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Topographical variations of soil respiration in the deciduous forest -In the case with extremely immature soil from weathered granite-

机译:落叶林土壤呼吸的地形变化 - 风化花岗岩极其未成熟土的情况 -

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This study considers the time series data of soil respiration and its spatial variation in a small mountainous catchment which is located on complex terrain in Japan. Soil respiration rate was measured for 96 soil collars in the small mountainous catchment (1.6ha) in this study. The relationships between soil temperature, soil moisture content and measured soil respiration rate could be expressed by one function in spite that measured places were located at different topographical locations. The relative difference between calculated and measured soil respiration rate was 23%. The time series data of daily soil respiration was estimated by this function used with the monitoring data of soil temperature and soil moisture content ratio at 5 places inthis cachment. These daily soil respiration rates fluctuated at almost the same time and relative variation ranges between 73-122% in one year.
机译:本研究考虑了土壤呼吸的时间序列数据及其在日本复杂地形上的小山地集水区中的空间变化。在本研究中的小山区集水区(1.6Ha)中测量了土壤呼吸速率为96个土圈。土壤温度,土壤水分含量和测量土壤呼吸率之间的关系可以通过一种功能表达,因为测量的地方位于不同的地形位置。计算和测量的土壤呼吸率之间的相对差异为23%。通过这种功能估算了每日土壤呼吸的时间序列数据,该函数与土壤温度和土壤水分含量比的监测数据发生在5个放血术中。这些日常土壤呼吸率在几乎相同的时间和相对变化范围内的距离为73-122%。

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