2019年连云港近岸海域水质环境分析与综合评价

于2019年春、夏、秋季对连云港近岸海域海水中营养盐、重金属等共19项指标进行3个航次采样监测。依照海水水质评价标准统计分析站点达标率,采用有机污染物指数法和富营养化指数法,对调查海域海水有机污染、营养水平等进行综合评价。结果表明:2019年连云港市海域站位全年达标率为86.4%,达标面积为6543 km²,占管辖海域面积的98.0%,水质质量较往年有所好转,主要超标物为无机氮、活性磷酸盐。调查海域海水的有机污染和富营养化程度均处于良好状况,近岸海水水质总体上要劣于远岸水质,且随季节的更替呈现波动性变化。     

云龙湖水质调查与评价

对云龙湖水质进行了调查与评价.在云龙湖东湖、西湖区各设置3个采样点,监测水体中TN、TP、Imn、NH3-N、DO和SD指标;分别使用模糊识别法和湖泊综合营养指数对水体进行水质评价与富营养化评价,结果表明,云龙湖水质级别为III类,其中TN、TP超标明显,水体呈现中度富营养化;不同功能区水质差异明显,东湖区水质优于西湖...     

太湖流域2005年10月水质状况

2005年10月，太湖湖体平均水质为Ⅳ类，富营养化程度平均处于中富营养水平。与《太湖水污染防治“十五”计划》湖体水质目标相比，西部沿岸区和东部沿岸区有超标现象，其余湖区各项指标均达到水质目标要求。江苏省境内太湖流域出入湖河流21个控制断面（苏州苏东河越溪桥因河道整治无法采样）中，有14条河流水质符合2005年水质目标类别要求，达标率为70．0％；9条主要人湖河流中有6条河流水质达标，达标率为66．7％。45个环湖河流行政交界断面中，     

钦州湾近岸海域水质状况及富营养化分析

2012年5月钦州湾近岸海域水质监测结果表明,钦州湾近岸水温、盐度、pH、溶解氧等基本环境参数均有利于亚热带海洋生物的生长繁殖;溶解无机氮(DIN)和活性硅酸盐(SiO2-3-Si)均显示过剩,但溶解无机磷(DIP)具有低磷特征,高的氮磷比值使PO3-4-P可能成为浮游植物生长的潜在限制因子,且COD部分站位出现超标现象。污染指数(A)和单因子污染指数(Pi)结果显示,近期整个钦州湾近岸水域污染程度达到2级,属于开始受到污染,水质受到化学耗氧有机物不同程度的污染,超标率达到30%。富营养状态指数结果表明,钦州湾近岸海域总体尚未达到富营养化,但局部区域已出现富营养化状况。COD对富营养化的贡献率平均值及范围为72.46%(67.36%~83.96%),COD已成为影响钦州湾近岸海域富营养化的重要因素。     

古运河营养元素分布特征及富营养化趋势分析

根据2005～2009年各季度对镇江古运河水体多项指标的监测资料,分析了古运河水体中N、P营养元素的时空分布特征,选用营养状态质量指数法对水体营养状态进行了评价,并预测了古运河水体的富营养化趋势。结果表明,古运河水体中营养元素随年度呈先增后减的特征,而年内季度分布不明显,空间分布基本呈从上游向下游递增的规律;2005～2009年,古运河水体连年处于富营养水平,2007年最为严重,但自2007年以来,水体营养水平逐年下降,水体富营养化趋势有所减缓。     

云龙湖不同功能区水质监测与评价

以徐州市云龙湖东西两湖区为对象,研究其不同功能区水质状况,从而为云龙湖水体保护提供理论依据。在云龙湖东湖、西湖区各设置3个采样点,监测水体中总氮、总磷、高锰酸盐指数和溶解氧指标;采用熵权法确定各水质指标权重,继而对水质进行定量综合评价。评价结果表明:云龙湖水体水质为III类,其中TN、TP超标明显,水体已呈现富营养化;不同功能区水质差异明显,东湖区水质优于西湖区,云龙湖功能区划分对水质有显著性影响。     

