1 Introduction

Coal has manifold uses, as for instance, solid fuel, gives coke for metallurgical use, coal chemicals and many more. Several chemical products can be produced from the coal and/or its by-products. Coal has several advantages when considered as a feedstock for aromatic chemicals and carbon based materials. It can be used in producing activated carbon (AC), carbon molecular sieve (CMS), specialty carbon materials (viz.: fullerene, artificial graphite, artificial diamond), composites of coal with other polymers, humic acid preparations etc.

Hence, the study molecular structure of coals and their structurally modified counter parts are very much essential to understand their basic nature and for suitability towards more meaningful industrial utilization. Coal is essentially a very heterogeneous and complex material and many models have been proposed to understand the molecular structure of it and their structurally modified counterparts (Domazetis and James 2006; Mathews and Chaffee 2012; Li et al. 2015; Yan et al. 2020). Earlier, Hirsch (1954) carried out X-ray diffraction studies of low rank coals and anthracite. He found that the low rank coals up to carbon content 85% have “open structure”. Many studies like Transmission Electron Microscopy (TEM), Scanning Electron Microscopy (SEM), XRD, FTIR, Raman Spectroscopy, X-ray Photoelectron Spectroscopy (XPS), Nuclear Magnetic Resonance (NMR) and High-resolution Transmission Electron Microscopy (HR-TEM), have been used for coal molecular structure determination (Solum et al. 1989; Dangyu et al. 2011; Baysal et al. 2016; Barbara et al. 2019; Jing et al. 2019).

The role of X-ray diffraction is very important in coal science. Powder diffraction technique can be used to study the different phases present in coal. To address the heterogeneity of coal, this technique is immensely important as it uses relatively large amount of the sample and collects most of the intensities scattered from the sample (Lu et al. 2001). Coal has an intermediate structure between graphite and amorphous carbon, so-called turbostratic structure or random layer lattice structure (Maity and Mukherjee 2006). It also contains significant amount of highly disordered material, amorphous carbon, which is responsible for the background intensity of the diffractograms. However, recent developments of computer techniques have enabled more accurate calculations and detailed analysis of XRD profiles. Wertz's group (Wertz 1998; Wertz and Bissell 1994, 1995; Wertz and Quin 2000) has made extensive studies of coals using XRD technique and quantitatively characterized both mineral matter and organic matrix of coals. XRD analysis is a fundamental method for evaluating carbon stacking structure. The degree of graphitization, the interlayer spacing (d002), and the crystallite size (Lc), aromaticity (fa), average number of aromatic layers (Nc) and XRD rank parameter (I26/I20) have been established as the parameters for evaluating structure of highly crystalline carbon materials (Boral et al. 2015).

FTIR spectroscopy exploits the fact that molecules absorb or transmit specific frequencies that are characteristic of their structure. For coal, it is generally studied in mid-infrared zone, approximately 4000–400 cm−1 wave number range. Infrared spectroscopy gives information on the vibrational and rotational modes of motion of a molecule and hence an important technique for identification and characterization of functional groups. The Infrared spectrum of an organic compound provides a unique fingerprint, which is readily distinguished from the transmission patterns of all other compounds. Fourier transform is used to process the data from interferometer instrument. Modern FTIR instrument uses a laser-light, powerful computer and advanced software. The software performs processing, manipulation, plotting, resolution enhancement, peak position, area measurement, library searching (Painter et al. 1978; Painter and Colemon 1979; Solomon et al. 1990; Tamarkina et al. 2002). Radial distribution function (RDF) obtained from Fourier Transformation of molecular scattering is used to examine the molecular level structuring of coal. Tamarkina et al. (2002) used FTIR to study modification of different rank coals in equimolar nitric acid and acetic anhydride mixture.

