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长江口区有机碳同位素地球化学 被引量:34
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作者 蔡德陵 f.c.tan J.M.Edmond 《地球化学》 CAS CSCD 北大核心 1992年第3期305-312,共8页
本文将有机碳稳定同位素方法用于研究长江口和东海中的颗粒有机碳的来源和运移。洪水期中采集的颗粒有机碳的δ^(13)C范围为—25.4——19.7×10^(-3),这说明在河口区中河流有机碳与海洋有机碳的混合作用。枯水期样品δ^(13)C值的范... 本文将有机碳稳定同位素方法用于研究长江口和东海中的颗粒有机碳的来源和运移。洪水期中采集的颗粒有机碳的δ^(13)C范围为—25.4——19.7×10^(-3),这说明在河口区中河流有机碳与海洋有机碳的混合作用。枯水期样品δ^(13)C值的范围是—26.6——23.7×10^(-3),表明陆源有机碳占优势。东海陆架区沉积有机碳的δ^(13)C值呈现出一个较窄的数值范围(—22.9——20.8×10^(-3)),说明它们主要是海洋性来源。 展开更多
关键词 石炭 同位素 地球化学
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Sources and transport of particulate organic carbon in the Amazon River and its estuary 被引量:2
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作者 Cai Deling f.c.tan J.M.Edmond 《Acta Oceanologica Sinica》 SCIE CAS CSCD 1989年第4期601-601,共1页
Stable carbon isotope ratios have been used to study the sources of particulate organic carbon(POC) in the Amazon River and its tributaries, and to examine the transport of the riverine POC intothe oceanic environment... Stable carbon isotope ratios have been used to study the sources of particulate organic carbon(POC) in the Amazon River and its tributaries, and to examine the transport of the riverine POC intothe oceanic environment. POC in the upper reaches of the Amazon River has more positive δC values(--24.5‰ to -- 28.0‰) than that in the middle and lower reaches (--27.9‰ to -- 30.1‰). TheδC of POC from the tributaries is generally more negative than that observed in the Amazon mainchannel. This δC datum shows that the POC in the Amazon main channel is predominantly of terres-trial origin rather than a result of in situ production. A large range of δC values (--17.5‰ to -28.4‰) is observed in the Amazon Estuary and plume. and is considered as the result of the mixing 展开更多
关键词 Sources and transport of particulate organic carbon in the Amazon River and its estuary
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