1 Introduction

Humic acid has received tremendous research attention due to its wide range of application in the field of electrochemical devices (Yin et al. 2014; Wasiński et al. 2014; Zhu et al. 2015), agriculture sectors (Janos and Kozler 1995), rubber industry, colour industry, veterinary science, human medicine, nanoscience (Erdogan et al. 2007; Niu et al. 2011; Zhou et al. 2011; Peng et al. 2012; Zhang et al. 2013; Tang et al. 2017), waste water treatment (Liu et al. 2008; Li et al. 2011; Jiang et al. 2014; Tang et al. 2014), and as a dispersant of ceramic powders (Souza and Braganca 2018). Humic acid can also be used as raw material for the synthesis of graphene oxide (Powell and Beall 2015; Duraia and Beall 2015a), humic acid-based humidity sensor (Duraia et al. 2015b). The humic acid was generally isolated from lignite and also from coal by some researchers (Tripathi et al. 2009; Das et al. 2015, 2017a, b; Tang et al. 2017; Wang et al. 2017; Xiao et al. 2018; Cheng et al. 2019). However, the physico-chemical properties and mass production of humic acid from different types of coal is dependent upon the rank and coalification process (Stevenson 1994; Kurkova et al. 2004).

Different methods such as oxidation followed by alkaline extraction (Erdogan et al. 2007), solid phase activation process (Tang et al. 2017), bioconversion (Xiao et al. 2018; Tripathi et al. 2009), KOH-hydrothermal process (Cheng et al. 2019), non-catalytic oxidation with oxygen (Dekker et al. 1990), oxidation using nitric acid (Rousa et al. 1994), alkaline extraction followed by acidic precipitation and membrane separation (Skhonde et al. 2006), oxidation with H2O2 and KMnO4 (Fong et al. 2007), and the method applied by the International Humic Substance Society (IHSS) (http://humic-substances.org) are used to isolate humic acid from coal.

The utilization of the low-quality coals to make value-added products are increasing progressively among the carbon researchers and industries due to the sharp fall of good and high-quality coal around the world (Das et al. 2013, 2016, 2017a, b, 2019). Thus, the production of humic acid from low-quality coal is one of the new focus areas of research to facilitate the value-added products (Tripathi et al. 2009; Das et al. 2013, 2015, 2017; Cheng et al. 2019; Souza and Braganca, 2018). In our earlier studies, we reported the fabrication of humic acid from Cenozoic age high sulphur Northeast region (NER) of Indian coal (Das et al. 2013, 2015, 2017a, b) and their uses as a host material for the synthesis of iron oxide nanocomposite material followed by catalytic application (Das et al. 2017a, b).

In the present investigation, the fabrication of coal-based humic acid is reported and a feasibility study is also reported for application in acid mine drainage (AMD) water treatment and electrochemical devices such as capacitors. Although, humic acid has wide range of applications, but most of the humic is commercially purchased (Yin et al. 2014; Wasiński et al. 2014; Zhu et al. 2015) and the use of coal-based humic acid in AMD water treatment (particularly for Northeast region of India) and electrochemical devices is found to be sparse in the literature.

Acid mine drainage (AMD) is a severe problem created in the high sulfur coalmines around the world including in Northeast region of Indian (Baruah et al. 2010a, b; Chabukdhara and Singh 2016; Dutta et al. 2017, 2018). The mine spoils generated during mining of coals is highly enriched with sulfur and pyrite upon oxidation and hydrolyzing releases acid water (Baruah et al. 2005, 2006; Baruah and Khare 2007, 2010a, 2010b; Chabukdhara and Singh 2016; Dutta et al. 2017, 2018). The AMD waters lower the pH of the streams, completely kill aquatic lives, increase acidity in the nearby soil during overflow and releases toxic metals at low pH (Baruah et al. 2005, 2006, Baruah and Khare 2007, 2010a, 2010b; Chabukdhara and Singh 2016; Dutta et al. 2017, 2018). Many toxic and heavy elements like V, Cr, Mn, Ni, Cu, Zn, As, Cd, Sb, and Pb are present in the AMD waters of Northeast India and create adverse environmental effect in the vicinity of collieries (Baruah et al. 2010a, 2010b; Chabukdhara and Singh 2016; Dutta et al. 2017, 2018). The concentration of Fe, Mn, Zn, Cu, Ni, and Pb in mine-waters of the Jaintia and Makum coalfields of Northeastern region of India is reported to high as compared to the other mining sites of India (Chabukdhara and Singh 2016).