To study the structural variations, four samples have been collected from Jharia Basin of India. Jharia Basin coal is very important as it is the only caking/coking coal producing horizon of India. The coal bearing horizon of the basin is subdivided into two stratigraphic formations, viz., Barakar and Raniganj. The Barakar Formation coals are the only source of the prime coking coal of India, while the Raniganj measure coals are the high volatile medium coking coals. For all the coal seams, it is observed that their maturity gradually decrease from west towards east, in both the coal measures. Coals of the Barakar Formation are generally low in moisture (0.5%–2.0%) and medium to low volatile caking coal. The coals of the Raniganj Formation contain slightly higher moisture and high volatile matter content than the coals of Barakar Formation. All the samples are demineralized with standard HCl + HF treatment method to avoid the effect of mineral matter in instrumental analyses (Maity and Mukherjee 2006). Each of the demineralized coal samples has been modified with nitric acid treatment in glacial acetic acid and in aqueous medium (Maity and Choudhury 2008). Thus, twelve numbers of samples have been prepared in total for the present study.

2 Experimental

2.1 Collection of sample

Jharia basin forms a part of the Damodar valley basins which includes Jharia, Raniganj, Bokaro, Karanpura and Ramgarh coalfields. These coalfields are separated from each other by Precambrian rocks in the outcrops. Jharia Coalfield (JCF) is situated about 260 km northwest of Kolkata in the heart of Damodar valley mainly along the north of the Damodor River. The coalfield is bounded between latitude N23º37′–N23º52′ and longitudes E86º06′–E86º36′ and lies within the district of Dhanbad. This sickle shaped coal basin extends for about 38 km in an east–west direction and a maximum of 19 km in north–south direction and covers an area of about 456 km2. Out of this area; Barakar formation occupies an area of 216 km2, Raniganj Formation 54 km2 and rest Barren Measures 180 km2 (Krishnan 1982).

The general stratigraphic succession (Chandra 1992) of the area is that the basement of metamorphic rocks overlain by the Talchir Formation followed by the Barakar Formation, which is the main coal bearing horizon. Above it, comes the Barren Measures (devoid of coal), which is followed by the coal-bearing Raniganj Formation. The Raniganj Formation is the uppermost coal bearing Formation in the Jharia coalfield. The thickness of Barakar Formation is about 800–1250 m with about 25 coal horizons, out of which 18 are regionally persistent. The upper coal measures of Raniganj Formation is approximately 800 m thick and contains 12 coal horizons, of which 4 to 5 are persistent in nature. In both the formations, the persistent coal seams have been numbered from bottom.

The present study is carried out on coals from of Mohuda (MH), Gasalitand (GT), Salanpur (SL) and Shatabdi (ST) mines of Jharia Coalfield which forms a part of the Damodar Valley basin. The details of coal samples are shown in Table 1.

Table 1 Details of the collected samples
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The coal samples are crushed to below 212µ (IS 436 Part 1/Sec 1 2001) for this study, while samples for petrographic analysis are prepared by controlled crushing with below 1 mm size (IS 9127 Part 2 2002). The Gross Calorific Value (GCV) is measured (Standard: ASTM D5865) by Automatic Bomb calorimeter (Model AC-350 isoperibol bomb calorimeter, Leco, USA). The ultimate analysis of coal involves determination of the elemental composition of coal and is expressed in terms of weight percentages of carbon (C), hydrogen (H), nitrogen (N), sulphur (S), and oxygen (O). Percentages of elemental C, H, N and S are determined analytically while O is obtained by difference from hundred. Information derived from ultimate analysis is used for selection of coal for various efficient utilization purposes. Carbon, hydrogen and nitrogen percentages of each of the air-dried samples are determined by the Leco (USA) make CHN-1000 analyzer (ASTM D5373 2016). Analysis of sulphur (Standard: ASTM D5016 2016) is done by Leco (USA) (Make SC-132), which is a microprocessor-based instrument and it has a control console for each system and a measurement unit with a built-in-balance.

The maceral analyses and vitrinite reflectance of each sample have been carried out in micro-petrographic analysis of coal. The maceral analysis is carried as per standard (IS 9127 Part 3 2002) procedure. The IS 9127 Part 5 2004, is used for reflectance measurement. Reflected light polarized microscopes (Make: Leitz; Model: MPV Compact, Germany and Make: Leica, Model: DMRX P HC, Germany) have been used to study the maceral composition and reflectance measurements of the samples.

2.2 Demineralization of samples

All the raw coal samples contain inorganic mineral matter. The intensity of the diffraction peaks of these inorganic minerals is much sharper and stronger than that of the broad humps of the organic matter present in coal. It is very difficult to obtain accurate crystalline peaks of organic matters in X-ray diffraction pattern of crystalline organic matters in presence of inorganic mineral matters. So, the mineral matters present in coal are removed by demineralizing the coal samples using standard HCl + HF solution to alleviate this problem (Maity and Mukherjee 2006).

