• Spectroscopy and Spectral Analysis
  • Vol. 42, Issue 8, 2325 (2022)
Jun-hang DONG1,*, Zhen-li ZHU1,1; 2; *;, Han-qing DING1,1; 2;, Peng-ju XING1,1;..., Fei-yang ZHOU1,1; 2;, Hong-tao ZHENG2,2; and Xing LIU1,1;|Show fewer author(s)
Author Affiliations
  • 11. State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
  • 22. Faculty of Materials Science and Chemistry, China University of Geosciences, Wuhan 430074, China
  • show less
    DOI: 10.3964/j.issn.1000-0593(2022)08-2325-09 Cite this Article
    Jun-hang DONG, Zhen-li ZHU, Han-qing DING, Peng-ju XING, Fei-yang ZHOU, Hong-tao ZHENG, Xing LIU. Research Progress of Isotope Analysis Method Based on Optical Spectroscopy[J]. Spectroscopy and Spectral Analysis, 2022, 42(8): 2325 Copy Citation Text show less
    233U, 235U and 238U emission spectra in the 424.37~424.45 nm wavelength regions for the certified isotopic reference material IRMM-199 containing ~0.45 mg·kg-1 each of 233U, 235U, and 238U as well as a conventional U single-element standard solution (238U and 234U) are also additionally displayed. 233U (424.398 nm), 235U (424.412 nm) and 238U (424.437 nm) can be clearly distinguished, and 234U can also be effectively identified[11]
    Fig. 1. 233U, 235U and 238U emission spectra in the 424.37~424.45 nm wavelength regions for the certified isotopic reference material IRMM-199 containing ~0.45 mg·kg-1 each of 233U, 235U, and 238U as well as a conventional U single-element standard solution (238U and 234U) are also additionally displayed. 233U (424.398 nm), 235U (424.412 nm) and 238U (424.437 nm) can be clearly distinguished, and 234U can also be effectively identified[11]
    Emission spectra of (a) atomic carbon emission line, (b) molecular isotopic band during LAMIS of carbon isotope sampleSpectrometer resolution, gate delay and width were 0.02 nm, 4 μs and 2 μs, respectively[25]
    Fig. 2. Emission spectra of (a) atomic carbon emission line, (b) molecular isotopic band during LAMIS of carbon isotope sample
    Spectrometer resolution, gate delay and width were 0.02 nm, 4 μs and 2 μs, respectively[25]
    LA-TDLAS spectra (6Li and 7Li) at delay time of 340 μs after ablation pulse[43]
    Fig. 3. LA-TDLAS spectra (6Li and 7Li) at delay time of 340 μs after ablation pulse[43]
    Z-AAS determination of (a) 198Hg, 200Hg, 201Hg, and 202Hg isotopes (symbols) and the simulation results (solid lines) and (b) mixed isotopes of 200Hg and 198Hg and the natural Hg[8]
    Fig. 4. Z-AAS determination of (a) 198Hg, 200Hg, 201Hg, and 202Hg isotopes (symbols) and the simulation results (solid lines) and (b) mixed isotopes of 200Hg and 198Hg and the natural Hg[8]
    Absorption of 14N and 15N-isotopes of N2O centered at ~2 188.688, ~2 188.756 and ~2 188.938 cm-1, respectivelyThe measured data (green points) and fitted curves (red lines) are shown in the upper trace and the residuals (blue lines) in the lower trace[52]
