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1.
The contribution of urban runoff to organic contaminant levels in harbour sediments near two Norwegian cities 总被引：1，自引：0，他引：1
Cornelissen G Pettersen A Nesse E Eek E Helland A Breedveld GD 《Marine pollution bulletin》2008,56(3):565-573
The main aim of the present study was to compare the quality of particle emissions (urban runoff and settling particles in rivers and harbours) to the quality of top-layer bed sediments, for two Norwegian harbours (Oslo and Drammen). A sub-aim was to investigate whether non-industrial urban runoff contributed to the organotin load of sediments, apart from leaching from ship hulls. Time-integrated samples of stormwater runoff were obtained in an innovative manner, by sampling man-holes in the stormwater system. Settling particles were sampled with sediment traps. The study focused on PAHs, PCBs and organotin compounds. Contaminant levels were generally a factor of 2-10 (PAHs) and 3-30 (TBT) lower in emitted riverine and runoff particles than in top-layer bed sediments, except for PCBs in Oslo harbour (only 20-30% lower). Significant levels of tributyltin (TBT; median 140mug/kg) were shown in runoff particles, showing that TBT can also be emitted via urban sources, since the sampled man-holes were not in areas where dry-docking activities take place. Possible land-based TBT sources include long-lasting house paint and use of TBT as PVC stabilizer and timber preservative. Since there are ongoing emissions into the two studied harbour areas, it is concluded that the addition of an actively sorbing capping material such as activated carbon might be the best remediation alternative. 相似文献
2.
底泥覆盖对浅水湖泊藻源性湖泛的控制模拟 总被引：1，自引：1，他引：0
湖泛的发生与湖泊底部氧化还原条件和致黑致臭物充足供给直接相关.利用黄土和细沙对太湖湖泛易发区(月亮湾)底泥进行覆盖,模拟在湖泛可形成条件下,底泥-水体系及其界面主要物化性质与感官变化过程.结果表明:0.5 cm黄土和1.0 cm细沙的覆盖,从水色和嗅味半定量角度达到了对湖泛黑臭的控制,与对照组相比,覆盖组底泥间隙水中主要致黑物Fe2+浓度仅为对照组的1/3,主要致臭物甲硫醇和二甲基三硫醚等浓度则不到50%.进一步分析底部水体和底泥性质发现:经覆盖处理底部水体的溶解氧浓度提高近1倍,氧化还原电位基本处于250 m V以上水平,覆盖层1 cm左右表层氧化还原电位和p H均远高于对照底泥.以黄土为主的底泥覆盖,主要因阻隔了下层底泥中物质迁移供给和对厌氧微生物参与的控制,以及黄土本身性质对湖底物化环境的影响等,在藻体大量聚集和死亡的水柱环境中,较好地阻止了致黑致臭物的形成,从而较有效控制湖泛的发生. 相似文献
3.
The effects of tributyltin (TBT) on the seagrass Ruppia maritima were studied in two growth experiments. Plants were sampled at stations in Odense Fjord and Lunkebugten, Denmark, and replanted in reference sediment without TBT, reference sediment spiked with TBT, and in impacted sediment sampled in the highly TBT contaminated (7-57 microg kg (-1) dw) Odense Fjord. Plant performance was studied at weekly intervals for 3-4 weeks, by measuring net photosynthetic activity, respiration, relative growth rate (RGR) and number of leaves. Net photosynthetic activity in plants from spiked and impacted sediment was reduced by up to 60% relative to reference plants. Respiration both increased and decreased in response to TBT exposure, while RGR was generally lower in plants from contaminated sediments (reduced by 8-25%). The effects of spiked and impacted sediment differed between the experiments, which could be partly explained by the bioavailability of TBT in the two treatments, but also by adaptation of the plants from Odense Fjord to TBT. Measurements of enhanced TBT concentrations in the sediments in Odense Fjord suggest an impact of TBT on R. maritima is possible under in situ conditions. 相似文献
4.
Peeter Nõges Lea Tuvikene Tiina Nõges Anu Kisand 《Aquatic Sciences - Research Across Boundaries》1999,61(2):168-182
5.