Therefore, the treatment of AMD water needs attention for removal of toxic heavy metals before the aqueous discharge is allowed to enter streams and water ways. Dowarh et al. (2009) reported the eco-restoration of overburden dumping sites of coal mine area in Tirap collieries, Northeast India to mitigate AMD problems along with the environmental adverse effect. Baruah et al. (2010b) also carried out a pilot plant study for the treatment of AMD water from coalmines of Meghalaya, Northeast India based on the sequential alkaline treatment coupled with biological processing. The nano-mineralogy (Dutta et al. 2017) and physico-chemical analysis of aqueous leaching (Dutta et al. 2018) of the coal, coal-mine overburden, and AMD water from Northeastern coalfield of India was also reported. However, a suitable and adaptable method is still required to mitigate the AMD problem in the high sulfur coal-mine area of Northeastern region of India.

Therefore, a feasibility study has been made to solve the issues related to the AMD of Northeastern region of India by using coal-derived humic acid since it has an excellent metal complexing ability (Pahlman 1988; Saied et al. 2005; Das et al. 2015) and has been used for waste water treatment by several workers (Liu et al. 2008; Jiang et al. 2014; Li et al. 2011; Tang et al. 2014). The humic acid was reported to be superior for removing of toxic metals such as Cd, Hg, and Pb as compared to the CaO in the pH range 4–8 (Pahlman 1988). It was found that humic acid metal interaction is pH dependent and forms chelates more strongly with metals in + 2(II) oxidation state. The reactivity order for metal ion-humic acid chelations is reported to be in the order of Pb2+>Cu2+> Fe2+> Ni2+> Zn2+> Cr3+ (Saied et al., 2005).

The present work also describes the electrochemical performance of the coal-derived humic acid with a promising potential for application in the field of electrochemistry (Yin et al. 2014; Wasiński et al. 2014; Zhu et al. 2015). In contrast, the study would make a new path in coal-based carbon materials for using in AMD water treatment and electrochemical devices.

2 Experimental sections

2.1 Coal sample and reagents

The coal sample from the Northeastern region of India was selected for this study. The raw coal sample (ROM) was manually crushed to below 1/8″ sizes and ball milled to powder form (0.211 mm sizes). Analytical grade chemical such as H2O2 (30%), NaOH, HCl, Copper (II) chloride dehydrate, and Cadmium chloride were commercially purchased. Polyvinylidene fluoride (PVDF) and N-methyl 2-pyrrolidine (NMP) were also commercially purchased and used for the electrochemical characterization of the coal-derived humic acid. Standard humic acid (Sigma Aldrich) was also commercially purchased and used for the comparative study with the coal-derived humic acid.

2.2 Chemical and analytical characterizations

The proximate (moisture, ash content, volatile matter, and fixed carbon) and elemental analyses (carbon, hydrogen, and sulfur) of the raw coal, oxidized coal, and coal-derived humic acid were done by using TGA 701 Thermogravimetric Analyzer, Truspec CHN Macro Determinator, and S-144 DR Sulfur Analyzer as per the standard ASTM D7582-15, ASTM D3176-15, and ASTM D3176-15 methods, respectively. In order to evaluate the thermal stability of the coal-derived humic acid, thermal analyses (non-isothermal) were carried out by using a thermal analyzer (Model: Netzsch STA 449F3) at a heating rate of 5 °C per min in a nitrogen atmosphere from room temperature to 1000 °C. The UV–Vis (Ultraviolet–visible) spectra were recorded with a UV–Visible Spectrophotometer (UV 1000+, Lab India). An FTIR spectrometer (SPECTRUM 100, Perkin Elmer, USA) associated with IR software was used to record the Fourier-transform infrared (FT-IR) spectra of the coal-derived humic acid and humic acid-metal complexes by using KBr pellets with 4 cm−1 spectral resolution. The surface morphology was analyzed by using a field emission-scanning electron microscope (FE-SEM) (ZEISS SIGMA, Carl ZEISS Microscopy, accelerating voltage: 0.5–30 kV) integrated with an Oxford energy dispersive X-ray spectroscopy (EDS). The SEM images were further developed by “ImageJ” (version 1.47) software.

