引用本文:	李奕洁,宋贵生,胡素征,XIE Hui-Xiang.2014 年夏季长江口有色溶解有机物(CDOM)的分布、光学特性及其来源探究.海洋与湖沼,2015,46(3):670-678.

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2014 年夏季长江口有色溶解有机物(CDOM)的分布、光学特性及其来源探究
李奕洁,宋贵生,胡素征,XIE Hui-Xiang
1.天津科技大学海洋科学与工程学院天津 300457;2.加拿大魁北克大学里穆斯基海洋研究所魁北克里穆斯基 G5L 3A1

摘要:

通过测定有色溶解有机物(CDOM)的吸收光谱、荧光光谱、溶解有机碳(DOC)浓度, 探究了2014 年夏季长江口CDOM 的来源及河口混合行为。结合吸收系数a(355)、光谱斜率S_275-295、比紫外吸光度SUVA₂₅₄ 与盐度的关系, 结果表明南港水道受黄浦江输入影响显著, 北港水道由长江径流控制呈保守性混合行为, 二者CDOM 的物质结构性质较为相似。DOC 的浓度可通过a(275)与a(295)模拟估算: ln[DOC] = 4.94-0.87ln[a(275)] + 0.90ln[a(295)], a(275)<8.0 m^-1; ln[DOC] = 4.77-6.79ln[a(275)] + 8.05ln[a(295)], a(275)≥8.0 m^-1。模拟结果表明, 在长江口及邻近海域, CDOM 对DOC 具有示踪意义。利用三维荧光光谱-平行因子分析(EEMs-PARAFAC)技术, 可得到夏季长江口FDOM 含有3 个类腐殖质组分(C2, C4 和C5)和3 个类蛋白质组分(C1, C3 和C6)。类腐殖质组分具有相似的来源及地球化学行为, 且与a(355)及盐度存在显著相关性; 类蛋白质组分则与a(355)及盐度之间无显著相关性, 揭示其与区域内微生物的活动有关。

关键词: 有色溶解有机物溶解有机碳三维荧光-平行因子分析吸收光谱河口混合行为

DOI：10.11693/hyhz20140900251

分类号:

基金项目:陆海间碳循环关键生物地球化学过程及机理研究, 2013CB956601 号; 海洋中无色溶解有机物的光敏及生物降解的研究,41376081 号。

附件

OPTICAL CHARACTERIZATION, DISTRIBUTION AND SOURCES OF CHROMOPHORIC DISSOLVED ORGANIC MATERIAL (CDOM) IN THE CHANGJIANG RIVER ESTUARY IN JULY 2014

LI Yi-Jie¹, SONG Gui-Sheng¹, HU Su-Zheng¹, XIE Hui-Xiang^1,2,3,4,5

1.Tianjin University of Science & Technology, Tianjin 300457, China;2.Institut des sciences de la mer de Rimouski, Université3.du Qué4.bec à Rimouski, Rimouski, Qué5.bec G5L 3A1, Canada

Abstract:

Absorption and fluorescence spectroscopy, along with dissolved organic carbon (DOC) quantification, were employed to examine the sources and estuarine mixing behavior of chromophoric dissolved organic matter (CDOM) in the Changjiang River estuary in July 2014. CDOM abundance (as quantified by the absorption coefficient at 355 nm, a(355)), the absorption spectral slope over 275-295 nm (S_275-295), and the specific UV absorbance at 254 nm (SUVA₂₅₄) were all generally conservative across the freshwater-saltwater transitional zone. A localized elevation of CDOM occurred downstream in the mouth of the Huangpu River, revealing a subtle difference in the mixing pattern of CDOM between the North Port and the South Port, where as the constitutive property between the two ports was similar. DOC concentration ([DOC]) can be predicted from the CDOM absorption coefficients at 275 nm (a(275)) and 295 nm (a(295)): ln[DOC] = 4.94-0.87ln[a(275)] + 0.90ln[a(295)], a(275)<8.0 m^-1; ln[DOC] = 4.77-6.79ln[a(275)] + 8.05ln[a(295)], a(275)≥8.0 m^-1. The regression results demonstrate that CDOM absorbance could be used as the DOC tracer along the Changjiang River estuary. EEMs-PARAFAC (excitation-emission matrix fluorescence spectroscopy-parallel factor) analysis identified three humic-like components (C2, C4, and C5) and three protein-like components (C1, C3 and C6). The humic-like components possessed similar origins and correlated with a(355) and salinity. The protein-like components C1 and C6 were not significantly correlated to salinity and a(355), suggesting the protein-like components were closely related to the in situ microbial activities.

Key words: CDOM DOC EEMs-PARAFAC absorption spectra estuarine mixing behavior