以自主研发的煅烧改性净水厂污泥（C-WTPS）作为污染底泥活性覆盖材料,室内静态模拟实验研究C-WTPS覆盖强度对控制底泥磷释放效果的影响,分析C-WTPS和底泥中不同形态磷含量变化,探讨C-WTPS薄层覆盖对上覆水体中pH、DO和ORP的影响.结果表明,实验历时40天,在底泥TP释放强度为6.25~10.87 mg/（m2·d）时,覆盖强度为0.25、0.50、1.00、1.50和2.00 kg/m2的C-WTPS对TP平均削减率分别为59.68%、75.71%、88.75%、92.42%和96.28%,可见覆盖强度为1.00 kg/m2以上的C-WTPS能控制底泥中90%以上TP释放.C-WTPS吸附的磷主要以无机磷（IP）中的铁铝结合态磷（NAIP）形式存在,有机磷（OP）和钙磷（AP）形式较少.C-WTPS促进了底泥中易释放形态磷迁移到C-WTPS中,并转化较为稳定的形态磷,可见C-WTP覆盖不仅控制了底泥磷释放,而且也削减了底泥磷释放风险.C-WTPS覆盖后,上覆水体中pH开始呈现下降趋势,最终维持在pH=7范围波动;C-WTPS覆盖强度越大,上覆水体pH下降也明显;C-WTPS覆盖改善上覆水体中DO和ORP环境的效果不明显. 相似文献
6.
Solute transfer across the sediment surface of a eutrophic lake: I. Porewater profiles from dialysis samplers 总被引：6，自引：0，他引：6
Noel R. Urban Christian Dinkel Bernhard Wehrli 《Aquatic Sciences - Research Across Boundaries》1997,59(1):1-25
Porewater profiles often are used to identify and quantify important biogeochemical processes occurring in lake sediments.
In this study, multiple porewater profiles were obtained from two eutrophic Swiss lakes using porewater equilibrators (peepers)
in order to examine spatial and seasonal trends in biogeochemical processes. Variability in profile shapes and concentrations
was small on spatial scales of a few meters, but the uncertainty in calculated diffusive fluxes across the sediment surface
was, on average, 35%. Focusing of Fe and Mn oxides toward the lake center resulted in systematic increases in porewater concentrations
and diffusive fluxes of Fe2+ and Mn2+ with increasing water depth; these fluxes are postulated to be regulated by the pH-dependent dissolution of reduced-metal
phases. Despite higher concentrations of inorganic carbon, NH
4
+
, Si and P in pelagic compared to littoral sites, diffusive fluxes of these substances across the sediment surface increased
only slightly or not at all with increasing water depth. Porewater profiles did reveal temporal changes in Fe2+, Mn2+, Ca2+ and Mg2+ that were an indirect result of the large, seasonal changes in seston deposition, but no clear seasonal variations were found
in diffusive fluxes of nutrients across the sediment surface. The intense mineralization occurring at the sediment surface
was not reflected in the porewater profiles nor in the calculated diffusive fluxes. Calculated diffusive fluxes across the
sediment surface resulted from decomposition occurring primarily in the top 5–7 cm of sediment. Diffusive fluxes from this
subsurface mineralization were equal to the solute release from mineralization occurring at the sediment-water interface.
Buried organic matter acts as a memory of previous lake conditons; it will require at least a decade before reductions in
nutrient inputs to lakes fully reduce the diffusive fluxes into the lake from the buried reservoir of organic matter. 相似文献
7.
