Abstract
Raman spectroscopy is a powerful method for determining the densities of gas species in fluid inclusions, especially for H2-bearing inclusions in which the microthermometry approach is difficult to apply. The relationships between Raman peak position and H2 density have been recorded in several previous studies. However, systematic discrepancies exist among these studies. In this study, the Raman spectral parameters (peak position, width, and intensity) of the vibrational bands of H2 (Q1(0), Q1(1), Q1(2), and Q1(3)) were systematically measured at temperatures from 25 to 400 °C and pressures up to 150 MPa using a high-pressure optical cell. The variation in each parameter as a function of H2 density was discussed. Several calibration polynomials derived from the measured peak positions and peak widths of these vibrational bands and the peak intensity ratios of Q1(1) to Q1(n = 0, 2, 3) were established to determine H2 densities up to 0.062 g/cm3 at 25 °C. For natural fluid inclusions, the peak position of the Q1(1) band is the best choice for density determination mainly because (i) Raman spectra derived from fluid inclusions are not always of applicable qualities and the strongest intensity Q1(1) band could be obtained easier than others, and (ii) the peak position is insensitive to instrumental factors. The relationship between the peak position of Q1(1) band and density can be represented by ΔQ1(1) = 90,246.070 × ρ4 – 5471.203 × ρ3 + 770.944 × ρ2– 41.038 × ρ (r2 = 0.999), where ρ is the density of H2 in g/cm3; ΔQ1(1) (cm–1) is the difference between the obtained peak position of Q1(1) band of H2 and the known peak position of Q1(1) band of H2 at near-zero density. This polynomial is independent of instrumental factors and can be applied in any laboratory, as long as the peak position of H2 with a near-zero density is known. The effects of temperature on the relationship between these spectral parameters and H2 density were also examined.

Introduction
Hydrogen is an important component in many geological environments, and its major sources are usually supposed to involve biological and abiotic processes. The mechanisms for biological processes mainly include organic matter fermentation and anaerobic oxidation of carbon monoxide,1,2 and those for abiotic processes consist of mantle degassing,3,4 radiolysis,5–8 the serpentinization reaction,9,10 the low‐temperature reactions associated with active fault movements,11,12 and basaltic magma crystallization.13,14 Although the appearances of H2 in fluid or melt inclusions are rarely reported, H2-bearing inclusions have been found in many geological environments, including igneous rocks,15,16 uranium deposits,17–19 high‐grade metamorphic rocks,20,21 fault planes, 22 and hydrothermal environments.23,24 Among these, H2-rich fluids are commonly found in uranium deposits5,6,17,18 and hydrothermal environments.25,26 In addition, hydrogen has also been found in experiments that simulated the water–rock interaction and redox reactions in natural hydrothermal environments. 27 H2 fluid in the earth system plays an important role, and its origin and evolution have attracted more and more attention because of its value to chemosynthetic life and to our understanding of the redox state, and its influence on geochemical evolution.28–30
Determining densities of H2 in the H2-bearing fluid inclusions is important for knowing the physicochemical state and related processes that take place in geological environments. However, the microthermometric analysis of H2-bearing fluids has long been hampered owing to the extremely low temperature of the triple point of H2 (–259.2 °C), which prevents freezing H2 with the frequently used coolant, liquid N2. 31 The limitation makes the laser Raman spectroscopy currently the only reliable tool for studying H2‐bearing inclusions.16,31
Raman parameters, such as peak position and peak width, can be used to determine the properties of H2-containing gases. May et al.32–35 reported the first Raman characteristics of gaseous, liquid, and solid H2 at temperatures (T) from 85 to 300 K and pressures (P) up to 200 MPa. Bischel and Dyer 36 measured the temperature and density dependence of the Raman peak position and peak width of H2 at temperatures from 77 to 480 K and pressures up to 3.4 MPa. Rahn et al. 37 reported the self-broadening coefficients of H2 Q(0–5) Raman transitions from 295 to 1000 K and 0.2–5 MPa. Li et al. 38 studied the density and temperature dependences of the peak position and peak width of hydrogen vibrational Raman bands from 50 to 400 °C and 5–40 MPa. Fang et al. 31 presented the Raman peak position, peak width, peak height, and peak area of the vibrational bands of H2 and CH4 in pure H2, CH4 gases, and their mixtures at room temperature and pressures up to 40 MPa. Although these reports have documented density-dependent variations in the Raman spectra of H2, the relationship between Raman peak position of vibrational bands (Q1(0), Q1(1), Q1(2), and Q1(3)) and H2 density at room temperature has not been investigated systematically. The results of May et al. 32 and Fang et al. 31 show that different laboratories have their calibration curves for this Raman shift–density relationship, and so cannot be used in other laboratories.
