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| Distribution and key influential factors of dissolved oxygen off the Changjiang River Estuary (CRE) and its adjacent waters in China | |
Chi, Lianbao1,2,3; Song, Xuxian1,2,3; Yuan, Yongquan1,2 ; Wang, Wentao1,2; Zhou, Peng1,2,3; Fan, Xin1,2,3; Cao, Xihua1,2; Yu, Zhiming1,2,3
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| 2017-12-15 | |
| Source Publication | MARINE POLLUTION BULLETIN
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| ISSN | 0025-326X |
| Volume | 125Issue:1-2Pages:440-450 |
| Corresponding Author | Song, Xuxian(songxx@qdio.ac.cn) ; Yu, Zhiming(zyu@qdio.ac.cn) |
| Abstract | Based on two multidisciplinary investigations conducted in summer and winter 2015, the distribution of dissolved oxygen (DO) and the associated seasonal variations off the Changjiang River Estuary (CRE) were studied. The DO content was high in winter, ranging from 6.81-10.29 mg/L, and the distribution was mainly controlled by temperature and salinity. The DO concentration was 1.92-9.67 mg/L in summer, and a hypoxic zone (DO < 3 mg/L) covered 14,800 km(2), which was mainly controlled by stratification and organic matter decomposition. The hypoxic zone exhibited a "dual-core" structure and the differences in the biochemical and physical processes between the southern and northern regions were compared: the northern region exhibited stronger pycnocline intensity; while larger biomass and higher TOC as well as TN contents were observed in the southern region. Hypoxia in the northern region might be mainly dominated by stratification, while that in the southern region was mainly associated with organic matter decomposition. |
| Keyword | Changjiang River Estuary Hypoxia Stratification Organic matter decomposition |
| DOI | 10.1016/j.marpolbul.2017.09.063 |
| Indexed By | SCI |
| Language | 英语 |
| Funding Project | Strategic Priority Research Program of the Chinese Academy of Sciences[XDA11020302] ; Natural Science Foundation of China-Shandong Joint Fund for Marine Science Research Centers[U1606404] ; National Key Research and Development Program[2016YFE0101500] ; AoShan Talents Cultivation Program ; Qingdao National Laboratory for Marine Science and Technology ; Strategic Priority Research Program of the Chinese Academy of Sciences[XDA11020302] ; Natural Science Foundation of China-Shandong Joint Fund for Marine Science Research Centers[U1606404] ; National Key Research and Development Program[2016YFE0101500] ; AoShan Talents Cultivation Program ; Qingdao National Laboratory for Marine Science and Technology |
| WOS Research Area | Environmental Sciences & Ecology ; Marine & Freshwater Biology |
| WOS Subject | Environmental Sciences ; Marine & Freshwater Biology |
| WOS ID | WOS:000418727000060 |
| Publisher | PERGAMON-ELSEVIER SCIENCE LTD |
| Citation statistics | |
| Document Type | 期刊论文 |
| Identifier | http://ir.qdio.ac.cn/handle/337002/157775 |
| Collection | 海洋生态与环境科学重点实验室 |
| Corresponding Author | Song, Xuxian; Yu, Zhiming |
| Affiliation | 1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China 2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China |
| First Author Affilication | Institute of Oceanology, Chinese Academy of Sciences |
| Corresponding Author Affilication | Institute of Oceanology, Chinese Academy of Sciences |
| Recommended Citation GB/T 7714 | Chi, Lianbao,Song, Xuxian,Yuan, Yongquan,et al. Distribution and key influential factors of dissolved oxygen off the Changjiang River Estuary (CRE) and its adjacent waters in China[J]. MARINE POLLUTION BULLETIN,2017,125(1-2):440-450. |
| APA | Chi, Lianbao.,Song, Xuxian.,Yuan, Yongquan.,Wang, Wentao.,Zhou, Peng.,...&Yu, Zhiming.(2017).Distribution and key influential factors of dissolved oxygen off the Changjiang River Estuary (CRE) and its adjacent waters in China.MARINE POLLUTION BULLETIN,125(1-2),440-450. |
| MLA | Chi, Lianbao,et al."Distribution and key influential factors of dissolved oxygen off the Changjiang River Estuary (CRE) and its adjacent waters in China".MARINE POLLUTION BULLETIN 125.1-2(2017):440-450. |
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