Hydrogen in natural diamond: Quantification of N3VH defects using SIMS and FTIR data

IF 3.6 2区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Chemical Geology Pub Date : 2024-05-24 DOI:10.1016/j.chemgeo.2024.122185
Felix V. Kaminsky , Veniamin B. Polyakov , Boris Ya. Ber , Dmitry Yu. Kazantsev , Galina K. Khachatryan , Svetlana N. Shilobreeva
{"title":"Hydrogen in natural diamond: Quantification of N3VH defects using SIMS and FTIR data","authors":"Felix V. Kaminsky ,&nbsp;Veniamin B. Polyakov ,&nbsp;Boris Ya. Ber ,&nbsp;Dmitry Yu. Kazantsev ,&nbsp;Galina K. Khachatryan ,&nbsp;Svetlana N. Shilobreeva","doi":"10.1016/j.chemgeo.2024.122185","DOIUrl":null,"url":null,"abstract":"<div><p>A set of ten diamonds from different sources representing the main types of physical classification (IaA, IaAB, IaB and IIa) has been first explored by FTIR spectroscopy and SIMS calibrated by hydrogen ion implantation. The concentrations of hydrogen in the studied diamonds measured by SIMS range between 9.98 and 47.6 at.ppm or from 1.76 × 10<sup>18</sup> to 8.40 × 10<sup>18</sup> at./cm<sup>3</sup>. The 3107 cm<sup>−1</sup> absorption line has been detected by FTIR spectroscopy (resolution near 1 cm<sup>−1</sup>) in five studied diamonds (IaB and IaAB). The 3107 cm<sup>−1</sup> IR absorption lines due to H defects in these diamonds have been successfully described by the Lorentzian shape and their parameters have been evaluated. Based on the linear regression equation relating intensities of the 3107 cm<sup>−1</sup> IR absorption lines in the studied diamonds with their H defect concentrations, the H defect IR absorption at 3107 cm<sup>−1</sup> in diamond has been quantified. The absorption calibration constant for diamond's 3107 cm<sup>−1</sup> absorption line is 386 ± 64 ppb cm<sup>2</sup>. The corresponding cross-section per one H defect <em>σ</em><sub>3107</sub> (cm<sup>2</sup>) = (9.34 ± 1.25) × 10<sup>−18</sup> /<em>Γ</em> (cm<sup>−1</sup>), <em>Γ</em> is the full width at half maximum (FWHM) of the 3107 cm<sup>−1</sup> absorption line. Based on a widely accepted interpretation that the H defect resulting in the 3107 cm<sup>−1</sup> IR absorption peak in diamonds is the N<sub>3</sub>VH defect, the values of the obtained calibration constant and cross-section have been assigned to the N<sub>3</sub>VH defect in diamond. The equations relating concentration of the N<sub>3</sub>VH defect ([N<sub>3</sub>VH]) with the 3107 cm<sup>−1</sup> IR absorption line integrated intensity (<em>I</em><sub>3107</sub>) and intensity (<em>α</em><sub>3107</sub>) are as follows: [N<sub>3</sub>VH] (ppb) = (386 ± 64) <em>I</em><sub>3107</sub>; [N<sub>3</sub>VH] (ppm) = (0.607 ± 0.080) <em>α</em> <sub>3107</sub> (cm<sup>−1</sup>)<em>Γ</em> (cm<sup>−1</sup>). Hydrogen impurities that do not contribute to the IR absorption at the 3107 cm<sup>−1</sup> peak were detected in all studied diamonds.</p></div>","PeriodicalId":9847,"journal":{"name":"Chemical Geology","volume":null,"pages":null},"PeriodicalIF":3.6000,"publicationDate":"2024-05-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Chemical Geology","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0009254124002651","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0

