太湖聚藻区水华易发季节沉积物磷的分布特征

为了探讨太湖聚藻区月亮湾在水华易发季节及前后沉积物磷的赋存及迁移特征,采用欧洲标准测试委员会框架下发展的SMT磷形态分级方法对月亮湾由冬季至夏季（1～7月）表层沉积物（5 cm）分层的磷形态分析发现,总磷和无机磷呈现逐渐下降的趋势,平均含量分别为53553和42590 mg/kg。但有机磷则在冬季至夏初降低,随后从夏初开始上升并于7月达最大值,平均含量为8772 mg/kg,是冬季的14～18倍,表明藻类聚集和沉降对表层沉积物有机磷含量产生显著影响。在监测的这几个月中,无机形态磷均于春季4月达到最大值,而且与1、6和7月表现出显著的差异性（P <005）。铁磷为无机磷主要形态,平均含量达到18686 mg/kg,占无机形态磷质量分数的4443%,且4月、5月和6月沉积物铁磷含量表现出显著的差异性（P <005）。其次是铝磷和钙磷,平均含量分别达到12949和9748 mg/kg,为无机形态磷质量分数的3118%和2318%,各月份沉积物铝磷含量表现出显著的差异性（P<005）,而钙磷却无显著性差异。沉积物中可交换态磷的含量虽然较少（平均444 mg/kg）,但其冬季至春季逐渐升高、春季至夏季逐渐降低的现象,表明在生长季节可交换态磷从沉积物向上覆水柱释放,为藻类复苏和生长提供物资基础。分析还发现,铁磷、铝磷和有机磷均与可交换态磷存在较好相关性,无机磷与总磷的相关性最为显著,表明研究区沉积物中总磷的含量与分布主要受控于无机磷     

Chlorpyrifos in surface waters before and after a federally mandated ban

Samples collected from rural and urban streams in the City of Denton, Texas, USA were analyzed for the organophosphorus pesticides diazinon and chlorpyrifos during the years preceding and following a United States Environmental Protection Agency ban on many chlorpyrifos uses. A network of 70 monitoring stations, based mainly on topography and hydrological considerations, were established within the three main watersheds of Denton. Monitoring stations were sampled monthly from March through August during periods of normal flow (baseflow), resulting in a total of 308 samples and 311 samples collected during 2001 and 2002, respectively. Pesticide concentrations were determined using commercially available enzyme-linked immunosorbent assays (ELISA) specific for each pesticide. Results from this temporally and spatially dense monitoring effort were used to illustrate the impacts of a ban on most chlorpyrifos sales that was imposed in December 2001. The total number of samples exhibiting concentrations above method lower limits of detection (LLD) decreased between 2001 and 2002 for both chlorpyrifos and diazinon. The total number of sites exhibiting at least one sample with concentrations above the LLD for chlorpyrifos, however, significantly decreased (Fisher's exact test, p<0.0001, n=70) when comparing 2001 (before the ban) with 2002 (after the ban). Similar analyses indicated no significant difference (Fisher's exact test, p=0.50, n=70) in the number of sites exhibiting detectable diazinon concentration between 2001 and 2002. Our results indicate that the cessation of retail chlorpyrifos sales at the end of 2001 resulted in a highly significant decrease in the surface water occurrences of this pesticide during 2002.     

The migration of reactor-produced tritium in Lake Huron

Two exceptional releases of tritium from the Bruce Nuclear Power Development into Lake Huron occurred during September 1983. Although not of health significance, these releases gave an opportunity to study the transport of tritium in lake water near the reactor site. Water samples were collected daily during September and October from drinking water stations at Port Elgin, 20 km northeast of the site, and at Kincardine, 18 km southwest. Tritium was detected only at Port Elgin because of the general counter-clockwise circulation of the lake. The travel times of the tritiated water from each of the releases to Port Elgin were between two and four days. These lengths of time are in agreement with those calculated from the velocity of the current and the distances. The diluted concentrations of tritium at Port Elgin were estimated by the classical diffusion equation. Fair agreement was found between calculated and measured values.     