以我国南方丘陵区红壤小流域为研究对象,对不同土地利用方式坡面下的4个水塘底泥中养分含量作了分层比较研究(0-5 cm,5-10 cm,10-15 cm,15-20 cm,20-25 cm,25-30 cm)．结果表明:4个水塘底泥养分含量差异明显,在0-15 cm泥层有机碳、全氮、速效氮和全磷含量以邻近村庄的水塘(简称C塘)底泥最高,其次为板栗园坡下的水塘(简称B塘),水稻田坡面下水塘(简称S塘)和花生地坡面下水塘(简称H塘)最低;在15-30 cm泥层,有机碳和速效氮含量以B塘最高,而全氮和全磷含量则以C塘最高;有效磷含量除C塘0-15 cm底泥外,其余均为痕量．表明土地利用方式对其坡面下水塘底泥养分含量影响明显．各水塘底泥养分随泥层加深均呈递减趋势,其中全氮和速效氮减幅以C塘最大,分别为36．0％和38．7％,有机碳和全磷减幅则以B塘最大,为29．4％和31．9％;各塘底泥养分含量的最大降幅主要在浅层底泥,水塘养分积累加速表明近年来农村面源污染加剧．传统农业耕作方式的改变是农村水体底泥养分含量增加的主要原因之一． 相似文献
8.
太湖底泥悬浮中营养盐释放的波浪水槽试验 总被引：46，自引：9，他引：37
波浪水槽中研究了小波掀沙(波高8.77cm,波周期0.8s)和大波掀沙(波高12.31cm和13.29cm,波周期1.0s)对太湖沉积物悬浮及N、P营养盐释放的作用规律.结果显示:小波掀沙时,底泥并未发生大量悬浮,SS浓度最高时仅13.6mg/L;大波掀沙时,底泥大规模悬浮,SS浓度最高达达245.2mg/L水体悬浮物、营养盐浓度变化滞后波高变化1h以上.当波高改变1h后,水体悬浮物、N、P营养盐浓度才改变到相应的平衡浓度.除总磷浓度显著提高外,小波掀沙对水体N、P浓度的影响很小,大波掀沙则显著提高了水体总氮、总溶解氮、总磷、总溶解磷、氨氮(NH4 -N)、溶解性活性磷(SRP),其中NH4 -N、SRP最大增幅达30％和20％.小波和大波掀沙过程中,水体溶解氧浓度均持续增加,掀沙2h后增高2mg/L,溶解性有机碳持续下降,2h后下降33％-51％.试验结果表明,掀沙过程中水体充氧及颗粒物的絮凝、吸附作用可能是限制NH4 -N、SRP浓度增高的重要因素之一. 相似文献
9.
以江苏扬州古运河富营养化水体为对象,现场围隔实验研究生物沸石薄层覆盖削减富营养化水体磷负荷可行性,考察生物沸石覆盖削减上覆水、底泥间隙水和底泥中不同形态磷的削减效果,讨论生物沸石覆盖修复过程中不同形态磷转化机制.结果表明,覆盖强度为2 kg/m2的生物沸石覆盖(厚度约2 mm)对上覆水中总磷的削减率为57.41%,对上覆水中正磷酸盐的削减率为60.03%;对底泥间隙水中正磷酸盐的削减率为59.80%;对表层底泥(0~20 cm)中总磷削减率为11.28%,对无机磷削减率为11.82%,对有机磷削减率为11.11%.生物沸石覆盖能将底泥中不稳定的无机磷(可溶性磷、铁结合态磷、铝结合态磷)或少部分较稳定的无机磷(钙结合态磷)转化为稳定的无机磷(包裹磷),说明生物沸石覆盖不仅能削减液相中磷负荷,而且能将固相中不稳定的无机磷转化为稳定的无机磷;可见,生物沸石薄层覆盖能有效削减富营养化水体磷负荷,利用生物沸石薄层覆盖削减富营养化水体磷负荷是可行的,但需要进一步研究富营养化水体底泥生物薄层覆盖修复过程中不同形态无机磷转化机制. 相似文献
10.
Transplanted common whelk (Buccinum undatum) (Mollusca, Gastropoda) accumulated fairly high levels of organotins (tributyltin (TBT) and triphenyltin (TPT)) during exposure in three harbours with different TBT contamination. This did not though lead to an increase in imposex frequency in the adult females studied. Simulating harbour dredging in an experiment using suspended sediment from one of the harbours only resulted in a low concentration of TBT in the tissues of the common whelk and subsequently no changes in the occurrence and degree of imposex. The common whelk seemed to receive the main part of TBT from the water column and the limited bioaccumulation in the experiment indicates that desorption of TBT from the suspended sediment was slow. After TBT has been totally banned, dredging of contaminated sediments will cause increased exposure of the biota to TBT. Due to slow desorption the increase may however, be slight and temporary to pelagic and epibenthic species unless the settled particles are resuspended. 相似文献
11.
