AMS radiocarbon measurements were started at Peking University in 1992
with a modified HICONEX 834 ion source. Some archaeological samples w
ere measured at a sensitivity of 10(-14) with ca. 1.7% precision for m
odern samples. We have made many improvements in our first two years o
f operation: a high-intensity Cs sputtering ion source was installed;
the graphite sample preparation technique was investigated; and the sy
stem stability has been improved. The blank sample background is curre
ntly ca. 0.006 MC and a precision within 1% can be reached for modern
samples. Geological, archaeological, environmental and biomedical samp
les can be measured routinely. We present some typical applications.