Analysis of microcystins in cyanobacteria blooms and surface water samples from Meiliang Bay,Taihu Lake,China

Taihu Lake is the third largest freshwater lake in China. In recent years, the water pollution of cyanobacteria blooms has become a severe problem in this area. Microcystins (MCs) are an important group of toxic compounds mainly produced by some cyanobacteria species and have both acute and chronic hepatotoxic effects on animals and humans. This paper presents the first data on the identification and detection of MCs in both natural occurring cyanobacteria blooms and surface water samples (0-0.5 m), collected from Meiliang Bay, Taihu Lake, China. A conventional method for extraction and isolation of MCs from cyanobacteria blooms was applied. High-performance liquid chromatography (HPLC) analysis showed that the main toxic component in the cyanobacteria materials was MC-LR. The monoclonal antibody (mAb) against MC-LR produced by hybridoma technique was employed for direct competitive ELISA to detect the concentrations of MCs in bloom and water samples collected in 2001. The results not only revealed the presence of MCs but also temporal variations of MCs levels of three sampling stations in Meiliang Bay in 1 year. It is obvious that the MC contents were relatively higher during warm months and related with the status of eutrophication. Our study indicates the threat associated with MCs in water body of Taihu Lake. To prevent the MCs potential hazard on public health in this area, some necessary measures of monitoring and control of growth of cyanobacteria are urgently needed.     

东平湖表层沉积物中磷的形态分布特征研究

以东平湖表层沉积物为研究对象,应用连续提取法测定了其中的总磷(TP)、弱吸附态磷(NH4Cl P)、铝磷(Al P)、铁磷(Fe P)、钙磷(Ca P)、残渣磷(Res P)、有机磷(OP)等形态磷的含量,探讨了东平湖表层沉积物中磷的形态分布特征。研究结果表明：东平湖表层沉积物中总磷的平均含量为79538 mg/kg,与我国其他湖泊相比含量较高。表层沉积物中的磷主要以无机磷的形式存在,含量为3849~1158.3 mg/kg,约占沉积物中总磷的8076%。各形态无机磷的含量在〖JP+1〗沉积物中的含量大小顺序为：Ca P>Res P>Al P+Fe P>NH4Cl P,分别占无机磷的448%、312%、231%和09%。老湖码头和湖心岛附近沉积物中有机磷含量略高于其他区域,这与两处附近均有大片网箱养殖区和接纳较多生活污水有关。生物可利用磷在东平湖沉积物中的含量较高,平均为2458 mg/kg,占总磷的309%,沉积物中磷向上覆水释放的潜在风险较大。     

Apparent 85Kr ages of groundwater within the Royal watershed, Maine, USA

Specific 85Kr activity is mapped from 264 domestic and municipal wells sampled during 2002-2004 in the Royal watershed (361 km2), Maine. Gas samples are collected at 20 m, 40 m, and > 50 m interval depths within the unconfined aquifers. Gas extraction for 85Kr from wells is obtained directly via a wellhead methodology avoiding conventional collection of large sample volumes. Atmospheric 85Kr input to the recharge environment is estimated at 1.27 Bq m(-3) by time-series analyses of weighted monthly precipitation (2001-2004). Numerical simulation of Kr gas transport through the variable unsaturated zones to the water table suggests up to 12-year time lags locally, thus biasing the 85Kr groundwater ages. Apparent 85Kr ages suggest that approximately 70% of groundwater near 20 m depth was recharged less than 30 years BP (2004). Mass-age transport modeling suggests that post mid-1950s recharge penetrates to part of the basin's floor and that older groundwater seeps from the underlying fractured bedrock may occur.     

