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111.
长江口及邻近海域富营养化趋势分析及与环境因子关系   总被引:1,自引:0,他引:1  
依据2007-2009年春、夏季在长江口及邻近海域(包括长江口、杭州湾和舟山渔场)的调查监测资料,采用富营养指数法、潜在性富营养化法和有机污染指数法对该海域的富营养化状况、时空分布特征及与环境因子的关系进行了分析评价。富营养指数法计算结果表明:富营养化覆盖比例很高,达到70%以上;在春季,该海域的富营养化程度呈现上升趋势,所占比例从2007年的77.0%上升到2009年的89.8%,在夏季最低达到89.3%,最高到100.0%。3年来,富营养化在春、夏2季基本上处于逐年增加趋势,富营养化趋势越来越明显。在春季富营养指数平面分布呈由近岸向远海逐渐递减的趋势,梯度分布明显,其中,杭州湾富营养化情况较严重;夏季其平面分布与春季类似,但长江口和杭州湾两个水域的富营养指数的等值线都比较密集,夏季的富营养化情况较为严重。潜在性富营养化法计算结果表明:该海域富营养级主要集中在III级(富营养)和V P级(磷中等限制潜在性富营养);春、夏2季时,长江口V P级所占比例均从0.0%增加到66.7%,受磷限制性富营养化程度越来越高。另外,营养盐结构显示,N/P比值从9.1到50.9,营养盐比例明显不平衡,势必影响浮游生物的生长。有机污染指数法计算结果表明:该海域有机污染指数主要处于5级(重污染),水质污染严重;长江口春、夏2季5级的比例均从50.0%分别上升到83.3%和100.0%,杭州湾分别从60.0%和80.0%均上升到100.0%;舟山渔场分别从22.2%和66.7上升到66.7%和77.7%,说明受污染程度逐年上升。另外,3年来春、夏2季长江口有机污染指数达5级的占50%以上,杭州湾60%以上,舟山渔场20%以上,杭州湾受污染情况最为严重,其次是长江口,舟山渔场最小。在春、夏2季有机污染平面分布表现为污染程度从西向东、从北向南逐渐降低?  相似文献   
112.
渤海海峡跨海通道建设环境影响研究   总被引:3,自引:0,他引:3  
渤海海峡跨海通道建设是一项高技术、高投入的特大战略性工程,工程建设具有重大的经济、军事和政治意义,但是也必将对环境产生重大影响。本文在对各界专家一致推荐的“伏贴式隧道和隧道桥”方案进行简要分析的基础上.论述了对工程建设进行环境影响研究的必要性,提出了环境影响评价工作程序与工程决策生命周期的耦合过程,以便从工程源头控制环境影响的产生;初步探讨了工程施工期和运营期的环境影响识别内容,结果表明:采用“伏贴式隧道和隧道桥”方案,相对于其它方案对资源、生态环境的干扰和影响是最小的;并提出了预防和减缓不良环境影响的对策措施,为工程的环保施工与运营提供科学依据。  相似文献   
113.
从2009年7月~2010年3月每月采集西太湖表层水样,分析叶绿素含量﹑蓝藻细胞裂解速率﹑磷酸盐浓度的变化,并通过切向流超滤系统分离得到的高分子量(1kDa~0.5μm)溶解性有机物的碳氮比值和高分子量溶解性有机碳浓度的变化.结果表明,西太湖蓝藻细胞裂解速率在11月达到最大值(0.43d-1),而磷酸盐和高分子量溶解性有机碳浓度分别在12月与9月达到最大值.细胞裂解速率与磷酸盐﹑高分子量溶解性有机碳浓度之间没有相关性,说明水华过后影响磷酸盐浓度﹑高分子量溶解性有机碳的因素很多,蓝藻细胞裂解只是其中重要因素之一.藻类水华的出现可能导致水体中其它磷形态(如有机磷)与磷酸盐之间的迁移转化,而大型浅水湖泊扰动导致的沉积物再悬浮和水华过后频繁的细菌活动都可能是影响高分子量溶解性有机碳的因素.秋季水华过后蓝藻细胞裂解释放的有机碳进入微食物网循环,引起细菌活动频繁,而溶解性有机物中含碳化合物比含氮化合物容易降解,所以碳氮比值逐渐减少.此外细菌通过硝酸盐合成溶解性有机氮也可能是碳氮比值减少的一个重要原因.  相似文献   
114.
