An automatic peak deconvolution method for Raman spectra of terrestrial carbonaceous material for application to the geothermometers of Kouketsu et al. (2014)

IF 1 4区 地球科学 Q4 GEOSCIENCES, MULTIDISCIPLINARY
Island Arc Pub Date : 2022-10-19 DOI:10.1111/iar.12467
Shunya Kaneki, Yui Kouketsu
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Abstract

Carbonaceous material undergoes changes in its maturity mainly in response to its thermal history. Among the various geothermometers based on Raman spectra of carbonaceous material, those proposed by Kouketsu et al. (2014) have been employed to investigate the temperatures experienced by terrestrial rocks that undergo low- to medium-grade metamorphism. Although their geothermometers use spectral parameters that can be determined only by peak deconvolution, criteria for setting the initial conditions for nonlinear least-squares fitting have not been specified, which may generate unnecessary errors in the estimated temperatures owing to differences in fitting results among data analysts. To address this issue, we developed a code that automatically calculates the parameters required for the geothermometers of Kouketsu et al. (2014); that is, the widths of the D1- and D2-bands. Our code yields parameter values consistent with those of Kouketsu et al. (2014) for the same Raman data and is applicable to datasets other than those used to develop it. The geothermometers based on the obtained results show a comparable performance to Kouketsu et al. (2014). Errors in the estimated temperatures caused by variation in Raman systems and the subjective selection of the fitting method are smaller than the uncertainties of the geothermometer itself, so long as the temperature is calculated by following the procedures of the present study. Although this study focused only on geothermometers that require peak deconvolution, the development of those based on fitting-free Raman parameters and on the reaction kinetics of carbonaceous material should be investigated in future studies.

Abstract Image

陆地碳质物质拉曼光谱峰自动反褶积方法在Kouketsu等(2014)地温计中的应用
碳质物质成熟度的变化主要是对其热历史的响应。在各种基于碳质物质拉曼光谱的地温计中,Kouketsu et al.(2014)提出的地温计被用于研究经历中低变质作用的陆相岩石所经历的温度。虽然他们的地温计使用的光谱参数只能通过峰反褶积确定,但没有规定非线性最小二乘拟合初始条件的设置标准,这可能会由于数据分析人员之间拟合结果的差异而在估计温度中产生不必要的误差。为了解决这个问题,我们开发了一个代码,可以自动计算Kouketsu等人(2014)的地温计所需的参数;即D1和d2波段的宽度。对于相同的拉曼数据,我们的代码产生的参数值与Kouketsu等人(2014)的参数值一致,并且适用于用于开发它的数据集以外的数据集。基于所得结果的地温计显示出与Kouketsu等人(2014)相当的性能。只要按照本研究的程序计算温度,由拉曼系统的变化和拟合方法的主观选择引起的温度估计误差小于地温计本身的不确定性。虽然本研究只关注需要峰反褶积的地温计,但基于无拟合拉曼参数和碳质物质反应动力学的地温计的发展应该在未来的研究中进行研究。
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来源期刊
Island Arc
Island Arc 地学-地球科学综合
CiteScore
2.90
自引率
26.70%
发文量
32
审稿时长
>12 weeks
期刊介绍: Island Arc is the official journal of the Geological Society of Japan. This journal focuses on the structure, dynamics and evolution of convergent plate boundaries, including trenches, volcanic arcs, subducting plates, and both accretionary and collisional orogens in modern and ancient settings. The Journal also opens to other key geological processes and features of broad interest such as oceanic basins, mid-ocean ridges, hot spots, continental cratons, and their surfaces and roots. Papers that discuss the interaction between solid earth, atmosphere, and bodies of water are also welcome. Articles of immediate importance to other researchers, either by virtue of their new data, results or ideas are given priority publication. Island Arc publishes peer-reviewed articles and reviews. Original scientific articles, of a maximum length of 15 printed pages, are published promptly with a standard publication time from submission of 3 months. All articles are peer reviewed by at least two research experts in the field of the submitted paper.
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