12.
在浅水湖泊中,沉降在沉积物中的营养盐易受到水流的扰动再释放出来,而沉水植物可以在一定程度减少营养盐的释放.借助自主开发的生态水槽,在40 d的实验周期内检测动、静水条件下有、无苦草(Vallisneria natans L.)时沉积物、上覆水中磷含量变化,旨在为沉水植物对湖泊沉积物营养盐释放量的影响估算及水环境质量评价提供科学依据.结果表明:动水条件下,沉积物在没有苦草的保护下总磷含量下降21.8%,而有苦草的保护下总磷含量下降17.7%.苦草根系从周围沉积物中吸收磷,1~4 cm沉积物层的吸收量高于4~8 cm沉积物层.动水槽的上覆水中总溶解态磷浓度和总颗粒态磷浓度均大量增加,并且总颗粒态磷浓度相对于总溶解态磷浓度占较大比例.苦草减少了沉积物中磷的释放,并对上覆水中正磷酸盐有明显的吸收作用. 相似文献
13.
Survival of transplanted Zostera marina L. (eelgrass) and environmental conditions (water quality, bottom sediments, sedimentation on leaves and flow regime) were studied concurrently in the center, edge, and at the outside of a eelgrass meadow located in a eutrophic coastal zone in northern Hiroshima Bay, Seto Inland Sea, Japan. Eelgrass transplants at the outside of the meadow declined significantly, whereas those at the center were consistently well established. Silt content in the bottom sediments at the outside was higher than that at the center. The sediment was oxic from the surface to 2 cm deep at the center, whereas those at the edge and the outside were reductive almost from the surface. The sediment characteristics typical in eutrophic water seemed to be a factor responsible for the deterioration of eelgrass meadows. Although suspended solid concentrations in the water columns were almost the same, the amount of sediments deposited on leaves of eelgrass at the outside was higher than that at the center of the meadow. The amount of the deposition at the outside seems to be enough to inhibit photosynthesis; i.e. photosynthetic photon flux density (PPFD) available for eelgrass was only 36% of that without any deposition. The deposition in the center, however, was small enough to allow 84% of the original PPFD. Flow rates, determined at 30 cm above the bottom, a half height of average eelgrass, suggested that the rate at the outside was not enough to remove deposited sediments from the surface of eelgrass leaves. Thus, the large amount of sediment deposition caused by water pollution and/or eutrophication seemed to be another factor to inhibit the survival of eelgrass at the outside edge of the meadow. 相似文献
14.
Milankovitch forcing of bioturbation intensity in deep-marine thin-bedded siliciclastic turbidites 总被引：1，自引：0，他引：1
Thomas G. Heard Kevin T. Pickering Stuart A. Robinson 《Earth and Planetary Science Letters》2008,272(1-2):130-138
Trace fossils have been used to infer a Milankovitch-type control on pelagic and hemipelagic sediments, but there have been no comparable studies in deep-marine siliciclastic turbidite successions. Here, we present the results of a quantitative analysis of trace-fossil abundance and intensity in an essentially continuous, Middle Eocene, 230-m-long (Well A6) core, comprising very thin- and thin-bedded siliciclastic turbidites in the deep-marine Ainsa basin, Spanish Pyrenees. After removing the sediment slides and debris flow deposits, as these represent geologically instantaneous events approximately two orders of magnitude thicker than the typical laminated turbiditic sediments in the core, spectral analysis was conducted on the bioturbation intensity data. Spectral analysis of bioturbation intensity in the A6 core suggests, for the first time from a siliciclastic turbidite succession at a tectonically active plate margin (thrust-top basin in a foreland basin), a cyclicity that is interpreted to reflect the 41-kyr and an ~ 112-kyr (possibly an average of the 95- and 125-kyr) Milankovitch frequencies. We propose that this drove environmental changes in bottom-water conditions in the Ainsa basin, most likely leading to critically varying levels of oxygenation (stratification) of bottom waters. Our age model for the Ainsa basin (~ 4 km of deep-marine sediments in ~ 10 Myr) yields an average sediment accumulation rate of ~ 40 cm kyr− 1, that is consistent with that inferred from the spectral analysis (~ 30 cm kyr− 1) for fine-grained sedimentation. An implication of these results is that global environmental change, probably glacio-eustasy, acted as a driver on deep-marine siliciclastic sedimentation patterns during the Middle Eocene. 相似文献
15.