Radionuclide contamination of sediment deposits in the Ob and Yenisey estuaries and areas of the Kara Sea

The Ob and Yenisey rivers are major contributors to total riverine discharge to the Arctic Ocean. Several large nuclear facilities discharge into these rivers, which could affect actual and potential discharges of radionuclides to the Arctic region. This article presents new radionuclide concentration and grain-size data resulting from analyses of several sediment samples collected during research cruises in the Ob and Yenisey estuaries and adjacent areas during 2000 and 2001. Results indicate that discharges from the main nuclear facilities do not constitute a major contribution to the level of radioactive contamination in the marine areas studied, though Co-60 was detected at low concentrations in some sediment horizons. However, the aggregate contamination from different sources is not radioecologically significant in sediments within the study area, maximum Cs-137 levels being approximately 80 Bq kg(-1) dry weight.     

Impact of trace metals and nutrients levels on phytoplankton from the Kuwait coast

The impact of marine pollution was estimated from seven stations of Kuwait coastal waters. The mean concentrations of all trace metals in seawater (0.07-7.04 microg/l) and in phytoplankton (14.90-52.01 microg/g) revealed less phytoplankton abundance in Stations IV VI during the four seasons. However, a relative surge in the phytoplankton abundance, with an increase in the mean concentrations of all trace metals in seawater (0.15-8.94 microg/l) and phytoplankton (22.82-61.25 microg/g), was observed in Station II. A low phytoplankton abundance was noted in Stations I, III, and VII despite low mean concentrations of all the trace metals in seawater (0.11-5.77 microg/l) and phytoplankton (1.40-20 microg/g) during the four seasons. Statistical tests revealed significant difference in Fe, Ni, and Pb between the four seasons in seawater and Fe and Co in phytoplankton. No significant difference in trace metals between locations was observed in seawater and in phytoplankton. The major nutrients in all the four seasons were found in the magnitude of SiO3 > NO3 > PO4 in all the stations, and thus, support the presence of rich diatoms and dinoflagellates than other phytoplankton groups. The seven stations also represented indicator species of oil and industrial waste pollution.     

淮河干流大型底栖动物群落结构及水质生物学评价

2011年3月、6月、9月和12月对淮河干流大型底栖动物群落进行了取样调查,共采集到大型底栖动物4门41科94种。结果分析表明,淮河干流大型底栖动物群落结构具有一定的时空变化。在时间尺度上,生物密度呈极显著的季节性变化(p=0.002),其最大值332.5 ind./m2出现在6月,最小值96.6 ind./m2则出现在9月;生物量的变化趋势与生物密度不同步,其最大值155.8 g/m2出现在9月,最小值40.0 g/m2则出现在3月,且季节性差异不显著。冗余分析(RDA)结果表明,溶解氧、盐度、溶解性总固体、水温和底质类型是影响底栖动物群落结构的主要环境因子。Shannon-Wiener多样性指数的季节性变化不显著,Margalef丰富度指数的季节性差异极显著(p=0.000);自上游至下游,这2个指数的变化规律表现出高度的一致性,其水质评价结果表明淮河干流水质总体上处于中度污染的水平。     

Atmospheric bulk deposition to the Lagoon of Venice Part II. Source apportionment analysis near the industrial zone of Porto Marghera, Italy

Multivariate statistical analyses were applied to measurements of atmospheric deposition of total particulate (TSP), inorganic elements (Al, Ca, Na, K, Mg, Si, Mn, Fe, Zn, Ni, Cr, Cu, Pb, Cd, As, Hg, V and S) and organic compounds (PAH, PCB, HCB and PCDD/F) collected in four stations, all located in the Lagoon of Venice. Aerosols at the scale of the basin (i.e., within a distance of 20 km) were mainly characterised by two end-members, one natural (composed of mineral particulate and marine spray) and one anthropogenic (with at least two different source components), affecting the sites in various ways. Variability at the two distant (>20 km) sites (Valle Dogà, Valle Figheri) was mainly due to natural components, whereas the other two stations (city of Venice, Dogaletto, approximately 5 km) were mainly impacted by industrial (and urban) sources. Total annual inputs were compared with the limits recently set by law (maximum allowed discharge=MAD). In the year of study, MAD values were exceeded for total As, Cd, Hg, Pb, dissolved Zn, PAH and PCDD/F. These results indicate that industrial sources gave rise to a quasi-permanent compositional (background) effect near the industrial area. The risk associated with atmospheric deposition should be quantified within the DSPIR framework to avoid future negative consequences in populations living in the vicinity of Porto Marghera.     