陆源有机污染对舟山海域大型底栖生物分布的影响

2009年4月对舟山海域进行了25个站位的底栖生物调查,结合同期进行初级生产力、海水水质等的调查数据,分析了初级生产力、富营养化等环境因子对舟山海域大型底栖生物分布的影响。结果表明,舟山海域大型底栖生物共获得84种,多毛类是主要优势类群。舟山海域大型底栖生物平均生物量为11.62g/m²,平均丰度为208.5个/平方米,多样性指数(H')为1.64。舟山海域大型底栖生物的生物量、丰度和多样性指数均呈现由近岸向外海递增的趋势。应用相关性统计分析表明,舟山海域大型底栖生物的分布与海水化学耗氧量(COD)、无机氮(DIN)、磷酸盐(DIP)、富营养化指数和底层溶解氧(DO)存在显著负相关;与初级生产力、盐度和透明度存在显著正相关。说明陆源有机污染、盐度、透明度、初级生产力和底层溶解氧是影响舟山海域大型底栖生物分布的主要因素,其中陆源有机污染是最主要的影响因素。     

天津近岸海域水污染评价

为了认识天津近岸海域水质主要污染指标及污染物随年份的演变规律,根据1996年—2007年天津近岸海域水质监测数据,对天津近岸海域水污染状况进行了时空分析。结果表明,天津近岸海域水质总体呈恶化趋势,劣Ⅳ类海域面积比例呈增加趋势,主要污染因子为无机氮。提出,应确立治海先治陆的思想理念,建立陆源污染排放总量控制制度;加强对海上作业的管理,加强保护开发海域的生态环境。     

江苏近岸海域富营养化现状评价与成因分析

应用综合污染指数法和富营养化指数法评价了2010年度江苏近岸海域水质状况。结果表明,50%的海水水质测点已显现出不同程度的富营养化迹象;影响江苏近岸海域的首要污染物为无机氮和活性磷酸盐,二者污染分担率之和近50%;现阶段造成江苏近岸海域水体富营养化的主要因素来源于入海河流和直排海污染源的氮磷输入,与"十五"末相比,全省主要入海河流TN排放量增长约284%,TP排放量增长约451%。     

河北省近岸海域氮磷变化及其影响因素分析

根据2011—2018年河北省近岸海域海水、入海河流、降水中氮和磷的监测数据,分析了海水中氮和磷的变化趋势及其影响因素。结果表明：2011—2018年,河北省近岸海域海水中无机氮（DIN）和无机磷（DIP）的平均浓度均低于第二类海水水质标准,海域富营养化状况以贫营养和轻度富营养为主,超标（第二类海水水质标准限值）点位和中度、重富营养区域主要集中在沧州市近岸海域。河北省近岸海域海水中DIN的平均浓度在2011—2014年、2015—2017年呈现阶段性上升趋势,2018年大幅下降;DIP的平均浓度在2011—2013年无明显波动,2014年陡增后开始逐年下降;N/P在2011—2014年无明显变化,2015—2018年呈逐年上升趋势。自2016年起,入海河流中氨氮和总磷的平均浓度、降水中氨氮的平均浓度均呈逐年下降趋势。近岸海域海水、入海河流、降水中的氮和磷表现出一定的相关性和协同性,陆源污染输入总量降低是海水中氮磷浓度降低的主要原因。应警惕污染物控制力度的不同所导致的海水中生源要素结构的改变,及其引发的潜在海洋生态风险。     

Seasonal appearance of Chlorophyceae phytoplankton bloom by river discharge off Paradeep at Orissa Coast in the Bay of Bengal