de Oliveira AJ Hollnagel HC Lima Mesquita Hde S Fontes RF 《Marine pollution bulletin》2007,54(7):921-927
Physical and chemical characteristics of intertidal sediments and their relationships with bacteria and cyanobacteria were analyzed at four stations at Pereque Beach. Granulometric analysis showed that Pereque beach has sediment that is classified as sand. The lowest value of the sediment C/N rates (6.08), mainly due to a higher concentration of organic nitrogen, was found at the northern part of Pereque Beach, where organic matter of marine source was more prominent. In this area, density (9.6x10(6)cells cm(-3)), biomass (1992.04ngC cm(-3)) and activity of bacteria were higher than at the southern end. In contrast, cyanobacteria density varied from 2.0 to 4.0x10(5)cells cm(-3), with biomass and total chlorophyll a of the sediment being higher at the southern part, where there are water input from Pereque River and higher organic matter of continental origin. The variability in the microbial population is discussed in the light of the sediment granulometry, organic matter quality, fresh water inflow and pollution. 相似文献
16.
Dahllöf I Agrenius S Blanck H Hall P Magnusson K Molander S 《Marine pollution bulletin》2001,42(8):689-695
The effect of tri-n-butyl tin (TBT) on an intact marine sediment community after five months exposure was investigated. Changes in the structure of macro- and meiofauna communities were determined, as well as the functional diversity of the microbial community using BIOLOG microplates for Gram negative bacteria. Development of tolerance in the microbial community was investigated using Pollution Induced Community Tolerance (PICT) experiments with fluxes of nutrients as effect indicators. TBT affected the structure and recruitment of the macro- and meiofauna at nominal additions of 30-137 micromol TBT/m2 sediment. Number of species, diversity, biomass and community similarity was reduced at these concentrations compared to control. Species that molt seemed to be the most tolerant since they were predominant in boxes that had received the highest TBT addition and echinoderms were the most sensitive species. Renewed addition of TBT in PICT experiments with sediment from each boxcosm showed that TBT had an effect on individual nutrient fluxes from all sediments. Analyses of the flux patterns revealed a memory of previous TBT exposure, either due to induced tolerance or other community conditioning. 相似文献
17.
The paper reports PHc contamination in water, sediment and biota of the coastal area of Bassein-Mumbai in relation to relatively less polluted sites (Dabhol and Ratnagiri) off the west coast of India. To facilitate inter-comparison three standards have been used though the results are reported in terms of SAM (Residue of Saudi Arabian Mix crude). The concentration of PHc in water off Bassein-Mumbai varies widely (2.9-39.2 microg l(-1)) as compared to the average baseline (2.8 microg l(-1)) with higher values generally confined to creeks and estuaries. The higher concentration of PHc in the bottom water of shallow areas is attributed to the contribution from the sediment-associated petroleum residue. High concentration of PHc in the surficial sediment of inshore area Ratnagiri (107.7 ppm, dry wt) is perhaps the remnants of an oil spill that occurred in the Bombay High region on May 17, 1993. The majority of values of PHc concentration in the surficial sediment of the Bassein-Mumbai region exceed 15 ppm (dry wt) against the expected background (<3 ppm, dry wt) and the trend is indicative of transfer of PHc loads from the inshore areas to the open-shore sediments. The PHc concentration of 0.8-2.6 ppm (dry wt) in sediment deposited prior to the first global commercial use of petroleum in core R5 represents the biogenic background. Based on the period of industrialisation and the horizon of PHc accumulation, a sedimentation rate of 0.2 and 1.0 cm y(-1) respectively is estimated for cores U11 and U12. Substantial increase in the concentration of PHc in sediment after 1950 in cores T8 and T10 correlates well with the establishment of refineries on the western shore of the Thane Creek in 1955-1960. A minor peak in most cores in the top 10 cm sediment probably results from biological transfer of PHc lower into the sediment by benthic organisms. Excess of PHc retained in the sediment of the Bassein-Mumbai region over the biogenic background is estimated at 40,000 t. The PHc residues (1.8-10.8 ppm, wet wt) in fish caught off Bassein-Mumbai do not suggest bioaccumulation. 相似文献
18.
