长江流域资源与环境 >> 2010, Vol. 19 >> Issue (19): 1075-.

• 生态环境 • 上一篇    下一篇

上海地区酸雨类型格局转变研究

 梅雪英, 杨扬, 方建德   

  1. (1.暨南大学水生生物研究中心|热带亚热带水生态工程教育部工程研究中心|广东 广州 510632;2.环境保护部华南环境科学研究所|广东 广州 510655 )〖
  • 出版日期:2010-09-20

REGIME SHIFT OF ACID RAIN TYPE IN AREA OF SHANGHAI

MEI XueYing1| YANG Yang1| FANG Jiande1|2   

  1. (1.Research Center of Hydrobiology| Jinan University, Engineering Research Center of Tropical and Subtropical Aquatic Ecological Engineering|Ministry of Education, Guangzhou |510632, China|2. South China Institute of Environmental Sciences of the Ministry of Environmental Protection, Guangzhou 510655, China)〖
  • Online:2010-09-20

摘要:

采用STARS(Sequential 〖WTBX〗t〖WTBZ〗test analysis of regime shifts),以降水中SO2-4、NO-3以及SO2-4/NO-3为指标,研究了上海地区酸雨类型在1991~2006年的格局转变规律。上海地区降水中SO2-4含量在1991~2006年具有两种格局,2004年发生转变;转变前的SO2-4含量平均12670 mg/L,转变后SO2-4含量大幅度降低,平均6525 mg/L;降水中NO-3含量存在3种格局,两次转变;1996年转变前的NO-3浓度相对较低,平均1842 mg/L;此次转变后升高,平均2622 mg/L;2005年再次发生转变,使得NO-3含量下降,平均1998 mg/L;与NO-3含量的格局类似,SO2-4/NO-3也存在着3种格局,两次转变;1995年转变前,SO2-4/NO-3平均7316;此次格局转变后,SO2-4/NO-3降为5666;2000年的格局转变中SO2-4/NO-3降为3635。表明NO-3对酸雨的贡献逐渐增加,SO2-4对酸雨的贡献逐渐减弱,酸雨类型逐渐由硫酸型酸雨过渡成硫酸和硝酸混合型酸雨,并逐渐接近硝酸型酸雨。上海地区酸雨类型格局在1991~2006年发生5次格局转变,其格局转变指数(RSI)在1995、1996,2000,2004和2005年分别为0826、0260、0959,1378和0066。〖

Abstract:

At present,acid rain has aroused great concerns of people,but little previous research has been completed on regime shift of acid rain type.Based on the content of SO2-4,NO-3 and SO2-4/NO-3 in the rain of Shanghai,the regime shifts of acid rain type from 1991 to 2006,were studied by adopting the STARS(sequential 〖WTBX〗t〖WTBZ〗test analysis of regime shifts).There were two regimes of the SO2-4 content;one shift happened in 2004.Before the shift,it was 12.670 mg/L on average;after that,it decreased sharply to 6.525 mg/L.Whereas,there were three regimes,two shifts,of the NO-3 content.Before the first regime shift in 1996,it was 1.842 mg/L on average,after that,it increased to 2.622 mg/L on average till the second shift in 2005,then it decreased again to below 2.000 mg/L on average.Similar to the regime of NO-3 content,there were also three regimes of SO2-4/NO-3,shift twice.Before the first shift in 1995,SO2-4/NO-3 was 7.316;after that,it decreased to 5.666 till the second shift in 2000,then it decreased further to 3.635 on average.These indicated that during 1991~2006 in area of Shanghai,the contribution of NO-3 to acid rain increased,while the contribution of SO2-4 to acid rain decreased.The acid rain types were turning from sulfuric acid rain to sulfuric and nitric acid rain complex type,approaching the nitric acid rain type.Altogether,there were 5 regime shifts of acid rain type during 1991~2006 in area of Shanghai.The regime shift indices (RSI) were 0.826,0.260,0.959,1.378 and 0.066 in 1995,1996,2000,2004 and 2005,accordingly.〖

No related articles found!
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!