首页 | 本学科首页   官方微博 | 高级检索  
相似文献
 共查询到18条相似文献,搜索用时 203 毫秒
1.
陈荷生  李幼芬 《湖泊科学》1998,10(S1):59-66
According to the social and natural conditions of Taihu Lake Basin, the planning objectives and some ideas for water pollution prevention in Taihu Lake and its surrounding river-lake system are proposed.  相似文献   

2.
The outline of Taihu Lake Basin, including the geographical and hydrometeorological characteristics, its main functions and resource-environmental state and problems facing in Taihu Lake were introduced.  相似文献   

3.
In accordance with the natural, geographic, and ecological characteristics of the Taihu Lake Basin, and the relation between the water body of Taihu Lake and its surrounding environment, an area, which has tight relevance with the water environment of Taihu Lake, was token as the main investigation region. The area was named as the Taihu Lake Region. Some factors, such as TN, TP, CODCr that characterized the main environmental problem, the eutrophication were selected when conducted the pollution sources investigation on in Taihu Lake Region. The categories, distribution, pollution contribution to the Lake of dijferent pollution sources, as well as the routes of pollutants entering the Lake were basically made clear. Pollution sources that must be preferentially controlled and the direction of controlling those main pollutants, such as TN, TP, CODCr, were proposed. Base on the investigation, a series of eco-systematic approaches for controlling Taihu Lake eutrophication were put forward. They are ecosystem regulation, nutrient substances transferring along food chain, trophic masse degrading step by step along the route from a pollution source to the Lake, building ecological preventive zone of the Lake, as well as the ecological measures for point sources treatment and so on.  相似文献   

4.
Two sediment cores, one 396 cm long from west Taihu Lake, another 246 cm long from east Taihu Lake, are interpreted from the analysis of their magnetic susceptibility, total organic carbon, total nitrogen, total pigments, organic carbon isotope, hydrogen index, saturated hydrocarbons, 14C dating and surficial sediment conditions. The west Taihu Lake core is the longest one studied in this lake so far, and has provided us the most complete environmental and climatic information for this lake. The results from the west Taihu lake core indicate that Taihu Lake has undergone the following stages:from ca.14 300 to 13 300 aB.P. Taihu Lake was in low lake-level, and there existed exposed features from the proxies reflecting arid paleoclimate. From ca.13 300 to 12 400 aB.P. an arid transitional stages occurred with a slightly warmer and wetter climate. From ca. 12 400 to 10 900 aB.P. a period of large climatic fluctuation occurred and from 10900-10 000 aB.P. a warm period developed with deep water and strongly reducing sediments. During ca.10 000-7 200aB.P., a cool transitional period alternating with a warm climate occurred. It was warm and wet during 7 200-5 700aB.P.; some proxies changed violently in 5 050aB.P., reflecting obvious changes in material source and a probable interruption of sedimentation. The east Taihu Lake history from ca. 6 550 to 6 450 aBP, the climate was cold and dry, and gradually turned warm and wet in ca. 6 450-6 050 aBP. It was warm and wet in ca. 6 050-5 800 aBP and had a cold tendency in 5 800-ca. 5 000 aBP. An abrupt change occurred at ca. 5 000 aBP, and the lake sediment in the uppmost part was disturbed by wave action indicating shallow water conditions.  相似文献   

5.
翟淑华 《湖泊科学》1998,10(S1):123-128
Taihu Lake is the third largest fresh water lake in China, locating in Yangtze Delta as the richest area of China. At present, eutrophication problem is severe in Taihu Lake. This paper, in view of ecological system, presents analysis of the composition structural characteristics of Taihu Lake environment regarded as a whole ecological system, energy and substances circulation between ecological factors. The Taihu Lake ecological environment is proceeding a lake evolution period, i.e. middle-eutrophic to eutrophic. Therefore the diversion water''from Yangtze River to Taihu Lake through the Wangyu River acts to change external agent function for Taihu ecological system, i.e. increasing water quantity of Taihu Lake may rise water level and speed up flow exchanging. Moreover, with harnessing measures for pollution sources to reduce input of nutrients, natural evolution procedure of Taihu ecological environment may slow down to subsequently improve Taihu ecological environment.  相似文献   

6.
秦佩瑛  陈荷生 《湖泊科学》1998,10(S1):67-74
The water pollution situation of Taihu Lake, general conditions of the main inflow rivers to Taihu Lake, the compiling principles, the harnessing measures for polluted water and major inflow rivers to the lake, and the total quantity control plan were analyzed.  相似文献   

