Applied Surface Science 536 (2021) 147990 Contents lists available at ScienceDirect Applied Surface Science journal homepage: www.elsevier.com/locate/apsusc Raman study of D* band in graphene oxide and its correlation with reduction T A Young Leea,b, Kihyuk Yanga, Nguyen Duc Anha, Chulho Parka, Seung Mi Leec, Tae Geol Leeb, , ⁎ Mun Seok Jeonga, ⁎ a Department of Energy Science, Sungkyunkwan University, Suwon 16419, Republic of Korea Nanosafety Team, Safety Measurement Institute, Korea Research Institute of Standards and Science, Daejeon 34113, Republic of Korea c Surface Analysis Team, Interdisciplinary Materials Measurement Institute, Korea Research Institute of Standards and Science, Daejeon 34113, Republic of Korea b ARTICLE INFO ABSTRACT Keywords: Raman spectroscopy Reduced graphene oxide Thermal reduction Density functional perturbation theory Reduced graphene oxide (rGO) is a graphene-like material that exhibits high productivity for a wide range of industrial applications. To promote the application of rGO, it is important to not only produce high-quality rGO but also precisely evaluate the output. The intensity ratio of the D to G band in the Raman scattering is commonly used to assess the defect density of the carbon materials; however, this ratio is limited to evaluate the reduction degree of rGO because of the ambiguity arising from the superposition of the bands. In this study, we investigate the relationship between the intensity ratio of D* to G band and the reduction of graphene oxide (GO) to evaluate the degree of reduction of rGO. The spectral analysis of GO and rGO, along with systematic research of the thermally reduced GO synthesized via thermal treatment (100–900 °C) revealed a strong linkage between the D*/G intensity ratio and the C/O atomic ratio. The atomic vibrational relationships were elucidated by the assignment of the D* band, based on the density functional perturbation theory calculations. These findings explain the atomic vibrational properties of rGO and provide an indicator of the quality of rGO to optimize its performance for applications. 1. Introduction Graphene is a two-dimensional plane sheet of sp2-hybridized carbon atoms that are arranged in a honeycomb lattice structure. Since the development of defect-free monolayer graphene using mechanical exfoliation in 2004 [1], graphene has been widely utilized in diverse fields such as supercapacitor electrodes [2], conductive agents [3], active electrode materials for lithium-ion batteries [4], and biosensors [5,6], owing to its strong merits of a large specific surface area, excellent electrical properties, high chemical stability, extreme sensitivity, and high mechanical properties [7–9]. High-quality graphene is prepared via bottom-up techniques such as chemical vapor deposition [10], and epitaxial growth on silicon carbide [11]. However, the commercialization of these methods is economically unviable because of their limited scalability and the need for high temperature and vacuum conditions. For the industrial mass production of graphene, reduced graphene oxide (rGO), a graphene-like sheet, was developed by reducing the oxygen-containing functional groups of graphene oxide (GO) [12,13]. Raman spectroscopy has been widely employed to characterize the ⁎ molecular structures of carbon products, because of the resonantly enhanced Raman scattering of carbon materials; thus, graphene shows well-defined vibration bands [14]. In addition, Raman spectral analysis allows the assessment of the disorder and defects in carbon materials through the measurement of the intensity ratio of the D band to G band (I(D)/I(G) ratio) [15]. Nevertheless, in the case of GO and rGO, it is necessary to reconsider whether the I(D)/I(G) ratio provides accurate information, considering the ambiguity of the vibration information due to the superposition of the bands [16]. In addition, the intensity ratio falls unexpectedly in the high-defect density regimes since a large number of amorphous carbons attenuate all the Raman modes [17]. To find alternatives to the I(D)/I(G) ratio, researchers have investigated other Raman bands through the deconvolution of the Raman spectra of GO and rGO. The spectral parameters have been investigated and correlated with the structural properties, which revealed their relationship with the oxygen content, crystallinity, and degree of disorders of rGO. The positions of the D'' and D* peaks obtained after