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| 珠江口横门大气氮、磷干湿沉降的初步研究 | |
| 引用本文： | 樊敏玲,王雪梅,王茜,林文实,金辉.珠江口横门大气氮、磷干湿沉降的初步研究[J].热带海洋学报,2010,29(1):51-56. |
| 作者姓名： | 樊敏玲 王雪梅 王茜 林文实 金辉 |
| 作者单位： | 1. 中山大学环境科学与工程学院,广东,广州,510275;中国科学院南海海洋研究所,广东,广州,510301;中国科学院研究生院,北京,100049 2. 中山大学环境科学与工程学院,广东,广州,510275 3. 上海市环境监测中心,上海,200030 |
| 基金项目： | 国家自然基金(40875076) |
| 摘 要： | 通过对2006年12月至2007年11月中山横门的大气沉降采样分析, 初步探讨了珠江口大气氮、磷干湿沉降的特征。结果表明, 观测期间铵态氮(NH4+-N)、硝态氮(NO3--N)、总氮(TN)、总磷(TP)降雨量加权平均浓度分别为0.82、0.52、2.14、0.039mg.L-1, 干湿总沉降通量分别为1.584、1.142、4.295和0.055g.m-2.a-1。NH4+-N、NO3--N和TN干、湿沉降通量相当, 而TP以湿沉降为主。TN大气沉降通量春、夏、秋三季相当, 均明显高于冬季, TP则以夏季最大, 秋季次之, 而冬季最小。 |
| 关 键 词： | 干沉降 湿沉降 营养盐 沉降通量 珠江口 |
| 收稿时间： | 2008-11-22 |
| 修稿时间： | 2009-4-28 |
Atmospheric deposition of nitrogen and phosphorus into the Hengmen of Pearl River Estuary |
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| FAN Min-ling,WANG Xue-mei,WANG Qian,LIN Wen-shi,JING Hui.Atmospheric deposition of nitrogen and phosphorus into the Hengmen of Pearl River Estuary[J].Journal of Tropical Oceanography,2010,29(1):51-56. | |
| Authors: | FAN Min-ling WANG Xue-mei WANG Qian LIN Wen-shi JING Hui |
| Affiliation: | 1. School of Environmental Science and Engineering, Zhongshan University, Guangzhou 510275, China; 2. South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China; 3. Graduate University of Chinese Academy of Sciences, Beijing 100049, China; 4. Shanghai Environment Monitoring Center, Shanghai 200030, China |
| Abstract: | To understand the characteristics of atmospheric nutrient deposition into the Pearl River Estuary, measurements of dry and wet depositions of nitrogen and phosphorus were made at Hengmen in Zhongshan from December 2006 to November 2007. Results showed that, on an annual basis, volume-weighted concentrations in wet deposition for ammonium nitrogen (NH4+-N), nitrate nitrogen (NO3--N), total nitrogen (TN), total phosphorus (TP) were 0.82, 0.52, 2.14, 0.039mg.L-1, respectively; their corresponding annual deposition fluxes (dry + wet) were 1.584, 1.142, 4.295 and 0.055g.m-2.a-1, respectively. The budget of wet deposition corresponded with that of dry deposition for NH4+-N, NO3--N and TN, and wet deposition was the major source for TP. Seasonal change of total deposition fluxes for TN showed no significant difference among spring, summer and autumn, while that for TP was highest in summer, lower in autumn, and lowest in winter. |
| Keywords: | dry deposition wet deposition nitrogen and phosphorus deposition flux Pearl River Estuary |
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