In this study, using a high‐pressure optical cell (HPOC), 39,40 we systematically collected Raman spectra of pure H2 at temperatures from 25 to 400 °C and pressures up to 150 MPa. The relationship between the Raman parameter (peak position, peak width, and peak intensity ratio) and H2 density was established, and the applicability of these spectral parameters was evaluated. The effects of temperature on the relationships were also discussed.
Experimental Method
Apparatus and Procedures
An HPOC was used in this study for the Raman spectroscopic analyses of pure H2 in isothermal or isobaric experiments, and the apparatus and procedures are similar to those described previously in detail.31,41 The HPOC is a capillary tube (200 μm inner diameter, 665 μm outer diameter, and ∼25 cm length), which can be connected to a high-pressure system. The pressure was maintained by a pump (HiP # 37-5.75-60) using water as the pressure medium and was monitored from an Omega PX91N0-35KSV digital pressure transducer (241 MPa full scale, accurate to ±0.5% of full scale) with an Omega DP41-8-230 manometer. A Linkam CAP500 heating–cooling stage, with the accuracy of ±0.1 °C from 0 to 100 °C and ±0.5 °C for temperatures near 400 °C, 42 was used for temperature control. Raman spectra were collected at various pressures and temperatures, and the measured pressures and temperatures were used to calculate H2 density based on the equation of state of H2 formulated by Leachman et al. 43 from the National Institute of Standards and Technology (NIST) Chemistry WebBook (https://webbook.nist.gov/chemistry/).
Collection and Calibration of Raman Spectra
The Raman vibrational bands of H2 were obtained on a JY/Horiba LabRAM HR Evolution Raman system equipped with a frequency-doubled neodymium-doped yttrium aluminum garnet (Nd:YAG) laser (532 nm) excitation whose output laser power is approximately 14 mW, a 50× long-work-distance Olympus objective with 0.35 numerical aperture, and an 1800 groove/mm grating with a spectral resolution of about 0.65 cm−1. Three spectra were collected at each P–T condition, and each spectrum was collected with two accumulations.
The spectral resolution can be promoted to 0.03 cm−1 using a curve fitting technique.44,45 Therefore, the measured spectra for H2 were fitted by the program PeakFit v.4.12 (AISN Software Inc.) using a summed Gaussian–Lorentz function, which is the best fit function for vibrational bands of H2 with the highest R
2
greater than 0.99 for each spectrum. The peak position and full width at half‐maximum (FWHM) were determined using the program PeakFit v.4.12, whereas peak intensities for H2 were derived from integration using GRAMS AI software (Galactic Industries). Note that here, peak intensity is in terms of the integrated intensity of the peak, not the integrated area. The separation between the Ne lines at 3907.37 cm−1 and 4363.75 cm−1 was used to calibrate the peak positions of H2. The real Raman peak positions (υreal) of the vibrational bands of H2 were obtained from the following relationship:
46
Results and Discussion
In this study, only the four vibrational bands of H2 (Q1(0), Q1(1), Q1(2), and Q1(3)) were systematically investigated because the pure rotational lines of H2 (from approximately 350 to 1050 cm−1) are usually hindered by the stronger Si–O bands of silicate host minerals (from approximately 300 to 1200 cm−1) when analyzing natural fluid inclusions. 31 Both Q1(0) and Q1(2) and Q1(1) and Q1(3) correspond to the vibrational Raman bands of para‐hydrogen and ortho‐hydrogen, respectively. 38 Figure S1 (Supplemental Material) shows the four vibrational bands (Q1(0), Q1(1), Q1(2), and Q1(3)) of H2 at 25 °C and pressures up to 150 MPa.
Variation in the H2 Peak Position and the Equations for H2 Density Calculations
Figure 1 shows the peak positions of the vibrational (Q1(0), Q1(1), Q1(2), and Q1(3)) bands of H2 as a function of density near room temperature based on May et al.,
32
Fang et al.,
31
and this study. Interestingly, the peak positions of the four vibrational bands behave similarly: their wavenumbers decrease first and then increase with increasing gas density. This likeness in behavior indicates that the observed perturbation is due primarily to the variation in vibrational frequency.