deconvolution, which was performed using a combination of five functions, show good correlations with the oxygen content and can thus be used to estimate the degree of reduction [18]. Raman metrics with D' and G bands were Corresponding authors. E-mail addresses: tglee@kriss.re.kr (T.G. Lee), mjeong@skku.edu (M.S. Jeong). https://doi.org/10.1016/j.apsusc.2020.147990 Received 4 July 2020; Received in revised form 22 September 2020; Accepted 24 September 2020 Available online 28 September 2020 0169-4332/ © 2020 Elsevier B.V. All rights reserved. Applied Surface Science 536 (2021) 147990 A.Y. Lee, et al. Fig. 1. SEM images of (a) GO and (b) rGO. (c) Photograph of GO and rGO dispersions in water. (d) UV–Vis absorption spectra of GO and rGO. Fitted Raman spectra of (e) GO and (f) rGO, respectively. developed to investigate the degree of reduction. The difference in the positions of the inferred D mode and the apparent G mode is associated with GO reduction [16]. Furthermore, the second-order Raman bands show a direct correlation with the electrical resistance of laser-reduced GO [19]. However, these relations are only partially described due to a lack of understanding of the origins of the peaks. In this study, we propose a combined approach that involves the experimental findings of the spectral changes and the theoretical calculations of the Raman band, with the aim of determining the relationship between the intensity ratio of the D* band to the G band (I (D*)/I(G)) and the degree of reduction. The spectral analysis of GO and rGO and the systematic study of a series of thermally reduced GO synthesized via thermal treatment (100–900 °C) revealed a strong relationship between the I(D*)/I(G) ratio and the C/O atomic ratio. The atomic vibrational relationships were ascertained through the D* band assignment based on the density functional perturbation theory (DFPT) calculations. The D* band is known to originate from the sp3 orbital, such that observed in nanocrystalline diamonds with small grain sizes where the selection rule is relaxed [20], sp3-rich phases [21], and hexagonal diamonds [22]. Unlike the above-mentioned studies, the origin of the D* band was postulated and suggested to originate from trans-polyacetylene in the grain boundaries [23]. In this study, we found that the D* band originated from the vibrations of carbon atoms that were restricted by oxygen-containing groups, as determined by performing the DFPT simulation; this implies that the D* band intensity is affected by the remaining oxygen-containing groups. 2.2. Characterization 2. Experimental details 3. Results and discussion 2.1. Preparation of samples 3.1. Comparative analysis of GO and rGO A series of thermally treated GO (t-GO) was prepared by annealing the GO (GO-V50, Standard Graphene Inc.) in a furnace at the temperature range of 100–900 °C for 1 h under a vacuum pressure of 10−3 Torr. The morphologies of GO and rGO (GO-V50, RGO-V50, Standard Graphene Inc.) were examined by SEM. As can be seen in Fig. 1(a) and (b), rGO exhibits the wrinkled and folded morphologies caused by thermal fluctuations after thermal reduction [25]. As another difference between the two, the color of the aqueous dispersion distinguishes a brownish-yellow GO solution and a black rGO solution (Fig. 1(c)) [26]. The UV–Vis absorption spectrum of Fig. 1(d), the black line represents Scanning electron microscopy (SEM) analysis was performed using a Hitachi S-4800 scanning electron microscope operated at 10 kV. Ultraviolet–visible (UV–Vis) absorption spectroscopy was performed with a SHIMADZU UV-1800 spectrophotometer using aqueous solutions of GO (0.2 mg/ml) and rGO (0.2 mg/ ml). X-ray photoelectron spectroscopy (XPS) was performed using a Thermo Fisher Scientific KAlpha+ spectroscope with an Al K source at full width at half maximum value lower than 0.5 eV. Raman spectra were measured using a WItec Alpha 300 Raman spectrometer with 1800 lines/mm using a 532 nm laser. The laser power was set as 50µ W after using a 100× 0.9NA objective lens to avoid the laser-induced reduction of GO [24]. The exposure time was 180 s per spectrum. Calibration was performed using a silicon standard (520 cm−1). X-ray diffraction (XRD) analysis of the solid powder state was performed using a Bruker D8-Advance X-ray diffractometer. Fourier transform infrared (FT-IR) spectroscopy was conducted on a Nicolet iS10 FTIR spectrometer in the attenuated total reflectance mode. The FT-IR spectra were recorded at room temperature in the spectral range of 650–4000 cm−1. 