3.1 Overall effect of biochar addition
We assessed the global effect of biochar addition on anaerobic methanogenesis by calculating the grand mean of the Hedge's d for 156 published data pairs of treatment versus control (Fig. 2). Results show a d value of 5.70 ± 1.04, which evidences a large effect size and implies that the presence of biochar statistically induces an increase in biomethane in most investigations. Yet sporadic studies have also shown the inhibitory effect of biochar or no effect (Cheng et al., 2018; Shen et al., 2016). This discrepancy is probably due to the high heterogeneous nature of biochar (Diao et al., 2020; Gao and Goldfarb, 2019), suggesting that biomethane production may be enhanced by specific biochar properties, as discussed below.
3.2 Effect of biochar feedstock
We calculated d values of feedstock including sludges, manure, herbaceous and lignocellulosic waste, and wood and sawdust (Fig. 2). All feedstock types show high d values from 4.71 ± 1.72 to 7.99 ± 1.51, implying that biochar addition improves biomethane generation whatever the type of feedstock. Furthermore, there is no statistical difference within feedstock types, sludges displaying the highest d of 7.99. Manure, plant waste and woody materials appear equally competitive with Hedge's d values around 5.0. Results on sludges are supported by the fact that sludge biochar provides more nutrients for fermentative bacteria and methanogens (Wang et al., 2020). Biochar from sludge has also induced significant effects on pollutant removal and heavy metal adsorption (Diao et al., 2020; Regkouzas and Diamadopoulos, 2019; Singh et al., 2020), which may be explained by a more favorable living environment for microorganisms. Overall, the slight advantage of sludge biochar in terms of methanogenesis is likely due to its ability to adsorb and store nutrients for activating methanogens. We conclude that biochar improves methanogenesis for all biochar feedstocks, but there is no statistical advantage of the feedstock type.
3.3 Effect of pyrolysis temperature
We calculated d values of biochar produced by pyrolysis below 500°C, of 6.72 ± 1.86, between 500 and 700°C, of 6.40 ± 1.11, and above 700°C, of 0.840 ± 1.50 (Fig. 2). Results imply that biochar favors biomethane generation below 700°C. There is no significant difference between 500–700°C-produced biochar and biochar produced below 500°C. On the other hand, pyrolysis above 700°C induces a drastic decline of biomethane promotion. These findings may be explained by changes of molecular structure with temperature (Hao et al., 2018). Indeed, Keiluweit et al. (2010) observed a gradual change in the molecular structure of plant biomass-derived biochar with temperature. High-temperature biochar is characterized by fewer labile compounds at the surface of biochar particles, and therefore less microbial substrates for fermentative bacteria and methanogenic archaea (Bruun et al., 2011). This explanation is strengthened by the declining CH4 and N2O emissions from soils amended with high-temperature biochar, which are thus better suited for mitigation of greenhouse gas emissions (Cayuela et al., 2015). By contract, slow pyrolysis at low temperature yields more biochar with diverse chemical groups (Chen et al., 2019; Sohi et al., 2010), which are likely to promote biomethane production in anaerobic digester or emission from soils (Jeffery et al., 2016). Overall, our findings show that biochar produced below 700°C improves methanogenesis. Pyrolysis at lower temperature will also save energy.
3.4 Effect of biochar conductivity
Biochars having low conductivity, below 450 µS/cm, show a much higher d value, of 7.58 ± 1.79, than high-conductivity biochar, displaying a d value of 2.06 ± 1.29 (Fig. 2). Low conductivity biochar is therefore statistically more effective at accelerating biomethane production. This finding is unexpected because recent research suggests that biochar acts as an electron shuttle, which should favor microbial activity (Viggi et al., 2017; Xiao et al., 2019b; Yuan et al., 2018). Nonetheless, a recent report shows that electrical conductivity of biochar is controlling only the rate of anaerobic degradation, not the yield of biogas (Rasapoor et al., 2020). Conductivity does not appear as a precise factor to choose which biochar is beneficial for the degradation of environmental waste, and some studies suggest that attributing rising biomethane production to high material conductivity requires caution (Martins et al., 2018; Van Steendam et al., 2019). Overall, our findings show that low conductivity biochar favors methanogensis, yet underlying mechanisms are unclear.