32
The initial decrease in the frequency with density is associated with the predominance of intermolecular attractive forces in this range, whereas the later increase must be ascribed to repulsive forces at high densities.
34
The minimum peak positions for Q1(0), Q1(2), and Q1(3) correspond to the density of ∼ 0.0205 g/cm3 (at 30 MPa), whereas the minimum peak position for Q1(1) corresponds to the density of ∼ 0.033 g/cm3 (at 55 MPa) (Table S1, Supplemental Material). Peak positions of the four vibrational bands of H2 from three available data sets as a function of density at near room temperature. Uncertainties of peak positions of the four vibrational bands (±0.02 cm–1) are smaller than the data dot size.
As shown in Fig. 1, the Raman shifts–density relationships of the three data sets are almost parallel to each other at room temperature, revealing that systematic difference among these data sets can be eliminated by following the method described for the CH4 system.47–49 Here, ΔQ1, instead of the peak position of H2, was used as a variable to remove the systematic differences among different Raman laboratories (Fig. 2), where ΔQ1 = υρ–υ0, the difference between the peak positions of H2 at elevated densities (or pressures) (υρ) and a near-zero density (or at near 1 atm P) (υ0). The peak positions of Q1 (n = 0, 1, 2, 3) bands of H2 with near-zero density (or near 1 atm P) and experimental temperatures for our study, May et al.
32
and Fang et al.
31
are listed in Table I. Noting that the study of Fang et al.
31
was done in our laboratory about three years ago, and the υ0 has a discrepancy of 0.29 cm–1 from this study. Relationship between ΔQ1 (n = 0, 1, 2, 3) and density from this study compared with previous works, where ΔQ1 (n = 0, 1, 2, 3) = υρ–υ0, the difference between the peak positions at elevated density (υρ) and near-zero density (υ0). The dotted curves are the least squares fit of our data (Eq. 2 and Table II). Peak positions of Q1(n = 0, 1, 2, 3) bands of H2 with a near-zero density (or near 1 atm P) (υ0) and experimental temperatures.
Temperature-dependent coefficients (a, b, c, and d) and correlation coefficient (r) of the Raman wavenumber for Q1(n) according to Eq. 2.
Variation in the H2 Peak Width and the Equations for H2 Density Calculations
The peak width values of the Q1 (n = 0, 1, 2, 3) bands of H2 are represented by the FWHM. The Doppler effect and collisional broadening play substantial roles in controlling the FWHM as the density increases.36,37 At very low pressures, the Doppler effect dominates, and the collisional effect can be neglected. With increasing pressure, collisional broadening plays the dominant role in the FWHM changes as the density varies. According to the diffusion model,
36
the relationship between the FWHM and density can be expressed by the simple equation:
Fitting parameters for the Q1(n = 0, 1, 2, 3) band of H2 according to Eq. 4.

Relationship between ΔQFWHM of the four vibrational bands of H2 and density. ΔQFWHM represents the difference between the FWHM at increasing densities and 0.0016 g/cm3 (2 MPa) in cm–1. The dotted lines are least squares fits of our data (Eq. 4 and Table III). Uncertainties of FWHM of the four vibrational bands (±0.01 cm–1) are smaller than the data dot size.
Variation in Peak Intensity Ratios and the Equations for H2 Density Calculations
The Raman peak positions and FWHM values of Q1 (n = 0, 1, 2, 3) bands of H2, both of which are sensitive to density, have been reported as density indicators.32–38 However, Fang et al. 31 found that in H2‐dominated fluids with mixed CH4, the peak intensity ratios of the Q1(1) band to Q1(3) band are sensitive to pressure and insensitive to composition, indicating that the relative peak intensity of Q1(1) and Q1(3) of H2 is a better alternative for pressure determination. In this study, the peak intensity ratios of the Q1(1) band to Q1(n = 0, 2, 3) bands were investigated. Over the entire density range from 0 to 0.0623 g/cm3, the peak intensity ratios are from 5.55 to 16.73 for Q1(1)/Q1(0), 5.63 to 7.48 for Q1(1)/Q1(2), and 7.19 to 14.13 for Q1(1)/Q1(3), corresponding to the variation in the peak intensity ratios with 11.18 for Q1(1)/Q1(0), 1.85 for Q1(1)/Q1(2), and 6.94 for Q1(1)/Q1(3) (Table S3, Supplemental Material). Therefore, the effect of density on the peak intensity ratios of Q1(1) to Q1(2) is small compared to those of Q1(1) to Q1(0) and Q1(1) to Q1(3). The differences in the peak intensity ratios of Q1(1) to Q1(0) and Q1(1) to Q1(2) are very small at low density (<0.01 g/cm3) and then increase with density.