Abstract

A set of ten diamonds from different sources representing the main types of physical classification (IaA, IaAB, IaB and IIa) has been first explored by FTIR spectroscopy and SIMS calibrated by hydrogen ion implantation. The concentrations of hydrogen in the studied diamonds measured by SIMS range between 9.98 and 47.6 at.ppm or from 1.76 × 1018 to 8.40 × 1018 at./cm3. The 3107 cm−1 absorption line has been detected by FTIR spectroscopy (resolution near 1 cm−1) in five studied diamonds (IaB and IaAB). The 3107 cm−1 IR absorption lines due to H defects in these diamonds have been successfully described by the Lorentzian shape and their parameters have been evaluated. Based on the linear regression equation relating intensities of the 3107 cm−1 IR absorption lines in the studied diamonds with their H defect concentrations, the H defect IR absorption at 3107 cm−1 in diamond has been quantified. The absorption calibration constant for diamond's 3107 cm−1 absorption line is 386 ± 64 ppb cm2. The corresponding cross-section per one H defect σ3107 (cm2) = (9.34 ± 1.25) × 10−18 /Γ (cm−1), Γ is the full width at half maximum (FWHM) of the 3107 cm−1 absorption line. Based on a widely accepted interpretation that the H defect resulting in the 3107 cm−1 IR absorption peak in diamonds is the N3VH defect, the values of the obtained calibration constant and cross-section have been assigned to the N3VH defect in diamond. The equations relating concentration of the N3VH defect ([N3VH]) with the 3107 cm−1 IR absorption line integrated intensity (I3107) and intensity (α3107) are as follows: [N3VH] (ppb) = (386 ± 64) I3107; [N3VH] (ppm) = (0.607 ± 0.080) α 3107 (cm−1)Γ (cm−1). Hydrogen impurities that do not contribute to the IR absorption at the 3107 cm−1 peak were detected in all studied diamonds.

Abstract Image

查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
天然金刚石中的氢:利用 SIMS 和 FTIR 数据量化 N3VH 缺陷
我们首先通过傅立叶变换红外光谱和 SIMS(通过氢离子植入进行校准)对代表主要物理分类类型(IaA、IaAB、IaB 和 IIa)的不同来源的十颗金刚石进行了研究。通过 SIMS 测量,所研究钻石中的氢浓度介于 9.98 和 47.6 at.ppm 之间,或 1.76 × 1018 至 8.40 × 1018 at./cm3 之间。通过傅立叶变换红外光谱法(分辨率接近 1 cm-1),在五颗研究的钻石(IaB 和 IaAB)中检测到了 3107 cm-1 吸收线。这些钻石中因 H 缺陷而产生的 3107 cm-1 红外吸收线已成功地用洛伦兹形状进行了描述,并对其参数进行了评估。根据所研究金刚石中 3107 cm-1 红外吸收线强度与 H 缺陷浓度之间的线性回归方程,对金刚石中 3107 cm-1 处的 H 缺陷红外吸收进行了量化。金刚石 3107 cm-1 吸收线的吸收校准常数为 386 ± 64 ppb cm2。每一个 H 缺陷对应的横截面 σ3107 (cm2) = (9.34 ± 1.25) × 10-18 /Γ (cm-1),Γ 是 3107 cm-1 吸收线的半最大全宽 (FWHM)。根据广泛接受的解释,即在金刚石中产生 3107 cm-1 红外吸收峰的 H 缺陷是 N3VH 缺陷,所获得的校准常数和横截面值被归结为金刚石中的 N3VH 缺陷。N3VH 缺陷浓度([N3VH])与 3107 cm-1 红外吸收线综合强度(I3107)和强度(α3107)的关系式如下:[N3VH](ppb)= (386 ± 64) I3107;[N3VH](ppm)= (0.607 ± 0.080) α 3107 (cm-1)Γ (cm-1)。在所有研究的钻石中都检测到了不影响 3107 cm-1 峰红外吸收的氢杂质。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
Chemical Geology
Chemical Geology 地学-地球化学与地球物理
CiteScore
7.20
自引率
10.30%
发文量
374
审稿时长
3.6 months
期刊介绍: Chemical Geology is an international journal that publishes original research papers on isotopic and elemental geochemistry, geochronology and cosmochemistry. The Journal focuses on chemical processes in igneous, metamorphic, and sedimentary petrology, low- and high-temperature aqueous solutions, biogeochemistry, the environment and cosmochemistry. Papers that are field, experimentally, or computationally based are appropriate if they are of broad international interest. The Journal generally does not publish papers that are primarily of regional or local interest, or which are primarily focused on remediation and applied geochemistry. The Journal also welcomes innovative papers dealing with significant analytical advances that are of wide interest in the community and extend significantly beyond the scope of what would be included in the methods section of a standard research paper.
期刊最新文献
Editorial Board Uptake time and enrichment mechanism of rare earth elements in deep-sea bioapatite Seawater-oceanic crust interaction constrained by triple oxygen and hydrogen isotopes in rocks from the Saglek-Hebron complex, NE Canada: Implications for moderately low-δ18O Eoarchean Ocean Editorial Board Intense intrusion of low-oxygen waters into mid-Cambrian surface ocean carbonate factories
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1