46, p < 0.05). In this study, the biochar-treated soil did not exhibit a significant increase in SOC levels ( Fig. 2b), even though the biochar used had a high TC content (78.3%) and C/N ratio (121). This could be attributed to the lower Walkley–Black C content (1.82%) in the biochar ( Table 1). Adding biochar OSI-906 in vivo to the soil caused a significant increase in the CEC and in the amount of exchangeable cations in the amended soils, suggesting an improvement in soil fertility

and nutrient retention. The improvement of the CEC can be attributed to the high SSA (340 m2 g− 1) of the biochar, which resulted from its porous structure (Fig. 1a). Additionally, slow oxidation of the biochar increased the number of carboxylic

groups, which in turn increased the CEC of the amended soil. These results agreed with those of Lehmann selleck compound (2007), who indicated that the CEC of the biochar increased with aging, primarily because of the increased carboxylation of carbon through abiotic oxidation (Cheng et al., 2006). Our results confirmed that biochar can improve the exchangeable cation status of the soil, especially for calcium, which correlated with the results of Lehmann et al. (2003), and Chan et al. (2008), who believed that original inhibitors nutrients in the biochar itself supplied the exchangeable cations in degraded soils. Other than chemical properties, the incorporation of biochar into the soil has also been found to influence microbial activity. Previous studies have used MBC as an indicator to evaluate microbial activity in soils (Chan

et al., 2008 and Kimetu and Lehmann, 2010). In this study, the higher MBC contents were always found in the biochar-amended soils at 0 d, 63 d and 105 d, indicating that biochar application could effectively increase microbial activity in the soils. In addition, the highest microbial activity was considered to occur at date of 21 d, even the control soil, because the highest MBC contents were found at 21 d for each treated soil (Fig. 3). Furthermore, the result showed that the significantly higher MBC content was still Sodium butyrate found in the 5% biochar-amended soil at the end of the incubation (105 d). This indicated that higher application rate of the biochar could maintain microbial activity in the soils for a longer period. Liang et al. (2006) indicated that microbial populations could be even higher in soil rich in black carbon. The higher MBC contents in the biochar-amended soils could be attributed to a higher pH (5.0–6.0) in these soils than in the control. The pH in the 5% biochar-amended soil was more suitable for the growth of microbes, especially for fungal hyphae, which also agreed with Wuddivira et al. (2009). That increased pH in the biochar-amended soils lead to an increase in microbial activity was further demonstrated by a significantly positive correlation between pH and MBC in the soils (Table 3).