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Factors controlling decomposition rates of fine root litter in temperate forests and grasslands

机译:温带森林和草原细根凋落物分解速率的控制因素

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Fine root decomposition contributes significantly to element cycling in terrestrial ecosystems. However, studies on root decomposition rates and on the factors that potentially influence them are fewer than those on leaf litter decomposition. To study the effects of region and land use intensity on fine root decomposition, we established a large scale study in three German regions with different climate regimes and soil properties. Methods In 150 forest and 150 grassland sites we deployed litterbags (100 mu m mesh size) with standardized litter consisting of fine roots from European beech in forests and from a lowland mesophilous hay meadow in grasslands. In the central study region, we compared decomposition rates of this standardized litter with root litter collected on-site to separate the effect of litter quality from environmental factors. Standardized herbaceous roots in grassland soils decomposed on average significantly faster (24 +/- 6 % mass loss after 12 months, mean +/- SD) than beech roots in forest soils (12 +/- 4 %; p < 0.001). Fine root decomposition varied among the three study regions. Land use intensity, in particular N addition, decreased fine root decomposition in grasslands. The initial lignin:N ratio explained 15 % of the variance in grasslands and 11 % in forests. Soil moisture, soil temperature, and C:N ratios of soils together explained 34 % of the variance of the fine root mass loss in grasslands, and 24 % in forests. Grasslands, which have higher fine root biomass and root turnover compared to forests, also have higher rates of root decomposition. Our results further show that at the regional scale fine root decomposition is influenced by environmental variables such as soil moisture, soil temperature and soil nutrient content. Additional variation is explained by root litter quality
机译:细根分解显着促进了陆地生态系统中元素的循环。但是,关于根分解速率和可能影响根分解速率的因素的研究少于对凋落物分解的研究。为了研究区域和土地利用强度对细根分解的影响,我们在三个德国气候条件和土壤特性不同的地区进行了大规模研究。方法在150个森林和150个草原地点,我们部署了带有标准垃圾的垃圾袋(100微米目),垃圾由森林中欧洲山毛榉和草原低地中温干草草甸的细根组成。在中心研究区域,我们将这种标准化垃圾的分解速率与现场收集的根垃圾进行了比较,以将垃圾质量的影响与环境因素分开。草原土壤中标准化的草根平均分解速度(12个月后质量损失为24 +/- 6%,平均+/- SD)比森林土壤中的山毛榉根分解速度更快(12 +/- 4%; p <0.001)。细根分解在三个研究区域之间有所不同。土地利用强度,特别是氮的添加,减少了草地的细根分解。最初的木质素:氮比解释了草原中15%的变化和森林中11%的变化。土壤水分,土壤温度和土壤C:N比值​​一起解释了草原细根质量损失方差的34%和森林中24%。与森林相比,具有更高的优良根生物量和根周转率的草原,其根分解率也更高。我们的结果进一步表明,在区域尺度上,细根分解受到环境变量的影响,例如土壤湿度,土壤温度和土壤养分含量。根凋落物质量解释了其他变化

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