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AbstractAbstract
[en] Studies have been completed that have demonstrated that there are two mechanisms for the neutralization of 218Po+ ions formed by the decay of 222Rn. In the presence of oxygen, an oxide species is formed. It has been determined as part of the present work that this oxide species has an ionization potential in the range of 10.35 to 10.53 eV and that it can be neutralized by extracting electrons from lower ionization potential trace gases. It has also been found that a second mechanism is responsible for neutralization in the absence of oxygen. The behavior of NO2 in the range of 50 ppB to 1 ppM in N2 was explored. For NO2 concentrations above 700 ppB, complete neutralization was observed. For lower concentrations, a concentration dependent degree of neutralization was observed. Studies are now being initiated to examine the kinetics of these neutralization processes. 27 references, 3 figures, 4 tables
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Source
Mar 1984; 24 p; Available from NTIS, PC A02/MF A01 as DE84009145
Record Type
Report
Literature Type
Progress Report
Report Number
Country of publication
ALPHA DECAY RADIOISOTOPES, ATOMIC IONS, BETA DECAY RADIOISOTOPES, BETA-MINUS DECAY RADIOISOTOPES, CHALCOGENIDES, CHARGED PARTICLES, CHEMISTRY, DAYS LIVING RADIOISOTOPES, DECAY, ENVIRONMENTAL TRANSPORT, EVEN-EVEN NUCLEI, HEAVY NUCLEI, IONS, ISOTOPES, KINETICS, MASS TRANSFER, MINUTES LIVING RADIOISOTOPES, NITROGEN COMPOUNDS, NITROGEN OXIDES, NUCLEAR DECAY, NUCLEI, OXIDES, OXYGEN COMPOUNDS, POLONIUM COMPOUNDS, POLONIUM ISOTOPES, RADIOISOTOPES, RADON ISOTOPES
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