Each ten grams of air dried sample of 212 µ (X 72 mesh) size is accurately weighed and transferred to a Teflon beaker. To this 60 mL of concentrated HCl of 36.5 wt% is added slowly keeping it in a water bath. The temperature of the water bath is kept at 60 ºC. The mixture is stirred vigorously by a Teflon rod for three hours. Then the coal is filtered and washed with hot distilled water to remove HCl. The filtered HCl-treated coal is again treated with 60 mL concentrated HF solution of 48 wt% purity. The mixture is again kept in water bath of 60 ºC and stirred for another three hours. Finally, the HF treated coal is filtered and washed with hot distilled water to remove HF from coal. Removal of acid from coal is confirmed by pH test of the samples. Then residual coal in the filter paper is dried in an air-oven for 5–6 h at 50 °C. The Demineralization is confirmed by the weight loss of the coal samples to at least less than 2% effective mineral matter for the samples.

2.3 Chemical modification procedures

Structural modification is carried by oxidative pretreatment of coal. Two types of chemical treatments are carried out for each of the demineralized coal samples to make structurally modified coals (SMCs). The demineralized coal samples are treated with concentrated nitric acid in different media viz. in glacial acetic acid and in aqueous media to form SMCs (Maity and Choudhury 2008).

2 g of demineralized coal is weighed accurately and 10 mL of glacial acetic acid is mixed thoroughly in beaker. The mixture is kept in a water bath at a temperature of 15–20 ºC by adding ice to the water bath. The temperature of the bath is monitored so as to maintain the desired temperature. To this mixture, 3 mL of concentrated nitric acid (HNO3 at 68 wt%) is added drop by drop and stirred thoroughly. This 3 mL HNO3 was mixed to the mixture of coal and glacial acetic for at least half an hour duration and after that kept for 24 h. After 24 h, the mixture is diluted with 250 mL/g distilled water and left for another 24 h. The mixture is then filtered and washed with hot distilled water till neutralization (pH value is approx. 7.0) is attained. Then the treated coal is dried in an air-oven at 50 ºC for 5–6 h and kept in desiccators. After treatment of each sample the difference in weight is measured.

In the second treatment, two grams of demineralized coal is taken in a refluxing condenser. Pure nitrogen gas is purged through it before the treatment. Then 60 mL of 30% nitric acid is mixed to the coal. The coal acid mixture is heated at 105 ± 5 ºC and stirred well. The reaction continues for 8–10 h or till the end of any gas evolution from the coal-acid mixture. The residue left in the flask is filtered and washed with hot distilled water till any trace of nitric acid is removed and neutralization is confirmed by pH test. After each treatment, the sample is dried in an air-oven at 50 ºC for 5–6 h and kept in desiccators and the difference in weight is calculated using the formula:

$$\Delta {\text{ wt}}\% =\left( {W_{{\text{f}}} {-}W_{{\text{i}}} } \right)/W_{{\text{i}}}$$

where, Wf and Wi are the final and initial weight of the coal sample after and before treatment of coal respectively.

The demineralized coal samples are coded with suffix (D), nitric acid treated coals in glacial acetic acid medium with suffix (G) and aqueous nitric acid treated coals with (A). As for example the Mohuda demineralized coal (MHD), viz. (MHG) for Mohuda nitric acid treated coals in glacial acetic acid medium and (MHA) for aqueous nitric acid treated coals.

