The ^10Be/^7Be ratio is a sensitive tracer for the study of atmospheric transport, particularly with regard to stratosphere-troposphere exchange. Measurements with high accuracy and efficiency are crucial to ^7Be and ...The ^10Be/^7Be ratio is a sensitive tracer for the study of atmospheric transport, particularly with regard to stratosphere-troposphere exchange. Measurements with high accuracy and efficiency are crucial to ^7Be and ^10Be tracer studies. This article describes sample preparation procedures and analytical benchmarks for ^7Be and ^10Be measurements at the Xi＇an Accelerator Mass Spectrometry（Xi＇an-AMS） laboratory for the study of rainwater samples. We describe a sample preparation procedure to fabricate beryllium oxide（Be O） AMS targets that includes co-precipitation, anion exchange column separation and purification. We then provide details for the AMS measurement of ^7Be and ^10Be following the sequence BeO^-→Be^2＋→Be^4＋ in the Xi＇an- AMS. The ^10Be/^7Be ratio of rainwater collected in Xi＇an is shown to be about 1.3 at the time of rainfall. The virtue of the method described here is that both ^7Be and ^10Be are measured in the same sample, and it is suitable for routine analysis of large numbers of rainwater samples by AMS.展开更多
The rare isotope ^236U has a half-life of 2.342（3）×107 years, and is produced principally by thermal neutron capture on ^235U. The isotopic atom ratio of ^236U/^238U depends on the integral thermal neutron flux...The rare isotope ^236U has a half-life of 2.342（3）×107 years, and is produced principally by thermal neutron capture on ^235U. The isotopic atom ratio of ^236U/^238U depends on the integral thermal neutron flux received by the material of interest. ^236U is potentially useful as a ＂fingerprint＂ for indicating the presence of neutron-irradiated uranium usually originating from nuclear activity. By extracting negative molecular ion UO^- from the uranium oxide target, simulating the ^236U^16O^- beam transport with ^238U^16O^- and ^208Pb2^16O^- pilot molecular ion beam, transporting the ^236U-containing ion beam with a high resolution injection magnet analyzer and electrostatic analyzer system, and finally identifying and detecting ^236U with a time-of-flight detector （TOF）, a method for AMS （Accelerator Mass Spectrometry） measurement of ^236U was established on the HI-13 Accelerator AMS system at China Institute of Atomic Energy.展开更多
In the present study, the analytical method for ^129iodine （^129I） in ferromanganese crusts is developed and ^129iodine/^127iodine （^129I/^127I） ratio in ferromanganese crusts is measured by the accelerator mass s...In the present study, the analytical method for ^129iodine （^129I） in ferromanganese crusts is developed and ^129iodine/^127iodine （^129I/^127I） ratio in ferromanganese crusts is measured by the accelerator mass spectrometry （AMS）. The developed method is applied to analyze ^129I/^127I ratio in two ferromanganese crusts MP5D44 and CXD08-1 collected from the Mid-Pacific Ocean. The results show that ^129I/^127I ratio in MP5D44 and CXD08-1 crusts varies from 7×10^-14 to 1.27×10^-12, with the lowest value falling on the detection limit level of AMS reported by previous literatures. For the depth distribution of ^129I/^127I, it is found that both MP5D44 and CXD08-1 crusts have two growth generations, and the ^129I/^127I profiles in two generations all displayed an approximate exponential decay. According to the ^129I/^127I ratio, the generate age of bottom layer of MP5D44 and CXD08-1 was estimated to be 54.77 and 69.69 Ma, respectively.展开更多
Background The deep-sea ferromanganese crust(DSFC)is a natural archive for recording the history of the Earth’s evolution,as one of the most common authigenic assemblages in marine sediments.Although the depositional...Background The deep-sea ferromanganese crust(DSFC)is a natural archive for recording the history of the Earth’s evolution,as one of the most common authigenic assemblages in marine sediments.Although the depositional age dating using meteoric ^(10)Be has been successfully used in the study on the chronology of DSFC,the research on ^(26)Al has not seen relevant reports in this aspect due to the influence of factors such as measurement sensitivity and ^(26)Al in situ production.Method The first exploration for ^(26)Al chronology in DSFC was carried out by using accelerator mass spectrometry(AMS)measurements of ^(10)Be and ^(26)Al,and the comparison of relationship between isotopic ratios and concentrations of Al and Be.Results The growth rates of G.R=(1.44±0.09)mm/Ma,(3.58±0.29)mm/Ma,(1.52±0.10)mm/Ma and(2.93±0.14)mm/Ma are derived using ^(10)Be/^(9)Be,^(26)Al/^(27)Al ratios,^(10)Be and ^(26)Al concentrations,respectively.Conclusion The ^(26)Al chronological methods have been explored based on a DSFC sample and encouraging results were obtained.The results are preliminary and insufficient;some information is still needed to explain the difference between ^(26)Al and ^(10)Be chronology.展开更多
基金Supported by National Natural Science Foundation of China(11205161)CAS Key Technology Talent Program
文摘The ^10Be/^7Be ratio is a sensitive tracer for the study of atmospheric transport, particularly with regard to stratosphere-troposphere exchange. Measurements with high accuracy and efficiency are crucial to ^7Be and ^10Be tracer studies. This article describes sample preparation procedures and analytical benchmarks for ^7Be and ^10Be measurements at the Xi＇an Accelerator Mass Spectrometry（Xi＇an-AMS） laboratory for the study of rainwater samples. We describe a sample preparation procedure to fabricate beryllium oxide（Be O） AMS targets that includes co-precipitation, anion exchange column separation and purification. We then provide details for the AMS measurement of ^7Be and ^10Be following the sequence BeO^-→Be^2＋→Be^4＋ in the Xi＇an- AMS. The ^10Be/^7Be ratio of rainwater collected in Xi＇an is shown to be about 1.3 at the time of rainfall. The virtue of the method described here is that both ^7Be and ^10Be are measured in the same sample, and it is suitable for routine analysis of large numbers of rainwater samples by AMS.
