基于太赫兹谱的同位素分析

IF 1.4 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Acta Geochimica Pub Date : 2023-06-21 DOI:10.1007/s11631-023-00622-w
Qijun Chen, Yun Liu
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引用次数: 0

摘要

太赫兹时域光谱(THz-TDS)作为太赫兹研究领域中一种新的有前景的检测技术,由于其在感兴趣物质的特征光谱、宽光谱和无损分析方面的优势,在许多领域具有非常广泛的应用潜力。本文首次用太赫兹时域光谱法测量了12CO和13CO混合气体在0.5–2.5 THz光谱范围内的太赫兹吸收光谱。根据它们的旋转能和由此产生的太赫兹光谱的差异,可以清楚地区分几种同位素。实验结果表明,由于旋转能的差异,12CO和13CO在0.5–2.5 THz的光谱范围内具有明显的特征吸收峰,根据实验值可以计算旋转常数B来区分这两种气体的同位素结构。将本实验测得的特征吸收峰的频率位置和根据实验值计算出的旋转常数B与以往的理论计算和实验结果进行了比较,结果吻合良好。这一结果为开发更复杂的太赫兹仪器来检测不同的同位素奠定了基础。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

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Isotopic analysis based on terahertz spectrum

As a new promising detection technology in the terahertz research field, the terahertz time-domain spectroscopy (THz-TDS) has very broad application potential in many fields because its advantage on the characteristic spectrum, wide spectrum and non-destructive analysis of interested substances. In this paper, the terahertz absorption spectra of gases mixed with 12CO and 13CO in the spectrum range of 0.5–2.5 THz are measured by terahertz time-domain spectroscopy for the first time. Several isotopologues can be clearly distinguished based on the difference in their rotational energies and the consequent terahertz spectrum. The experimental results show that 12CO and 13CO have obvious characteristic absorption peaks in the spectrum range of 0.5–2.5 THz due to the difference in rotational energy, and the rotational constant B can be calculated according to the experimental values to distinguish the two gaseous isotopologues. The frequency positions of the characteristic absorption peak measured by this experiment and the rotation constant B calculated according to the experimental values are compared with those previous theoretical calculations and experimental results, and they are in good agreement. This result lays a foundation for developing more sophisticated terahertz instruments to the detection of different isotopologues.

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来源期刊
Acta Geochimica
Acta Geochimica GEOCHEMISTRY & GEOPHYSICS-
CiteScore
2.80
自引率
6.20%
发文量
1134
期刊介绍: Acta Geochimica serves as the international forum for essential research on geochemistry, the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems such as the Earth‘s crust, its oceans and the entire Solar System, as well as a number of processes including mantle convection, the formation of planets and the origins of granite and basalt. The journal focuses on, but is not limited to the following aspects: • Cosmochemistry • Mantle Geochemistry • Ore-deposit Geochemistry • Organic Geochemistry • Environmental Geochemistry • Computational Geochemistry • Isotope Geochemistry • NanoGeochemistry All research articles published in this journal have undergone rigorous peer review. In addition to original research articles, Acta Geochimica publishes reviews and short communications, aiming to rapidly disseminate the research results of timely interest, and comprehensive reviews of emerging topics in all the areas of geochemistry.
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