SHAO Lei LI XueJie GENG JianHua PANG Xiong LEI YongChang QIAO PeiJun WANG LiaoLiang & WANG HongBin State Key Laboratory of Marine Geology Tongji University Shanghai China Guangzhou Marine Geological Survey Ministry of Land Resources Guangzhou China CNOOC Ltd. Shenzhen Shenzhen China 《中国科学D辑(英文版)》2007,50(7):1060-1066
There are some active bottom currents on the northern continental slope of the South China Sea (SCS). Reflection seismic profiles show that the bottom current channels occur in the water depth range of 1000 to 2700 m,extending from the NE to the SW,leading to accumulation of discontinuous drifts with higher sedimentation rates on the eastern side of the channel. The stacking pattern of the layers sug-gests that these drifts propagated southwestward,following the direction of the bottom currents. One sedimentary drift to the southeast of the Dongsha Islands has the highest sedimentation rate of 97cm/ka in the last 12 ka. The sedimentary characteristics of the sediment layers indicate that these bottom currents are most likley caused by the water movement of a branch of the West Pacific Ocean Current,which enters the northern SCS via the Bashi Strait. Once formed,the bottom currents trans-port sediments along the northern slope of SCS southwestward and finally disappear into the central basin of the SCS. Due to the bottom current activity,the deep-sea sedimentary process in the northern SCS is complex. 相似文献
19.
This paper examines dioxin profiles in bottom sediments from Tokyo Bay, Japan using sedimentation dating based on 210Pb measurements and dioxin measurements based on particle size distributions. Dioxin concentrations in surface sediment ranged from 3.2 to 52 pg-TEQ g(-1), with the concentrations in the bay back and central region being higher than those at the front of the bay. The vertical dioxin concentration in sediment core samples showed peak levels from years 1962 to 1980, with the maximum being 110 pg-TEQ g(-1). Principal component analysis indicates that the main source of dioxins in bottom sediment from the back of bay are herbicides such as CNP, while in the front of bay atmospheric deposition due to incineration activities are responsible. Dioxins in bottom sediment were mainly found in the particles <75 microm in size. 相似文献
20.
Over a three-year period, quantification of faecal indicators and the molecular detection of Escherichia coli and Salmonella were monitored in sediments from three contrasting mudflats of the Seine estuary (France). The elevation of the mudflat surface was monitored concurrently using a high-resolution altimeter. During the period of the study, estuarine mudflats were areas of deposition for faecal-indicator bacteria and were mainly controlled by sedimentary processes. In the intertidal freshwater and subtidal mudflats, the highest abundances of faecal-indicator bacteria were counted during a depositional period. Maximum levels were observed in the freshwater mudflats during periods of high flow: thermotolerant coliforms: 3.9 x 10(4) cfu cm(-2), enterococci: 1.2 x 10(4) cfu cm(-2), Clostridium perfringens spores: 9.8 x 10(5) spores cm(-2). Loss of culturability of enteric bacteria in sediment microcosms demonstrated the remediatory capacity of the mudflats, even if they might be a secondary source of bacteria-forming spores to the water column through erosion and resuspension events. 相似文献