2.3 Isolation of humic acid from coal

The humic acid was isolated from the coal sample as per the method reported in our previous studies (Das et al. 2013, 2015, 2017a, b). Briefly, 100 g of powder coal samples were oxidized by using 250 mL hydrogen peroxide (30%) in an ice-cold condition. After the exothermic reaction cease, the reaction mixture was cooled to room temperature, filtered, and washed with distilled water until the pH of the filtrate became neutral. The oven dried oxidized coal samples was then refluxed with 1N NaOH solution for 6 hrs with continuous stirring, cooled to room temperature and kept for overnight. The mixture was then filtered and the alkali soluble portion was collected. The alkali soluble portion was then acidified to pH 1–1.5 by using 6.0 M HCl and kept overnight in order to precipitate the humic acid. After complete precipitation, the humic acid was collected by centrifugation, purified with dilute HCl and washed with ultra-pure water until the filtrate became neutral. The final product of humic acid was recovered, freeze dried, and stored for subsequent analysis.

2.4 Metal-humic acid complex formation study

The complex formation study was conducted by using 0.1% (W/V) solution of coal-derived humic acid with metal ions such as Copper (Cu2+) and Cadmium (Cd2+). Cu2+ and Cd2+ solutions were prepared from respective Copper (II) chloride dehydrate and Cadmium (II) chloride analytical grade salt, respectively. Both the solution was prepared in 0.1 N NaOH and kept for half an hour. The FTIR spectra of the dried precipitates i.e. humic acid-metal complex was recorded and compared with that of the coal-derived humic acid.

2.5 Treatment of acid mine drainage (AMD) water with coal-derived humic acid

For these experimental purposes, AMD water were obtained from the Shkentalang point source, Jaintia Hills, Meghalaya and treated with coal-derived humic acid solution. For that purpose, 1% (W/V) and 0.5% (W/V) coal-derived humic acid solution in 0.1N NaOH were prepared. AMD water was treated with coal-derived humic acid solutions (in 4:1 proportions) for four different time periods (5, 60, 180 min, and over night). The mixtures were filtered and concentrations of Zn, Cu, Cd, and Pb in all samples were determined by using a Atomic Absorption Spectrometer (Model: A Analyst-700, Make: Perkin Elmer). The pH of the original AMD water and the humic acid treated AMD water samples were also determined by using a microprocessor-based pH meter (model 1012E).

2.6 Electrochemical properties of coal-derived humic acid

The electrochemical properties of coal-derived humic acid were tested in a electrochemical work station (VSP3 and FlexP0160; BioLogic Science) using three electrode system (Ag/AgCl as the reference electrode and Pt-wire as the counter electrode) in order to check the suitability for application in electrochemical devices. The synthesized coal-derived humic acid was coated on a glassy carbon electrode and used as working electrode. The slurry of electrode material was prepared by mixing of coal-derived humic acid and polyvinylidene fluoride (PVDF) binder in a ratio of 93:7 and N-Methylpyrrolidone (NMP) as solvent. The slurry was ultrasonicated for approximately six hours for homogenous mixing. Then the slurry was coated on glassy carbon working electrode. In the present investigation, 1 M H2SO4 was used as an aqueous electrolyte.

3 Results and discussion

3.1 Characterizations of raw coal and isolated coal-derived humic acid

The physico-chemical properties of the raw coal and isolated humic is summarized in Table 1, which indicates the coal to be of low-ash and high-sulfur in nature. The surface morphology (SEM analysis) of the coal-derived humic acid is found to be not smooth, and flakes sheets are appeared (see Fig. 1a, b), which are mainly composed of carbon (76.05 at.%) and oxygen (22.67 at.%) as confirmed from the SEM-EDX analysis (Fig. 1c, d).

