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LI Chaoli (李朝历), HE Ming(何明), ZHANG Wei (张伟), WU Shaoyong (武绍勇), LI Zhenyu (李振宇), HE Xianwen (何贤文), et al. AMS Measurement of 36Cl with a Q3D magnetic spectrometer at CIAE[J]. Plasma Science and Technology, 2012, 14(6): 543-547. DOI: 10.1088/1009-0630/14/6/25
Citation: LI Chaoli (李朝历), HE Ming(何明), ZHANG Wei (张伟), WU Shaoyong (武绍勇), LI Zhenyu (李振宇), HE Xianwen (何贤文), et al. AMS Measurement of 36Cl with a Q3D magnetic spectrometer at CIAE[J]. Plasma Science and Technology, 2012, 14(6): 543-547. DOI: 10.1088/1009-0630/14/6/25

AMS Measurement of 36Cl with a Q3D magnetic spectrometer at CIAE

  • The ratio of 36Cl/Cl can determine the exposure age of surface rocks and monitor the secular equilibrium of 36Cl of sedimentary and igneous rock in groundwater. Due to the uncertainty effects of different chemical separation processes for removing 36S, there is a high degree of uncertainty in 36Cl Accelerator Mass Spectrometry (AMS) measurements if the ratio of 36Cl/Cl is lower than 10-14 A 36Cl AMS higher sensitivity measurement has been set up by using a ΔE-Q3D method at the China Institute of Atomic Energy (CIAE). The performances of ΔE-Q3D method for 36Cl-AMS measurement had been systemically studied. The experimental results show that the ΔE-Q3D method has a higher isobar suppression factor. Taking advantage of direct removing 36S, the sample preparation can be simplified and the uncertainty effects of different chemical separation processes can be reduced in 36Cl AMS measurements.
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