7.
黄漪平  诸敏 《湖泊科学》1998,10(S1):85-94
Lake Taihu, the third largest fresh water lake in China, with a surface area of 2 338 km2, is located in the Changjiang River Delta, the most advanced economic zone in China. During the last two decades, the rapid economic development of local agriculture and industry both in the urban and rural areas of the region has made great advances. Great quantieis of pollutants have been discharged into the lake, its nutrient content has increased continuously, and phytoplankton blooms have occurred in some areas. Water quality protection in Lake Taihu is very important because of its close relation with economical development and people''s daily life. It is urgent to have comprehensive pollution control in Lake Taihu. Based on water quality monitoring data in Lake Taihu from 1987 to 1994, the dynamic variations of water quality and eutrophication trends have been analyzed, showing obvious spatial and temporal variations. The main water quality factors were compared with the standard for drinking water and indicate considerable change with the seasons. Some basic strategies to protect water quality and prevent eutrophication are discussed.  相似文献   

8.
陈荷生  范成新 《湖泊科学》1998,10(S1):117-122
The eutrophication of Lake Taihu is becoming more serious day by day and more urgent to be comprehensively harnessed. The lake sludge is considered as a important polluting factor. To control the internal pollution source of Lake Taihu and restore its water ecological environment, this paper put forward an idea of the dredging for environmental purposes. It was on the basis of the research on the sludge storage and physical/chemical characteristics. The technical keys are sludge-dredging depth, time, method and sludge treatment. The requirements and scheme for the environmental dredging work in Lake Taihu were also analyzed in detail.  相似文献   

9.
太湖富营养化问题及其综合控制对策   总被引:1,自引:1,他引:0  
范成新  陈荷生 《湖泊科学》1998,10(S1):95-100
On the basis of nine-time current situation investigation for eutrophication of Taihu Lake during 1991-1995, this paper evaluated the trophic levels in the different periods and analyzed the development of the main nutrient content in the nearest 35 years. The results show that the trophic level of Taihu Lake is in the transition state from meso-eutrophic to eutrophic. The eutrophhic and hypereutrophic waters account for 10% or so. The limiting nutrient, P, rises most rapidly, which causes the ratio of N:P to decrease. The increase of P content is still one of the main factors giving rise to the eutrophication of Taihu. LakeSome proposals of comprehensive countermeasure for the eutrophication are put forward. They include the pollution source control of the basin, the littoral multiple management, optimal dispatch of water conservancy facilities, the engineering of helping Taihu Lake with diversion of the Changjiang River, and as well as the setting of the water quality protection and legal system.  相似文献   

10.
The presence of roads, farm house foundations, wells and Liangzhu period cultural relics in the bottom of Lake Taihu attest to the fact that this shallow depression was probably dry between 4 and 5 thousand years ago. This interpretation is corroborated by the sudden disappearance of algal pigments at sediment depths carbon-14 dated at 4-5 thousand years before present.In winter, the stronger winds are predominantly from the northeast. These winds result in a powerful counterclockwise current that transports lake sediments and has altered the very shape of the lake over the last 300 years. Winds produce a complex mixing pattern in Lake Taihu with storm induced sediment deposition occurring near the lake''s center.During approximately 240 days of the year, the wind blows across Lake Taihu with sufficient force to mix it to its bottom. As a result, this polymictic lake rarely becomes anoxic and dissolved oxygen at the mud water interface is maintained at or above 4 mg·l-1. The consequences of this high dissolved oxygen are quite impressive as high organic loading to the lake would otherwise render its bottom waters anaerobic killing many of its natural inhabitants.Because suspended solids reduce (attenuate) light penetration, the major primary production takes place in the top metre of the lake (mean Secchi Transparency-0.25 m). Suspended clays are slow to settle and wind mixing keeps fine-grained suspended solids in suspension in all but the most quiet backwaters of the lake.In the recent past about 23 000 metric tonnes of phytoplankton were produced in Lake Taihu. This large production represents only about 5% of the total influx of organic material entering the lake. In summer and fall, cyanobacteria such as Microcystis spp. and Anabaena spp. dominate most of the lake. Recently, however, mixotrophic flagellates displaced cyanobacteria as the dominant algae in parts of Lake Taihu with high bacteria and high suspended solids (e.g. Wuli and Meiliang Bay). In the future, facultative heterotrophs may come to dominate an ever larger portion of the lake waterc column.  相似文献   

11.
巢湖、太湖蓝藻湖靛及其提取物的动物毒性初步研究   总被引:1,自引:0,他引:1  
瞿文川  苏晨伟 《湖泊科学》1996,8(2):156-160
对国内淡水湖泊巢湖、太湖中的蓝藻湖靛及其提取物(藻胆蛋白),进行了动物毒性实验。实验动物为昆明种小白鼠,采用灌胃法给药。给药后小白鼠均无中毒症状,一周内无死亡。说明巢湖、太湖中蓝藻湖靛及其提取物,对以小白鼠为代表的哺乳类动物消化系统,基本不产生毒性。这对于开发两湖中的蓝藻作为鱼、家禽等饲料和提取其中的植物蛋白(藻胆蛋白)作为营养食品添加剂等有一定意义。  相似文献   

