Ⅰ. INTRODUCTIONThe <sup>36</sup>Ar(n,p)<sup>36</sup>Cl reaction is of importance to the study of the origin of <sup>36</sup>Cl nuclei in the nature. The natural <sup>36<...Ⅰ. INTRODUCTIONThe <sup>36</sup>Ar(n,p)<sup>36</sup>Cl reaction is of importance to the study of the origin of <sup>36</sup>Cl nuclei in the nature. The natural <sup>36</sup>Cl (half-life : 3.01 x 10<sup>5</sup> a) as a geochrometer and a long-lived radioisotope tracer has its potential applications in geoscience. The origin of <sup>36</sup>Cl in the nature is a basic question in the geological studies with <sup>36</sup>Cl. In recent literature, two展开更多
基金Project supported by the National Natural Science Foundation of China.
文摘Ⅰ. INTRODUCTIONThe <sup>36</sup>Ar(n,p)<sup>36</sup>Cl reaction is of importance to the study of the origin of <sup>36</sup>Cl nuclei in the nature. The natural <sup>36</sup>Cl (half-life : 3.01 x 10<sup>5</sup> a) as a geochrometer and a long-lived radioisotope tracer has its potential applications in geoscience. The origin of <sup>36</sup>Cl in the nature is a basic question in the geological studies with <sup>36</sup>Cl. In recent literature, two