Vertical profiles and enrichment pattern of natural radionuclides in monazite areas of coastal Kerala

Detailed studies on radionuclides concentration in different environmental matrices of high background areas were undertaken in the coastal areas of Karunagapalli, Chavara, Neendakara and Kollam to study the distribution and enrichment of the radionuclides in the region. The sand samples collected at different distances from sea waterline and at different depths, were analysed for primordial radionuclides by gamma spectrometry. The activity of primordial radionuclides was determined for the different size fractions of sand to study the enrichment pattern. The highest activity was found confined in 125-63 microm particle size fraction in sand. The minimum (232)Th activity was 9.4 Bq kg(-1), found in Kollam at a depth of 10-20 cm, 40 m away from waterline in 500-250 microm particle size fraction and maximum activity of 136,811.2 Bq kg(-1) was observed in Chavara in grains of size 125-63 microm at a depth of 0-10 cm for a sample collected 20 m away from waterline. The lowest (226)Ra activity observed was 29.6 Bq kg(-1) at Kollam beach for a sample 40 m away from waterline in grains of size 1000-500 microm and at a depth of 20-30 cm and the highest activity observed was 10,309 Bq kg(-1) in grains of size 125-63 microm for a sample collected at a distance 20 m away from waterline and at a depth of 0-10 cm. The activity of (40)K was below detectable level in most of the samples collected from the high background monazite area. The (232)Th, (226)Ra activities decrease with depth for the samples collected 20 m away from the waterline and increase with depth for the samples collected 40 m away from the waterline at Chavara and Kollam beaches. No definite correlation was found between variation of the concentrations of (232)Th and (226)Ra with depth at Karunagapalli and Neendakara beach sands. There exists a strong correlation between (226)Ra and (232)Th activities in the region. The results of these investigations are presented and discussed in this paper.     

Seasonal variation of Ra/Ra ratio in seaweed: implications for water circulation patterns in coastal areas of the Noto Peninsula, Japan

To examine water circulation patterns of coastal water, 72 seaweed (Sargasso) samples and 27 coastal water samples were collected from coastal areas of the Noto Peninsula, Japan, during the period from December 1998 to June 2002. The (228)Ra and (226)Ra activities of those samples were measured by low-background gamma-ray spectrometry. There was a wide range of activities of (228)Ra (0.5-2Bq/kg-fresh) and (226)Ra (0.5-1.2Bq/kg-fresh) in the Sargasso samples. The (228)Ra/(226)Ra activity ratio of Sargasso samples exhibited seasonal variation with minimum values in June ((228)Ra/(226)Ra= approximately 1) and maximum values in December (1.5-2.5), which was mainly governed by changes in (228)Ra activity. It is also notable that the seasonal variation of the (228)Ra/(226)Ra ratio of Sargasso is in approximate agreement with that of the ambient coastal water. Sargasso samples appear to have retained the (228)Ra/(226)Ra ratio of the ambient coastal waters, and the temporal variations in that ratio provide insight into seasonal changes in water circulation in the Noto Peninsula coastal area.     

Biotesting of water from Peter the Great Bay,Sea of Japan,using the microalga <Emphasis Type="Italic">Dunaliella salina</Emphasis>

Water samples from zones with different levels of anthropogenic pollution in Peter the Great Bay, the Sea of Japan, were subjected to biotesting on the microalga Dunaliella salina. A distinct inhibitory effect on microalgal cultures was revealed in tests of water from Amur Bay. Water samples from stations in the Tumannaya River mouth and off Frugelm Island (in the southwestern part of Peter the Great Bay) and from Gaidamak Bight (Vostok Bay) had little effect on D. salina growth.     

