Effects of biochar pyrolyzed at varying temperatures on soil organic carbon and its components: influence on the soil active organic carbon

被引:0
|
作者
Zhao S.-X. [1 ]
Yu X.-L. [1 ]
Li Z.-H. [1 ]
Yang Y. [1 ]
Liu D. [1 ]
Wang X.-D. [1 ,2 ]
Zhang A.-F. [1 ]
机构
[1] College of Natural Resources and Environment, Northwest A&F University, Yangling
[2] Key Laboratory Plant Nutrition and the Agri-environment in Northwest China, Ministry of Agriculture, Yangling
来源
Huanjing Kexue/Environmental Science | 2017年 / 38卷 / 01期
关键词
Active organic carbon; Biochar; Microbial biomass carbon; Organic carbon; Readily oxidized organic carbon; Water soluble organic carbon;
D O I
10.13227/j.hjkx.201604058
中图分类号
学科分类号
摘要
Soil active organic carbon is the most important carbon pool and a good indicator in ecosystem management due to its great significance in soil carbon cycling and soil quality. In order to investigate the effect of biochar(BC)addition on soil organic matter fractions, apple tree twigs were used to produce BC at 300, 400, 500 and 600℃, respectively. Elemental analysis and Fourier transform infrared (FTIR) spectroscopy were used to determine the characteristics of BC. Four kinds of BC were added into soils at five application rates(0, 0.5%, 1%, 2% and 3%) and incubated at 25℃ in lab for over 360 days. Soil organic carbon (SOC), microbial biomass carbon (MBC), water soluble organic carbon (WSOC) and readily oxidized organic carbon (ROC) were measured during the incubation. The mass fraction of carbon (C) in the generated BC ranged from 62.20%-80.01%, while hydrogen (H) ranged from 2.72%-5.18% and Oxygen (O) ranged from 15.98%-30.92%. The increasing temperature increased the mass fraction of C, while decreased the O and H mass content, as well as the ratio of H/C and O/C. The addition of BC significantly increased SOC, and the treatments amended with BC500 had the highest increments. Compared with the control treatment (CK), the addition of BC produced at temperatures below 400℃ increased the contents of MBC, WSOC and ROC during the incubation, at the end of the incubation, BC300 treatments significantly increased the contents by 38.25%, 82.09% and 63.53% (P<0.05), respectively; BC400 treatments significantly increased the contents by 26.07%, 65.61% and 48.09% (P<0.05), respectively; while lower contents of MBC, WSOC and ROC were found in the treatments amended with BC produced at temperatures above 400℃ after 40-60 d incubation. After 360 d of incubation, the contents of MBC, WSOC and ROC were significantly decreased by 0.27%,13.48% and 14.67% in BC500 treatments and 7.80%,14.66% and 15.79% in BC600 treatments (except for the MBC in BC500 treatment) (P<0.05). The relative contents of ROC ranged from 3.39% to 15.65%, BC application decreased the relative content of ROC, suggesting that the increase was in proportion to the stability of organic carbon in the soil. Considering the content and quality of SOC, when the BC products were applied to the Loutu soil, 500℃ was the optimal temperature for preparing apple-derived BC due to its significant increase of the soil organic carbon and a slight decrease of the relative content of soil active organic carbon. © 2017, Science Press. All right reserved.
引用
收藏
页码:333 / 342
页数:9
相关论文
共 50 条
  • [1] Brandao M., Canals L.M.I., Clift R., Soil organic carbon changes in the cultivation of energy crops: Implications for GHG balances and soil quality for use in LCA, Biomass and Bioenergy, 35, 6, pp. 2323-2336, (2011)
  • [2] Harris Z.M., Spake R., Taylor G., Land use change to bioenergy: a meta-analysis of soil carbon and GHG emissions, Biomass and Bioenergy, 82, pp. 27-39, (2015)
  • [3] McLauchlan K.K., Hobbie S.E., Comparison of labile soil organic matter fractionation techniques, Soil Science Society of America Journal, 68, 5, pp. 1616-1625, (2004)
  • [4] Wang Y., Song X.S., Wang J., Et al., Effect of drying-rewetting alternation on soil carbon pool and mineralization of soil organic carbon, Acta Pedologica Sinica, 51, 2, pp. 342-350, (2014)
  • [5] Sheng H., Zhou P., Zhang Y.Z., Et al., Loss of labile organic carbon from subsoil due to land-use changes in subtropical China, Soil Biology and Biochemistry, 88, pp. 148-157, (2015)
  • [6] Wander M.M., Traina S.J., Stinner B.R., Et al., Organic and conventional management effects on biologically active soil organic matter pools, Soil Science Society of America Journal, 58, 4, pp. 1130-1139, (1994)
  • [7] Gregorich E.G., Monreal C.M., Carter M.R., Et al., Towards a minimum data set to assess soil organic matter quality in agricultural soils, Canadian Journal of Soil Science, 74, 4, pp. 367-385, (1994)
  • [8] Lehmann J., A handful of carbon, Nature, 447, 7141, pp. 143-144, (2007)
  • [9] Fang Y., Singh B., Singh B.P., Et al., Biochar carbon stability in four contrasting soils, European Journal of Soil Science, 65, 1, pp. 60-71, (2014)
  • [10] Purakayastha T.J., Kumari S., Pathak H., Characterisation, stability, and microbial effects of four biochars produced from crop residues, Geoderma, 239-240, pp. 293-303, (2015)