Yang Fan, Cao Xinde, Gao Bin, Zhao Ling, Li Feiyue
School of Environmental Science and Engineering, Shanghai Jiao Tong University, Shanghai, 200240, China.
Environ Sci Pollut Res Int. 2015 Jun;22(12):9184-92. doi: 10.1007/s11356-014-4067-1. Epub 2015 Feb 13.
Although previous work has explored and reported the influence of biochar on the fate and transformation of soil nitrogen (N), the governing mechanisms are still unclear. In this study, an incubation experiment was first conducted to investigate the overall fate of NH4 (+)-N in two soils: Gleyi-Stagnic Anthrosols (pH = 6.31) and Argi-Udic Ferrosols (pH = 5.05) amended with rice straw biochar. In addition, batch sorption experiments were designed to explore the potential mechanisms of NH4 (+)-N transformation in biochar-amended soils. Results showed that the KCl extractable NH4 (+)-N concentrations in the amended Anthrosols and Ferrosols decreased by 9-35 and 5-22 %, respectively, compared to the unamended soils, but limited nitrification of NH4 (+)-N into NO3 (-)-N was observed in both soils. In Anthrosols, biochar increased NH4 (+)-N sorption, but it decreased N biotransformation (mineralization, nitrification, and assimilation) into NO3 (-)-N. It implies that the chemical sorption is a dominant process in the biochar-amended soil. As for Ferrosols, biochar seemed to have less effect on either NH4 (+) sorption or biotransformation. Biochar addition promoted NH3 emission in both soils due to the elevated pH, but the overall amount of the N emission losses were negligible.
尽管先前的研究已经探讨并报道了生物炭对土壤氮素(N)的归宿和转化的影响,但其控制机制仍不明确。在本研究中,首先进行了一项培养实验,以研究添加稻草生物炭的两种土壤:潜育性水稻土(pH = 6.31)和铁聚潮湿雏形土(pH = 5.05)中NH4(+)-N的总体归宿。此外,还设计了批量吸附实验,以探究生物炭改良土壤中NH4(+)-N转化的潜在机制。结果表明,与未改良土壤相比,改良后的水稻土和铁聚潮湿雏形土中KCl可提取的NH4(+)-N浓度分别降低了9-35%和5-22%,但在两种土壤中均观察到NH4(+)-N向NO3(-)-N的硝化作用有限。在水稻土中,生物炭增加了NH4(+)-N的吸附,但降低了N向NO3(-)-N的生物转化(矿化、硝化和同化)。这意味着化学吸附是生物炭改良土壤中的主要过程。至于铁聚潮湿雏形土,生物炭对NH4(+)吸附或生物转化的影响似乎较小。由于pH值升高,添加生物炭促进了两种土壤中的NH3排放,但N排放损失的总量可以忽略不计。