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2篇 您的检索式:作者名="F.C.Tan"
    题名 作者 年代 出处 被引量
1长江口区有机碳同位素地球化学显示文摘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。蔡德陵 F.C.Tan J.M.Edmond 1992地球化学1992,21,3:33
2Sources and transport of particulate organic carbon in the Amazon River and its estuary显示文摘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 δ 13C values(--24.5‰ to -- 28.0‰) than that in the middle and lower reaches (--27.9‰ to -- 30.1‰). Theδ 13C of POC from the tributaries is generally more negative than that observed in the Amazon mainchannel. This δ 13C 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 δ 13C values (--17.5‰ to -28.4‰) is observed in the Amazon Estuary and plume. and is considered as the result of theCai Deling F.C.Tan J.M.Edmond 1989Acta Oceanologica Sinica1989,8,4:1
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