Characteristics of the monsoonal bloom of phytoplankton at Orissa Coast in the Bay of Bengal were studied through bimonthly observation from April 2001 to December 2002. Three photosynthetic pigments chlorophyll-a (Chl a), chlorophyll-b (Chl b) and carotenoid (Car) were analyzed by absorption spectroscopic method. The seasonal variation of Chl a included phytoplankton bloom in the coastal area during monsoon period. The water column integrated Chl a reached to 68 mg m(-2) at the station-1(St1), and amounted to 20 mg m(-2) at 30 km off the river mouth during August 2001. In contrast the same amount was found at 15 km off the Mahanadi river mouth during August 2002. Salinity during this period varied from 5 psu at the St1 to 27 psu at the edge of the bloom area. The total amount of river discharge in the monsoon period calculated from daily river discharge data reported by Water Resources Department in India was 84 x 10(9) m(3) during 2001 and 20 x 10(9) m(3) during 2002. Both nitrate and phosphate concentrations showed negative quadratic relationship with salinity throughout the observation period. Extrapolated nitrate and phosphate concentration discharge from the Mahanadi river were 10.8 and 4 microg-at l(-1), respectively. Microscopic identification revealed dominance of fluvial Chlorophyceae and diatoms during the monsoon period showing influence of the freshwater discharge.     

Desert disturbance assessments of regional oil exploitation by Aster and ETM+ images in Taklimakan Desert China

To feed its rapidly growing energy demand, oil exploitation in China has never been more intensive. The most obvious characteristics of oil exploitation are progressive and regional, which can be monitored by remote sensing, such as land use and cover change, either perpetual or temporary, during oil field development such as construction of oil well, roads, transportation systems and other facilities. In this paper, the oil field located on the north edge of Taklimakan Desert, in the Tarim River watershed in northwest of China. The disturbance effects of regional oil exploitation were the main content of regional environmental managements and monitoring. Based on Enhanced Thematic Mapper Plus (ETM+) and Aster images, analyzed regional land use and landscape change from 2001 to 2003. By the comparison, it can be concluded that the ecological quality was deteriorating in these 3 years. The woodland was degrading to grass and dessert. The area of woodland dropped from 9.06 km(2) in 2001 to 3.24 km(2) in 2003 with a 64.23% decrease. At the same time, the area of shrubbery lessened 18.23%. On the other hand, the whole area of dessert and Saline soils inflated from 15.08 km(2) in 2001 to 25.36 km(2) in 2003. The patch number of bare land did climb dramatically, but single patch area increased. The research demonstrated that dessert and Saline soils patches were activated by the human behavior and climate change. The information from the ETM+ and Aster images was proved be an effective and efficient way to be applied in regional environmental managements.     

National assessment of sea level rise using topographic and census data for Turkish coastal zone

Turkish coastal zone elevation to sea level rise was illustrated by using digital elevation model and Geographical information systems methods. It was intended to determine several parameters such as population, settlements, land use, wetlands, contribution to national agricultural production and taxes at risk by using high resolution SRTM topographic, orthorectified Landsat Thematic Mapper Mosaics and census data with GIS methods within 0-10 m elevation of national level. All parameters were examined for coastal cities, coastal districts, settlements and villages' status. As a result of the analysis of data set, it was found that approximately 7,319 km(2) of land area lies below 10 m contour line in Turkey, and is hence highly vulnerable to sea-level rise. 28 coastal cities, 191 districts and 181 villages or towns are located below 10 m contour line in study area. In the short term, for the struggle of negative impact of sea level rise, the findings suggest that the Ministry of Environment should declare new areas as protection areas and develop special environmental programs for national level.     

无锡市国控环境空气自动监测站点周边裸土分布高分辨率遥感监测

以无锡市为研究区,使用过境时间相近的哨兵2号Sentinel-2和Landsat8影像,综合使用NDSI、NDISI、MNDWI、LST等指数进行决策树分类,获得10 m高空间分辨率的土地利用分类结果和裸土分布,裸土提取精度达到94.13%。统计了无锡市与8个国控环境空气自动监测站点1、2、3 km缓冲区范围内的裸土分布情况,并与各站点监测的大气颗粒物浓度进行相关性分析。结果表明,国控环境空气自动监测站点周边裸土面积对颗粒物浓度有较大影响,其中对PM₁₀浓度的影响明显大于PM_2.5;相比于1 km和3 km,2 km缓冲区范围内的裸土面积对PM₁₀浓度的影响最大,建议环境管理部门重点关注无锡地区国控监测站点周边2 km范围内的裸土扬尘源分布情况。     

