夜间增温对冬小麦土壤微生物量碳氮及其活性的影响

Impact of nighttime warming on soil microbial biomass carbon/nitrogen and activity in main winter wheat cropping areas in China

  • 摘要: 全球气候变暖存在明显的昼夜不对称性, 夜间气温升高幅度显著高于白天, 但目前关于夜间增温对土壤微生物影响的田间研究尚较少。为此, 本研究采用夜间被动式增温系统(passive nighttime warming, PNW), 在我国冬小麦主产区(石家庄、徐州、许昌和镇江)进行全生育期田间增温试验, 于2008-2010年监测了土壤微生物对夜间增温的响应。结果显示, 与不增温对照相比, 夜间增温可显著降低土壤微生物量碳、氮含量和微生物活性。冬小麦整个生育期中, 夜间增温分别使石家庄、徐州、许昌和镇江试验点土壤微生物量碳平均降低11.4%、7.8%、10.9%和8.5%, 微生物量氮平均降低15.2%、16.7%、13.8%和8.4%, 微生物呼吸速率平均下降6.6%、9.6%、7.0%和11.1%。在整个增温过程中, 石家庄、徐州、许昌和镇江试验点土壤水分含量分别下降8.8%、3.7%、3.8%和2.9%, 与对照相比差异不显著。同时, 该夜间增温系统使相应试验点0~5 cm土层的温度分别提高1.2 ℃、0.7 ℃、0.7 ℃和0.7 ℃。本试验表明, 夜间增温将可能通过改变土壤微生物特性而影响土壤碳/氮循环, 从而影响到土壤养分供应和冬小麦生长; 且表现出了一定的纬度差异性。

     

    Abstract: It has been predicted that global climate could warm further with greater increase in daily minimum temperature than in daily maximum temperature. However, little has remained known about the impact of nighttime warming on soil microbial growth and activity. Using the passive nighttime warming (PNW) technique, a 4-year field nighttime warming experiment was conducted during crop-growth periods at the Shijiazhuang, Xuzhou, Xuchang and Zhenjiang sites; covering the main winter wheat cropping regions in China. Soil moisture, soil temperature (0~5 cm), soil microbial biomass and activity were determined under field conditions in 2008-2010. The results showed that nighttime warming significantly decreased soil microbial biomass carbon (C) and nitrogen (N) as well as microbial activity. Compared with the ambient treatment, nighttime warming reduced soil microbial biomass C on average by 11.4%, 7.8%, 10.9% and 8.5%, soil microbial biomass N by 15.2%, 16.7%, 13.8% and 8.4%, and microbial respiration rate by 6.6%, 9.6%, 7.0% and 11.1% at Shijiazhuang, Xuzhou, Xuchang and Zhenjiang sites, respectively. The corresponding soil moisture was 8.8%, 3.7%, 3.8% and 2.9% lower in the warmed plots than in the ambient plots, but all the effects were insignificant. The corresponding temperatures in the 0~5 cm soil layer were higher by 1.2 ℃, 0.7 ℃, 0.7 ℃ and 0.7 ℃ in the warmed plots than in the ambient plots. These results suggest that nighttime warming altered soil C/N cycle and winter wheat growth by influencing soil microbial biomass and microbial activity with certain latitude differences.

     

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