Norway spruce fine root dynamics and carbon input into soil in relation to environmental factors

J. Leppälammi-Kujansuu
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引用次数: 3

Abstract

Knowledge of the quantity of belowground litter carbon (C) input is scarce but highly valued in C budget calculations. Specifically, the turnover rate of fine roots is considered as one of the most important parameters in the estimation of changes in soil C stock. In this thesis Norway spruce (Picea abies L. (Karst.)) fine root lifespan and litter production were studied and their responses to nutrient availability and temperature were examined. Aboveground foliage and understory litter C inputs were also quantified. Furthermore, fine root isotopic C ages were compared to fine root lifespans. Increased nutrient availability and higher temperature shortened spruce fine root lifespan both in the manipulation treatments and along a latitude gradient. Fertilization improved tree growth and the absolute amount of litter production, both belowand aboveground. Soil warming, by contrast, increased the belowground litter production in relation to aboveground foliage litterfall but did not lead to long-term increases in aboveground tree growth. In warmed soil, the changes in spruce short root morphology indicated nutrient deficiency. The results indicated that in nutrient limited forests climate warming is unlikely to increase the aboveground tree growth in the long-term. Fine root litter C input into the soil in relation to the aboveground litter C input was higher towards lower fertility, due particularly to the greater contribution of understory vegetation. The structural 14 C age of fine roots was consistently 3 6 years older than fine root lifespan determined with the minirhizotron method indicating that root growth may use also use stored or recycled C. In almost all stands, fine root litter C input into the soil at least equalled the aboveground input, which confirms the significance of belowground litter production in the boreal forest C cycle. The importance of understory vegetation was also significant. In addition on understory vegetation, different stand age and tree species, more studies should also focus on the shift in the litter production pattern from aboveto belowground along environmental change as this may have an impact on litter C quality and soil C storage in boreal forest soils.
挪威云杉细根动态与土壤碳输入与环境因子的关系
对地下凋落物碳(C)输入量的了解很少,但在碳预算计算中很有价值。其中,细根周转率被认为是估算土壤碳储量变化最重要的参数之一。以挪威云杉(Picea abies L. (Karst.))为研究对象,研究了其细根寿命和凋落物产量及其对养分有效性和温度的响应。地上落叶和林下凋落物C输入量也被量化。此外,细根同位素C年龄与细根寿命进行了比较。在不同纬度梯度和不同处理下,养分有效性的提高和温度的升高缩短了云杉细根的寿命。施肥改善了树木的生长和地上和地下凋落物的绝对数量。相比之下,土壤变暖增加了地上落叶凋落物的地下凋落物产量,但没有导致地上树木生长的长期增加。在温暖土壤中,云杉短根形态的变化表明养分缺乏。结果表明,在营养有限的森林中,气候变暖不太可能长期促进地上树木的生长。细根凋落物对土壤的碳输入相对于地上凋落物对低肥力的碳输入更高,特别是由于林下植被的贡献更大。细根的结构碳年龄始终比用微氮化法测定的细根寿命大36年,这表明根系生长既可以利用储存的碳,也可以利用回收的碳。在几乎所有林分中,细根凋落物向土壤的碳输入至少等于地上的碳输入,这证实了地下凋落物生产在北方森林碳循环中的重要性。林下植被的重要性也显著。除了对林下植被、不同林龄和不同树种的凋落物生产模式,还应更多地关注随环境变化从地上到地下的变化,因为这可能影响凋落物C质量和土壤C储量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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