12.
太湖五里湖水环境综合整治的设想   总被引:19,自引:6,他引:19  
顾岗  陆根法 《湖泊科学》2004,16(1):57-61
在分析太湖五里湖水环境现状和污染成因的基础上,提出生态清淤、污水截流、退渔还湖、动力换水、生态修复、护岸整治等一系列水环境综合整治工程措施,并分析各项工程实施对污染物去除量的估算,预测对五里湖水质改善的影响和效果,进行五里湖、梅梁湖水环境综合治理的探索,为全太湖和其他湖泊水环境综合治理提供科学依据.  相似文献   

13.
吴小根 《湖泊科学》1992,4(3):54-60
历史时期,太湖是不断扩展的,其平均扩展速率为0.37km~2/a。据沙量平衡分析与计算表明。因湖岸崩塌和太湖水系的输沙作用,近期太湖的泥沙淤积量为9.28×10~5t/a.泥沙数量虽然不大,但经过长期的积累,对太湖演变具有深刻影响。就自然演变趋势而言,近期太湖面积仍以0.168km~2/a的速率扩大,容积则以3.95×10~5m~3/a的速率减小,太湖正进一步向浅平方向演变。然而,因围湖造田,建国以来,太湖的面积则以4.58km~2/a的速率在减小。  相似文献   

14.
太湖定振波的初步研究   总被引:1,自引:0,他引:1  
张文华 《湖泊科学》1992,4(4):23-28
初步分析研究了太湖定振波的变化规律,结果表明:(1)东、西太湖有各自的振动周期,东太湖变化范围在181—292min,平均为243min;西太湖在120—540min,平均为400min。(2)观测到的最大振幅(1/2波高)为120—130mm。(3)用差分法对定振波的特征值进行了近似估算,其周期误差为20min。(4)定振波引起的湖流相当大,当振幅为100mm时,最大流速可达±20cm/s。(5)定振波振幅的突变与气压场、风场和降水分布不均匀并在短期内发生突变有关。  相似文献   

15.
太湖湖体水环境容量计算   总被引:7,自引:1,他引:6  
范丽丽  沙海飞  逄勇 《湖泊科学》2012,24(5):693-697
针对太湖风生流的特点,提出考虑风向风速频率修正及污染带控制的水环境容量计算方法,建立了太湖水量水质数学模型,并结合水文水质资料对流场和浓度场进行模拟和验证.在控制单个污染带面积为1~3 km2,污染带总长度为湖岸线长度10%的基础上采用该方法进行计算,计算结果更可靠.太湖CODcr的水环境容量为132727 t/a,TN的水环境容量为7700 t/a.  相似文献   

16.
东太湖的环境质量现状调查评价   总被引:5,自引:2,他引:5  
石建华 《湖泊科学》1994,6(2):166-170
通过1990—1991年东太湖的水文、水质、底质和生物凋查,对其水质作出评价并探求营养现状。结果表明:东太湖的水质状况良好,营养状况已进入中富营养状态叶。  相似文献   

17.
太湖梅梁湾冬季湖流特征   总被引:1,自引:1,他引:1  
2003年元月在盛行西北偏北风的情况下,对位于太湖北部的梅梁湾进行了面上湖流调查,发现梅梁湾湾口的湖流较为稳定,以向南流为主,且流速相对较大,最大达8cm/s,梅梁湾西岸有稳定的向北流,而从五里湖口至拖山附近的梅梁湾东线湖水由北向南流动,且在中部附近分为两支,一支向西,再流向北以补偿西岸的向北流,另一支扩散至整个梅梁湾南部,向南流经湾口进入太湖.在梅梁湾东北部,发现有弱辐合中心,该范围内Chl.a和TP、TN的含量明显高于周围水域.从所有点的垂直运动判断,梅梁湾水流以弱上升运动为主,大小为2cm/s以下.从水量平衡分析,以梅梁湾流入太湖为主要特征,水量补给主要来自于北部的五里湖和直湖港及武进港.  相似文献   

18.
太湖自然渔业及其发展策略   总被引:10,自引:7,他引:3  
渔业是太湖的主要功能之一,它对改善水环境具有重要意义,但又受制于环境的影响而变化,从太湖渔业结构分析,目前太湖自然渔业整体捕捞强度过大、资源破坏严重,依据太湖多年渔获物捕捞结果,系统分析了太湖鱼类群落结构及其演变动态,通过对太湖不同生态区域渔获物产量和组成的分析,研究了太湖自然渔业特征及存在问题,提出了严格控制捕捞渔具规格和捕捞强度、合理调整开捕时间、调整放流鱼种结构和比例,合理发展湖泊渔业的思路,同时,依据太湖生物资源现状,分析了太湖自然渔业潜力,提出太湖渔业发展要加强渔业环境建设、加强渔业对水环境改善功能的研究.  相似文献   

设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号