2001—2018年浙江省酸雨变化特征及影响因素分析

利用2001—2018年浙江省32个城市酸雨观测资料,结合数理统计和GIS空间插值,分析了全省降水酸度变化、化学组分特征及其影响因素。研究结果表明,以2009年为拐点,浙江省酸雨污染呈先加重后减轻的趋势,降水酸度和酸雨率均得到显著改善。2009年后,轻酸雨城市的比例不断上升。至2018年,全省大部分城市均处于轻酸雨区,并有部分非酸雨城市出现。降水中的硫酸根离子浓度呈显著下降趋势,硝酸根离子浓度呈波动变化,但变化不显著。硫酸根离子与硝酸根离子的当量浓度比值呈显著下降趋势,由2002年的3.48降至2018年的1.35,酸雨类型由硫酸主导型向复合型转变。二氧化氮、硝酸根离子和可吸入颗粒物是影响降水pH的主要因素,氮氧化物对浙江省降水酸度的影响不断增大。因此,在加强区域硫氮协同控制的同时,着力加强氮氧化物深度减排是进一步改善浙江省酸雨状况的关键。     

Characterizing wetland change at landscape scale in Jiangsu Province, China

Human activities produced great impacts on wetlands worldwide. Taking Jiangsu Province, China, as a representative wetland region subject to extensive human activities, the aim of this study is to understand the conversion trajectory and spatial differentiation in wetland change from a multi-scale perspective. Based on multi-temporal Landsat images, it was found that the natural wetlands decreased by 11.2% from 1990 to 2006 in Jiangsu Province. Transition matrices showed that the conversion of natural wetlands to human-made wetlands (mostly aquaculture ponds) was the major form of natural wetland reduction, accounting for over 60% of the reduction. Percentage reduction and area reduc tion of natural wetlands were respectively quantified within different wetland cover zones using a moving window analysis. Average percentage reduction showed a decreasing tendency with increasing wetland cover. The high-cover and mid-cover zone presented the largest area reduction at the scales of 1-2 km and 4-8 km, respectively. Local hotspots of natural wetland reduction were mapped using the equal-interval and quantile classification schemes. The hotspots were mostly concentrated in the Lixiahe marshes and the coastal wetland areas. For the area reduction hotspots, the quantile classification presented larger area and more patches than the equal-interval classification; while an opposite result was shown for the percentage reduction hotspots. With respect to the discontinuous distribution of the natural wetlands, area reduction could be more appropriate to represent reduction hotspots than percentage reduction in the study area. These findings could have useful implications to wetland conservation.     

Monitoring the changing position of coastlines using aerial and satellite image data: an example from the eastern coast of Trabzon, Turkey

Coastline mapping and coastline change detection are critical issues for safe navigation, coastal resource management, coastal environmental protection, and sustainable coastal development and planning. Changes in the shape of coastline may fundamentally affect the environment of the coastal zone. This may be caused by natural processes and/or human activities. Over the past 30 years, the coastal sites in Turkey have been under an intensive restraint associated with a population press due to the internal and external touristic demand. In addition, urbanization on the filled up areas, settlements, and the highways constructed to overcome the traffic problems and the other applications in the coastal region clearly confirm an intensive restraint. Aerial photos with medium spatial resolution and high resolution satellite imagery are ideal data sources for mapping coastal land use and monitoring their changes for a large area. This study introduces an efficient method to monitor coastline and coastal land use changes using time series aerial photos (1973 and 2002) and satellite imagery (2005) covering the same geographical area. Results show the effectiveness of the use of digital photogrammetry and remote sensing data on monitoring large area of coastal land use status. This study also showed that over 161 ha areas were filled up in the research area and along the coastal land 12.2 ha of coastal erosion is determined for the period of 1973 to 2005. Consequently, monitoring of coastal land use is thus necessary for coastal area planning in order to protecting the coastal areas from climate changes and other coastal processes.     

