Radionuclides 14C and 129I Tracing Studies in Xi'an AMS Center
Abstract
Radionuclides 14C and 129I are good tracers for investigation of environmental change. The radiocarbon content (Δ14CO2) observations are used to trace recently added fossil fuel CO2 in the atmosphere for evaluating and constraining the CO2 emission and 129I can be used for monitoring of nuclear environmental safety. Base on newly established multi-elements 3MV AMS in the Xi'an AMS Center, 14C and 129I research for environmental change have been carried out. Here we report some new results. Air samples and annual plants were collected for fossil fuel CO2 emission in Xi'an area, China. Fossil fuel contributes 1.16%-8.36% of the CO2 concentration found in air in southeastern Xi'an City. The fossil fuel CO2 emissions reach at the largest peak at the end of March and the beginning of July. Between April and June, the emissions are lowest. Fossil fuel-derived CO2 of city center can be an order of magnitude larger than in nearby rural environments. 129I and 127I concentrations in soil, vegetation, river water and precipitation collected from Xi'an area, China are analyzed, The results indicate the mean value for environmental 129I/127I ratios in the investigated area is 2.06×10-9, which is 1-3 orders of magnitude lower than the ratios observed in Europe, but comparable with those observed in the locations far from direct effect of point release sources and at similar latitude. The result indicates Xi'an region is not directly influenced by any nuclear facilities currently and the data can be used to establish the baseline of 129I in China and to monitor 129I variation for evaluation of the effect and safe operation of the nuclear facilities in the future.
- Publication:
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AGU Fall Meeting Abstracts
- Pub Date:
- December 2011
- Bibcode:
- 2011AGUFMGC43B0906Z
- Keywords:
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- 1030 GEOCHEMISTRY / Geochemical cycles;
- 1040 GEOCHEMISTRY / Radiogenic isotope geochemistry;
- 1094 GEOCHEMISTRY / Instruments and techniques;
- 1600 GLOBAL CHANGE