基金Supported by NSAF (National Nature Science Fundation-China Academy of Engineering Physics Fundation) (10576040)
文摘The rare isotope ^236U has a half-life of 2.342（3）×107 years, and is produced principally by thermal neutron capture on ^235U. The isotopic atom ratio of ^236U/^238U depends on the integral thermal neutron flux received by the material of interest. ^236U is potentially useful as a ＂fingerprint＂ for indicating the presence of neutron-irradiated uranium usually originating from nuclear activity. By extracting negative molecular ion UO^- from the uranium oxide target, simulating the ^236U^16O^- beam transport with ^238U^16O^- and ^208Pb2^16O^- pilot molecular ion beam, transporting the ^236U-containing ion beam with a high resolution injection magnet analyzer and electrostatic analyzer system, and finally identifying and detecting ^236U with a time-of-flight detector （TOF）, a method for AMS （Accelerator Mass Spectrometry） measurement of ^236U was established on the HI-13 Accelerator AMS system at China Institute of Atomic Energy.
基金The National Natural Science Foundation of China under contract No.41073044
文摘In the present study, the analytical method for ^129iodine （^129I） in ferromanganese crusts is developed and ^129iodine/^127iodine （^129I/^127I） ratio in ferromanganese crusts is measured by the accelerator mass spectrometry （AMS）. The developed method is applied to analyze ^129I/^127I ratio in two ferromanganese crusts MP5D44 and CXD08-1 collected from the Mid-Pacific Ocean. The results show that ^129I/^127I ratio in MP5D44 and CXD08-1 crusts varies from 7×10^-14 to 1.27×10^-12, with the lowest value falling on the detection limit level of AMS reported by previous literatures. For the depth distribution of ^129I/^127I, it is found that both MP5D44 and CXD08-1 crusts have two growth generations, and the ^129I/^127I profiles in two generations all displayed an approximate exponential decay. According to the ^129I/^127I ratio, the generate age of bottom layer of MP5D44 and CXD08-1 was estimated to be 54.77 and 69.69 Ma, respectively.
基金National Natural Science Foundation of China,11775157,Kejun Dong.
文摘Background The deep-sea ferromanganese crust(DSFC)is a natural archive for recording the history of the Earth’s evolution,as one of the most common authigenic assemblages in marine sediments.Although the depositional age dating using meteoric ^(10)Be has been successfully used in the study on the chronology of DSFC,the research on ^(26)Al has not seen relevant reports in this aspect due to the influence of factors such as measurement sensitivity and ^(26)Al in situ production.Method The first exploration for ^(26)Al chronology in DSFC was carried out by using accelerator mass spectrometry(AMS)measurements of ^(10)Be and ^(26)Al,and the comparison of relationship between isotopic ratios and concentrations of Al and Be.Results The growth rates of G.R=(1.44±0.09)mm/Ma,(3.58±0.29)mm/Ma,(1.52±0.10)mm/Ma and(2.93±0.14)mm/Ma are derived using ^(10)Be/^(9)Be,^(26)Al/^(27)Al ratios,^(10)Be and ^(26)Al concentrations,respectively.Conclusion The ^(26)Al chronological methods have been explored based on a DSFC sample and encouraging results were obtained.The results are preliminary and insufficient;some information is still needed to explain the difference between ^(26)Al and ^(10)Be chronology.