Table 1 Physico-chemical properties of the raw coal and isolated humic acid (wt%)
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Fig. 1
figure 1

a, b SEM analysis of coal-derived humic acid, c, d SEM-EDX of coal-derived humic acid

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In the UV–Vis spectra of coal-derived humic acid (Fig. 2a), the peak observed at around 220–300 nm is due to the π→ π* transition of π -electron of the aromatic groups present in coal-derived humic acid (Das et al. 2013, 2015, 2017a, b). Similar results were also obtained after recording the UV–Vis spectra of standard humic acid as shown in Fig. 2a. The degree of humification and condensation of aromatic carbon network was also investigated by determining the E4/E6 ratio (Abs465/Abs665) and ∆ log K (log Abs400-log Abs600) (Campitelli et al. 2006; Das et al. 2015). The E4/E6 ratio and ∆ log K was found to be almost identical for coal-derived humic acid and standard humic acid (Table 2). The ∆ log K value of the coal-derived humic acid is found to be ≤ 0.6, indicating the high degree of humification (Matsui et al. 1984; Das et al. 2015).

Fig. 2
figure 2

a UV–visible spectra of coal-derived humic acid and standard humic acid, b thermal analysis of coal-derived humic acid, c FTIR spectra of coal-derived humic acid and standard humic acid, d FTIR spectra of coal-derived humic acid and its metal complex with Cu (II) and Cd (II) ions, e FTIR spectra of coal-derived humic acid and its metal complex with Cu (II) and Cd (II) ions in the range of 1000–1500 cm−1, f removal of metals from AMD water by coal-derived humic acid

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Table 2 UV–visible spectroscopic data
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The thermal stability of the coal-derived humic acid was evaluated by carrying out the thermogravimetric analysis (TGA) of the sample as shown in Fig. 2b. The weight loss is generally observed with increase of temperature. The initial weight loss (12.39%) observed in the range of 30–150 °C is due to the loss of free moisture (Skhonde et al. 2006, Fong et al. 2007). Between 150–400 °C, weight loss (17.58%) is observed due to the decarboxylation reaction and loss of least stable carboxylic acids (Skhonde et al. 2006, Kolokassidou et al. 2007). Between 400–800 °C, mass loss (19.39%) is observed due to the loss of more stable phenolic acids group (Skhonde et al. 2006, Kolokassidou et al. 2007). The conversion of aliphatic C-H group to aromatic C-H group takes place at a temperature 200–600 °C (Skhonde et al. 2006, Kolokassidou et al. 2007, Lu et al. 1997). The maximum weight loss is observed at 286 °C due to the loss of methyl and other aliphatic groups. The residual mass is found to be 42.55% at 1000 °C in nitrogen environment. Thus, the coal-derived humic acid is found to be relatively stable up to about 200 °C; above which a mass loss is experienced.

The FTIR spectra of coal-derived humic acid and humic acid-metal complexes provide information on structure, functional groups, and information of modes of complexes. The FTIR spectra were recorded for coal-derived humic acid, standard humic acid, and humic acid-metal complexes (Cu and Cd) (see Fig. 2c–e), and the corresponding peak assignments are summarized in Table 3. The FTIR spectra of coal-derived humic acid is compared with the standard humic acid and found to be similar in nature (Fig. 2c, Table 3) and is also in accordance with the results reported earlier (Das et al. 2015, 2013, 2017a, b). The FTIR intensity within the range of 3000–3500 cm−1 for Cu- and Cd-humic acid complexes is higher than the coal-derived humic acid due to the hydration of water and change in the dipole moment that is caused by change of electronic environment (Erdogan et al. 2007). The absorption band appeared at 1600–1650 cm−1 is due to the C=C, C=O, and COO− group and the intensity is found to be increased for metal-humic acid complexes (Cu-humic acid and Cd-humic acid) because of the formation of complexes between metal ion with the functional group as well as change in dipole moment the functional group (Erdogan et al. 2007). The two new bands appeared at 1187 cm−1 and 1111 cm−1 due to formation of complex structure between carboxylic acid group of the coal-derived humic acid and metal ions (Cu and Cd). The carboxylic acid groups of coal-derived humic acid may take part in the complex formation via both ionic and non-ionic bonding (Baruah 1982; Steelink 2002), while salicylic acid type chelates may be formed by the metal ions with the OH groups where both the carboxyl and phenolic groups are involved (Baruah 1982).

