鄱阳湖流域水化学环境参数的变化特征  

SPATIOTEMPORAL VARIATIONS OF HYDROCHEMISTRY PARAMETERS IN THE POYANG LAKE CATCHMENT

作　　者：胡春华[1] 周文斌[1] 

机构地区：[1]南昌大学鄱阳湖环境与资源利用教育部重点实验室,江西南昌330029

出　　处：《长江流域资源与环境》2014年第3期427-433,共7页Resources and Environment in the Yangtze Basin

基　　金：国家水体污染控制与治理科技重大专项(2008zx07526-008-03);国际科技合作资助项目(2006DFB91920);"十一五"国家科技支撑计划重点项目(2007BAB23CO2);国家自然科学基金(40672159;41040032;41261097);鄱阳湖环境与资源利用教育部重点实验室支持项目(13005879;13005870);中国经济改革实施技术援助项目(支援期TCC5jxspyhzxh09-03)

摘　　要：分别于2010年2月和7月,对鄱阳湖湖区和入湖河流的pH、TDS以及主要离子浓度进行了测定,分析了主要离子组成的时空变化特征及其影响机制。结果表明,鄱阳湖流域水体属于弱矿化度软水,Ca2+是湖水和河水的主要阳离子,分别占阳离子总数的59.35%、49.89%;HCO-3是湖水和河水的主要阴离子,分别占阴离子总数的53.37%、59.37%,水质类型为Ca-HCO-3型水;主要离子组成和TDS浓度具有明显的季节和沿程变化特征,这与降雨季节性变化以及不同水系的地质背景有关;从河流水系上游至湖区的水化学特征依次为HCO-3型、HCO-3-SO2-4和SO2-4型。从水化学控制机制上看,鄱阳湖丰水期受大气降水作用和地质条件影响显著,而枯水期降雨量大大减少,主要受岩石风化、蒸发沉淀作用和人为输入的影响。除此之外,SO2-4型水的增加与长江干流酸化以及丰水期长江顶托倒灌现象有密切关系。The main ions in lake and river water are an essential part of water chemical characteristics. Climate conditions control the changing trend of hydrochemical indexes in a large scale, while geological conditions determine the differences in its distribution.Thus, climate and environment have their important function to indicate the spatiotemporal variation of water chemistry. The Poyang Lake is the largest freshwater lake of China, and its hydrology is controlled by humid monsoon climate. The rainfall in the region and the volume of the lake are subject to large seasonal variation. With rapidly increasing urbanization and water contamination, a better understanding of the hydroehemical parameters of the region is necessary. Hydrochemical investigations were carried out in the Poyang Lake catchment.pH,TDS and major ions were determined from the Poyang Lake and its inflow river to analyze the spatial and temporal variation characteristics of the major ions in Feb. （dry season） and Jul. （wet season） ,2010.And the possible controlling factors were discussed.The results indicated that water in the Poyang Lake catchment was Ca-HCO-3 type,soft water with low mineralized degree.Ca2＋ was the dominant cation in lake and river water, which were 59.35% and 49.89 % of the total cations, respectively. On the other hand, HCO-3 was the dominant anion in lake and river water,which were 53.37% and 59. 37% of the total antions,respectively. The annual mean values of the total dissolved solids （TDS） in lake and river water were 63.81 mg/L and 58.7 mg/L,respectively,approaehing to the mid-value of the whole world large rivers（65mg/L）.Besides, the composition of the major ions and TDS showed significant temporal and spatial variation, namely,

关 键 词：鄱阳湖流域 主要离子组成 时空变化 控制机制 

分 类 号：X143[环境科学与工程—环境科学]