海气CO_2通量的溶解无机碳δ^(13)C值示踪研究进展  

PROGRESS IN AIR-SEA FLUXES OF CARBON DIOXIDE TRACED BY DISSOLVED INORGANIC CARBON STABLE

作　　者：刘启明[1] 林锦美[1] 张金丽[1] 黄志勇[1] 鲁中明[2] 

机构地区：[1]集美大学生物工程学院,福建厦门361021 [2]厦门大学近海海洋环境科学国家重点实验室,福建厦门361005

出　　处：《海洋湖沼通报》2008年第3期53-60,共8页Transactions of Oceanology and Limnology

基　　金：国家自然科学基金(40406023;40771185);福建省自然科学基金(D0710021)联合资助

摘　　要：海洋是地球表面上碳的重要贮存库,是全球碳循环系统的一个重要子系统,国际上研究海气间CO2交换调控机制的工作长期以来倍受关注。文章简要阐述海气CO2通量研究概况和对海水溶解无机碳δ13CDIC指标的地球化学特征的分析基础上,综述海气CO2通量的溶解无机碳稳定同位素示踪研究进展,并对该方法存在问题和研究发展趋势作了分析与展望。The isotopic composition of dissolved inorganic carbon （DIC） in marine and estuarine environments has been studied in some detail because of its role in determining the isotopic composition of inorganic/organic matter and its applications to the study of various natural processes. The δ^13CDIC values in sea waters is controlled by the sources and sinks of carbon and results from isotope fractionation both between solid, dissolved and gaseous phases. In this paper, based on the analysis of the stable isotopes geochemical characteristics of dissolved inorganic carbon, we intended to review and synthesize the recent advances in Air-sea Fluxes of Carbon Dioxide traced by stable carbon isotopes.

关 键 词：海气交换 CO2 溶解无机碳 稳定碳同位素 

分 类 号：P734.2[天文地球—海洋化学]