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机构地区:[1]浙江大学环境与资源学院,杭州310029 [2]浙江省环境监测中心,杭州310012 [3]浙江省水文局,杭州310036 [4]湖州市环境监测站,浙江湖州313000 [5]湖州市水文站,浙江湖州313000
出 处:《安全与环境学报》2009年第3期106-109,共4页Journal of Safety and Environment
基 金:浙江省重大科技专项(2007C3002;2006C13054)
摘 要:根据2005-2007年浙江省环太湖河道水量巡测资料及水质监测资料,分析2005-2007年浙江省环太湖河流进出水量、水质及污染负荷的时空变化。结果表明,近儿年浙江环太湖河道水质总休上保持稳定,净入湖水量保持负值,其中苕溪是浙江入湖和出湖水量的最大贡献者。环太沏河流的入湖、出湖COD_(Mn)和总磷污染负荷通量呈增加趋势,而氨氮入湖与出湖通量下降。从净入湖量分析,COD_(Mn)和总磷污染负荷以外流为主,而氨氮以入流为主,存在一定程度的滞留。This article is to give a statistic report on the pollutant influx variations of all the rivers surrounding Taihu Lake in Zhejiang Province. Knowing the pollutant flux variations of the nearby rivers can help to provide a sound background for making effective policies and decisions for pollution control in Taihu Lake Basin. Based on the statistics data on the water quality and quantity of the rivers surrounding Taihu Lake in Zhejiang from 2005 to 2007, we have made a thorough analysis over the temporal and spatial variation of water quantity, quality and pollutant influx of the above said rivers. The results of statistics and analysis show that the water quality of the rivers can be generally said regular and steady. The indexes, such as CODMn, TP of the most measured sections of the rivers can be categorized into National Grade Ⅲ . But, as an exception, most sections measured of Changxing can only be up to National Grad Ⅳ. From the point of view of physical and chemical compositions, the index of TN in some sections is over the state standard. The net water inlet volume from the rivers proves negative in recent years. For example, Tiaoxi River, being the main contributor of water volume inlet and outlet of Taihu Lake in all rivers, whose inlet water quantity accounts for over 60 % water quantity of the total region water inlet. On the contrary, the water quantity of inlet was more than that of outlet in the region of Changxing. Based on the water quality and quantity of inlet and outlet of the rivers, the influx and out-flux of CODMn and total phosphorus has been growing, though that of NH3 - N is declining in the past 3 years. The results have shown that the CODMn and total phosphorus out-flux were more than that of influx. There were about 6 000 t/a CODMn net influx and 76 - 78 t/a total phosphorus net out-flux out of the Lake. Comparatively speaking, the ammonia nitrogen out-flux turns to be less than that of influx. There were about 60 - 200 t/a net ammonia nitrogen influx into Taihu Lake, which has crea
分 类 号:X52[环境科学与工程—环境工程]
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