2.4 X-ray diffraction analysis

X-ray Diffraction (XRD) analysis is performed by a D-8 ADVANCE (Bruker AXS, Germany) X-ray Diffractometer. This is used to collect the X-ray intensities of the demineralized and treated coals in the 2θ range of 10°–90° with Bragg–Brentano geometry, using parallel beam Cu Kα (40 kV, 40 mA) radiation. An X-ray amorphous sample holder is used for coal sample loading, and the scan is made in locked couple step scan mode (0.02°/step), with 2 s at each step.TOPAS 3.0 from Bruker AXS (2005), Germany is used for de-convolution of the diffractograms in the 2θ region of 10°–35°. Two symmetrical Gaussian peaks are fitted for determination of π-band and γ-band to determine the d002 and position of γ-band (Dγ) respectively. XRD profile curve fitting of two Gaussian peaks for the Mohuda (MH) demineralized coal in the range of 10°–35° is shown in Fig. 1 as an example. The carbon-related peaks around 20°–26°can be categorized into π (002-band) and γ-band for aromatic and aliphatic chains respectively. The π-band due to aromatic ring stacking occurs near 26°, while γ-band around 20°, are believed to be derived from aliphatic chains. TOPAS 3.0 software is used for refinement of π-band and γ-band to determine the d002, position of γ-band (Dγ), average crystallite size (Lc), average number of aromatic layers (Nc), ratio of intensity of π-band and γ-band (I26/I20) and aromaticity (fa) (Maity and Mukherjee 2006; Boral et al. 2015). The software package uses the fundamental parameter approach (FPA) and is therefore capable of estimating the instrumental influence. The Double-Voigt approach in TOPAS is used with both calculated FPA and measured instrument functions. XRD analyses are carried out for all the demineralized coal samples and their corresponding SMCs formed by nitration in glacial acetic acid medium and aqueous medium.

Fig. 1
figure 1

XRD profile curve fitting of two Gaussian peaks for the Mohuda (MH) demineralized coal in the range of 10°–35°

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2.5 Fourier transform infra red spectroscopy

Fourier transform infra red spectroscopy (FTIR) is extensively used for quantitative as well as for qualitative analysis in almost all fields of science (Painter et al. ; Painter and Colemon 1979; Solomon et al. 1990; Jing et al. 2019; Wu and Zhang 2019). Bruker (Germany) make 3000 Hyperion Microscope with Vertex 80 model FTIR-imaging system has been used to analyze the samples.

The FTIR spectra of all the samples are carried out in the range of spectral band of 4000 to 450 cm−1. For each sample analysis, thirty two scans are co added at a resolution of 2 cm−1. For spectral analysis, KBr matrix method is applied to prepare the samples. Sample and dry KBr in the ratio of 1:100 are ground and mixed in an agate mortar. Pellets of 13 mm diameter are prepared using 250 mg of this mixture by pressing it in an evacuated die at 10 tonnes pressure in a hydraulic press. Origin 6.1 software is used to de-convolute FTIR spectrum and multi-peak Gaussian probability density function fit obtained for each functional group. Multi-peak Gaussian probability curve fit of FTIR analysis of Mohuda (MH) coal is shown as an example in Fig. 2. The area under each functional group is calculated for demineralized as well as treated coals in glacial acetic acid and in aqueous nitric acid with the help software.

Fig. 2
figure 2

Multi-peak Gaussian probability curve fit of FTIR analysis of Mohuda (MH)

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3 Results and discussions

3.1 Coal properties

Proximate, Ultimate, Gross Calorific Value (GCV) and Petrographic analyses data of the raw coals are shown in Table 2. The dry mineral free volatile matter (VMdmf) contents show that (MH, GT and SL) belong to medium volatile coals (25.8%–30.3%), while ST having 21.0 wt % VM yield belongs to low volatile coal. Fixed carbon (FCdmf) ranged between 69.7% and 79.0% and GCVdmf of the samples vary between 8450 and 8640 kcal/kg and are of high maturity. The Cdmf content of studied coals varies between 86.46% and 90.88% and also indicates that the samples are matured bituminous coals. The dry mineral free hydrogen, nitrogen and oxygen ranges from 5.19%–5.87%, 1.71%–1.98% and 1.82%–5.30% respectively, typical of Indian bituminous coal. The sulphur content of Indian Gondwana coals are generally less than 1% and it ranges between 0.47% and 0.64% in the present study (Table 2).

Table 2 Proximate, ultimate, gross calorific value and petrographic analyses of coals
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Petrographic analyses of coals reveal vitrinite reflectance (VRr) 0.85%–1.24% (Table 2). Mineral free vitrinite content varies between 70.8% and 37.9%, liptinite 0.4% and 4.6% and inertinite between 37.9% and 70.8%. The volatile matter yield is the combined effect of maceral contents of the coals (Borrego et al. 2000; Guerrero et al., 2013). It is considered to be the highest for liptinite maceral followed by vitrinite and inertinite. It can be seen from the analyses that liptinite content of the samples are not very significant. Hence, a plot between vitrinite content and volatile matter is drawn (Fig. 3) which shows a straight line curve with R2 value of 0.87. This is obvious as with increase of temperature, maturity increases (increase in reflectance) resulting devolatilization and decrease in VM (Alonso et al. 2001) and hydrogen content also decreases with decrease in VM (Table 2).

