3.1 Effects of Carbon Sources and Nutrients on the Acidification of Coal Gangue
As shown in Figure 2, the pH of the control group and treatment groups showed a downward trend within 35 d after the start of the experiment, indicating that the coal gangue exhibited different degrees of acidification. Among the groups, the pH of the CK treatment decreased significantly from 6.03 to 4.37 from 0-7 d, while the pH of all the treatment groups increased slightly and was significantly higher than that of the control group. The pH of the control group and the treatment groups decreased from 14-21 d, with a greater decrease in pH in the treatment groups. The pH of each treatment group was still higher than that of the control group after 14 d, but the difference was not significant. This may be due to the depletion of exogenous nutrients added to the gangue, resulting in a decrease in heterotrophic microbial activity. By comparing the T1, T2, and T3 treatments, we concluded that further addition of inorganic salt and changes to the concentration of additives does not significantly alter the pH of the coal gangue leachate.
Conductivity EC is commonly used to characterize the soluble salt content in solutions. Figure 3 shows the changes in conductivity for the different treatments within 0–35 d after the beginning of the experiment. The EC of all the treatment groups increased to varying degrees due to the addition of exogenous substances at the beginning of the experiment. During the experiment, the EC of the leachate of the control group remained essentially stable, while the EC of the treatment groups first increased and then decreased with time. The EC of the T1 treatment decreased from 1078 µS•cm−1 to 663 µS•cm−1 and then increased to 1232. After 28 d, the EC of the T1 treatment group was significantly higher than that of the control group and other treatment groups. The minimum EC values of the T2 and T3 treatments were 365 and 412, respectively, which occurred at 28 d. These results showed that the addition of carbon sources and inorganic salt did not significantly increase the soluble salt content of the leachate of coal gangue, while the addition of a carbon source (sodium lactate) alone led to a significant increase in the EC of the leachate, which may be due to the change in microbial community composition on the surface of the coal gangue.
3.2 Effects of adding carbon sources and nutrient salts on bacterial species diversity in coal gangue
The microbial diversity index of each treatment is shown in Table 3. In ecology, the Chao index and Ace index are commonly used to estimate the total number of species. The four treatments had the same relationship according to both the Chao index and the Ace index, and the order from high to low was Tx4 > Tx3 > Tx1 > Tx2. The Shannon index and Simpson diversity index are commonly used to reflect the alpha diversity index. The alpha diversity index of the control group (Tx4) was the highest, followed by those of Tx3, Tx1, and Tx2. The Shannon evenness index reflects the distribution uniformity of the individual number of species in a community. The experimental data showed that the distribution uniformity of all the treatment groups was lower than that of the control group (Tx4), indicating that the number of dominant species in the treatment groups increased and constituted higher proportion in the community.
The experimental results show that the addition of exogenous nutrients reduces the microbial diversity in coal gangue, causing the colony structure to tend to be individualized and further increasing the dominance of the dominant bacteria, which is consistent with the finding of Marris’s study that the application of biochar reduces the diversity of soil microorganisms (Marris, 2006). Su et al. (2020) suggested that the addition of a carbon source may affect the activities and metabolic mechanisms of some functional microorganisms in the soil, thus altering the distribution of organic carbon in the soil carbon pool and ultimately leading to a decrease in both soil bacterial community diversity and species abundance.
Table 3
Alpha diversity index statistics
Sample | Chao | Ace | Shannon | Shannon evenness | Simpson |
Tx-1 | 468.00 | 466.23 | 4.34 | 0.71 | 0.06 |
Tx-2 | 313.00 | 312.26 | 3.95 | 0.69 | 0.07 |
Tx-3 | 603.43 | 588.64 | 4.38 | 0.69 | 0.05 |
Tx-4 | 764.49 | 758.69 | 5.13 | 0.78 | 0.01 |
3.3 Effects of adding carbon sources and nutrient salts on the bacterial community structure in coal gangue
More than 1200 bacterial genera were identified in coal gangue samples through high-throughput sequencing analysis. The collinearity of the main phyla with relative abundance in the top 10 is shown in Fig. 4. The common dominant phyla in the treatment groups and the control group were Proteobacteria (38.53%-53.45%), Actinobacteria (11.43%-17.10%), and Bacteroidetes (1.94%-7.01%), which constituted 54%-72% of the bacterial species in the samples. Firmicutes in the treatment group was relatively predominant, with a relative abundance of more than 30%, while the relative abundance of Firmicutes in the control group was only 3.8%. The abundance of Acidobacteria and Gemmatimonadetes was higher in the control group (at 4.0% and 4.4%, respectively), while the abundance of these two types of bacteria in the treatment groups was lower than 1%. Studies have shown that pH, nitrate-nitrogen, and organic carbon are important factors affecting the abundance and distribution of Proteobacteria and Acidobacteria (Yao et al.,2016; Zhou et al.,2020).
