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The effect of soil warming on bulk soil vs. rhizosphere respiration

机译:土壤变暖对块状土壤与根际呼吸的影响

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There has been considerable debate on whether root/rhizosphere respiration or bulk soil respiration is more sensitive to long-term temperature changes. We investigated the response of belowground respiration to soil warming by 3 degrees C above ambient in bare soil plots and plots planted with wheat and maize. Initially, belowground respiration responded more to the soil warming in bare soil plots than in planted plots. However, as the growing season progressed, a greater soil-warming response developed in the planted plots as the contribution of root/rhizosphere respiration to belowground respiration declined. A negative correlation was observed between the contribution of root/rhizosphere respiration to total belowground respiration and the magnitude of the soil-warming response indicating that bulk soil respiration is more temperature sensitive than root/rhizosphere respiration. The dependence of root/rhizosphere respiration on substrate provision from photosynthesis is the most probable explanation for the observed lower temperature sensitivity of root/rhizosphere respiration. At harvest in late September, final crop biomass did not differ between the two soil temperature treatments in either the maize or wheat plots. Postharvest, flux measurements during the winter months indicated that the response of belowground respiration to the soil-warming treatment increased in magnitude (response equated to a Q(10) value of 5.7 compared with similar to 2.3 during the growing season). However, it appeared that this response was partly caused by a strong indirect effect of soil warming. When measurements were made at a common temperature, belowground respiration remained higher in the warmed subplots suggesting soil warming had maintained a more active microbial community through the winter months. It is proposed that any changes in winter temperatures, resulting from global warming, could alter the sink strength of terrestrial ecosystems considerably.
机译:关于根/根际呼吸或整体土壤呼吸是否对长期温度变化更为敏感,存在大量争论。我们调查了裸露土壤样地和小麦和玉米种植地中地下呼吸对土壤温度升高3℃以上的反应。最初,地下呼吸比裸露地块对土壤变暖的反应要强于种植地块。但是,随着生长季节的进行,随着根/根际呼吸作用对地下呼吸作用的下降,种植地上的土壤变暖反应也随之增强。根/根际呼吸对总地下呼吸的贡献与土壤变暖响应的大小之间存在负相关关系,表明散装土壤呼吸比根/根际呼吸对温度更敏感。根/根际呼吸对光合作用提供的底物的依赖性是观察到的根/根际呼吸的较低温度敏感性的最可能解释。在9月下旬收获时,两种土壤温度处理的最终作物生物量在玉米田或小麦田中都没有差异。冬季收获后的通量测量表明,地下呼吸对土壤变暖处理的响应幅度有所增加(响应的Q(10)值为5.7,而生长季的响应为2.3)。但是,这种反应似乎部分是由于土壤变暖的强烈间接影响引起的。当在常温下进行测量时,在加热的子图中地下呼吸仍然较高,这表明在整个冬季,土壤变暖都保持了更活跃的微生物群落。建议由全球变暖引起的冬季温度的任何变化都可能极大地改变陆地生态系统的汇聚强度。

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