MEASUREMENT OF THE ^(36)Ar(n, p)^(36)Cl CROSS SECTION  

作　　者：蒋崧生 T. K. HEMMICK P. W. KUBIK D. ELMORE H. E. GOVE S. TULLUI T. Z. HOSSAIN 

机构地区：[1]Institute of Atomic Energy, P. O. Box 275(49), Beijing 102413, PRC [2]Nuclear Structure Research Laboratory, University of Rochester, Rochester, N Y 14627 , USA [3]Analytical Technology Division, Research Laboratories, Eastman Kodak Company, Rochester, N Y 14650 , USA

出　　处：《Chinese Science Bulletin》1990年第4期346-347,共2页

基　　金：Supported by the University of Rochester

摘　　要：The measurement of ³⁶Cl in the nature is of importance in geoscience. The ³⁶Cl reaction induced by cosmicray neutrons in the atmosphere has been considered as a significant source for the formation of ³⁶Cl. In 1968, Onufriev calculated the fallout rate of ³⁶

关 键 词：GEOSCIENCE neutron MAGNITUDE quartz BUFFALO irradiated BLANK filled COULOMB cadmium 

分 类 号：N[自然科学总论]