2.3. Theoretical calculations The origin of the D* band was determined using the local density approximation of the DFPT method implemented with the Cambridge Serial Total Energy Package (CASTEP) code. The computational details are provided in the Supplementary Information (S5). 2 Applied Surface Science 536 (2021) 147990 A.Y. Lee, et al. planar sp2 carbons into the tetrahedral sp3 carbons, resulting in the peak broadening of the XRD peaks (Fig. 4) [40]. As can be seen, the XRD spectrum of ordered GO exhibits a sharp peak at 11.6°, while that of the amorphous rGO exhibits a broad peak at 25.8°. The difference in the width and position of the peaks indicates that the reduction process caused damage to the graphene plane and augmented the generation of defects while decreasing the interlayer distances from 0.76 nm to 0.34 nm due to the loss of oxygen-containing groups [41]. GO with – * plasmon peak at 230 nm and n− * shoulder peak at 270 nm. In the red line of rGO, the peak shifted to 270 nm because of the restoration of the conjugated structure [27]. Fig. 1(e) and (f) show the Raman spectra of GO and rGO in the spectral range of 1000 cm−1 to 1800 cm−1. The Raman spectra were deconvoluted using Lorentzian curves, which consist of the first-order Raman modes, namely: D*, D, D'', G, and D' bands. The D band, which is located at 1330–1350 cm−1, arises from the defects and disorders in the carbon lattice and the double resonant processes near the K point of the Brillouin Zone (BZ) boundary [28]. The G band at 1583 cm−1 corresponds to the Ramanallowed E2g optical phonon [29]. The D'' band at 1500–1550 cm−1, is related to the amorphous phase and its intensity is inversely related to the crystallinity [30]. The D' band at 1620 cm−1 corresponds to an intra-valley resonance with the G band and undergoes splitting due to impurities [31]. The D* band at a 1050–1200 cm−1 originates from the sp3 orbital, which is similar to the D* band observed for nanocrystalline diamonds with small grain sizes [20], sp3-rich phases [21], and hexagonal diamonds [22], disordered graphite lattice [32], polyene [33], and trans-polyacetylene in the grain boundaries [23]. Based on the origins of the D and G bands, the I(D)/I(G) ratio can be used to quantify the defects in carbon materials. The comparative spectroscopic analysis of GO and rGO reveals significant changes in Raman peak intensities due to the heat treatment that resulted in a thermal reduction, folding of structures, impurities, hybridization structures (sp1, sp2, and sp3), lattice contraction, exfoliation, and defect formation [34]. However, the conventional I(D)/I(G) ratio does not provide sufficient details to allow the evaluation of rGO due to the overlapping of the Raman bands [16]. Furthermore, due to the dispersion of the D band, the I(D)/I(G) ratio increases with a decrease in laser excitation energy [35]. Additionally, in high-defect density regimes, the intensity ratio decreases since the numerous amorphous phases of the carbons dampen all the Raman modes [17]. Another difference in the Raman spectra of GO and rGO is the significant increase in the intensity of the D* band of rGO as compared to that of GO (Fig. 1(e) and (f)). We compared the difference in the D* band intensities of GO and rGO, depending on the fitting of various combinations of Lorentzian and Gaussian curves (Fig. S1). To confirm the reliability of the fitted results of the different deconvolutions, we compared three types of band combinations: five Lorentzian curves, four Lorentzian curves, and one Gaussian and four Lorentzian curves. These three combinations listed have low values close to 1 of reduced 2 for fitting the Raman spectra of carbon materials [36]. The Raman spectra fitted by the combinations shown in Fig. S1 indicate that the intensity of the D* band increased after reduction, regardless of the fit combinations. To prove that the five Lorentzian curves used for fitting the Raman spectra are suitable, additional Raman scattering measurements were performed at a different laser excitation wavelength of 633 nm to show the non-dispersive characteristics of the G band and the shifting of the D band [37] (Fig. S2 and Table S1). As shown in Fig. 2, the peak area and peak intensity ratios of the Raman bands indicate that the differences in both the I(D*)/I(G) ratios and the area ratios of the