The relationship between the peak intensity ratios and density obtained in this study can be expressed as the following equation (Fig. 4): Relationship between ΔPIR (Q1(1)/Q1(n = 0, 2, 3)) and density. ΔPIR (Q1(1)/Q1(n = 0, 2, 3)) represents the difference between the peak intensity ratios at elevated densities and near-zero density. The solid lines are least squares fits of our data (Eq. 5 and Table IV). Uncertainties of ΔPIR (Q1(1)/Q1(n = 0, 2, 3)) (±0.1) are smaller than the data dot size. Fitting parameters according to Eq. 5.
Error Analysis
The accuracy of the H2 density derived from Raman parameters (peak position, peak width, and peak intensity ratio) of vibrational bands of H2 with Eqs. 2, 4, and 5 are primarily affected by Eq. 1, the accuracy of the measured Raman spectral parameters of H2 and Eq. 2 the accuracy of the calculated values using Eqs. 2, 4, and 5. To realize the maximum accuracy, a high-resolution grating and a narrow slit were used during the measurement, and the spectra were collected with a single spectral window. Additionally, each spectrum had two accumulations. The vibrational bands of H2 were collected three times at each density and their average value was presented as the measured value. The uncertainties of spectral parameters (peak position, peak width, and peak intensity ratio) are estimated based on the standard deviation of the three consecutive measurements of spectra at each density (Tables S1, S2, and S3, Supplemental Material). In addition, peak positions and peak widths were obtained by fitting the summed Gaussian–Lorentzian curve for each H2 Raman spectrum and corrected with two neon emission lines. The fitting curve was found to be the best fit curve for the H2 peak in this study with the highest r2 greater than 0.99 for each spectrum. Therefore, the maximum uncertainty of H2 peak positions coming from the peak position fitting (±0.01 cm–1) and calibration (±0.01 cm–1) is estimated to be about ±0.02 cm–1, the uncertainty of H2 peak widths resulting from peak fitting is about ±0.01 cm–1, and the error of peak intensity ratio arising from integration is about 0.1.
The uncertainty of the H2 density derived from Eq. 2 can be estimated by using the following relations:
49
As shown in Fig. 5, the accuracy of density was drawn with increasing density in the range of 0∼0.062 g/cm3. The error of H2 density derived from measured peak position with Eq. 2 is quite small in the range of 0∼0.011 g/cm3 and 0.035∼0.062 g/cm3 for Q1(0) band, 0∼0.020 g/cm3 and 0.043∼0.062 g/cm3 for Q1(1) band, 0∼0.008 g/cm3 and 0.031∼0.062 g/cm3 for Q1(2) band, and 0∼0.008 g/cm3 and 0.031∼0.062 g/cm3 for Q1(3) band, respectively. However, out of these ranges, the error is quite large, and the accuracy of H2 density obtained from Eq. 2 is much lower (Fig. 5a). Fortunately, the error of H2 density determined with measured peak width is pretty small (<0.0007 g/cm3) for four vibrational bands of H2, especially for the Q1(3) band (<0.0003 g/cm3) (Fig. 5b). The error of H2 density obtained with measured peak intensity ratio is relatively small, mainly the Q1(1)/ Q1(0) at densities higher than 0.023 g/cm3 and the Q1(1)/ Q1(3) at densities lower than 0.023 g/cm3 (Fig. 5c). The error of H2 density determined with measured (a) Raman shift, (b) peak width, and (c) peak intensity ratio, drawn with the density of H2, with the uncertainty of the H2 peak position of 0.02 cm–1, peak width of 0.01 cm–1, and peak intensity ratio of 0.1.
To test the reliability of the calibration polynomials derived from the measured Raman spectral parameters (peak position, peak width, and peak intensity ratio) for H2 density determination, several samples were prepared in the HPOC with known densities of 0.00910∼0.03173 g/cm3. The calculated ρ values from measured peak position, peak width, and peak intensity ratio, according to Eqs. 2, 4, and 5, are listed in Table S4 (Supplemental Material), and they agree well with the sample densities with the average absolute deviations of less than ±7%.
