Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Wushan, Guangzhou, 510640, People's Republic of China.
Environ Monit Assess. 2010 Dec;171(1-4):429-39. doi: 10.1007/s10661-009-1289-7. Epub 2010 Jan 6.
With the aim of understanding the seasonal distribution of deposition fluxes of nitrogen (N) and sulfur (S) in South China, a main acid deposition region in China, precipitation samples were collected and analyzed from Guangzhou area, between March 2005 and February 2006. The estimated wet deposition of N (including ammonium nitrogen (NH(4)-N) and nitrate nitrogen (NO(3)-N)) and S (sulfate sulfur (SO(4)-S)) during the monitoring period were 40.47 kg N ha(-1) and 65.29 kg S ha(-1), respectively. The average deposition of NH(4)-N was ∼1.5 times of the NO(3)-N deposition, suggesting that the reduced and oxidized N depositions were comparable in the study area. The S and N depositions in the rainy season were greater than those in the dry season, showing great seasonal variation, which was consistent with both the distribution of precipitation and the period of fertilizer application for agriculture. The N and S wet deposition fluxes in Guangzhou were greater than those in Beijing and Zhengzhou, located in the northern China, but comparable to the level of Chongqing, located in the southwestern China, another major acid deposition region. The atmospheric N and S depositions in these cities from north to south were affected by both intensive agricultural and industrial activities.
为了了解中国主要酸沉降区——华南地区氮(N)和硫(S)沉降通量的季节性分布,于 2005 年 3 月至 2006 年 2 月在广州地区采集并分析了降水样本。监测期间,N(包括铵态氮(NH4-N)和硝态氮(NO3-N))和 S(硫酸盐硫(SO4-S))的湿沉降量分别为 40.47 kg N ha-1和 65.29 kg S ha-1。NH4-N 的平均沉降量约为 NO3-N 沉降量的 1.5 倍,表明在研究区域中,还原态和氧化态 N 的沉降量相当。雨季的 S 和 N 沉降量大于旱季,表现出很大的季节性变化,这与降水分布和农业施肥期一致。广州的 N 和 S 湿沉降通量大于位于中国北方的北京和郑州,但与位于中国西南部另一个主要酸沉降区的重庆相当。这些城市从北到南的大气 N 和 S 沉降受到密集的农业和工业活动的影响。