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Comparison of the variation of soil respiration in carbon cycle in temperate and subtropical forests and the relationship with climatic variables

机译:温带亚热林中碳循环中土壤呼吸变异的比较及气候变量关系

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Forest soil respiration (SR) has become a vital issue in global change ecology because of its critical role in global warming processes. However, SR remains the least understood component of the terrestrial carbon cycle because of its high spatial-temporal variability, inaccessibility of the soil substrate, and the high cost of measurement equipment. This study investigated the spatial and temporal variations of SR in six temperate and subtropical forest sites in eastern China. Seasonal variations of SR, the relationship between SR and soil temperature (ST) and volumetric water content (SW) were analyzed. Mean monthly SR varied seasonally and peaked in summer. SR varied temporally with ST (R-2 = 0.43 similar to 0.79) in different sites and varied spatially with latitude (R-2 = 0.68). The responses of SR to the changes of SW varied across different sites and forest types. Their relationships were simulated by piecewise functions in the north three sites. The modules of ST and SW showed that ST is the dominant environmental factor in regulating seasonal dynamics of SR. This study is the first to examine the temporal and spatial variations of SR using a consistent method in situ in temperate and subtropical forests in eastern China. The results provide a scientific basis for accurately assessing future soil CO2 efflux as a result of climate changes, and aid predictions of the changes of forest SR.
机译:由于其在全球变暖过程中的关键作用,森林土壤呼吸(SR)已成为全球变革生态学的重要问题。然而,由于其高空间 - 时间可变性,土壤基材的高成本和测量设备的高成本,SR仍然是陆地碳循环的最不理解的组成部分。本研究调查了中国东部六个温带和亚热带森林地点SR的空间和时间变化。分析了SR的季节变异,分析了SR和土壤温度(ST)和体积含水量(SW)之间的关系。平均每月SR季节性季节性和峰值达到峰值。在不同部位的ST(R-2 = 0.43时,SR在时间上随时间变化,并在不同的位置在空间上变化(R-2 = 0.68)。 SR对不同地点和森林类型的SW变化的反应。他们的关系是通过北三个地点的分段功能模拟的。 ST和SW的模块显示ST是调节SR季节性动态的主导环境因素。本研究是第一个在中国东部的温带和亚热带林中使用一致方法检查SR的时间和空间变化。结果为准确评估了由于气候变化而准确评估未来土壤二氧化碳流出的科学依据,并援助森林SR变化的援助预测。

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