ABSTRACT. Actinide isotopes are present in environmental samples at ultra-trace levels ( 236 U concentration is quoted to be on the order of pg/kg or fg/kg). Their detection requires the resolution of mass spectrometry (MS) techniques, but only accelerator mass spectrometry (AMS) has the sensitivity required. In order to perform the isotopic ratio measurements of actinides, such as 236 U/ 238 U, an upgrade of the Center for Isotopic Research on Cultural and Environmental Heritage accelerator (CIRCE) in Caserta, Italy, has been performed. The system was originally equipped for radiocarbon AMS measurements. The main difficulty of AMS measurement of 236 U is the intense neighboring beam of 238 U. Although most of the 238 U ions are suppressed by means of magnetic and electrostatic elements, a small fraction of this intense beam can interfere with the rare isotopes. This paper reports the preliminary results of the 236 U/ 238 U isotopic ratio measurement limit (<5.6 × 10 11 ), aimed also to better understand the origin of background ions. For this purpose, a large 16-strip silicon detector providing spatial resolution has been used. In addition, calculations to assess the performance of the system obtained by adding a high-resolution time of flight-energy (TOF-E) detector are discussed.
INTRODUCTIONThe processing of material for nuclear power plants (NPPs) and nuclear weapons (NW) together with all the activities correlated with production, transport, and reprocessing of nuclear fuel, has led to the release of a wide range of radioactive elements in the environment, such as uranium, plutonium, and fission and activation products. Since the relative concentrations of uranium and plutonium can vary from site to site, depending on the nature of the source material and on its subsequent irradiation history, all these sources do not contribute equally to the contamination in a given site. The long-lived radionuclide 236 U (the half-life of 236 U is 2.3 × 10 7 yr) is present in environmental samples at ultra-trace levels. Measurement of these isotopic ratios requires mass spectrometric techniques, but only AMS offers the sensitivity needed to measure 236 U/ 238 U at natural levels (10 9 to 10 13 ) because of its capability to suppress the background of isobaric molecules such as 235 UH .Conventional mass spectrometry, like thermal ionization (TI-MS) or inductively coupled plasma mass spectrometry (ICP-MS), suffers from isobaric interferences of hydrides, 235 UH , and from 238 U; the detection limits of these techniques for 236 U/ 238 U are 10 10 and 10 7 , respectively. Recently, increasing attention is being paid to the determination of 236 U/ 238 U at the level typically present in the environment (Fifield 2008;Quinto et al. 2009;Sakaguchi et al. 2009); these studies have demonstrated the potential of 236 U to serve as a tracer for geomorphologic processes and as sensitive fingerprints of releases from nuclear facilities.In nature, U stable abundant isotopes exist. For this reason, the sensitivity limit for the i...