共查询到18条相似文献,搜索用时 93 毫秒
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正本文以太湖西岸宜兴段湖滨带为研究对象,对沿岸水域水质进行采样分析,并对太湖西岸宜兴段湖滨带水质进行分区段研究,为有效地保护西太湖湖滨带生境提供参考。太湖滨湿地是湖泊湿地重要组成部分,它位于湖泊的湖滨带,是湖泊与其周围环境间物质和能量交换的重要通道,具有固岸护岸、拦截径流污染物、保持生物多样性以及景观美学等方面的价值,是湖泊生态系统的重要保护屏障。由于特殊的地理位置,湖滨带是湖泊水体中最易污染的区域。 相似文献
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本文论述了东太湖茭草资源的现状及对环境的影响,揭示其生态失调、利用价值下降的趋势,勾保护湖泊资源和水利功能,提出了开发治理对策。 相似文献
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定量研究金沙江上游巴塘河段梯级电站的水温累积影响,掌握河段的水温变化规律对工程的生态管理和环境修复具有重要意义。利用宽度平均的立面二维水温模型对巴塘、拉哇及叶巴滩电站单独运行及不同联合运行条件下的水温进行了数值模拟。结果表明,梯级电站联合运行使得下游巴塘库区最低水温出现延迟效应,库区水体同温化效应随梯级电站增加而放大;两级联合运行促使4月双温跃层结构和1月的逆温分布现象消失,三级联合运行造成4、5月双温跃层结构和12~翌年1月的逆温分布现象消失。下泄水温的年变幅随梯级电站增加而减小;两级联合运行时,变幅为13.0℃;三级联合运行时,变幅为10.2℃。下泄水温随着梯级电站的增加,延迟效应更加明显。将计算结果和天然水温相比,结果表明,上游电站联合运行对下游水温过程存在较大影响,其中不同联合运行情况下巴塘电站对水温累积影响的贡献率都极小。 相似文献
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《中国环境管理干部学院学报》2004,(3)
最新研究表明,洗涤剂中的磷对水体的富营养化有影响,但不是主导影响,更不是水体富营养化的惟一凶手。 中国科学院地理与湖泊研究所以太湖为例,就洗衣粉排磷对湖泊磷负荷的贡献率进行了定量调查,经过两年的调查和试验,得出了太湖流域地区各种途径对太湖流域水体磷的贡献率依次为:人体(粪便)排磷43.57%、洗衣排磷16.1%、畜禽排磷12.51%、农业(化肥流失)排磷11.89%、工业(污染)排磷7.41%、水产养殖排磷5.3%、其他排磷2.8%。 相似文献
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在综合科学考察的基础上,经过大量的水质化学数据的测试,阐明了可可西里地区湖泊的水化学基本特征。包括分析了流域盆地内天然降水、水系及湖泊的水质展布趋向,运用离子域随机图式聚类阐明了湖水物质来源条件,还对典型湖泊的水温、分异、相变等进行了介绍和讨论;采用难溶盐法对本区水体进行水化学分类,阐明了湖泊水化学类型的地域性及其与区域地质环境条件的关系。 相似文献
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太湖西北部尤其是梅梁湖水质较差,新沟河延伸拓浚工程实施后,可通过外排梅梁湖水改变太湖的水动力水质环境.利用Mike21建立太湖二维水动力水质数学模型,研究该工程实施后对太湖水动力水质的影响.研究得到:新沟河工程实施后,可有效改善梅梁湖的水动力条件,梅梁湖换水周期缩短13.3%;同时,梅梁湖CODMn、 TP、TN等主要... 相似文献
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A Drinking Water Crisis in Lake Taihu, China: Linkage to Climatic Variability and Lake Management 总被引:26,自引:0,他引:26
Boqiang Qin Guangwei Zhu Guang Gao Yunlin Zhang Wei Li Hans W. Paerl Wayne W. Carmichael 《Environmental management》2010,45(1):105-112
In late May, 2007, a drinking water crisis took place in Wuxi, Jiangsu Province, China, following a massive bloom of the toxin
producing cyanobacteria Microcystis spp. in Lake Taihu, China’s third largest freshwater lake. Taihu was the city’s sole water supply, leaving approximately
two million people without drinking water for at least a week. This cyanobacterial bloom event began two months earlier than
previously documented for Microcystis blooms in Taihu. This was attributed to an unusually warm spring. The prevailing wind direction during this period caused
the bloom to accumulate at the shoreline near the intake of the water plant. Water was diverted from the nearby Yangtze River
in an effort to flush the lake of the bloom. However, this management action was counterproductive, because it produced a
current which transported the bloom into the intake, exacerbating the drinking water contamination problem. The severity of
this microcystin toxin containing bloom and the ensuing drinking water crisis were attributable to excessive nutrient enrichment;
however, a multi-annual warming trend extended the bloom period and amplified its severity, and this was made worse by unanticipated
negative impacts of water management. Long-term management must therefore consider both the human and climatic factors controlling
these blooms and their impacts on water supply in this and other large lakes threatened by accelerating eutrophication. 相似文献
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利用二维模型求解太湖水质CODMn的研究 总被引:1,自引:0,他引:1
在二维黎曼近似解模型的基础上建立了太湖水质预测模型,并运用该模型对太湖的水质指标CODMn了模拟。模拟的结果跟太湖各监测站的测量值相接近,表明该模型能较好的运用于太湖的水质预测。 相似文献
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为明确太湖不同湖区CH4释放特征与释放潜力差异,采用水-气界面甲烷排放通量测定和室内厌氧培养,结合沉积物理化因子对太湖沉积物CH4释放特征及其释放潜力差异进行研究。结果表明,不同湖区水-气界面CH4排放通量存在显著差异;不同湖区、不同深度沉积物中CH4释放潜力也存在明显差异,且CH4释放潜力与含水率和总有机碳呈正相关,与盐度呈负相关;太湖沉积物产CH4潜力最大的途径为甲基途径,且主要集中在沉积物10~35cm深度。由此可知,太湖是CH4排放的净产生源,含水率、有机质和盐度等环境因子的差异以及沉积物深度均会影响沉积物甲烷排放和释放潜力,从而对太湖沉积系统的碳循环以及局部气候变化产生重要影响。 相似文献
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The incomplete understanding of the processes which control aquatic nitrous oxide (N2O) production is partially due to a lack of onsite data with which to describe the temporal resolution of N2O production. To help resolve this, we directly measured the N2O saturation (relative to atmospheric partial pressure) on an hourly basis over two survey periods (July and September 2003) in Lake Taihu, a large eutrophic lake in eastern China. July N2O saturations displayed a distinct diurnal pattern, opposite to those observed by others in subtropical streams, but similar to N2O emissions observed from incubated estuarine sediments. Correlative analyses indicate that biogeochemical processes operate as important controls on N2O production over very short time scales. Nitrous oxide production processes are not only regulated by O2 dynamics related to microalgal photosynthesis, but also closely related to organic matter decay at the sediment-water interface. While large-scale changes (approximately 25-fold) in N2O fluxes in Lake Taihu are a function of variable N loading, biogeochemical processes concerning O2 and N transformation at the sediment-water interface have significant (-twofold) impacts on the regulation of N2O production over very short time scales. Further, high temporal resolution research focused on developing a comprehensive understanding of lacustrine N2O production, including natural and anthropogenic loading and biogeochemical transformation processes, is clearly needed. 相似文献