3.5 Effect of biochar pH
Figure 2 displays the effect of biochar of different pH on biomethane production. Results show that varying the biochar pH induces no statistical difference in biomethane production, despite the fact that pH is known to modify fermentation rates (Begum et al., 2018; Feng et al., 2020; Mao et al., 2017). Yet, most investigations included in this meta-analysis did not report the pH of the system before and after biochar application, though pH is expected to vary widely because some biochar contain oxygen-containing organic anions and carbonates that increase alkalinity (Fidel et al., 2017; Yuan et al., 2011). Overall, varying the pH of biochar does not statistically improve methanogenesis.
3.6 Effect of surface area and biochar size
Values of d for biochar with BET surface area above 100 m2/g, of 5.06 ± 1.83, are not statistically different from those of biochar with surface area below 100 m2/g, of 4.45 ± 1.06 (Fig. 2). Similarly, the size to biochar particles does not appear to modify biomethane generation, yet a trend for higher d value is observed for particle size below 1 mm. This implies that smaller particles of biochar may be beneficial to the degradation of environmental waste. For instance, the addition of powdered biochar to a pig manure/wheat straw aerobic compost increased biomethane emissions by 57%, whereas granular biochar decreased biomethane emissions by 22% (He et al., 2018). On the contrary, other investigations have shown that large biochar particles promote methanogenesis (Cheng et al., 2018; Viggi et al., 2017). Overall, there is not a clear global effect of surface area and size on anaerobic degradation of waste and pollutant and biomethane production.
3.7 Effect of biochar concentration
Biochar concentration caused a strong and statistically significant difference in the strength of biomethane production, with a maximal impact for concentrations exceeding 10 g/L and a d value of 7.87 ± 0.35 (Fig. 2). Increasing biochar concentration is therefore a means to improve methanogenesis, which may further result in a promotion of waste degradation. This finding is supported by biochar properties that are likely to stabilize anaerobic digestion and rise biomethane yield (Gao et al., 2020; Lim et al., 2020). For instance, providing immobilization sites for microorganisms could explain the higher anaerobic degradation and methanogenic performance (Zhang et al., 2018; Zhang and Wang, 2020). Moreover, even though biochar itself is not a substantial source of labile carbon, biochar is a sponge-like material able to adsorb and store organo-mineral nutrients for further microbial feeding (Cross and Sohi, 2011; Demisie et al., 2014). In this line, elevated biochar concentrations have been shown to increase the availability of organic carbon for fermentation bacteria and methanogenic archaea (Zhang et al., 2020). Based on this, environmental waste and pollution can be degraded more easily. Overall, high biochar concentrations foster methanogenesis, yet underlying mechanisms remain undeciphered.
3.8 Methanogenic species
Values of d for acetoclastic methanogens, of 5.19 ± 2.06, and hydrogenetrophic methanogens, of 3.08 ± 1.4, are not statistically different, implying a similar contribution to biomethane production (Fig. 3). Both acetoclastic and hydrogenetrophic methanogens produce more biomethane following biochar addition. This finding is strenghtened by an investigation revealing that Methanosarcina, Methanosaeta and Methanobacterium methanogens predominate in paddy soil-amended biochar during the anaerobic decomposition of rice straw (Huang et al., 2020). Trophic methanogens, hydrogenetrophic and acetoclastic methanogens may actively participate in the methane production process. Indeed, reports have shown that methanogens that use acetate and hydrogen as substrates coexist in the anaerobic fermentation system (Madigou et al., 2019; Zhang et al., 2019). Compared to hydrogenetrophic methanogens, acetoclastic methanogens should contribute more to methane production with sufficient organic substrates (Garcia-Mancha et al., 2017; Lim et al., 2020; Xiao et al., 2019a). Overall, biochar addition improves biomethane production by methanogens, yet acetoclastic and hydrogenetrophic methanogens display similar performances.