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长江口溶解有机物光漂白和光矿化表观量子产率

孙欣 宋贵生 Xie Huixiang

孙欣, 宋贵生, Xie Huixiang. 长江口溶解有机物光漂白和光矿化表观量子产率[J]. 海洋学报, 2016, 38(4): 120-129. doi: 10.3969/j.issn.0253-4193.2016.04.011
引用本文: 孙欣, 宋贵生, Xie Huixiang. 长江口溶解有机物光漂白和光矿化表观量子产率[J]. 海洋学报, 2016, 38(4): 120-129. doi: 10.3969/j.issn.0253-4193.2016.04.011
Sun Xin, Song Guisheng, Xie Huixiang. The apparent quantum yields of dissolved organic matter photobleaching and photomineralization in the Changjiang River Estuary[J]. Haiyang Xuebao, 2016, 38(4): 120-129. doi: 10.3969/j.issn.0253-4193.2016.04.011
Citation: Sun Xin, Song Guisheng, Xie Huixiang. The apparent quantum yields of dissolved organic matter photobleaching and photomineralization in the Changjiang River Estuary[J]. Haiyang Xuebao, 2016, 38(4): 120-129. doi: 10.3969/j.issn.0253-4193.2016.04.011

长江口溶解有机物光漂白和光矿化表观量子产率

doi: 10.3969/j.issn.0253-4193.2016.04.011
基金项目: 国家自然科学基金——海洋中无色溶解有机物的光敏及生物降解的研究(41376081);国家重大科学研究计划973计划子课题——陆海间碳循环关键生物地球化学过程及机理研究(2013CB956601)。

The apparent quantum yields of dissolved organic matter photobleaching and photomineralization in the Changjiang River Estuary

  • 摘要: 溶解有机物(DOM)经太阳光照射导致其吸光度(光漂白)和溶解有机碳(光矿化)损失,从而影响水体生态系统光学特性及碳循环。本文通过测定冬季长江口及其邻近海域DOM光降解表观量子产率(AQY),初步探讨了DOM光反应活性在河口及陆架海的变化特征。DOM光降解AQY由口内至口外逐渐递减,且有色溶解有机物(CDOM)光漂白速率是溶解有机碳(DOC)光矿化速率的10倍。Φble(CDOM光漂白表观量子产率)和Φmin(DOC光矿化平均量子产率)在最大浑浊带以东海域与盐度和SUVA254分别呈显著的线性负相关与正相关,表明DOM光反应活性在长江口外受物理混合影响为主,且陆源DOM光反应活性比海源高。此外,最大浑浊带下游DOM光降解AQY显著低于上游。DOM光降解速率随波长的变化呈现非高斯分布,且峰值出现在330 nm,积分结果表明UVA是DOM光降解的主要贡献者。本研究结果将为完善我国东海碳通量模型提供帮助。
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  • 收稿日期:  2015-11-03
  • 修回日期:  2015-12-24

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