The distribution of the main genera in the treatment groups and the control group is shown in Figure 5. Arthrobacter, Enterococcus, Acinetobacter and Methylobacterium were the main dominant genera in the treatment groups, and the abundance of these genera increased in response to the addition of carbon sources. Arthrobacter is considered to degrade organic pollutants and adsorb heavy metals (Prasad et al., 2013; Sebai et al., 2011; Ye et al., 2014), and a variety of Arthrobacter strains that can grow with organic pollutants as carbon sources and energy sources have been isolated thus far (Arora & Jain, 2011; Cai et al., 2011; Wang et al., 2015). Enterococcus is considered to play an important role in the nitrogen and phosphorus cycles of ecosystems and can better adapt to coal gangue reclamation soil, with a higher relative abundance in reclaimed soil than in natural soil (Hou et al., 2017; Li et al., 2018). Methylobacterium is the main flora of the aerobic methane-oxidizing bacterial community. The input of inorganic nitrogen promoted the growth rate and relative abundance of Methylobacterium in the soil, which may be because it does not have the ability to fix nitrogen but relies only on the physiological characteristics of exogenous nitrogen to obtain nutrients.
In addition, the addition of OM and inorganic salt also increased the relative abundance of Listeria, which may be worth noting. Listeria is a common saprophytic bacterium in the soil that exists in various types of environments, and Listeria monocytogenes can cause foodborne diseases. The distribution of Listeria is regulated mainly by soil moisture, molybdenum concentrations, and salt concentrations (Liao et al., 2021). Yoon et al. (2021) reported that an increase in the richness and diversity of the soil bacterial community structure is beneficial in inhibiting the proliferation of Listeria.
The main members of the control group were Sphingomonas and Gemmatimonas, which are also involved in nitrogen and phosphorus cycling and improve soil physical and chemical properties (Chee-Sanford et al., 2019; Song et al.,2021). The abundance of these genera in the treatment groups was significantly reduced, which may be due to competition between bacterial communities. It is worth noting that Thiobacillus was not the dominant genus in the treatment groups or in the control group, indicating that Thiobacillus was not the main influencing factor of the oxidation or acid production in coal gangue in the early storage period of new coal gangue.
3.4 Effects of carbon source and nutrient addition on bacterial community function
The functions of the microbial community were predicted by the FAPROTAX database, focusing on the cycling functions of sulfur, carbon, hydrogen, and nitrogen. Different microbial functions and their corresponding abundance are shown in Table 4 (microbial functions with an abundance of 0 or that did not differ were removed).
The experimental group had stronger nitrification and denitrification, which could accelerate the nitrogen cycling rate. The low abundance of nitrogen-fixing microorganisms in the experimental group may be due to the addition of nitrogen, which reduced the dependence of microorganisms on nitrogen fixation. Moreover, the numbers of microorganisms involved in the sulfur cycle were increased in the experimental groups, which indicated that the addition of carbon sources and sulfate could increase the abundance of sulfur-metabolizing functional bacteria in microbial communities and that sulfate addition that continued after 7 days would not affect the sulfate respiration ability of microbial communities. The addition of carbon sources and nutrients enhanced the utilization of methyl compounds, aromatic compounds, and aliphatic compounds in microbial communities and reduced the degradation ability of chitin and hydrocarbons, which was mainly caused by changes in the main electron donors of microorganisms. In addition, almost no bacteria with iron respiratory function were found in any of the treatments, which was consistent with the bacterial community composition analysis results.
Table 4
Predicted functions of flora according to the FAPROTAX database
Group | Tx-1 | Tx-2 | Tx-3 | Tx-4 |
Nitrogen cycle | Nitrogen respiration | 700 | 458 | 675 | 503 |
Aerobic ammonia oxidation | 330 | 251 | 162 | 77 |
Nitrification | 330 | 264 | 198 | 87 |
Denitrification | 215 | 313 | 398 | 11 |
Nitrogen fixation | 217 | 230 | 270 | 423 |
Nitrite respiration | 249 | 313 | 415 | 11 |
Ureolysis | 3589 | 2715 | 1385 | 867 |
Sulfur cycle | Sulfate respiration | 72 | 119 | 96 | 0 |
Sulfur respiration | 0 | 0 | 33 | 0 |
Thiosulfate respiration | 0 | 0 | 12 | 0 |
Respiration of sulfur compounds | 72 | 119 | 141 | 0 |
Dark sulfide oxidation | 282 | 646 | 540 | 97 |
Dark thiosulfate oxidation | 49 | 0 | 0 | 5 |
Dark oxidation of sulfur compounds | 445 | 1156 | 1006 | 112 |
Carbon cycle | Methanol oxidation | 3572 | 2973 | 2084 | 25 |
Methylotrophy | 3572 | 3038 | 2084 | 71 |
Chitinolysis | 684 | 120 | 168 | 1940 |
Fermentation | 20069 | 24740 | 20116 | 389 |
Aromatic compound degradation | 3322 | 4582 | 3756 | 811 |
Aliphatic nonmethane hydrocarbon degradation | 144 | 98 | 240 | 14 |
Hydrocarbon degradation | 289 | 184 | 257 | 463 |
Chloroplasts | 316 | 439 | 2419 | 677 |
Phototrophy | 84 | 131 | 15 | 16 |
Other | Dark hydrogen oxidation | 179 | 313 | 428 | 11 |
Iron respiration | 0 | 0 | 33 | 0 |
Chlorate reducers | 26 | 31 | 7 | 0 |
Chemoheterotrophy | 36836 | 42122 | 33798 | 15028 |
To elucidate the response mechanism of the bacterial community to the addition of carbon sources and nutrients, the possibility of inferring microbial functions based on 16S rRNA sequences was provided by PICRUSt, which used a COG (orthologous group cluster) classification scheme to explore the possibility of collecting bacteria to develop adaptive metabolic functions. As shown in Fig. 6, the abundance of some COGs related to metal detoxification and organic degradation, such as transcriptional regulators (COG0583, COG1309, COG1846, COG2204) and dehydrogenase (COG1012, COG1028), was high. The abundance of COGs in the control group was higher than that in the other treatments or was essentially the same, except for COG0583. Hydrolases are known to be beneficial to the degradation of organic matter, while dehydrogenases (such as oxidoreductase) may be involved in the oxidation of S− (Zhang et al., 2019).
