| GAO Xuelu,SONG Jinming,LI Xuegang,YUAN Huamao,LI Ning. 2005. Spatial and temporal variations in pH and total alkalinity at the beginning of the rainy season in the Changjiang Estuary, China. Acta Oceanologica Sinica, (5):68－77 |
| Spatial and temporal variations in pH and total alkalinity at the beginning of the rainy season in the Changjiang Estuary, China |
| Spatial and temporal variations in pH and total alkalinity at the beginning of the rainy season in the Changjiang Estuary, China |
| Received:March 04, 2005 Revised:July 21, 2005 |
| DOI： |
| Key words:Changjiang Estuary pH total alkalinity spatial and temporal variations |
| 中文关键词: Changjiang Estuary pH total alkalinity spatial and temporal variations |
| 基金项目: |
| Author Name | Affiliation | E-mail | | GAO Xuelu | Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
Graduate School of Chinese Academy of Sciences, Beijing 100039, China | | | SONG Jinming | Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China | jmsong@ms.qdio.ac.cn | | LI Xuegang | Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China | | | YUAN Huamao | Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China | | | LI Ning | Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
Graduate School of Chinese Academy of Sciences, Beijing 100039, China | |
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| Abstract: |
| The results of field observation carried out in May 2003 were used to examine pH and total alkalinity behaviors in the Changjiang Estuary.It was showed that pH and total alkalinity took on clear spatial variations in values with the minima in the low salinity region.Like salinity, transect distributions of pH and total alkalinity (TA) in a downriver direction had a sharp gradient each.These gradients appeared in such a sequence that the TA gradient was earlier than salinity and pH gradients, and the salinity gradient was earlier than the pH gradient.These distribution characteristics seemed to be strongly influenced by the mixing process of freshwater and seawater, for both pH and total alkalinity had significant linear relationships with salinity and temperature.For pH, phytoplankton activities also had a significant impact upon its spatial distribution.During a period of 48 h, pH and total alkalinity changed within wide ranges for every layer of the two anchor stations, namely, Stas 13 and 20, which were located at the mixed water mass and seawater mass, respectively.For both Stas 13 and 20, pH and TA fluctuation of every layer could be very wide during a 4 h period.As a whole, the data of the two anchor stations showed that neither variations in salinity and temperature nor phytoplankton activities were the main factors strongly influencing the total alkalinity temporal variability on a small time scale.The data of Sta.20 implied that both salinity variation and phytoplankton activities had a significant influence on pH temporal variability, but the same conclusion could not be drawn from the data of Sta.13. |
| 中文摘要: |
| The results of field observation carried out in May 2003 were used to examine pH and total alkalinity behaviors in the Changjiang Estuary.It was showed that pH and total alkalinity took on clear spatial variations in values with the minima in the low salinity region.Like salinity, transect distributions of pH and total alkalinity (TA) in a downriver direction had a sharp gradient each.These gradients appeared in such a sequence that the TA gradient was earlier than salinity and pH gradients, and the salinity gradient was earlier than the pH gradient.These distribution characteristics seemed to be strongly influenced by the mixing process of freshwater and seawater, for both pH and total alkalinity had significant linear relationships with salinity and temperature.For pH, phytoplankton activities also had a significant impact upon its spatial distribution.During a period of 48 h, pH and total alkalinity changed within wide ranges for every layer of the two anchor stations, namely, Stas 13 and 20, which were located at the mixed water mass and seawater mass, respectively.For both Stas 13 and 20, pH and TA fluctuation of every layer could be very wide during a 4 h period.As a whole, the data of the two anchor stations showed that neither variations in salinity and temperature nor phytoplankton activities were the main factors strongly influencing the total alkalinity temporal variability on a small time scale.The data of Sta.20 implied that both salinity variation and phytoplankton activities had a significant influence on pH temporal variability, but the same conclusion could not be drawn from the data of Sta.13. |
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