Fig. 3
figure 3

Relation of Vitrinite content with respect to Volatile Matter

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3.2 Changes in weight on nitration

The change in weight due to treatment is shown in Table 3. It is observed that in glacial acetic acid medium, the weights of the samples have increased. Since, the medium is non-aqueous; less oxidation has taken place in the coal moieties resulting into gain in weight of all the studied samples. MH coal shows reduction in weight (shown with negative sign in the Table 3) in the case of nitration in aqueous medium. Rest of the samples treated with aqueous nitric acid has gained weight. MH being low in rank (VRr  = 0.85%) in comparison to the other three samples, oxidation is predominant phenomenon with simultaneous nitration in aqueous medium which has removed the aliphatic side chains resulting into decrease in weight of the said samples. Nitration is the predominant phenomena with simultaneous oxidation in stronger aqueous medium for higher rank coals.

Table 3 Change in weight due to nitration
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3.3 X-ray Diffraction studies

The results of X-ray scattering analysis are shown in Table 4. The d002 values of demineralized coals are plotted against VMdmf (wt%) (Table 2) and shown in Fig. 4. It is observed that d002 decreases with decrease in VMdmf and maintains a linear relationship with coefficient of determination, R2  = 0.82. It is known that d002 decreases with increase in maturity, vis-à-vis decrease in volatile matter yield of the coal (Lu et al. 2001).

Table 4 XRD analysis of demineralized and nitric acid treated coals
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Fig. 4
figure 4

Relation of d002 with respect to Volatile Matter

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It is found that the corresponding inter layer spacing of π-band (d002) are the least for raw coals followed by d002 values of treated coals in aqueous medium and then to glacial acetic acid medium (Table 4). The d002 values of demineralized coals as well as treated coals are plotted against dry mineral free carbon of coal samples (Cdmf) which is shown in Fig. 5a–c and it is observed that d002 value decreases with the increase of Cdmf. A similar relationship was found between d002 and elemental carbon (Maity and Mukherjee 2006; Sonibare et al. 2010, Manoj and Kunjonama 2012) for demineralized coals where a linear relationship between d002 and elemental Cdmf is established fact. The nature of the graphs is similar for the demineralized as well as treated coals. An inverse relationship is found between Cdmf and d002 (D), with increase in Cdmf content d002 decreases with R2  = 0.88 (Fig. 5a). Similar trend is also observed for the chemically modified coals having R2  = 0.93 and R2  = 0.94 for d002 (G) and d002 (A) respectively (Fig. 5b, c).

Fig. 5
figure 5

Relation of d002 with respect to Cdmf. a demineralized [(d002 (D)], b nitration in glacial acetic acid medium [(d002 (G)], c nitration in aqueous medium [(d002 (A)] coals respectively

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It is found that the corresponding d002 values of coals treated with nitric acid in glacial acetic acid and aqueous media are increased. Aqueous medium being stronger in the present studied mediums might have dissolved the more aliphatic content of coal resulting in relative increase of aromatic moieties which lead to decrease in inter layer spacing (d002) in comparison to nitration in glacial acetic acid medium.

The results of mean crystallite size (Lc) of demineralized coals and their SMCs formed due to nitration in glacial acetic acid medium and in aqueous medium are shown in Table 4. The Lc values of demineralized coals increase with increase in carbon content and vitrinite reflectance indicating crystallite sizes increase with increase in rank of the coals (Tables 2 and 4). Due to nitration, the disordering of molecular structure has taken place leading to decrease in mean crystallite size (Lc) of SMCs in comparison to the demineralized coals. Similar studies have been carried out by several other workers (Sonibare et al. 2010; Manoj and Kunjonama 2012) and corroborates with the present study.

