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Temporal Variations Of Atmospheric Depositional Fluxes Of 7be And 210pb Over 8 Years (2006–2013) At Shanghai, China, And Synthesis Of Global Fallout Data, Juan Du, Jinzhou Du, Mark Baskaran, Qianqian Bi, Dekun Huang, Yifei Jiang

Environmental Science and Geology Faculty Research Publications

7Be and 210Pb, two atmospherically delivered radionuclides, have been broadly applied to study the processes including air mass transport, soil erosion, and particle cycling in aqueous systems. These studies require temporal variations of their depositional fluxes. In the present work, monthly atmospheric bulk depositional fluxes of 7Be and 210Pb were measured over 8 years (December 2005 to December 2013) at Shanghai, China. The bulk depositional fluxes of 7Be and 210Pb varied from 17.9 to 421 Bq m−2 month−1 and 6.8 to 82.1 Bq m−2 month−1, respectively. The volume‐weighted activities ranged from 0.20 to 8.06 Bq L−1 for 7Be and 0.05 …

Age Determination Of Recent Cave Deposits Using Excess 210Pb - A New Technique, M. Baskaran, Thomas M. Iliffe

Environmental Science and Geology Faculty Research Publications

Cave deposits have been widely used as proxy recorders in deciphering palaeoclimate during the last glacial/interglacial maxima (∼ 120 ka) [Harmon et al., 1975; Atkinson et al., 1978; Goede and Harmon, 1983; Ayliffe and Veeh, 1989]. Palaeoclimatic studies of cave deposits for the past 1–1000 yr time scale require a precise dating technique, that until now has been lacking. Due to the multiple sources of carbon in speleothems, ¹⁴C dates obtained for recently deposited calcite are highly variable and thus, ¹⁴C dating techniques are not suitable to obtain speleothem ages for the past 1–1000 years.

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