Temperature Effect on the Relationship Between the H2 Raman Spectrum and Density
To investigate their temperature dependence, Raman spectra of H2 (in an HPOC) were collected at temperatures from 25 to 400 °C and pressures up to 150 MPa, and the neon lines were collected concurrently throughout the analysis. Noting that the sample chamber is very easy to crack when the experimental conditions are above 200 °C and 100 MPa. Therefore, for safety reason, the data under these conditions were not acquired, except for those obtained accidentally. Fig. S2 (Supplemental Material) shows the Raman spectra of the four vibrational bands (Q1(0), Q1(1), Q1(2), and Q1(3)) of H2 at 80 MPa from 25 to 400 °C, and two additional vibrational bands (Q1(4) and Q1(5)) at ∼4104 and ∼4075 cm–1, respectively, appeared at high temperatures (>100 °C). It also shows that the intensity of the Q1(0) band becomes weaker with increasing temperature, resulting in large uncertainties for the peak fitting procedure. In contrast, the intensity of the Q1(3) band becomes stronger at higher temperatures.
Peak positions of the four vibrational bands of gaseous H2 as a function of density at different temperatures (25∼400 °C) are shown in Fig. 6. The results show that the peak positions of the four vibrational bands of H2 shift to lower wavenumber and then shift to higher wavenumber as density increases at 25, 100, and 200 oC, and always shift to higher wavenumber at 300 and 400 °C. When the temperature increases at a constant density (>0.01 g/cm3), they shift to higher wavenumbers. The higher the density, the greater the temperature effect, which is consistent with previous observations.
38
This result indicates that the temperature strongly perturbs the vibrational motion of H2; thus, the temperature dependence of hydrogen Raman wavenumbers is stronger than those of other gases, such as H2S and CH4.41,48 The temperature-dependence coefficients (a, b, c, and d) of the Raman wavenumber are connected with vibrational coupling, isotropic intermolecular force, and the population of the initial rotational level. The values of a, b, c, and d for Q1 (n) (n = 0, 1, 2, and 3) over a temperature range of 100∼400 °C are shown in Table S5 (Supplemental Material). Therefore, to obtain an accurate H2 density from Raman peak positions at higher temperatures, the temperature effect should be considered. Peak positions of the four vibrational bands of gaseous H2 as a function of density at different temperatures (25∼400 °C).
The dependence of the FWHM on density at different temperatures is shown in Fig. S3 (Supplemental Material). At higher temperatures, the influence of the density on the FWHM is more obvious. This is because increasing the temperature accelerates the molecular thermal motion and the collision frequency. Compared to the Q1(0), Q1(1) and Q1(2) bands, the changes in the Q1(3) bandwidth show a weaker temperature dependence. The FWHMs of the Q1(0) band have large uncertainties due to their intensity being very weak, especially at high temperatures (Fig. S3).
Plots of the peak intensity ratios Q1(1)/Q1(n = 0, 2, 3) as a function of density are shown in Fig. S4 (Supplemental Material). When the density is low, the peak intensity ratios of Q1(1)/Q1(0) are very similar at different temperatures; then, the value of this ratio increases with density, and for a given density, it increases with temperature. However, the peak intensity ratios between Q1(1) and Q1(2) and between Q1(1) and Q1(3) decrease with increasing temperature at constant density. More interestingly, the slope of the plot of the peak intensity ratio of Q1(1) to Q1(2) versus density is very similar at different temperatures. For the peak intensity ratio of Q1(1) to Q1(3), the value changes greatly with the density at 25 °C, and then hardly changes with the density as the temperatures increase up to 400 °C. In other words, at high temperatures, the peak intensity ratio between Q1(1) and Q1(3) is independent of density and cannot be used as an indicator of density.
Density Determination of H2-Dominated Fluids
As mentioned above, the peak position and peak width (FWHM) of the four vibrational bands (Q1(0), Q1(1), Q1(2), and Q1(3)) of gaseous H2 and the peak intensity ratios Q1(1)/Q1(n = 0, 3) are sensitive to density. Although several quantitative equations for the determination of H2 density have been established at 25 °C, their applications to natural fluid inclusions remain optional because Raman spectra obtained from natural inclusions are not always of applicable qualities.