D* band to the G band of GO and rGO are significantly higher than the differences in the area and intensity ratios other pairs of the bands. XPS was performed to identify the chemical states of the elements in GO and rGO; the XPS profiles are presented in Fig. 3. In the XPS spectra of GO and rGO, the decomposed peaks of sp2 carbon, sp3 carbon, CeO, * transition appeared at 284.5, 285.2, 286.3, 288, and C]O, and 290.9 eV, respectively, which are consistent with the results of previous studies [38]. The atomic percentages of the CeO and C]O in rGO are weaker than those values of GO due to a decrease in the oxygen-related components as shown in Table 1; meanwhile the intensity of the peak corresponding to sp2 species increased, which resulted in a decrease in sheet resistance [38,39]. The thermal treatment led to the collapse and conversion of the 3.2. Spectral changes of thermally treated GO To systematically investigate the I(D*)/I(G) ratio, we analyzed the Raman spectra of GO that was reduced to varying degrees at different heat-treatment temperatures. Fig. 5 displays the fitted Raman spectra of GO thermally treated in the temperature range of 100–900 °C. In the Raman spectra of t-GO annealed above 600 °C (Fig. 5(f)–(i)), the D* band is more intense than the values at the temperature below 600 °C, thus it has a relatively high I(D*)/I(G) ratio and the value increases as the temperature increases. In contrast, the intensity of the G band decreased with increasing annealing temperature. The changes in the Raman peak intensities are attributed to the thermal reduction process that involves the removal of hydroxyl groups and the generation of CO gas [18]. The FT-IR spectra (Fig. S4) confirm the removal of the hydroxyl groups with increasing temperature. To decompose the hydroxyl group, a carbon source is required to yield CO gas [34]. Fig. 6(a) and (b) show the variations of Raman peak intensity ratios with temperature. To accurately capture the comparison of conventional I(D)/I(G) and I(D*)/I(G), we plotted the mean and standard deviations of the ratios obtained by measuring Raman spectra at three random positions. The intensity of the D band in Fig. 6(a) and the intensity of the D* band in Fig. 6(b) were normalized to the G peak intensity in order to plot the Raman intensity ratio against the annealing temperature. Fig. 6(c) shows the temperature-dependent atomic ratio measured by XPS results. After determining that the intensity ratio is more closely related to the C/O ratio, it is observed that the I(D*)/I(G) ratio is actually associated with the atomic ratio, rather than the I(D)/I (G) ratio. To show the relationship intuitively, the I(D*)/I(G) ratio was plotted against the oxygen atomic percentage, carbon-oxygen ratio, and carbon atomic percentage (Fig. S3(a–c)). The graphs indicate that the Raman intensity ratio is related to the reduction degree. As can be seen, the I(D*)/I(G) ratio decreased unexpectedly with an increase in temperature from 100 °C to 200 °C. Since temperatures below 225 °C are not high enough to reduce GO [42], it is difficult to determine whether the Raman spectral changes occurred due to the removal of the oxygen-containing groups. In the temperature range of the 100–200 °C, the change in water content affects the vibrations of the carbon lattice. This is because the evaporation of water molecules above 100 °C decreases the distance of the carbon interlayer [43], which in turn interferes with the vibrations of the carbon atoms, resulting to decrease the intensity of the D* band as well as the I(D*)/I(G) ratio. 3.3. Theoretical calculations of the D* band The first principle simulation based on DFPT calculations was performed to confirm the existence of the D* band. A vibrational analysis was performed to determine the vibrations of the atoms that gave rise to the peak near 1200 cm−1. Fig. 7(b) and (c) show the vibration of GO with hydroxyl groups attached above and below the graphene plane, respectively. The arrows represent the vibration vectors. Experimental results revealed the correlation between the C/O ratio and the intensity of the D* band above 600 ℃ (Fig. 6(b)) at which the C/O ratio was approximately 9:1 (Fig. 6(c)). In addition, the FT-IR spectra (Fig. S4) showed that the change in the concentration of the hydroxyl group during heating was greater than the changes in concentrations of the other groups. Furthermore, the conversion of epoxy groups into 3 