Distributions of dimethylsulfide and its related compounds in the Yangtze (Changjiang) River Estuary and its adjacent waters in early summer

被引:16
作者
Tan, Ting-Ting [1 ,3 ]
Wu, Xi [1 ,3 ]
Liu, Chun-Ying [1 ,2 ,3 ]
Yang, Gui-Peng [1 ,2 ,3 ]
机构
[1] Minist Educ, Key Lab Marine Chem Theory & Technol, Qingdao 266100, Peoples R China
[2] Qingdao Natl Lab Marine Sci & Technol, Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China
[3] Ocean Univ China, Coll Chem & Chem Engn, 238 Songling Rd, Qingdao 266100, Peoples R China
基金
中国国家自然科学基金;
关键词
Dimethylsulfide (DMS); Dimethylsulfoniopropionate (DMSP); Acrylic acid (AA); Yangtze (Changjiang) River Estuary; Distribution; Flux; EAST CHINA SEA; DIMETHYLSULFONIOPROPIONATE DMSP; ACRYLIC-ACID; SURFACE MICROLAYER; YELLOW SEA; DISSOLVED DIMETHYLSULFONIOPROPIONATE; PHOTOCHEMICAL TRANSFORMATION; SPATIAL VARIATIONS; SUBSURFACE WATER; COASTAL WATERS;
D O I
10.1016/j.csr.2017.08.012
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Dimethylsulfide (DMS) is an important and dominant sulfur compound that is transferred from the ocean to the atmosphere. In this study, the spatiotemporal variations in DMS concentrations and its two closely related compounds, namely, dimethylsulfoniopropionate (DMSP) and acrylic acid (AA), were investigated in the Yangtze (Changjiang) River Estuary and its adjacent waters, where the salinity changed dramatically in June 2014. The concentration ranges (average values) of DMS, DMSP, and AA were 1.10-27.5 (8.53), 5.93-195 (40.1), and 4.2-122.6 (17.9) nmol L-1 in the surface waters, respectively. The DMS and DMSP concentrations were higher in the study area than in its neighboring regions because of the high levels of nutrients originating in the Yangtze and Qiantang Rivers. However, the AA concentration was lower in the study area. Although no significant correlations were found between DMS, DMSP, or AA and salinity, high concentrations of DMS, AA, and DMSP were recorded between the salinity levels of 26 parts per thousand and 31 parts per thousand. DMS and AA concentrations were positively correlated with chlorophyll a. The average AA/(DMSP + AA) and DMS/(DMSP + AA) ratios were 36.9% and 17.1%, respectively. The vertical profiles of DMSP and DMS presented similar variation patterns, and high concentrations of both compounds were mostly detected in the surface waters. By contrast, AA showed a different variation pattern compared with those of DMSP and DMS because AA could have other potential sources. The low average sea-to-air flux of DMS (that is, 6.55 mu mol m(-2) d(-1)) was mainly attributed to the low wind speed in early summer.
引用
收藏
页码:89 / 101
页数:13
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