Table 3 Major infrared absorption bands (cm−1) for coal-derived humic acid, standard humic acid, and its metal complexes
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The physico-chemical, UV–Vis, and FTIR studies revealed the formation of humic acid from coal. The FTIR study indicates the formation of metal-humic acid complex.

3.2 AMD water treatment by using coal-derived humic acid

The extent of metal removal by coal-derived humic acid from AMD water sample is found to be independent of time as shown in Fig. 2f. The removal of metal from AMD water by using coal-derived humic acid found to be in the order of Pb > Cu > Zn > Cd (Fig. 2f) (Saied et al. 2005). But the extent of removal of Lead (Pb) increases more after 60 minutes when treated with 1% coal-derived humic acid solution. The pH of AMD water is found to be increased after treatment with coal-derived humic acid (see Table 4). A mechanism of isolation of humic acid from coal and their use for AMD water treatment is depicted in Fig. 3.

Fig. 3
figure 3

Plausible mechanism of isolation of humic acid from coal and use for the AMD water treatment

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Table 4 pH of original AMD water and coal-derived humic acid treated AMD water samples
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3.3 Formation mechanism and main control factors of humic acid

Humic acids consist of a mixture of weak aliphatic carbon chains and aromatic carbon rings, which are not soluble in water under acidic conditions but are soluble in water under alkaline conditions. In the coalification process, plant debris is first converted into humic substances and progressively humic substances are converted to peat, lignite, brown coal, bituminous coal, and finally into anthracite coal by condensation followed by diagenesis process (van Krevelen 1961; Stach et al. 1982; O’Keefe et al. 2013; Dai et al. 2020). During the coalification process, the oxygen content as –COOH decreases, and that as –OH increases relatively. Thus, the low-quality coals are much more suitable than high-quality coals for the extraction of humic acid (Cheng et al. 2019). In the present study, the sub-bituminous Cenozoic-age coal sample was selected from the Northeastern region of India. Oxidation of coal in presence of hydrogen peroxide destroyed the macromolecular structure of coal, leading to the breakage and deformation of weak chemical bonds and alkyl structure, the reduction of relative molecular mass, and increases the content of oxygen-containing functional groups (Fig. 3). The addition of NaOH also destroyed the chelating forces between humic acid and metal ions present in oxidized coal samples and solubilized the humic acid (Fig. 3). The alkaline soluble portion, which contains humic acid is separated from the humin portion (alkaline insoluble portion) via the filtration process. In an acidic medium, the hydrogen (H+) is bound to the surface functional groups of the humic acid. Due to these protonation phenomena of humic acid in an acidic medium, humic acid became hydrophobic and formed a micelle-like structure (Cheng et al. 2019; Souza and Braganca, 2018). The micelle-like structures completely expel the water around the humic acid molecules at pH 1–1.5 and as a result, the humic acid became insoluble and precipitates. The rank/grade of coal samples, sizes of the coal particles (small size coal particles increase the contact between the alkali and coal samples and leads to the enhancement in the humic acid yield), reaction conditions (temperature and time), and amount of alkali and pH at acidic medium are the main control factors for the production of humic acid.

3.4 Electrochemical properties of coal-derived humic acid

3.4.1 Cyclic voltammetry study

The cyclic voltammetry (CV) analysis was carried out to evaluate the oxidation-reduction behavior of coal-derived humic acid. CV analysis was done at different scan rates (10 mV/s, 20 mV/s, 50 mV/s, and 100 mV/s) in the potential range of − 0.2 to 0.2 V. Leaf-like structures were obtained, and oxidation-reduction peaks were found to be absent as shown in Fig. 4a. The absence of redox peaks revealed that electrochemical rate of charge and discharge is pseudo-constant over entire voltammetry cycles (Yang et al. 2012). The electrode material was observed to have a stable capacitive process as the curve is symmetric (Fig. 4a) (Gu et al. 2016) and showed electrical double layer capacitor properties. The specific capacitance (Csp) of the coal-derived humic acid was calculated by using the following Eq. (1):

$$\text{C}_{\text{sp}}=\frac{\int I\left(E\right)dE}{m\times \varDelta V\times v}$$
(1)

where, ‘\(\int I\left(E\right)dE\)’ is the area of the CV curve, ‘m’ is the mass (g) of the coated material, \(\Delta V\) is the potential range (V) and \(v\) is the scan rate. The specific capacitance is found to be 7, 4, 2, and 1 mF/g in the scan rates of 10, 20, 50, and 100 mV/s, respectively. The specific capacitance is found to be decrease as the scan rate increases, which may be due to the fact that the higher scan rates do not allow enough time for the ions to diffuse into the pores and less available surface area is used (Cao et al. 2018).