The variation of aromaticity (fa) of demineralized as well as nitric acid treated coal in glacial acetic acid medium and aqueous medium are shown in Table 4. It is found that corresponding fa values are least for demineralized coals followed by treated coals in glacial acetic acid medium and then to aqueous medium. The increase in aromaticity in aqueous nitric acid treated coals is much more than that of nitration in glacial acetic acid medium. This suggests that aqueous medium is stronger than that of glacial acetic acid medium and is capable of removing more aliphatic contents resulting in more increase in aromaticity. The change in weight in both the media also indicates towards a similar conclusion (Table 3). The aliphatic contents are easily removed by aqueous nitric acid resulting into decrease in weight for MH coal and for relatively higher rank coals also the increase in weight is less in comparison to nitric acid treated coals in glacial acetic acid medium.

The vitrinite reflectance (VRr) is also plotted against fa and shown in Fig. 6. It shows an almost straight line relationship with coefficient of determination of R2  = 0.9614 for demineralized coals, R2  = 0.9958 for treated coals in glacial acetic acid and R2  = 0.998 for coals with nitration in aqueous medium. It is to mention here that vitrinite reflectance is a very good indicator of rank and suggests that the aromaticity is more dependent on rank of the coals. The significant finding of this study is that nitration in the aromatic structure of coals is the predominant phenomenon with simultaneous oxy-destruction of aliphatic side chains resulting increase in the aromaticity. It also shows that aqueous medium being stronger between two media used for formation of SMCs of present study is capable of removing more aliphatic components resulting into more aromaticity of the samples in the said medium.

Fig. 6
figure 6

Relation of fa with respect to VRr %. a demineralized [(fa (D)], b nitration in glacial acetic acid medium [(fa (G)] and c nitration in aqueous medium [(fa (A)] coals respectively

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The average number of aromatic layers (Nc) for demineralized and the treated coals are shown in Table 4. It can be observed that Nc have increased with increase in Cdmf content (Table 2). Similar kind of relationship between Nc and Cdmf has also been observed for demineralized pyrolyzed coals (Takagi et al. 2004; Wu and Zhang 2019) as observed in the present work. Also, the Nc values are the highest for demineralized samples followed by the corresponding nitric acid treated coals in aqueous medium and then to glacial acetic acid medium. This suggests that in treated coals, the structure of the coals is disordered due to nitration which reduces the average aromatic layers of SMCs. The degree of disorder is more in the case of glacial acetic acid treated coals than in aqueous medium.

The results of intensity ratio of π- and γ- band (I26/I20) are also known as X-ray rank parameter and for demineralized and treated coals in both the media are shown in Table 4. The variation of I26/I20 values of raw as well as treated coals are plotted against Cdmf content and shown in Fig. 7. The nature of curves is similar for raw as well as treated coals in both the nitration media. A very good linear fit of the curves are observed having R2  = 0.9963 for demineralized coal (Fig. 7a). The nitric acid treated coals show linear increase of approx. R2  = 0.96 in glacial acetic acid medium and aqueous medium respectively (Fig. 7b, c). Thus, the chemical (Cdmf) and X-ray (I26/I20) rank parameters agree with each other to express the maturity of coal. Inter-layer spacing of γ-band (Dγ) occurs around 20° and is believed to be derived from aliphatic side chains of coal molecules. The Dγ values obtained for demineralized and SMCs formed do not show any trend in the present study (Table 4).

Fig. 7
figure 7

a–c Relation of I26/I20 with respect to Cdmf. a demineralized [(I26/I20 (D)], b nitration in glacial acetic acid medium [(I26/I20 (G)] and c nitration in aqueous medium [(I26/I20 (A)] coals respectively

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3.4 Fourier transform infrared spectroscopy (FTIR)

The broad strong stretching band of –OH (hydroxyl) group is shown in the range of 3600–3200 cm−1 produced mainly due to moisture in coal. In some of the samples stretch band of alkene (=CH2) of small to medium intensity of (3100–3010 cm−1) are observed. The 2950–2800 cm−1 appeared as sharp peak of medium intensity and are assigned to aliphatic and alicyclic –CH3, –CH2 and –CH groups; though the major contributor is the –CH2 groups. The peaks ~ 1700 cm−1 has appeared due to strong stretching band of carbonyl/ketone (C=O) group. The bending vibration of alkane (–CH3) appears in the range of 1470–1350 cm−1. The peaks ~ 1600 cm−1 are observed due to medium to stretching bands of C=C aromatic compounds. Ester and/or ether groups are formed at 1320–1210 cm−1. The region between 900 and 700 cm−1 is assigned to various bands related to aromatic, out-of-plane C-H bending, –OH group with different degree of substitution.

