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《Geochimica》 2004-06
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Stable carbon and nitrogen isotopes in the Wudinghe drainage basin

CAI De-ling 1,2 ,LI Hong-yan 3 ,ZHOU Wei-jian 1 ,LIU Wei-guo 1 ,CAO Yun-ning 1 1.State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment,Chinese Academy of Sciences,Xi ' an710075,China;2.First Institute of Oceanography,St ate Oceanic Administration,Qingdao266061,China;3.College of Chemistry and Chemical Engineerring,Ocean University of Chi na,Qingdao266003,China Correspondence should be addressed to CAI De-ling(E-mail:caidl@public.qd.sd.cn)Received October 29,2003;revised April 2,2004;accepted June 15,2004;published November,2004  
Biogenic elements(mainly carbon and nitrogen)and various pollutants in rivers undergo very complex environmental biogeochemical proc esses,such as transportation,and t ransformation,causing different e cological effects.It has an important scientific and practical significance to op en out their environmental behavior and to elucidate their distribution featu re on a district scale.An investigation of carbon and nitrogen isotope compositions in the Wudinghe drainage basin,whic h is a high turbid distributary in the middle reach of the Yellow River,was conducted.It is found that the values of stable carbon and nitrogen isoto pes of plants in the basin have wide ra nges,the carbon isotope values show bimod al characteristics,but nitrogen is otopes have no relativity to carbon o nes.A weak negative relativity exists between stable carbon and nitrogen isotopes in sediments along the river.St able carbon and nitrogen isotope values i n the suspended matter exhibit a good negative correlation,reflecting t he two main sources of suspended matter in t his river and conservative feature o f physical mixture.Based on the investigation of carbon stable isotopes of plants,soils and sediments f rom the Wudinghe drainage area,the contribution of C 3 plants to riverine particulate organic matter may be calculated to be 75%～80%.The dominating source of suspended orga nic matter in freshwater is eroded ma terial from land around the middle an d lower reaches.It also reflects the i sotopic characteristics of vegetation in this drainage basin,which is t hat the contribution from C 3 plants is predominant.The primary r esults of the investigation have pro ven that the naturally existing carbon and nitrogen isotop ic tracers should be very efficient means in studying the relationship of transportation fluxes of biogenic e lements in rivers with the precipita tion and runoff processes,as well as the relation of riverine substance to changes in t he terrestrial ecosystem environme nts.
【Fund】： 中国科学院地球环境研究所黄土与第四纪地质国家重点实验室开放基金项目(SKLLQG0002)
【CateGory Index】： P595
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