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引用本文:高学鲁,宋金明,李学刚,李 宁,袁华茂.长江口及杭州湾邻近海域夏季表层海水中的溶解无机碳[J].海洋科学,2008,32(4):61-67.
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长江口及杭州湾邻近海域夏季表层海水中的溶解无机碳
高学鲁1,2, 宋金明1, 李学刚1, 李 宁1, 袁华茂1
1.中国科学院海洋研究所海洋生态与环境科学重点实验室;2.中国科学院南海海洋研究所热带海洋环境动力学重点实验室
摘要:
根据2004年8月在长江口、杭州湾附近海域获得的调查资料对表层水中pH值、总碱度和溶解无机碳的分布特征及其与环境参数的关系进行了研究,并由此得到了溶解无机碳的组成情况。结果表明, HCO-3、CO2-3和CO2(T)占溶解无机碳浓度百分比分别为80.33%~97.75%、0.61 %~19.42%和0.25%~2.34% ,平均值分别为(93.28±3.68)%、(5.58±4.03)%和(1.14±0.43)%。水文、浮游植物等对各参数的分布具有重要影响,但对不同参数的影响程度不同。
关键词:  溶解无机碳  空间分布特征  影响因素  长江口及杭州湾邻近海域
DOI:
分类号:
基金项目:国家973 计划资助项目(2005CB407305) ;中国科学院百人计划资助项目(科人20032202) ;青岛市科技将才专项计划资助项目(04-3-JJ-03 ,05-2-JC-90)
Dissolved inorganic carbon in surface waters around the Changjiang Estuary and Hangzhou Bay in summer
Abstract:
Based on the data collected from the area around the Changjiang Estuary and Hangzhou Bay during the field observation carried out on August 2004, concentration, distribution and composition of dissolved inorganic carbon and two related parameters, namely pH and total alkalinity, in their surface waters were examined in this paper. On the whole, the concentration distributions of DIC, HCO-3 and CO2(T)decreased latitudinally from west to east, while those of pH and CO2-3 were reverse. HCO-3 accounted for 80.33 % to 97.75% of the DIC with an average of (93.28 ±3.68)%; CO2-3 accounted for 0.61% to 19.42% of the DIC with an average of (5.58±4.03)%; CO2(T) accounted for 0.25% to 2.34% of the DIC with an average of (1.14±0.43)%. The integration of many factors including the interaction among different water masses, phytoplankton activities and so on influenced on the spatial distribution characteristics of these parameters, while the degree of influence on these parameters varied greatly from one to another for a certain influence factor.
Key words:  dissolved inorganic carbon  spatial distribution  controlling factors  Changjiang Estuary and Hangzhou Bay adjacent areas
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