通过对南黄海中部49个表层沉积物样品进行总有机碳,粒度,多环芳烃和甲基菲等GS-MS定量分析,探讨了研究区沉积物中多环芳烃分布特征,分子组成,评估南黄海中部多环芳烃污染水平并识别其来源.研究表明,南黄海中部14种多环芳烃总量(ΣPAHs)在81.63~6567.31 ng/g之间,其中优控多环芳烃(ΣEPA PAHs)11种,含量为29.2~1029.1 ng/g,平均含量255.1 ng/g,与国内外其他地区相比有机污染水平为中-低;苝为研究区内主要多环芳烃,分布较为广泛,其含量占所有PAHs的6.40%~88.85%,低含量苝与人为活动有关,而高含量苝代表了陆源有机质输入;多环芳烃组成,异构体分析和甲基菲特征表明,研究区优控多环芳烃主要为煤和高等植物燃烧或不完全燃烧产物以气溶胶形式输入,但部分样品表现出明显的石油源特性也证实了石油燃料,原油泄露产生的多环芳烃客观存在.  相似文献   
115.
基于2011年7月(夏季)和2011年10月(秋季)北黄海海域2个航次的调查资料,对北黄海夏、秋季营养盐的时空分布特征及其影响机制进行了探讨.结果表明,夏、秋季北黄海营养盐的平均浓度分别为:NO3- (1.57±1.71), (5.93±3.84) μmol/L,NO2- (0.22±0.18), (0.88±0.93) μmol/L,PO43- (0.22±0.13), (0.40±0.23) μmol/L,Si(OH)4 (4.98±2.23), (6.71±3.24) μmol/L,NH4+ (1.35±0.90), (1.23±0.69) μmol/L,夏、秋季北黄海NO3-分别占溶解无机氮的49%和74%.2个季节近岸海域表层营养盐浓度均高于中部海域,底层浓度高于表层,高值区是冷水团区.各断面营养盐的垂直分布层化现象明显,受冷水团以及水体交换混合的共同影响,浓度由表至底逐渐升高.夏、秋季表底层N/P、Si/N和Si/P比值的水平分布为近岸海域高于中部海域,且夏季北黄海浮游植物的生长繁殖受磷限制.  相似文献   
116.
To examine the suitability of benthic foraminifera and their test deformations as bioindicators of pollution in coastal marine environments, we studied foraminifera and metal concentrations in 72 marine sediment samples, collected from the inner shelf along the Sicilian coast (Gulfs of Palermo and Termini) and on the south-eastern coast of Lampedusa Island. These areas are characterised by different environmental conditions. On the basis of pollution sources and foraminiferal assemblages, we recognised different zones in the Gulf of Palermo. The most polluted zones showed high metal concentrations, and low diversity of benthic foraminifera with species typical of stressed environments. By contrast, the lowest polluted zones showed a high population density and the highest percentages of epiphytes. Epiphytes were abundant where a Posidonia oceanica meadow was present and decreased in the most polluted zones. Sediments of the Gulf of Termini and Lampedusa exhibited high percentages of benthic foraminifera typical of well-oxygenated waters and low concentrations of metals, with the exception of sites located near sewage outfalls and harbour areas. Furthermore, even though deformed tests are commonly known in natural stressed environmental conditions, this study shows that in the most polluted zones, benthic foraminifera were characterised by the highest percentages of deformed individuals.  相似文献   
117.
Seven sediment samples from mangrove sediments of the Red Sea were taken in order to evaluate the possible contamination of the sediments by trace metals (iron (Fe), manganese (Mn), zinc (Zn), copper (Cu), lead (Pb) and cadmium (Cd)). Sequential extraction techniques were performed to study the different geochemical forms of these metals. X-ray diffraction analysis has been performed to correlate the mineralogical composition with the geochemical forms of the studied elements. The results of Fe and Mn contents indicate that they are in large part from lithogenous origin. The elevated concentrations are associated with the residual form ranged from 70 to 93% for Fe and 46 to 70% for Mn. The percentage of Zn, Cu, Cd and Pb in the non-residual form was much greater than that of the residual fractions. This reflects the high mobility and bioavailability of these metals in mangrove sediments of the Red Sea. X-ray diffraction analysis revealed the presence of silicate components including quartz, feldspars and clay minerals in some locality. Non-silicate components recorded in the study area as calcite as well as, Mg-calcite. Quantitatively both components i.e. silicate and carbonate varied according to their source material.  相似文献   
118.