    Fig. 5. Absorption of 14N and 15N-isotopes of N2O centered at ~2 188.688, ~2 188.756 and ~2 188.938 cm-1, respectively
    The measured data (green points) and fitted curves (red lines) are shown in the upper trace and the residuals (blue lines) in the lower trace[52]
    Spectra of AlCl (1:1, 35Cl/37Cl molar ratio solution) at wavelengths of: (a) 261.418 nm; (b) 261.695 nm; (c) 261.819 nm; (d) 262.238 nm; (e) 262.697 nm; (f) 263.216 nm; (g) 263.807 nm; and (h) 264.490 nmThey were obtained for 400 ng of Cl, 10 mg of Al and 20 mg of Pd. However, B shows two spectraof AlCl with different isotope abundance: in black, the one obtained for 400 ng of Cl of CRM NIST 975a (35Cl, 75.774%), and in red, the one obtained for 400 ng of Cl of CRM AE642 (37Cl, 98.122%)[53]
    Fig. 6. Spectra of AlCl (1:1, 35Cl/37Cl molar ratio solution) at wavelengths of: (a) 261.418 nm; (b) 261.695 nm; (c) 261.819 nm; (d) 262.238 nm; (e) 262.697 nm; (f) 263.216 nm; (g) 263.807 nm; and (h) 264.490 nm
    They were obtained for 400 ng of Cl, 10 mg of Al and 20 mg of Pd. However, B shows two spectraof AlCl with different isotope abundance: in black, the one obtained for 400 ng of Cl of CRM NIST 975a (35Cl, 75.774%), and in red, the one obtained for 400 ng of Cl of CRM AE642 (37Cl, 98.122%)[53]
    元素同位素发射峰波长/nm激发源样品引入检测器样品类型精密度/%Ref.
    B208.957(10B)
    208.960(11B)
    ICP喷雾进样CCD溶液0.59[12]
    U411.585(233U)
    411.594(235U)
    411.610(238U)
    ICPApex ECCD溶液[20]
    U
    Pu
    424.408(234U)
    402.148(238Pu)
    ICPApex QCCD溶液0.5~2.8[10]
    U424.412 2(235U)
    424.437 3(238U)
    LIBS固体ICCD土壤6[13]
    U424.412 2(235U)
    424.4373(238U)
    LIBS固体CCDAl2O3+UF64~10[14]
    U424.412 2(235U)
    424.437 3(238U)
    LIBS气体进样ICCDUF6-[16]
    H656.28(1Hα)
    656.10(2Hα)
    LIBS固体ICCD锆合金-[19, 21]
    Li670.799(6Li)
    670.779(7Li)
    LIBS固体ICCD碳酸锂粉末6[7]
    Table 1. Isotope analysis methods for optical emission spectroscopy
    元素目标分子跃迁过程分子发射波长
    区域/nm
    同位素发射峰
    位移/nm
    样品类型精密度
    /%
    参考
    文献
    B10BO, 11BOA2ΠiX2Σ+ν=-3)579~5855~8B2O3、BN固体0.9[23, 30]
    10BO2, 11BO2A2ΠuX2Πg493.1~580.618~89.5B2O3固体-[37]
    C, N12C14N, 12C15N, 13C14NB2Σ+X2Σ+ν=+1)354~3620.6石墨,苯甲酰胺-[26]
    13C12Cd3Πgα3Πuν=+1)473.7~475.30.1~1煤、金刚石-[26]
    HDHOA2Σ+X2Πν=0)306~3101~2重水气溶胶1.5~1.8[38]
    OH/DA2Σ+X2Πν=0)306~3200.12~4.15液态水、冷冻水0.3~0.7[39]
    NH/DA3ΠiX3Σ-ν=0)335.2~337.60.33~0.72液态水、冷冻水0.3~0.7[39]
    C13CN, 12CNB2Σ+X2Σ+ν=+1)350~3610.6CO2气体、尿素-[32]
    B2Σ+X2Σ+ν=-1)410~4260.8
    Fe56FeO, 54FeOD5ΔiX5Δiν=0)586.5~591.50.09~0.30模拟核电站
    结构材料
    0.07[36]
    Table 2. Isotope analysis methods by LAMIS
    Jun-hang DONG, Zhen-li ZHU, Han-qing DING, Peng-ju XING, Fei-yang ZHOU, Hong-tao ZHENG, Xing LIU. Research Progress of Isotope Analysis Method Based on Optical Spectroscopy[J]. Spectroscopy and Spectral Analysis, 2022, 42(8): 2325
    Download Citation