Even though the peak intensity ratios Q1(1)/Q1(0) and Q1(1)/Q1(3) of H2 are very sensitive to density (Fig. 4), they are highly dependent on the instrumental setting and sample quality. Similarly, even though the accuracy of density calculated with FWHM is very high, it is also worth noting that the FWHM not only changes with the instrumental setting, such as the wavelength of the laser, the groove density of grating, the slit width, and so on 49 but also is largely dependent on the type of fitting distribution curve and the baseline of the spectrum. The deviation of FWHM of H2 between the fitting Gaussian–Lorentzian curve and Gaussian curve can be up to 10%. However, the peak position of a pure Raman active species is independent of the instrumental factors. 50 It varies with the change of pressure and temperature since the nearest neighbor environment of the molecule changes with the change of density. 47 Absolute peak positions may be determined with an accuracy of better than ±0.02 cm–1 by reference to some standard; in our case, a neon lamp is used. Therefore, although the accuracy of density derived from peak position is much lower than those obtained with peak widths and peak intensity ratios, the peak position is most suitable for density determination.
According to this study, once the peak position of the vibrational bands of H2 in fluid inclusion is obtained in a laboratory, the value of D in Eq. 2 could be determined as long as the peak position at near-zero density υ0 was known, then the density of H2 in the fluid inclusion can be expediently obtained from Fig. 2 and Eq. 2. Among the four vibrational bands, the Q1(1) band has the strongest intensity and could be obtained easier than others, indicating that it is a better alternative for density determination. It is important to note that, for a given D, there may be two possible density values in the range of 0∼0.055 g/cm3 for the Q1(1) band. This trend is extraordinarily alike to that observed in simple fluids such as methane 49 that the peak position of H2 first shifts to lower wavenumber until it reaches a minimum, and then shifts to higher wavenumber with increasing density at constant temperature. 51 Noting that the density of H2 in the range of 0∼0.033 g/cm3 (corresponding to 0∼55 MPa) meets most of the geological environment.
Natural H2-bearing fluid inclusions commonly contain other volatile components, such as CH4, CO2, H2S, N2, O2, He, and H2O.5,29,46 Unfortunately, Raman spectroscopic studies of these mixtures remain quite limited. Fang et al. 31 found that the effect of the addition of CH4 on the peak position and peak width of Q1(1) band of H2 was quite small when the molar ratio of H2 to CH4 was ≥5, indicating that our calibration polynomial based on the peak position of Q1(1) band is reliable in H2‐dominated fluid with H2–CH4 gaseous mixtures. To study a wider range of mixtures of H2 with geologically important volatile components, additional experiments should be carried out.
Conclusion
This work provides the Raman spectral parameters, including peak position, width, and intensity, of the vibrational bands of H2 from 25 to 400 °C and pressures up to 150 MPa. We have discussed the variation in each parameter as a function of fluid density. Several calibration polynomials based on our experimental results were established to determine H2 densities up to 0.062 g/cm3 at 25 °C. Our data on the peak positions are independent of instrumental factors and are generally applicable to other laboratories, as long as the near-zero density peak position is obtained. Notably, the temperature has a great influence on these parameters and cannot be ignored. Thus, when using our method for the determination of the H2 density in H2-bearing fluid inclusions, the fluid inclusions should not be appreciably heated. In the application to natural inclusions, the peak position of the strongest intensity Q1(1) band is a better alternative for density determinations mainly because (i) Raman spectra obtained from natural inclusions are not always of applicable qualities and the strongest intensity Q1(1) band could be obtained easier than others and (ii) the peak position is insensitive to instrumental factors. Future experiments should be performed to determine how the peak position, peak width, and peak intensity ratio of H2 bands are affected by additional components in fluid inclusions.
Supplemental Material
sj-pdf-1-asp-10.1177_00037028221080489 - Supplemental material for Determination of H2 Densities Over a Wide Range of Temperatures and Pressures Based on the Spectroscopic Characterization of Raman Vibrational Bands
Supplemental material, sj-pdf-1-asp-10.1177_00037028221080489 for Determination of H2 Densities Over a Wide Range of Temperatures and Pressures Based on the Spectroscopic Characterization of Raman Vibrational Bands by Ying Chen and I-Ming Chou in Applied Spectroscopy
Footnotes
Acknowledgments
We thank Dr Nanfei Cheng of the Institute of Deep‐Sea Science and Engineering, Chinese Academy of Sciences for English editing.
Declaration of Conflicting Interests
The author(s) declared no potential conflicts of interest with respect to the research, authorship, and/or publication of this article.
Funding
The author(s) disclosed receipt of the following financial support for the research, authorship, and/or publication of this article: This study was funded by the Key Frontier Science Program (QYZDY‐SSW‐DQC008) of Chinese Academy of Sciences and the National Natural Science Foundation of China (No. 41973055).
Supplemental Material
All supplemental material mentioned in the text is available in the online version of the journal.
References
Supplementary Material
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