Applied Surface Science 536 (2021) 147990 A.Y. Lee, et al. Fig. 2. (a) Peak area ratios and (b) peak intensity (height) ratios of Raman bands of GO and rGO. The black and red dots represent GO and rGO, respectively. Mean and standard deviations were calculated by measuring Raman spectra at ten random positions. (For interpretation of the references to colour in this figure legend, the reader is referred to the web version of this article.) Fig. 3. Deconvoluted C1s peaks of (a) GO and (b) rGO, respectively. Table 1 The atomic percentage of each component determined from the C 1s peaks of GO and rGO. Sample sp2 sp3 CeO C]O pi-pi GO rGO 51.27 66.51 1.79 3.21 30.60 12.83 14.53 12.41 1.82 5.05 hydroxyl groups under atmospheric conditions resulted in the presence of a large number of hydroxyl groups which are stable oxygen-containing groups [44–46]. Therefore, in the DFPT model, GO has hydroxyl groups and a C/O ratio of 9:1. As shown in Fig. 7(a), under 532 nm irradiation, a weak Raman peak appeared at around 1200 cm−1, which was the frequency of interest. There was a discrepancy between the wavenumber values obtained using theoretical calculations and those determined via experimental observations, owing to the complicated structure of real GO. Because of the presence of the hydroxyl groups that restrict the intact vibrations of the hexagonal structure, the movement of carbon atoms near the hydroxyl group is weaker than the movement of the distant carbon atoms. With the reduction of GO, the hydroxyl group concentration decreased, which resulted in the restoration of the intrinsic vibrational properties of graphene; thus, the intensity of the Raman peak gradually increased with increasing annealing temperature. Fig. 4. XRD spectra of GO (top) and rGO (bottom). 4. Conclusions A comparative analysis of the Raman spectra of GO and rGO was performed, which showed the difference in the D* band intensity. The Raman spectra of t-GO were systemically investigated by comparing the variations in the I(D*)/I(G) ratio with those in the conventional I(D)/I (G) ratio as a function of the annealing temperature. The results showed 4 Applied Surface Science 536 (2021) 147990 A.Y. Lee, et al. Fig. 5. Fitted Raman spectra of t-rGO annealed at the temperatures ranging from 100 °C to 900 °C. Fig. 6. Variations in (a) I(D)/I(G) and (b) I(D*)/I(G) ratios with annealing temperature. The mean and standard deviations of all measurements are shown. (c) Change in the atomic ratio with annealing temperature determined from the XPS measurement. The black empty squares represent the carbon atomic percentage, blue empty squares represent the oxygen atomic percentage, and red-filled squares represent the carbon-oxygen ratio. that that the I(D*)/I(G) ratio is more closely related to the C/O ratio. The DFPT calculation results indicate that the D* band originates from the vibration of the carbon atoms restricted by the oxygen-containing groups. Therefore, the intensity of the D* band is affected by the residual oxygen-containing groups, such as the vaporization of water molecules at a low temperature and the elimination of oxygen-containing groups at a high temperature. The calculation results help reveal the origin of the D* band, evidencing that the band originates from the sp3 phase and carbon stretching vibrations, which explains the relationship between the I(D*)/I(G) ratio and the degree of reduction. Consequently, the D* band can serve as an indicator for the reduction degree of thermally reduced GO. This approach can not only be used to measure the quality of GO synthesized by various reduction methods but also have the potential to be used in general to carry out an accurate measure of the quality of rGO. Credit authorship contribution statement A Young Lee: Formal analysis, Investigation, Data curation, Writing-original draft, Visualization and Methodology. Kihyuk Yang: Calculations, Software, and Visualization. Nguyen Duc Anh: Investigation and Formal analysis. Chulho Park: Formal analysis. Seung Mi Lee: Calculations and Software. Tae Geol Lee: Validation, Supervision, Funding acquisition, Writing-review & editing, and Resources. Mun Seok Jeong: Conceptualization, Validation, Supervision, Writing-review & editing, Project administration. 5 Applied Surface Science 536 (2021) 147990 A.Y. Lee, et al. Fig. 7. (a) Raman spectrum of the D* band obtained from DFPT calculations. 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