Study of the ecology of mesopelagic fishes is central for assessing the active biological pump in the ocean, especially in the mesopelagic layers. The use of δ13C and fatty acid analysis can help to analysis the ecology of mesopelagic fishes. Here, we analysed the fatty acid composition of mesopelagic fishes from the continental northern slope of the South China Sea (NSSCS) and compared with nearshore SCS fishes and mesopelagic fishes collected from the Southern Ocean. The mesopelagic fishes had unusually high lipids, which resulted in Δδ13C values exceeding 1‰, more than the enrichment factor in the food web. The mesopelagic fishes had higher C18:1n-9/C18:1n-7 and C20:1n-9/ C18:1n-7 ratios compared with other fishes in the SCS, which confirmed that plankton were their main dietary source. The mesopelagic fishes from SCS and Southern Ocean had different ratios of C20:5n-3/C22:6n-3 (EPA/DHA), suggesting geographical locations and diet sources had obvious influence on their fatty acid composition. The SCS mesopelagic fishes had higher C20:4n-6/C22:6n-3 (ARA/DHA) and C20:4n-6/C20:5n-3 (ARA/EPA) ratios than mesopelagic fishes in the Southern Ocean, indicating the influence of physical factors on fatty acid composition. Thus, future studies of the fatty acids in mesopelagic fishes should consider both dietary sources and physical environments.  相似文献   
119.
In order to provide a background picture of the water quality of the Egyptian Red Sea a number of hydrological and chemical parameters have been measured bimonthly in 2000. Few data are available on this area, which is apparently subjected to an increasing human impact due to recreational (swimming and diving), industrial (mainly phosphate shipping and industry) and fishing/harbor activities. The results of the present study indicate that changes in the salinity and pH were not significant with highly oxygenated seawaters. The levels of suspended solids (as total suspended matter, TSM) and chlorophyll-a (Chl-a) were generally low and showed an homogeneous distribution in the study region. The ratio of chlorophyll-a to total suspended matter concentrations increased between November and March and decreased from May to September. Chlorophyll-a was significantly correlated with transparency and total suspended matter concentrations in July, September and November. Nitrogen, phosphorus and reactive silicate concentrations were generally low, and allowed classifying the Egyptian Red Sea coastal water as oligotrophic to mesotrophic. The middle region of the study area, which was located between Safaga and Qusair displayed relatively high phosphate contents when compared with other coastal areas. The high values of N:P ratios indicate that PO 4 -P is the limiting factor for phytoplankton growth in the Red Sea coastal waters, with the possible exception of the middle region. Significant relationships were found between chlorophyll-a concentrations and nutrient levels in different sampling periods. Spatial distribution patterns of the studied variables revealed that productivity of the Red Sea coastal waters is mostly controlled by phosphate concentrations, salinity, temperature and dissolved oxygen.  相似文献   
120.
The main results of research work carried out since 1998 with regard to the application of hydro-acoustic technologies for the evaluation of biomass and distribution of small pelagic fish species off the southern coast of Sicily are presented, taking into account information from hydrology and from ecology of the fish populations targeted. The biomass estimates and the population‐density charts presented concern the two main species, i.e. sardine Sardina pilchardus (Walbaum, 1792) and anchovy Engraulis encrasicolus (Linnaeus, 1758). Both the sardine and anchovy populations experienced large inter-annual fluctuations, with biomass estimates ranging from 6000 to over 36,000 tonnes (t) (sardine) and from about 7000 to 23,000 t (anchovy). Acoustic estimates are largely consistent with landings recorded in Sciacca (the main fishing port for small pelagic species in the study area) during the year following the evaluation surveys. In addition, trends in sardine and anchovy biomass estimates appears to be negatively correlated with the mean sea surface temperature calculated over the time intervals January–September (sardine) and June–November (anchovy) of the preceding year, which correspond to larval and juvenile growth periods of target species. Observed patterns would suggest the importance of enrichment processes relevant to the survival of early stages, so determining recruitment success and finally higher population sizes.  相似文献   
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