大气CO2浓度和温度升高对玉米和水稻根际土壤氮矿化速率的影响

Impact of elevated atmospheric CO2 concentration and temperature on nitrogen mineralization rates in the rhizosphere soils of corn and rice

  • 摘要: 为探究大气CO2浓度和温度升高对黑土区玉米和水稻根际土壤氮矿化能力的影响,比较旱田和水田根际土壤氮矿化过程对大气CO2浓度和温度升高响应的异同,本研究采用开顶式气室(Open-Top Chamber, OTC)模拟大气CO2浓度和温度升高条件,以正常大气CO2浓度(≈ 425 μmol·mol−1)、环境温度作为对照(CK),设置大气CO2浓度升高(≈ 700 μmol·mol−1)但温度不升高处理(EC)、大气CO2浓度不升高但温度升高(高于对照 2 ℃ ± 0.5 ℃)处理(ET)以及大气CO2浓度和温度同时升高处理(ECT),选取典型农田黑土种植玉米和水稻,分别在玉米的大喇叭口期、水稻的分蘖期(S1时期)以及二者的成熟期(S2时期)采集根际土壤样品,采用室内恒温培养法,系统监测了作物在上述两个生育时期根际土壤各形态氮素含量及净氮矿化速率的变化,并运用动力学模型进行拟合。结果表明:EC、ET及ECT对土壤氮素转化的影响存在显著的作物物种特异性和生长时期差异性,具体表现在:S1时期,EC处理提高了水稻根际土壤的净氨化与净氮矿化速率,ET处理增加了水稻根际土壤铵态氮和无机氮含量,而ECT不仅提高了水稻根际土壤铵态氮含量,还极显著地促进了玉米根际土壤的净氨化与净氮矿化速率;S2时期,各处理均显著抑制了水稻根际土壤的净氨化与净氮矿化速率,尤以ECT的抑制效应最为突出。进一步动力学分析表明,ECT显著改变了水稻根际土壤的氮矿化动力学参数,印证了其氮转化过程对气候变化的高度敏感性。研究结果将为构建和优化气候变化下黑土供氮潜力预测模型,以及制定适应未来气候变化的禾谷类作物农田氮肥养分管理策略提供数据支撑和理论依据。

     

    Abstract: To investigate the effects of elevated atmospheric CO2 concentration and temperature on soil nitrogen mineralization capacity in the rhizosphere of corn and rice in Mollisols, and to compare the similarities and differences in the responses of nitrogen mineralization processes in dryland and paddy fields to elevated CO2 concentration and temperature, this study used open-top chambers (OTC) to simulate elevated atmospheric CO2 concentration and temperature conditions. Using normal atmospheric CO2 concentration (≈ 425 μmol·mol−1) and ambient temperature as the control (CK), three treatments were established: elevated CO2 concentration (≈ 700 μmol·mol−1) without temperature increase (EC); ambient CO2 concentration with elevated temperature (2 ℃ ± 0.5 ℃ above the control) (ET); and simultaneous elevation of both CO2 concentration and temperature (ECT). Rhizosphere soil samples were collected at the large trumpet stage of corn and the tillering stage of rice (stage S1), as well as at the maturity stage of both crops (stage S2). Laboratory incubation was employed to systematically monitor the changes in various soil nitrogen forms and net nitrogen mineralization rates during the two growth stages, and kinetic models were applied for fitting. Results demonstrated that the effects of EC, ET, and ECT on soil nitrogen transformation exhibited significant crop specificity and temporal variability. In the S1 stage, EC enhanced net ammonification and nitrogen mineralization rates in rice soil, ET increased ammonium and inorganic nitrogen content in rice soil, while ECT significantly promoted these processes in corn soil. In the S2 stage, all treatments suppressed net ammonification and nitrogen mineralization in rice soil, with the most pronounced inhibition under ECT. Further kinetic analysis revealed that ECT markedly altered mineralization parameters in rice soil, highlighting its high sensitivity to climatic changes. These findings provide critical data and theoretical support for predicting nitrogen supply potential in Mollisols and optimizing nitrogen management strategies for cereal crops under future climate scenarios.

     

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