Seasonal variation of 228Ra/226Ra ratio in seaweed: implications for water circulation patterns in coastal areas of the Noto Peninsula, Japan

To examine water circulation patterns of coastal water, 72 seaweed (Sargasso) samples and 27 coastal water samples were collected from coastal areas of the Noto Peninsula, Japan, during the period from December 1998 to June 2002. The (228)Ra and (226)Ra activities of those samples were measured by low-background gamma-ray spectrometry. There was a wide range of activities of (228)Ra (0.5-2Bq/kg-fresh) and (226)Ra (0.5-1.2Bq/kg-fresh) in the Sargasso samples. The (228)Ra/(226)Ra activity ratio of Sargasso samples exhibited seasonal variation with minimum values in June ((228)Ra/(226)Ra= approximately 1) and maximum values in December (1.5-2.5), which was mainly governed by changes in (228)Ra activity. It is also notable that the seasonal variation of the (228)Ra/(226)Ra ratio of Sargasso is in approximate agreement with that of the ambient coastal water. Sargasso samples appear to have retained the (228)Ra/(226)Ra ratio of the ambient coastal waters, and the temporal variations in that ratio provide insight into seasonal changes in water circulation in the Noto Peninsula coastal area.     

近49年中国夏季制冷度日数的变化

利用全国531个气象站1960~2008年逐日平均气温资料,分析了近49 a来我国夏季制冷度日数的变化趋势,并以浙江省为例分析了制冷度日数与夏季空调降温电力负荷的关系。主要结论如下：我国日平均温度等于或高于26℃的日数（1971~2000年平均）大于10 d,夏季有制冷需求的站点主要分布在新疆、四川盆地和太行山 巫山 雪峰山一线以东地区,以及云南干热河谷地区。1960~2008年我国黄河以北地区夏季有制冷需求的站点6~9月平均气温从20世纪90年代中期开始呈现出较明显的上升趋势,使得制冷日数和度日数都相应增加;黄河以南、南岭以北地区近49 a来6~9月平均气温线性趋势不明显,制冷度日数变化不大;南岭以南地区6~9月气温持续上升,夏季制冷度日数的增加最为显著。以浙江省为例的分析显示,制冷度日数与夏季空调降温电力负荷有很好的线性相关关系,可以用来预测降温耗电量。
     

Studies of Np and Pu in the marine environment of Swedish-Danish waters and the North Atlantic Ocean

The long-lived anthropogenic radionuclides (237)Np, (239)Pu and (240)Pu were determined in marine environmental samples (seaweed and seawater) collected from Swedish-Danish waters and the North Atlantic Ocean at various locations on different occasions during the period 1991-2001. The measurements were performed with sector field Inductively Coupled Plasma Mass Spectrometry (ICP-MS) and conventional alpha spectrometry. The (237)Np activity concentrations in Fucus vesiculosus and surface seawater from the Swedish west coast and Danish waters ranged from 0.16+/-0.02 to 1.02+/-0.09 mBq kg(-1) (dry weight) and 0.65+/-0.02 to 1.69+/-0.02 mBq m(-3), respectively, depending on the location and sampling year. Most of the (237)Np in these waters is believed to originate from the Sellafield nuclear reprocessing plant, with some contribution from global fallout. The (240)Pu/(239)Pu atomic ratios in F. vesiculosus samples are reported in this study with an overall average of 0.17+/-0.03. The (237)Np and (239)Pu activity concentrations observed in surface seawater collected in North Atlantic waters ranged from 0.16+/-0.01 to 0.62+/-0.08 mBq m(-3) and from 0.64+/-0.05 to 4.27+/-0.08 mBq m(-3), respectively, and the (237)Np/(239)Pu atomic ratios were a good indicator of conservative behaviour of Np in marine waters.     