浙江近岸海域春季表层溶解氧饱和度分布及影响因素

根据2014年春季对浙江省近岸海域溶解氧的调查结果,结合现场的温度和盐度,得出溶解氧饱和度的平面分布,并在此基础上探讨了饱和度与温度、盐度、化学需氧量、浮游植物丰度之间的关系。结果显示,浙江省近岸海域溶解氧饱和度范围为92.1%~120%,均值为100%。总体呈西部沿岸低,东部外海高的平面分布趋势。溶解氧饱和度高值区与浮游植物丰度的高值区一致。低饱和区域化学需氧量含量基本高于1 mg/L。陆源径流和有机物质耗氧分解是沿岸低饱和区域主要控制因素,外海水和浮游植物光合作用是高饱和区域主要控制因素。径流和外海水对有机物质分解和浮游植物光合作用有一定的调控作用。     

A distributed modelling system for simulation of monthly runoff and nitrogen sources, loads and sinks for ungauged catchments in Denmark

We validated an existing physically based 3D MIKE SHE groundwater resource model (DK-model) at 175 Danish gauging stations covering different catchment sizes in order to calculate monthly water runoff in the 50% ungauged part of Denmark. Model performance was in most cases good (61% of gauging stations had a Nash-Sutcliffe (NS) coefficient >0.60) but nevertheless showed a large seasonal and georegion specific bias. Therefore, bias correction factors had to be developed before applying the DK-model simulations of runoff in the ungauged areas. Simulated monthly runoff from ungauged areas and the measured monthly runoff from 178 gauging stations were distributed to 2663 smaller Hydrological Units (ca. 15 km(2)) and linked with a new empirical model for flow-weighted monthly total nitrogen (TN) concentrations (R(2) = 0.43; P < 0.0001) developed based on 20 years of observations (1990-2009) in 83 small catchments for calculation of monthly gross diffuse TN-loads from HU's. Nitrogen retention was calculated in streams, lakes and wetlands utilising both lake specific models and rate coefficients to calculate N retention in surface water bodies. The whole model complex was linked in the DK-QN concept for simulation of monthly TN losses from point sources and diffuse sources, TN retention and resulting loadings to Danish coastal waters. The DK-QN model was validated in 118 gauged catchments and the model simulations had for >25% of the observations of monthly discharge weighted TN concentrations a NS larger than 0.26. Catchment specific monthly TN-loadings were modelled with a higher performance as 50% of the catchments had a NS greater than 0.75. The model concept allows calculation of N retention in streams, lakes and wetlands and the average annual model calculated N retention amounted to 21% of the modelled gross riverine TN loadings. The average annual gross TN loading to surface freshwater in Denmark derived from diffuse sources amounted to 97 000 tonnes N (91% of gross TN loadings) which is 54% of the total estimated N-leaching from the root zone on the Danish land area (212 000 tonnes N) during the period 1990-2009.     

Shoreline change analysis of Vedaranyam coast, Tamil Nadu, India

The coastal zone is one of the nation’s greatest environmental and economic assets. The present research aims at studying the shoreline changes along Vedaranyam coast using conventional and modern techniques including field sampling, remote sensing, and geographical information system (GIS). The study area was divided into three zones. Dynamic Land/Sea polygon analysis was performed to obtain the shore line changes at different time periods between 1930 and 2005. From the multidate shoreline maps, the rate of shoreline change was computed using linear regression rate and end point rate. Further, the shoreline was classified into eroding, accreting, and stable regions through GIS analysis. The eroding, accreting, and stable coastal stretch along Vedaranyam is observed as 18 %, 80.5 %, and 1.5 %, respectively. Net shoreline movement is seaward, i.e., the coast is progressive with an average rate of 5 m/year. A maximum shoreline displacement of 1.3 km towards the sea is observed near Point Calimere. During the Asian Tsunami 2004, the eastern part of the study area showed high erosion. Sediment transport paths derived from the grain size analysis of beach sediments collected during different seasons help to identify the major sediment source and sinks. Point Calimere acts as the major sink for sediments whereas Agastiyampalli and Kodiakkarai are found to be the major sources for the sediment supply along the Vedaranyam coast. Shoreline change study from field and satellite data using GIS analysis confirms that Vedaranyam coast is accreting in nature.