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西太平洋热带海域降水化学特征
引用本文:肖辉,沈志来,黄美元.西太平洋热带海域降水化学特征[J].环境科学学报,1993,13(2):143-149.
作者姓名:肖辉  沈志来  黄美元
作者单位:中国科学院大气物理研究所 北京100029 (肖辉,沈志来),中国科学院大气物理研究所 北京100029(黄美元)
摘    要:1988年在西太平洋热带海域采集雨水样品,分析结果表明,大部分样品偏酸性(pH<5.6).雨水的化学组成结构主要受海盐的影响,这与我国大陆上雨水的情况很不相同.将西太平洋热带海域降水化学特征与南印度海域和西大西洋海域的降水情况作对比分析,结果表明,前两个海域雨水中的SO~(2-)受非海盐源的影响比西大西洋海域的小.

关 键 词:海洋  降水  非海盐源  热带海域  酸雨
收稿时间:1/9/1991 12:00:00 AM

CHEMICAL CHARACTERISTICS OF TROPICAL WESTERN PACIFIC PRECIPITATION
Xiao Hui,Shen Zhilai and Huang Meiyuan.CHEMICAL CHARACTERISTICS OF TROPICAL WESTERN PACIFIC PRECIPITATION[J].Acta Scientiae Circumstantiae,1993,13(2):143-149.
Authors:Xiao Hui  Shen Zhilai and Huang Meiyuan
Institution:Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029,Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029 and Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029
Abstract:The wet-only marine precipitation samples of 46 from the Tropical Western Pacific Area (TWPA) were collected during a period of September 26 to October 27, 1988. The analyzed results indicated that the rainwater was acidic with an arithmetic mean pH of 5.30, a volume-weighted mean (VWM) pH of 5. 05, and a pH range of 3. 86 to 7. 02. There were two thirds of the samples with pH<5.60. The chemical components of rainwater in TWPA were dominated mainly by sea salt, but they were not simply diluted seawater solutions. The kind of construction of chemical components was different from that from inland area of China. Chemical comparison of the precipitation from TWPA with those in the Southern Indian Ocean Area (SIOA) and with those from Western Atlantic Area (WAA) demonstrated that the mean pH value, the total concentrations of anions and cations in rainwater from TWPA were the highest, followed by those from SIOA. About one thirds of the SO_4~2- Concentrations in the rainwaters from TWPA and SIOA and nearly half of the SO_4~2- in the rainwater from WAA were contributed by non-sea-salt origins, which indicates that the influences of external origins on the SO_4~2- concentrations in rainwaters from TWPA and SIOA are smaller than that in WAA.
Keywords:marine precipitation  pH  non-sea-salt    
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