Fig. 4
figure 4

Electrochemical performance of coal-derived humic acid in three-electrode system in 1M H2SO4. a Cyclic voltammetry at different scan rate 10, 20, 50, and 100 mV/s respectively; b, c Chronopotentiometry (CP), d Potentio Electrochemical Impedance Spectroscopy (PEIS) with Nyquist plot and equivalent circuit

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3.4.2 Chronopotentiometry (CP)

The charge storage performance and stability of the coal-derived humic acid after several charge and discharge cycles were studied by using chronopotentiometry (CP) analysis (Fig. 4b, c). CP was performed in the potential range of – 0.2 to 0.2 for 1000 cycles and found to be stable. The curve was found to be symmetric and linear and the quick current voltage response indicated good electrochemical performance. The linear curve with constant slopes over the total range of potential is observed (Shabeeba et al. 2018). The specific capacitance is determined by using the following equation:

$$C_{\text{sp}}=\frac{Idt}{m\times \Delta V}$$
(2)

where ‘I’ is the discharge current (A), ‘dt’ is the discharge time (s), \(\Delta V\) is working potential window (V), and m signifies mass (g) of active electrode. The specific capacitance is found to be 22 mF/g.

3.4.3 Potentio-electrochemical impedance spectroscopy (PEIS)

PEIS measurement was done in the frequency range 100 mHz to 100 kHz and data is plotted as Nyquist diagram. The Fig. 4d shows a half semicircular curve which can be explained by presence of surface passive layer. The equivalent circuit of Nyquist plot is plotted by using Bio-logic software associated with the equipment. In the circuit, R1 is electrolyte resistance, Q is the double layer electrical capacity and R2 is charge transfer resistance (Dimitrijević et al. 2019). R1 is found to be 8.32 Ω and R2 is 324 kΩ, and Q is 3.6 microF/s. The deviation from an ideal semicircle was attributed to the frequency dispersion and the inhomogeneity of the passive layer surface (Liu et al. 2018).

The electrochemical properties of the coal-derived humic acid can be improved by the use of suitable activating agents in the synthesis process and with the addition of additives in the electrode material. The energy density and power density can be improved by using organic electrolyte and hence by increasing the potential window. In order to improve the conductive properties of the material, great attention has to be given in the electrode fabrication process in the future.

4 Conclusions

This study leads to the conclusion that humic acid can be easily isolated from inferior quality coals of the Northeastern region of India. The amount of isolation of humic acid from coal depends upon the rank/grade of the coals. The coals having low ash, high carbon content, high oxygen-containing functional groups are suitable for isolation of humic acid. The product developed meets the standards laid down by the International Humic Substances Society (IHSS). The isolated coal-derived humic acid is found to be effective in removing toxic metals like Cu, Cd, Pb and Zn from AMD water samples leading to the management of AMD. Moreover, the pH of the AMD water is also found to increase by the addition of coal-derived humic acid solution indicating their suitability for use in the treatment of acidic water, reclamation of acidic soil, and as a metal detoxification agent for various purposes. The complex formation ability of coal-derived humic acid also promotes retention and accumulation of heavy metal and may also play a vital role in the agricultural sectors as a soil conditioner. Moreover, the coal-derived humic acid possesses optimizable electrochemical properties and promising specific capacitance of 7 mF/g at scan rate 10 mV/s (cyclic voltammetry analysis) and 22 mF/g with cycling stability over 1000 cycles within the potential window 0.4 V (charge-discharge analysis). The optimizable and easily processable coal-derived humic acid can be used as a low-cost, environmentally friendly, and non-toxic carbon electrode material for electrochemical capacitors.