目的建立基于^(87)Sr/^(86)Sr和δ^(13)C稳定同位素比质谱法(stable isotope ratio mass spectrometry,IRMS)的进口大麦产地溯源技术。方法样品干燥粉碎后,经硝酸消解,锶特效树脂净化后利用热电离质谱法(thermal ionization mass spectr...目的建立基于^(87)Sr/^(86)Sr和δ^(13)C稳定同位素比质谱法(stable isotope ratio mass spectrometry,IRMS)的进口大麦产地溯源技术。方法样品干燥粉碎后,经硝酸消解,锶特效树脂净化后利用热电离质谱法(thermal ionization mass spectrometry,TIMS)分析检测^(87)Sr/^(86);样品用锡囊包裹后,利用元素分析-稳定同位素比质谱法分析检测δ^(13)C;利用SPSS 25.0软件对进口大麦的^(87)Sr/^(86)Sr和δ^(13)C进行正态性验证、方差分析、事后多重比较分析和判别分析。结果不同进口国大麦中的^(87)Sr/^(86)Sr和δ^(13)C具有显著性差异,经判别分析,进口自澳大利亚、法国和美国的大麦可以达到100%正确判别率,整体正确判别率达到86.2%,若将美国和加拿大进口的大麦归类为北美洲进口大麦,则可实现进口自北美、法国和澳大利亚大麦的100%正确判别率。结论利用^(87)Sr/^(86)Sr和δ^(13)C可以对不同进口国大麦进行产地溯源分析。展开更多
Infrared signal detection is widely used in many fields.Due to the detection principle,however,the accuracy and range of detection are limited.Thanks to the ultra stability of the^(87)Sr optical lattice clock,external...Infrared signal detection is widely used in many fields.Due to the detection principle,however,the accuracy and range of detection are limited.Thanks to the ultra stability of the^(87)Sr optical lattice clock,external infrared electromagnetic wave disturbances can be responded to.Utilizing the ac Stark shift of the clock transition,we propose a new method to detect infrared signals.According to our calculations,the theoretical detection accuracy in the vicinity of its resonance band of 2.6μm can reach the order of 10-14W,while the minimum detectable signal of common detectors is on the order of 10^(-10)W.展开更多
To analyze the genesis of Sr isotopes in groundwater of Hebei plain, time-accumulative effect of ^87Sr/^86Sr ratio was studied. It is shown that ^87Sr/^86Sr ratio increases with the increasing age and depth of groundw...To analyze the genesis of Sr isotopes in groundwater of Hebei plain, time-accumulative effect of ^87Sr/^86Sr ratio was studied. It is shown that ^87Sr/^86Sr ratio increases with the increasing age and depth of groundwater and has a positive correlation to 4Heexc and a negative correlation to δ^18O and δD.The groundwater is divided into three groups to discuss the relation between ^87Sr/^86Sr ratio and Sr^2+ content: ① moderate Sr^2+ content and higher ^87Sr/^86Sr ratio (water Ⅰ); ② lower Sr^2+ content and higher ^87Sr/^86Sr ratio (water Ⅱ); and ③ higher Sr^2+ content and lower ^87Sr/^86Sr ratio (water Ⅲ), that is hot water. On the basis of integrated analysis, it was considered that ① the radiogenic Sr in the Quaternary groundwater (Q4-Q1) originates from weathering of silicate rich in Na and Rb, mainly from plagioclase; ② the radiogenic Sr of hot water in Huanghua port is attributed to carbonate dissolution, with lower ^87Sr/^86Sr ratio and higher Sr/Na ratio; ③ the recharge area is laterally recharged by the groundwater flowing through igneous and metamorphic rocks, with moderate ^87Sr/^86Sr ratio. However, the formation mechanism of Sr isotopes in Tertiary groundwater needs further studies.展开更多
文摘目的建立基于^(87)Sr/^(86)Sr和δ^(13)C稳定同位素比质谱法(stable isotope ratio mass spectrometry,IRMS)的进口大麦产地溯源技术。方法样品干燥粉碎后,经硝酸消解,锶特效树脂净化后利用热电离质谱法(thermal ionization mass spectrometry,TIMS)分析检测^(87)Sr/^(86);样品用锡囊包裹后,利用元素分析-稳定同位素比质谱法分析检测δ^(13)C;利用SPSS 25.0软件对进口大麦的^(87)Sr/^(86)Sr和δ^(13)C进行正态性验证、方差分析、事后多重比较分析和判别分析。结果不同进口国大麦中的^(87)Sr/^(86)Sr和δ^(13)C具有显著性差异,经判别分析,进口自澳大利亚、法国和美国的大麦可以达到100%正确判别率,整体正确判别率达到86.2%,若将美国和加拿大进口的大麦归类为北美洲进口大麦,则可实现进口自北美、法国和澳大利亚大麦的100%正确判别率。结论利用^(87)Sr/^(86)Sr和δ^(13)C可以对不同进口国大麦进行产地溯源分析。
基金Project supported by the National Natural Science Foundation of China (Grant No.12274045)。
文摘Infrared signal detection is widely used in many fields.Due to the detection principle,however,the accuracy and range of detection are limited.Thanks to the ultra stability of the^(87)Sr optical lattice clock,external infrared electromagnetic wave disturbances can be responded to.Utilizing the ac Stark shift of the clock transition,we propose a new method to detect infrared signals.According to our calculations,the theoretical detection accuracy in the vicinity of its resonance band of 2.6μm can reach the order of 10-14W,while the minimum detectable signal of common detectors is on the order of 10^(-10)W.
基金This paper is supported by China Geological Survey Project (No. 200320150002).
文摘To analyze the genesis of Sr isotopes in groundwater of Hebei plain, time-accumulative effect of ^87Sr/^86Sr ratio was studied. It is shown that ^87Sr/^86Sr ratio increases with the increasing age and depth of groundwater and has a positive correlation to 4Heexc and a negative correlation to δ^18O and δD.The groundwater is divided into three groups to discuss the relation between ^87Sr/^86Sr ratio and Sr^2+ content: ① moderate Sr^2+ content and higher ^87Sr/^86Sr ratio (water Ⅰ); ② lower Sr^2+ content and higher ^87Sr/^86Sr ratio (water Ⅱ); and ③ higher Sr^2+ content and lower ^87Sr/^86Sr ratio (water Ⅲ), that is hot water. On the basis of integrated analysis, it was considered that ① the radiogenic Sr in the Quaternary groundwater (Q4-Q1) originates from weathering of silicate rich in Na and Rb, mainly from plagioclase; ② the radiogenic Sr of hot water in Huanghua port is attributed to carbonate dissolution, with lower ^87Sr/^86Sr ratio and higher Sr/Na ratio; ③ the recharge area is laterally recharged by the groundwater flowing through igneous and metamorphic rocks, with moderate ^87Sr/^86Sr ratio. However, the formation mechanism of Sr isotopes in Tertiary groundwater needs further studies.