摘要
测试了南极阿德雷岛两个湖泊 (Y2和G)沉积物的2 10 Pb和137Cs比度 .根据2 10 Pb和137Cs比度垂向变化特征 ,采用CRS模式对G湖进行了定年 ,年龄跨度大约为 134± 43年 ,并据此计算了G湖的沉积速率 .近大约 10 0年来G湖呈增长变化的沉积速率以及沉积物2 10 Pb ,137Cs蓄积量和沉降通量远大于大气直接沉降 ,可能是温度升高引起该地区大量冰雪 (盖 )融水携带补充的结果 .
The activity of 210 Pb and 137 Cs of lake sediments, namely Y2 and G, respectively from Ardley Island, Antarctica have been measured. According to the profiles of 210 Pb and 137 Cs activity, we used CRS model to date the G lake, which spans about 134±43 years. Base on the dating, we estimate the velocity of deposition. The increased sedimentation rates and the inventories of 210 Pb and 137 Cs as well as their flux being higher than the atmospheric deposition could be reasonably attributed to the supply of a great amount of ice melt water.
出处
《湖泊科学》
EI
CAS
CSCD
2001年第1期93-96,共4页
Journal of Lake Sciences
基金
国家自然科学基金! (4 0 0 76 0 32 )
中国科学院创新项目! (KZCX2 - 30 3)联合资助
