摘要

Loess is the most important and the most typical continental classic sediments of Quaternary. So the measurement of In-situ produced cosmogenic Be-10 is expected to be used for the Loess stratigraphic age. But the production rate of In-situ produced cosmogenic Be-10, in Loess quartz is very low. It requires very high sensitivity and accuracy of measurement. This work has measured the concentrations of Be-10 of two layers in Loess section of Luochuan including L8, L9 and the concentrations of Be-10 in (of) blank sample with the HI-13 AMS system at China Insitute of Atomic Energy(CIAE), then calculated the content of Be-10 in loess quartz for each layer. The ratio of Be-10/Be-9 was found in the range of 10(-13). The background of Be-10/Be-9 was about 3x10(-14).