Leachability of elements from sub-bituminous coal fly ash from India

Environmental concerns regarding the potential contamination of soil, surface and ground water due to the presence of soluble metal species in the ash pond leachate is of great importance. Serial batch leaching was carried out simulating the rainwater condition of the study area to understand the behaviour of elements during leaching. The leachates were analysed for the elements Al, Ca, K, Mg, Na, P, S, Si, As, Ba, Fe, Mn, Mo, Ti, V, Pb, Zn, Co, Cr, Cu, Ni and Cd by inductively coupled plasma optical emission spectrometer (ICP-OES). It was found that Cd, Co, Cr and Ni did not leach from the ash while Cu and Pb concentrations were insignificant in the leachate regardless of liquid to solid (L/S) ratio. Most of the elements showed maximum concentrations at lower L/S ratio and then decreased with increasing L/S. The total cumulative concentrations of As, Mn and Mo were found to be higher than the World Health Organization (WHO) recommended values for drinking water while the concentrations of Fe, Mn and As exceeded the maximum allowable concentrations prescribed by the United States Environmental Protection Agency (USEPA). The pre and the post leached ash samples were analysed for morphology, specific surface area and mineralogical changes. Analysis of post-leached fly ash indicated changes in the specific surface area and morphology but no change in mineralogy.     

Bacteriological study of Upper Lake of Bhopal, India

In order to assess the water quallty of the upper lake of Bhopal (India) after the leakage of methyl isocyanate (MIC) gas from the Union Carbide factory, Bhopal, bacteriological study of the lake water was carried out. Water samples were collected from eight different sampling stations from the eastern, western, northern and southern sides of the lake. The study has revealed that the coliform bacteria are increased (24000/mL) at the onset of summer and are dropped to a minimum (120/mL) during monsoon season against the permissible limit of 100/mL recommended by the World Health Organisation (WHO) for water to be used for drinking purposes. The data collected show that the water quality of the Upper lake is deteriorated and is gradually becoming unfit for drinking.     

Estimates of upwelling rates in the Arabian Sea and the equatorial Indian Ocean based on bomb radiocarbon

Radiocarbon measurements were made in the water column of the Arabian Sea and the equatorial Indian Ocean during 1994, 1995 and 1997 to assess the temporal variations in bomb 14C distribution and its inventory in the region with respect to GEOSECS measurements made during 1977-1978. Four GEOSECS stations were reoccupied (three in the Arabian Sea and one in the equatorial Indian Ocean) during this study, with all of them showing increased penetration of bomb 14C along with decrease in its surface water activity. The upwelling rates derived by model simulation of bomb 14C depth profile using the calculated exchange rates ranged from 3 to 9 m a(-1). The western region of the Arabian Sea experiencing high wind-induced upwelling has higher estimated upwelling rates. However, lower upwelling rates obtained for the stations occupied during this study could be due to reduced 14C gradient compared to that during GEOSECS.     

The extremely high 137Cs inventory in the Sulu Sea: a possible mechanism

Large-volume seawater samples were collected in the Sulu and South China Seas and their (137)Cs activities were determined by gamma-ray spectrometry using a low background type high-purity Ge detector. Vertical distributions of (137)Cs activity showed an exponential decrease in the South China Sea, whereas a subsurface maximum at 200m depth and monotonic decrease below 300m were observed in the Sulu Sea. A significant difference in intermediate water (137)Cs activities in the 500-2000m depth was observed between the Sulu and South China Seas, i.e., the (137)Cs activities in the Sulu Sea were remarkably higher than those in the South China Sea. The difference in the (137)Cs inventory below 500m was approximately 1200Bqm(-2) between the Sulu and South China Seas. The (137)Cs total inventory of 3200Bqm(-2) in the Sulu Sea was 5.7 times higher than that expected from global fallout. A possible mechanism controlling this extremely high (137)Cs total inventory may be inflows of the (137)Cs rich water masses through the Luzon Strait, lateral transport across the Mindoro Strait into the Sulu Sea, and then subduction into the deep layer in the basin.