Utilization of technology relevant to radiation and isotope in the archaeological research

Many kinds of scientific technology have been used in the archaeological research. Especially the methodologies relevant to radiation and isotope have contributed to archaeology, giving a lot of scientific information. Among these methodologies, the radiocarbon dating, proposed by Willard Libby, has the greatest contribution since 1950. In Japan some scientists introduced this dating method immediately after Libby's proposal. As the result, the start of the Jomon period, in which the rope pattern was applied for decoration of earthenware, was reconsidered to be about 10,000 years ago. Yoshimasa Takashima mastered this technique and did the dendrochronological study at University of Washington, Seattle, from 1960 to 1961. After that he started the radiocarbon dating in Kyushu University, Fukuoka. First he employed the proportional gas counter to measure 14C, requiring the complicated and time-consuming preparation of sample. When he restarted the radio-carbon dating with the authors in 1994 at Kyushu Environmental Evaluation Association (KEEA), he adopted the liquid scintillation counting method combined with the benzene synthesis from sample. Because this method is so convenient, many laboratories have adopted it as the conventional method in Japan. Since 1994, almost 100 samples have been treated every year in KEEA by this method. However this requires considerably much amount of sample, for example 20g in the case of wood. So that, in case of only small amount of sample can be obtained or a valuable sample is subjected to measurement, this method cannot be applicable. To resolve this problem, the accelerator mass spectrometer (AMS) has been used widely. In this method the atoms of 14C are counted directly, getting the high sensitivity and requiring very small amount of sample (order of mg). Recently, in KEEA, the radiocarbon dating using AMS was started under the cooperation with Center for Applied Isotope Studies (CAIS), University of Georgia. Another work of KEEA is the measurement of lead isotope ratios in the archaeological and environmental research. The lead isotope ratios, 207Pb/206Pb and 208Pb/206Pb, give useful information to understand the place or age in which an archaeological relic was produced. For example, as the lead isotope ratios are changeable depending on the difference of lead mine, it becomes possible to estimate the origin of relic containing lead as a component. Especially the origin of ancient bronze mirror can be estimated by this method. The lead isotope ratios are measured by ICP-MS easily. In addition, the source estimation of lead pollution in the environment can be done in the same manner. (author)