Factors controlling the nitrate in the DT-401 ice core in eastern Antarctica  

作　　者：LI ChuanJin REN JiaWen QIN DaHe XIAO CunDe HOU ShuGui LI YuanSheng DING MingHu 

机构地区：[1]State Key Laboratory of Cryospheric Sciences,Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences [2]School of Geographic and Oceanographic Sciences,Nanjing University [3]Laboratory of Polar Glacial Research,Polar Research Institute of China [4]Division of Cenozoic Geology and Environment,Institute of Geology and Geophysics,Chinese Academy of Sciences

出　　处：《Science China Earth Sciences》2013年第9期1531-1539,共9页中国科学（地球科学英文版）

基　　金：supported by the Foundation for Excellent Youth Scholars of CAREERI,CAS;the National Natural Science Foundation of China(Grant Nos.40776002,40825017,41171052);the Hundred Talent Project of Chinese Academy of Sciences;the Polar Scientific Explore Organizing Committee Foundation (Grant Nos.20080202&0852H71001);State Oceanic Administration of People's Republic of China Project on Climate in Polar Regions(Grant Nos.CHINARE2012-04-04 and CHINARE2012-02-02)

摘　　要：Nitrate,an oxidized product of NO x preserved in the polar ice cores,has often been used to estimate past changes of the atmospheric nitrogen cycle.A 102.65 m ice core drilled at DT-401(79°01'S,77°00'E) in 1999 provides an opportunity to investigate the possible influencing factors for the nitrate budget in the eastern Antarctica.We studied the relationship between the δ18O(representing the temperature),accumulation rate,volcanic deposition and the astronomical factors(such as the solar activities,supernovae,etc.),and the nitrate variation along the whole duration(2680-year) of the ice core.Prominent impacts of the accumulation rate acting on the nitrate flux rather than the concentration were detected.However,no significant correlation was found between the δ18O and the nitrate deposition characteristics(concentration and the flux variations).Volcanic deposition can significantly affect the deposition of nitrate with a decreasing trend accompanied by the nss-SO42(volcanic signal) peak values.Impacts of the solar activities on the nitrate deposition can be detected at this site,and three prominent periodicities(16.6,24.0 and 102.0 yr) were found for the nitrate concentration variations.Six climatic events(Dalton Minimum,Maunder Minimum,Sporer Minimum,Wolf Minimum,Oort Minimum and Medieval Maximum) during the past 1150 years were observed with lower nitrate values for the foregoing five events and higher value for the last one.Nitrate,an oxidized product of NO x preserved in the polar ice cores,has often been used to estimate past changes of the atmospheric nitrogen cycle.A 102.65 m ice core drilled at DT-401（79°01＇S,77°00＇E） in 1999 provides an opportunity to investigate the possible influencing factors for the nitrate budget in the eastern Antarctica.We studied the relationship between the δ18O（representing the temperature）,accumulation rate,volcanic deposition and the astronomical factors（such as the solar activities,supernovae,etc.）,and the nitrate variation along the whole duration（2680-year） of the ice core.Prominent impacts of the accumulation rate acting on the nitrate flux rather than the concentration were detected.However,no significant correlation was found between the δ18O and the nitrate deposition characteristics（concentration and the flux variations）.Volcanic deposition can significantly affect the deposition of nitrate with a decreasing trend accompanied by the nss-SO42（volcanic signal） peak values.Impacts of the solar activities on the nitrate deposition can be detected at this site,and three prominent periodicities（16.6,24.0 and 102.0 yr） were found for the nitrate concentration variations.Six climatic events（Dalton Minimum,Maunder Minimum,Sporer Minimum,Wolf Minimum,Oort Minimum and Medieval Maximum） during the past 1150 years were observed with lower nitrate values for the foregoing five events and higher value for the last one.

关 键 词：Factors controlling the nitrate in the DT-401 ice core in eastern Antarctica 

分 类 号：P343.6[天文地球—水文科学] S63[天文地球—地球物理学]