nighttime. For the daytime Zn and Pb account for the largest portion of the heavy metal elements. For the nighttime, Zn and Cr make the largest portion of the heavy metal elements. The concentrations of Mn were higher on fine particulates. The trace metals Cu and Cr in Taichung are probably due to particulates emitted by Taichung Fire Power Plants transported into the sampling area by the prevailing northwesterly wind.     

Spatial Variations of Heavy Metals in the East China Sea Continental Shelf Surface Sediments

Surface sediments collected from continental shelf of the East China Sea were analyzed for heavy metals (iron, manganese, copper, zinc, lead, cadmium), carbonate, organic carbon contents, and grain sizes. the range of concentrations observed were iron: 0.3-1.3 wt%, manganese: 2.3-14 μmole/g, copper: 7.1-184 μmole/g, zinc: 0.16-0.77μmiole/g, lead: 15-98 μmole/g, cadmium: 0.17-3.9 μmole/g, carbonate: 3.6-87 wt%, sand: 10-100%, silt: 0-70% and clay: 0-50%.

A zonal distribution pattern of the heavy metals was found in the East China Sea Continental shelf sediments. High concentrations of most heavy metals, organic carbon and fine-grained sediments were observed in the inner shelf zone, especially those near the discharge of the Yangtze River. Concentrations of these heavy metals decreased from the inner shelf to the shelf break region. High concentrations of metals were also found in sediments near Taiwan. Iron concentrations decreased north-east of the central shelf region. High concentrations of cadmium were found in the shelf break region where biogenic carbonate is predominant. This study showed that biogenic carbonate in the East China Sea shelf break region and the terrigenous sediments from the Yangtze River and island of Taiwan were the major sources of heavy metals. Heavy metal concentrations were strongly influenced by the content of the coarse-grained quartz sand present in the sediments.     

Sediment texture and nutrients of Arasalar estuary, Karaikkal, south-east coast of India

Sediment samples were collected for texture, composition and nutrient such as organic carbon, total nitrogen and total phosphorus for a period of two years from three stations in Arasalar estuary. The sediment temperature, pH and nutrients were higher during summer season and lower during monsoon season. At station 1, sediment texture was loamy sand during summer and premonsoon season. At station 2, clay type soil was recorded. Whereas, at station 3, clay was observed in summer and premonsoon and then it shifted to sandy loam type soil during monsoon. Sediment nutrients were lower than that of values of various ecosystem of India.     

Speciation of heavy metals in sediments from the Scheldt estuary,Belgium

A simple three-step sequential extraction procedure was applied to study the speciation of heavy metals in sediment from Scheldt estuary, and their relationship to sediment grain size and organic matter content. The sedimentary metal content was fractionated into carbonate and exchangeable, metals bound to organic matter and residual fractions. Sedimentary total metal content was also determined using an industrial microwave (ETHOS 900) HF/HNO₃ extraction method. The extracts were analysed for metals using inductively coupled plasma atomic emission spectrometry. The bioavailable fraction (exchangeable and metals bound to organic matter) comprised less than the other forms. Residue metals were the dominant form of metals in almost all studied sites. The average total metal content for the studied sites decreased in the order Fe>Cr>Cu>Co>Zn>Pb>Cd. Based on average values for the studied sites, the highest bioavailable metals in sediments were Cd (38%) from Westkapelle, Zn (17%) from Yerseke, Co (12%) from Domburg, Cr (9%) from Vlissingen, Fe and Pb each (2%) from Yerseke, and Cu (1%) from Domburg. Metal recovery was good, with<10% difference between the total metal recovered through the extractant steps and the total metal determined using HF/HNO₃ extract.     

Trophic structure of polychaetes in the São Sebastião Channel (southeastern Brazil)

Between November 1993 and August 1994, the spatial and seasonal trophic structures of polychaete annelids were studied in the São Sebastião Channel, southeastern Brazil, located between the mainland of São Paulo State and São Sebastião Island. Four sampling surveys were carried out with a van Veen grab of 0.1?m² at 15 stations. A total of 12?003 individuals (126 species) was recorded and separated into 14 feeding guilds. Data were analysed with univariate and multivariate techniques (cluster and canonical correspondence analysis). Results showed a strong correlation between trophic groups and sediment variables such as grain size and organic carbon content. The Channel was dominated by surface deposit-feeders, followed by carnivores. Suspension-feeders were confined to medium and coarse sandy sites, environments with high energy. Bottoms where silt, clay and organic carbon predominated showed low polychaete densities. In these places the pollution induced by the sewage discharge from Araçá underwater emissions and by the oil terminal Dutos e Terminais Centro Sul was evident. There were no significant seasonal variations in the trophic structure over the study period, except in fall when densities were low. The polychaetes' relationships within the benthic system are discussed.