In the samples of nitric acid treated coals, both in glacial acetic acid medium and aqueous medium, a distinct stretch asymmetric strong band of nitro (–NO2) groups of aromatic compound appears in the range of 1550–1490 cm−1. A–CH3 bending band and –CH2 group in bridges of variable intensity has been observed in the range of 1430–1290 cm−1. It has also been observed that strong stretch symmetrical nitro (NO2) group appears in the range of 1355–1315 cm−1 in nitric acid treated coals in both the media. Covalent nitro-groups (Ar–O–NO2) are formed at 1255–1300 cm−1. A strong stretch band of ether (C–O) appeared in 1300–1000 cm−1. A deformation bending arene bond of nitro-groups is absent in the range of 860–840 cm−1.

The FTIR curves of demineralized coals, nitration in glacial acetic medium and nitration in aqueous medium are suffixed by D, G and A respectively and shown in Figs. 8, 9, 10, 11. The areas of functional groups for all the demineralized as well as nitric acid treated coals in both non-aqueous and aqueous medium have been calculated by Gaussian probability density function using Origin 6.1 software and shown in Tables 5–8. In order to quantify the replacement of aliphatic side chains by nitro groups an attempt has been made to measure the area under peaks of aliphatic and alicyclic (–CH) functional group of vibration (2950–2800 cm−1) and bending vibration of alkane (–CH; 1470–1350 cm−1) are added for demineralized (raw) coals and corresponding nitric acid treated coals in both the media. The decrease in total areas of alkane group of raw and treated coals suggests the replacement of aliphatic side chains by nitro group. Total area of –CH3 group is decreased from 13.73 cm2 at 2917, 2853 cm−1 and at 1441 cm−1 for demineralized coal to 10.76 cm2 at 2922, 2856 and at 1449 cm−1 for MHG coal (Table 5). Total area decreased to 13.62 cm2 of –CH3 group in MHA at 2924, 2853 cm−1 and at 1450 cm−1 coal (Table 5).

Fig. 8
figure 8

FTIR curves of Mohuda (MH) coal

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Fig. 9
figure 9

FTIR curves of Gasalitand (GT) coal

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Fig. 10
figure 10

FTIR curves of Salanpur (SL) coal

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Fig. 11
figure 11

FTIR curves of Shatabdi (ST) coal

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Table 5 FTIR analysis of Mohuda (MH) coal
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Likewise, total area of 33.91 cm2 of –CH3 group in raw coal at 2917, 2856 cm−1 and at 1439 cm−1 is decreased to 21.47 cm2 at 2923, 2856 cm−1 and at 1452 cm−1 in GTG coal (Table 6) and total area of CH3 group is decreased to 13.59 cm2 at 2923, 2859 cm−1 and at 1447 cm−1 for SMC in aqueous medium (Table 6).

Table 6 FTIR analysis of Gasalitand (GT) coal
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Total areas of –CH3 group in demineralized coal at (2917 cm−1, 2854 cm−1 and at 1439 cm−1) is 13.91 cm2 decreased to 13.05 cm2 in SLG (2921 cm−1, 2855 cm−1 and at 1446 cm−1; Table 7) and area of CH3 group is decreased to 7.54 cm2 at 2922 cm−1, 2856 cm−1 and at 1449 cm−1 in SLA coal (Table 7).

Table 7 FTIR analysis of Salanpur (SL) coal
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Total areas of CH3 group in demineralized coal at (2918 cm−1, 2854 cm−1 and at 1440 cm−1) is 20.56 cm2 decreased to 20.13 cm2 in STG (2922 cm−1, 2856 cm−1 and at 1452 cm−1; Table 8) and total area of –CH3 group decreased to 19.99 cm2 in STA at 2922 cm−1, 2857 cm−1 and at 1447 cm−1 (Table 8).