Procrustes was used to characterize the potential consistency of bacterial species abundance, composition, and functional gene abundance composition based on COG functional annotation and genus species classification via PCA, the results of which are shown in Figure 7. The square deviation sum of Procrustes analysis was 0.1479, indicating a strong correlation between bacterial species abundance and functional gene abundance. At the same time, the similarity of Tx-1 and Tx-2 was highest, followed by Tx-3, and the similarity of functional gene abundance among the three treatments was higher than that of species abundance. Among the treatment groups, compared with that of the control group, the similarity in species abundance and functional gene abundance for these three treatment groups was the lowest.
In previous studies, the catalytic oxidation of oxidizing bacteria such as Thiobacillus ferrooxidans and Thiobacillus thiooxidans was considered an important cause of coal gangue acidification. Sasaki et al. (1998) showed that Thiobacillus ferrooxidans could significantly accelerate pyrite oxidation. Zhong et al. (1987) found that the iron release rate of inoculated pyrite samples was 60 times higher than that of uninoculated samples. However, the results of the present experiment show that the initial stage (0-28 d) of the stacking of the new coal gangue is the critical period for the pH decrease of the leachate and the main time period for the acidification of coal gangue. On the 28th day of the experiment, the bacterial community on the surface of the coal gangue samples was analyzed by 16S rRNA high-throughput sequencing. Thiobacillus was not the dominant genus in the bacterial community during this period, and the ferrous oxidation rate of the coal gangue leachate was only 9.91%, indicating that the microbial catalysis of ferrous oxidation by Thiobacillus was not obvious. These findings may imply that other factors may affect the acidification of coal gangue.
In the process of coal gangue acidification, a continuous decrease in pH leads to changes in the microbial community composition and function on the surface of coal gangue. With decreasing pH, the activity of some acidophilic bacteria (such as Thiobacillus) increases (Belzile et al., 1997), but these bacteria usually do not constitute the dominant genera at the beginning of the oxidation process of coal gangue. Therefore, Thiobacillus microorganisms were present only after the gangue had been oxidized for a period of time, which means that the dominance of Thiobacillus in the bacterial community may indicate that the oxidation process of coal gangue had entered the accelerated cycling stage. In another study, we evaluated the microbial community and composition during different periods of coal gangue oxidation. The results showed that Thiobacillus usually emerged and rapidly became the dominant genus after the gangue was exposed to air for approximately 50 d. This result may help us better understand the acidification mechanism of coal gangue under open-air conditions. Although attributing the initial acidification of coal gangue to ferrous ion oxidation promoted by Thiobacillus bacteria may not be completely accurate, it is still feasible to reduce the oxidation rate of coal gangue by inhibiting the activity of Thiobacillus bacteria, which prevents the oxidation process of coal gangue from entering the accelerated cycling stage (Hu et al., 2020).
Adding carbon sources and nutrient salts to coal gangue improved the bacterial community structure within the coal gangue, especially the dominance of sulfur-metabolizing bacteria, thus effectively inhibiting the production of acidic mine wastewater. Moreover, the addition of a carbon source effectively increased the number of microorganisms. However, the experimental results showed that the addition of sodium lactate and nutrient salts did not increase the diversity index of the bacterial community on the gangue surface but altered the relative abundance and dominance of different species of bacteria, prompting several functional bacteria (such as Arthrobacter and Enterococcus) to occupy a greater dominant position. However, bacterial growth rapidly consumed the carbon source. When the carbon source supply is stopped, the gangue was acidified quickly. Adding OM in the form of spraying a solution causes a large amount of solute to be lost with water, and only a small proportion of OM can be adsorbed onto the surface of the coal gangue, which makes it difficult to meet the needs of microbial growth. Solid organic waste such as peat, bagasse, and animal manure may be better choices for carbon sources; these sources could not only be implemented into new methods for waste disposal but also reduce environmental pollution caused by coal gangue acidification.