Department of Soil and Water Conservation, National Pingtung University of Science and Technology, Pingtung, 91201, Taiwan.
Department of Civil Engineering, National Pingtung University of Science and Technology, Pingtung, 91201, Taiwan.
Environ Pollut. 2021 Mar 1;272:116009. doi: 10.1016/j.envpol.2020.116009. Epub 2020 Nov 20.
Biochar has been proven as a soil amendment to improve soil environment. However, mechanistic understanding of biochar on soil physical properties and microbial community remains unclear. In this study, a wood biochar (WB), was incorporated into a highly weathered tropical soil, and after 1 year the in situ changes in soil properties and microbial community were evaluated. A field trial was conducted for application of compost, wood biochar, and polyacrylamide. Microstructure and morphological features of the soils were characterized through 3D X-ray microscopy and polarized microscopy. Soil microbial communities were identified through next-generation sequencing (NGS). After incubation, the number of pores and connection throats between the pores of biochar treated soil increased by 3.8 and 7.2 times, respectively, compared to the control. According to NGS results, most sequences belonged to Anaerolinea thermolimosa, Caldithrix palaeochoryensis, Chthoniobacter flavus, and Cohnella soli. Canonical correlation analysis (CCA) further demonstrated that the microbial community structure was determined by inorganic N (IN), available P (AP), pH, soil organic C (SOC), porosity, bulk density (BD), and aggregate stability. The treatments with co-application of biochar and compost facilitated the dominance of Cal. palaeochoryensis, Cht. flavus, and Coh. soli, all of which promoted organic matter decomposition and ammonia oxidation in the soil. The apparent increases in IN, AP, porosity, and SOC caused by the addition of biochar and compost may be the proponents of changes in soil microbial communities. The co-application of compost and biochar may be a suitable strategy for real world biochar incorporation in highly weathered soil.
生物炭已被证明是一种改善土壤环境的土壤改良剂。然而,生物炭对土壤物理性质和微生物群落的作用机制仍不清楚。本研究将一种木质生物炭(WB)添加到高度风化的热带土壤中,1 年后评估了土壤性质和微生物群落的原位变化。进行了一项田间试验,应用了堆肥、木质生物炭和聚丙烯酰胺。通过三维 X 射线显微镜和偏光显微镜对土壤的微观结构和形态特征进行了表征。通过下一代测序(NGS)鉴定了土壤微生物群落。与对照相比,生物炭处理土壤的孔隙数量和孔隙之间的连接喉道数量分别增加了 3.8 倍和 7.2 倍。根据 NGS 结果,大多数序列属于嗜热厌氧杆菌(Anaerolinea thermolimosa)、古生嗜热菌(Caldithrix palaeochoryensis)、黄杆菌(Chthoniobacter flavus)和土壤杆菌(Cohnella soli)。典范对应分析(CCA)进一步表明,微生物群落结构由无机氮(IN)、有效磷(AP)、pH 值、土壤有机碳(SOC)、孔隙率、体密度(BD)和团聚体稳定性决定。生物炭和堆肥共同处理促进了古生嗜热菌(Cal. palaeochoryensis)、黄杆菌(Chth. flavus)和土壤杆菌(Coh. soli)的优势地位,它们都促进了土壤中有机质的分解和氨氧化。生物炭和堆肥的添加引起的 IN、AP、孔隙率和 SOC 的明显增加可能是土壤微生物群落变化的推动者。堆肥和生物炭的共同应用可能是在高度风化土壤中实际应用生物炭的一种合适策略。