中国环境科学
中國環境科學
중국배경과학
China Environmental Science
2015年
9期
2754-2763
,共10页
王江飞%周柯锦%汪小泉%邓靖%吴柳芳%马晓雁%钟晓%蒲凤莲%施丽莉
王江飛%週柯錦%汪小泉%鄧靖%吳柳芳%馬曉雁%鐘曉%蒲鳳蓮%施麗莉
왕강비%주가금%왕소천%산정%오류방%마효안%종효%포봉련%시려리
杭嘉湖%氮素沉降%磷沉降%干湿沉降%反向云团轨迹
杭嘉湖%氮素沉降%燐沉降%榦濕沉降%反嚮雲糰軌跡
항가호%담소침강%린침강%간습침강%반향운단궤적
Hangjiahu%nitrogen deposition%phosphorous deposition%dry and wet deposition%air mass backward trajectory
通过2013年9月~2014年8月杭嘉湖地区杭州、嘉兴和湖州3个典型站点大气氮、磷沉降数据,探讨了杭嘉湖地区大气氮、磷沉降的污染特征.结果表明,目标地区内大气氮、磷沉降通量水平较高,分别为 4950.74~5585.80,65.25~69.72kg/(km2·a);直接降入水域中的氮、磷素分别为 6038.4,77.8t,分别相当于农业源的氮、磷入河量的 39.6%和 5.9%.氮沉降以湿沉降形式为主,磷沉降以干沉降形式为主;氮、磷湿沉降通量主要受降雨量影响,且随降雨量的增加而增加;氮、磷沉降存在时空差异性,大气氮干沉降通量以杭州、嘉兴地区为较高,大气磷干沉降通量以嘉兴地区为最高,大气氮湿沉降通量则以湖州、嘉兴地区为较高,大气磷湿沉降以湖州地区最高;时间尺度上,氮沉降夏秋两季最高,磷沉降以秋冬两季最高.
通過2013年9月~2014年8月杭嘉湖地區杭州、嘉興和湖州3箇典型站點大氣氮、燐沉降數據,探討瞭杭嘉湖地區大氣氮、燐沉降的汙染特徵.結果錶明,目標地區內大氣氮、燐沉降通量水平較高,分彆為 4950.74~5585.80,65.25~69.72kg/(km2·a);直接降入水域中的氮、燐素分彆為 6038.4,77.8t,分彆相噹于農業源的氮、燐入河量的 39.6%和 5.9%.氮沉降以濕沉降形式為主,燐沉降以榦沉降形式為主;氮、燐濕沉降通量主要受降雨量影響,且隨降雨量的增加而增加;氮、燐沉降存在時空差異性,大氣氮榦沉降通量以杭州、嘉興地區為較高,大氣燐榦沉降通量以嘉興地區為最高,大氣氮濕沉降通量則以湖州、嘉興地區為較高,大氣燐濕沉降以湖州地區最高;時間呎度上,氮沉降夏鞦兩季最高,燐沉降以鞦鼕兩季最高.
통과2013년9월~2014년8월항가호지구항주、가흥화호주3개전형참점대기담、린침강수거,탐토료항가호지구대기담、린침강적오염특정.결과표명,목표지구내대기담、린침강통량수평교고,분별위 4950.74~5585.80,65.25~69.72kg/(km2·a);직접강입수역중적담、린소분별위 6038.4,77.8t,분별상당우농업원적담、린입하량적 39.6%화 5.9%.담침강이습침강형식위주,린침강이간침강형식위주;담、린습침강통량주요수강우량영향,차수강우량적증가이증가;담、린침강존재시공차이성,대기담간침강통량이항주、가흥지구위교고,대기린간침강통량이가흥지구위최고,대기담습침강통량칙이호주、가흥지구위교고,대기린습침강이호주지구최고;시간척도상,담침강하추량계최고,린침강이추동량계최고.
Available data of atmospheric nitrogen and phosphorous deposition during Sep, 2013 to Aug, 2014, were collected from three typical monitoring stations of Hang-Jia-Hu area, which are located at Hangzhou, Jiaxing andg Huzhou city respectively. The pollution characteristics of this area were discussed. Annual bulk deposition of nitrogen and phosphorous were significantly high in range of 4950.74~5585.80 and 65.25~69.72kg/(km2·a); Atmospheric deposition of nitrogen, phosphorus into the water were 6038.4 and 77.8 tons, respectively, equivalent to 39.6% and 5.9% input amount of nitrogen and phosphorus by agricultural. The principal deposition form for nitrogen was wet deposition, while for and phosphorous, it was dry deposition. Wet deposition of nitrogen and phosphorous were affected by rainfall situation, and usually increased along with the rainfall amount. The spatial ariation characteristics of nitrogen and phosphorous showed that high dry atmospheric deposition of nitrogen (Hangzhou, Jiaxing), high dry atmospheric deposition of phosphorous (Jiaxing), high wet nitrogen deposition (Huzhou, Jiaxing), and high wet phosphorous of Huzhou. On the time scale, nitrogen deposition was much higher in summer and autumn, while phosphorus deposition was much higher in autumn and winter.