Yin Yan, Liu Yan, Yin Yun Feng, Ma Hong Liang, Gao Ren, Yang Yu Sheng
College of Geographical Science, Fujian Normal University, Fuzhou 350007, China.
Cultivation Base of State Key Laboratory of Humid Subtropical Mountain Ecology, Fuzhou 350007, China.
Ying Yong Sheng Tai Xue Bao. 2018 May;29(5):1389-1396. doi: 10.13287/j.1001-9332.201805.008.
Effects of addition of different biochars on soil organic carbon (SOC) mineralization were studied by the C-labelling technique for a better understanding of biomass resource utilization and carbon sequestration in subtropical Chinese fir (Cunninghamia lanceolata) plantation. An incubation experiment under 25 ℃ was performed over a period of 112 days to address how different biochar addition would affect the mineralization of native SOC. Biochars were produced from Schimasuperba or C. lanceolata litter at 350, 550 and 750 ℃, respectively. Results showed that the mineralization of native SOC was significantly accelerated during the first three days and subsequently suppressed from 7 to 112 days of incubation after C. lanceolata biochar addition compared to the control. In the S. superba biochar addition treatment, there was a significant increase in mineralization of native SOC within the first 14 days of incubation and then a rapid decrease from days 28 to 112. After 112 days incubation, all the three C. lanceolata biochar (350, 550 and 750 ℃) additions significantly inhibited the mineralization of native SOC. A similar trend was observed for the two S. superba biochar (350 and 550 ℃) additions but not for the S. superba biochar (750 ℃) addition. The decomposition rates of S. superba biochar and C. lanceolata biochar were 0.8%-2.8% after 112 days incubation and decreased with the increases of pyrolysis temperature. Under the same pyrolysis temperature, the decomposition rate of the S. superba biochar was significantly higher than that of the C. lanceolata biochar. In conclusion, both the raw material and pyrolysis temperature of biochars would be important factors driving the mineralization of native SOC and biochar degradation.
采用碳标记技术研究了添加不同生物炭对土壤有机碳(SOC)矿化的影响,以便更好地了解亚热带杉木人工林中生物质资源的利用和碳固存情况。在25℃下进行了为期112天的培养实验,以探讨不同生物炭添加如何影响原生SOC的矿化。生物炭分别由木荷或杉木凋落物在350℃、550℃和750℃下制备而成。结果表明,与对照相比,添加杉木生物炭后,原生SOC的矿化在培养的前三天显著加速,随后在7至112天受到抑制。在添加木荷生物炭的处理中,原生SOC的矿化在培养的前14天显著增加,然后在28至112天迅速下降。培养112天后,所有三种杉木生物炭(350℃、550℃和750℃)的添加均显著抑制了原生SOC的矿化。两种木荷生物炭(350℃和550℃)的添加也观察到类似趋势,但木荷生物炭(750℃)的添加未观察到。培养112天后,木荷生物炭和杉木生物炭的分解率为0.8%-2.8%,且随热解温度的升高而降低。在相同热解温度下,木荷生物炭的分解率显著高于杉木生物炭。总之,生物炭的原料和热解温度都是驱动原生SOC矿化和生物炭降解的重要因素。