首页 | 本学科首页   官方微博 | 高级检索  
     检索      

太湖西岸出入湖河口氮磷消减特征
引用本文:郭加汛,赵耕毛,郭西亚,张海涛,邓建才.太湖西岸出入湖河口氮磷消减特征[J].长江流域资源与环境,2017,26(9):1417.
作者姓名:郭加汛  赵耕毛  郭西亚  张海涛  邓建才
作者单位:(1. 南京农业大学资源与环境科学学院,江苏 南京 210095;2. 中国科学院南京地理与; 湖泊研究所湖泊与环境国家重点实验室,江苏 南京 210008)
基金项目:水体污染控制与治理科技重大专项(2014ZX07101-011),国家自然科学基金(41271213),中国科学院重点部署项目(KZZDEW-10)
摘    要:河流水体污染物消减作用是降低其入湖通量的重要方式,为探明太湖河流氮磷污染物消减速率时空变化特征,研究采用自主研发的原位培养装置,开展了太湖西岸出入湖河口总氮绝对消减速率(TNR_绝)、总氮相对消减速率(TNR_相)、总磷绝对消减速率(TPR_绝)、总磷相对消减速率(TPR_相)的变化特征研究。结果表明:西北部和西部河流夏、秋季TNR_绝和TPR_绝高于春、冬季,南部河流则为秋、冬季高于春、夏季。夏季西部和西北部河流TNR_绝和TPR_绝高于南部,冬季则相反,春、秋两季空间差异不明显。颗粒态总氮(PTN)浓度及水温是TNR_绝时空差异性的主要影响因素。TP浓度是TPR_绝的季节差异性的主要原因,不同季节TPR_绝空间差异的主要影响因素不同,春、夏、秋、冬四季主要影响因素分别为p H等水体物理性质、TP浓度和SS浓度、SS浓度、TP浓度。TNR_绝和TPR绝及其初始浓度是TNR_相和TPR_相时空差异的主要原因。

关 键 词:河流水体  氮磷  消减特征  时空特征

CHARACTERISTICS OF NITROGEN AND PHOSPHORUS REDUCTION IN THE INLET RIVERS AROUND WEST LAKE TAIHU
GUO Jia-xun,ZHAO Geng-mao,GUO Xi-ya,ZHANG Hai-tao,DENG Jian-cai.CHARACTERISTICS OF NITROGEN AND PHOSPHORUS REDUCTION IN THE INLET RIVERS AROUND WEST LAKE TAIHU[J].Resources and Environment in the Yangtza Basin,2017,26(9):1417.
Authors:GUO Jia-xun  ZHAO Geng-mao  GUO Xi-ya  ZHANG Hai-tao  DENG Jian-cai
Institution:(1. College of Resources and Environmental Sciences, Nanjing Agricultural University, Nanjing 210095, China; 2. State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese ; Academy of Sciences, Nanjing 210008, China)
Abstract:Reducing rivers nitrogen and phosphorus is an important method that can control the lakes nitrogen and phosphorus pollution.In order to explore the spatial and temporal variations of rivers nitrogen and phosphorus reduction rates around the Lake Taihu,total nitrogen (TN) and total phosphorus (TP) absolute reduction rates (Ra) and relative reduction rates (Rr) were measured through self-developed in-situ devices in the inlet rivers around west Lake Taihu in four seasons between 2014 and 2016.The TNRa of northwest and west rivers in summer or autumn were higher than those in spring or winter,and theTNRa of south rivers in autumn or winter were higher than those in spring or summer.In the summer the TNRa and TPRa of northwest and west rivers were significantly higher than that southwest rivers,and the rates of south rivers in winter were significantly higher than others (P<0.05).The rivers spatio-temporal TNRa differences were affected by particalate total nitrogen (PTN) and the seasonal water temperatures.The seasonal TPRa difference of was caused by seasonal difference of TP concentrations.The main reasons that affect season TPRa were various.The spring main factors were water physical properties such as pH,and the summer factor were TP and suspended solids;whereas the main autumn and winter factors were only suspended solids and TP,respectively.Those Lake Taihu rivers TNRr and TPRr were affected by TNRa and TPRa and its initial TN and TP concentration.
Keywords:river water  nitrogen and phosphorus  reduction characteristics  spatio-temporal characteristics
本文献已被 CNKI 万方数据 等数据库收录!
点击此处可从《长江流域资源与环境》浏览原始摘要信息
点击此处可从《长江流域资源与环境》下载免费的PDF全文
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