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利用拉曼光谱法对氮同位素比率进行精确评估。

Precision evaluation of nitrogen isotope ratios by Raman spectrometry.

作者信息

Yamamoto Junji, Hagiwara Yuuki

机构信息

Department of Earth and Planetary Sciences, Graduate School of Science Kyushu University Nishi-ku Japan.

Graduate School of Science Hokkaido University Kita-ku Japan.

出版信息

Anal Sci Adv. 2022 Oct 17;3(9-10):269-277. doi: 10.1002/ansa.202200020. eCollection 2022 Oct.

DOI:10.1002/ansa.202200020
PMID:38716263
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC10989615/
Abstract

We measured Raman spectra of N fluids obtained at 0.1-25 MPa at room temperature. The NN peak in the Raman spectrum of a low-pressure N fluid is difficult to detect because of the prevalence of a group of peaks attributed to rotational vibration of N. The Raman peaks of NN and N of N fluid at 25 MPa were acquired at various exposure times. The mean values and standard deviations of the peak height ratios and peak area ones of NN and N were examined for each time. The standard deviations of the peak height ratios and peak area ones were 2.2% and 1.9%, respectively, for 20 spectra acquired with peak height of 1 million counts of N. The uncertainties are about two times higher than those predicted from the noise of a CCD. Improvement of the pixel resolution can enhance the precision of the nitrogen isotope ratios by Raman spectroscopy.

摘要

我们测量了在室温下0.1 - 25兆帕压力下获得的N流体的拉曼光谱。由于存在一组归因于N的旋转振动的峰,低压N流体拉曼光谱中的NN峰很难检测到。在25兆帕压力下,N流体的NN和N的拉曼峰是在不同的曝光时间下采集的。每次都检查了NN和N的峰高比和峰面积比的平均值和标准偏差。对于以N的峰高为100万计数采集的20个光谱,峰高比和峰面积比的标准偏差分别为2.2%和1.9%。这些不确定性比根据电荷耦合器件(CCD)的噪声预测的结果高出约两倍。像素分辨率的提高可以通过拉曼光谱增强氮同位素比的精度。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a2a/10989615/614260bc3bf9/ANSA-3-269-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a2a/10989615/a2098dc5e3e8/ANSA-3-269-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a2a/10989615/474a055fb9e2/ANSA-3-269-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a2a/10989615/482c424c96f9/ANSA-3-269-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a2a/10989615/9d9f20184c44/ANSA-3-269-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a2a/10989615/a69c5739d6ba/ANSA-3-269-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a2a/10989615/f3556cbc292f/ANSA-3-269-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a2a/10989615/614260bc3bf9/ANSA-3-269-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a2a/10989615/a2098dc5e3e8/ANSA-3-269-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a2a/10989615/474a055fb9e2/ANSA-3-269-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a2a/10989615/482c424c96f9/ANSA-3-269-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a2a/10989615/9d9f20184c44/ANSA-3-269-g007.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a2a/10989615/a69c5739d6ba/ANSA-3-269-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a2a/10989615/f3556cbc292f/ANSA-3-269-g006.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9a2a/10989615/614260bc3bf9/ANSA-3-269-g002.jpg

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Fiber-Enhanced Raman Gas Spectroscopy for O-C-Labeling Experiments.纤维增强拉曼气体光谱学在 O-C 标记实验中的应用。
Anal Chem. 2019 Jun 18;91(12):7562-7569. doi: 10.1021/acs.analchem.8b05684. Epub 2019 May 3.
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Sci Rep. 2018 Apr 4;8(1):5662. doi: 10.1038/s41598-018-22227-7.
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Opt Express. 2014 Nov 17;22(23):27833-44. doi: 10.1364/OE.22.027833.
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Mantle wedge infiltrated with saline fluids from dehydration and decarbonation of subducting slab.地幔楔被脱水和俯冲板块脱碳产生的盐水流体渗透。
Proc Natl Acad Sci U S A. 2013 Jun 11;110(24):9663-8. doi: 10.1073/pnas.1302040110. Epub 2013 May 28.
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