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Litter contribution to diurnal and annual soil respiration in a tropical montane cloud forest

机译:在热带山地云雾森林中,凋落物对昼夜土壤呼吸的贡献

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Respiration of CO2 from soils (Rs) is a major component of the carbon cycle of ecosystems, but understanding is still poor of both the relative contributions of different respiratory sources to Rs, and the environmental factors that drive diurnal variations in Rs. We measured total and litter-free Rs at half-hourly intervals over full 24 h periods, and thereafter twice a month for 10 months in a tropical montane cloud forest (TMCF) in Peru. Total Rs declined by about 61% during the night as a result of variations in respiration rate in the litter, which were partly correlated with the soil surface air temperature. Most of the diurnal variation of Rs in this TMCF appears to be driven by respiration in the litter layer, which contributed 37% to the total soil CO2 efflux. Total Rs rates at this particular site would have been overestimated by 60% if derived from daytime measurements that had not been corrected for diurnal variations in Rs.
机译:从土壤(Rs)呼吸CO2是生态系统碳循环的主要组成部分,但对于不同呼吸源对Rs的相对贡献以及驱动Rs昼夜变化的环境因素的了解仍然很薄。我们在整个24小时内每半小时测量一次总的和无垃圾的Rs,此后在秘鲁的热带山地云雾森林(TMCF)中每月两次,共10个月。由于凋落物中呼吸速率的变化,夜间总Rs下降了约61%,这部分与土壤表面的气温有关。该TMCF中Rs的大多数昼夜变化似乎是由凋落物层的呼吸作用驱动的,其占土壤CO2总排放量的37%。如果从未针对Rs的昼夜变化进行校正的日间测量中得出,则该特定站点的总Rs率将被高估60%。

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