Table 8 FTIR analysis of Shatabdi (ST) coal
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This is a very significant finding that the decrease in total areas of alkane groups of demineralized and treated coals suggests the replacement of aliphatic side chains by nitro group.

4 Conclusions

The variation of molecular structure of selected coals of Jharia Basin of Indian and their modifications through nitric acid treatment in acetic acid and aqueous media shows that the changes in the structural parameters and the aromaticity of the treated coals are dependent upon coal rank and the medium of treatment. Nitration has increased weight of SMCs in non-aqueous medium for all the coals under the present study. Whereas, the nitration in aqueous medium shows loss in weight for Mohuda (MH) coal and gain in weight for higher rank coals. Nitration in aqueous medium occurs simultaneous with oxidation of the coal matrix which removes more aliphatic side chains in the coal moieties, resulting relative increase in weight than that of non-aqueous medium. Significant observation in the present study is that nitration in both the media is capable of removing the aliphatic side chains for the coals and aromaticity increases with increase in rank (vitrinite reflectance) of coal.

FTIR studies show that coal arenes of the raw coals are converted into nitro-arenes in SMCs, the corresponding ands at 1550–1490 and 1355–1315 cm−1 respectively. In the case of low rank coals, glacial acetic acid medium being milder medium might have resulted in the formation of covalent nitro groups (Ar–O–NO2) in the range 1300–1255 cm−1 which is absent in relatively stronger aqueous medium where oxidation is also active phenomenon. FTIR study of nitric acid coals treated in both the media show introduction of nitrogen (–N) and oxygen (–O) containing groups and newly formed aromatic nucleus different from the raw coals which confirms the formation of structurally modified coals (SMCs). The areas under each functional group for demineralized samples and their corresponding SMCs have been calculated. The results show that the content of alkane group is decreased in SMCs corresponding to aliphatic and alicyclic (–CH) functional group of vibration (2950–2800 cm−1) and bending vibration of alkane (–CH; 1470–1350 cm−1). The decrease in total areas of alkane group in treated coals than that of raw coals suggests the replacement of aliphatic side chains by nitro group.

The present study also reveals that in the SMCs of coals namely GT, SL and ST shows a considerable increase in aromaticity in aqueous medium and these are candidate coals for manufacturing of specialty carbon materials such as fullerene, artificial graphite, activated carbon and artificial diamond.

The major finding of this exhaustive study is highlighted below:

  1. (1)

    Nitration has increased weight of SMCs in non-aqueous medium for all the coals whereas the nitration in aqueous medium shows loss in weight for low rank coal (MH) and gain in weight for higher rank coals.

  2. (2)

    Nitration in aqueous medium occurs simultaneous with oxidation of the coal matrix which removes more aliphatic side chains in the coal moieties, resulting relative decrease in weight than that of non-aqueous medium.

  3. (3)

    During nitration, loss of aliphatic side chains is more in aqueous medium than that of glacial acetic acid medium results to the relative increase of aromatic moieties in aqueous medium.

  4. (4)

    The XRD structural parameters like mean crystallite size (Lc) and average number of aromatic layers (Nc) of corresponding SMCs have decreased in comparison to parent coals which indicate reorganization of spatial framework in SMC and disordering of crystallites.

  5. (5)

    Nitration in stronger aqueous medium has resulted into increase in XRD rank (I26/I20) than raw coals.

  6. (6)

    X-ray structural parameters are more dependent on coal rank and the content of macerals than only Cdmf.

  7. (7)

    FTIR studies show that coal arenes of the raw coals are converted into nitro-arenes in SMCs, the corresponding bands at 1550–1490 and 1355–1315 cm−1 respectively.

  8. (8)

    In the case of low rank coals, glacial acetic acid medium being milder medium might have resulted in the formation of covalent nitro groups (Ar–O–NO2) in the range 1300–1255 cm−1 which is absent in relatively stronger aqueous medium where oxidation is active phenomenon.

  9. (9)

    FTIR study of nitric acid coals treated in both the media show introduction of nitrogen (–N) and oxygen (–O) containing groups and newly formed aromatic nucleus different from the raw coals which confirms the formation of structurally modified coals (SMCs).

  10. (10)

    The decrease in total areas of alkane group of treated coals in comparison to raw coals suggests the replacement of aliphatic side chains by nitro group and hence area of –CH3 group is decreased.