长江口溶解无机碳循环的地球化学研究
A Geochemical Study on Carbon Cycling in the Changjiang Estuary
查看参考文献15篇
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文摘
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于2005年6月对长江口23个站点的溶解性无机碳及其同位素组成进行了采样调查.结果发现长江河流区水体的 pCO_(2)均处于过饱和状态,但在进入河口区后发生大幅度的下降;δ~(13) C_(DIC)为-10.0‰~-0.9‰,且随盐度发生梯度性变化;DIC和δ~(13)C_(DIC)值偏离河水、海水混合线,显示了长江河口碳的复杂生物地球化学过程,包括内部碳酸盐岩体系及外部生物的作用:河流区主要受水-气界面CO_(2)逸散的影响;河口区主要受光合作用的影响;海岸区则主要受碳酸盐类矿物沉淀作用的影响 |
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其他语种文摘
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Water samples collected along the Changjiang River estuary in June 2005were studied for their dissolved inorganic carbon(DIC)contents and their isotopic composition. We found that CO_(2) super-saturation significantly occurred in the riverine zone and decreased sharply in the coastal zone. Theδ~(13) CDIC values are within the range of -10.0‰and-0.9‰, and vary along the salinity gradient. The deviation of observed DIC concentrations andδ~(13) CDIC from the mixing equation between riverine and marine water indicates multiple processes controlling the carbon cycling in different zones. Degassing of CO2mainly occurred in the riverine zone, photosynthesis in the estuary zone and carbonate mineral precipitation in the coastal zone |
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来源
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地球与环境
,2010,38(4):409-413 【核心库】
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关键词
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长江
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河口
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溶解无机碳
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同位素
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CO_(2)
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地址
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中国科学院地球化学研究所, 环境地球化学国家重点实验室, 贵阳, 550002
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语种
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中文 |
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文献类型
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研究性论文 |
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ISSN
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1672-9250 |
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学科
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地质学 |
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基金
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国家自然科学基金重点项目
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国家自然科学基金创新研究群体项目
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文献收藏号
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CSCD:4108309
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