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Carbon, nitrogen and phosphorus stoichiometry in Pinus tabulaeformis forest ecosystems in warm temperate Shanxi Province, north China

机译:华北温带油松林生态系统中碳,氮和磷的化学计量

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摘要

Although carbon (C), nitrogen (N), and phos-phorous (P) stoichiometric ratios are considered good indicators of nutrient excess/limitation and thus of ecosystem health, few reports have discussed the trends and the reciprocal effects of C:N:P stoichiometry in plant-litter-soil systems. The present study analyzed C:N:P ratios in four age groups of Chinese pine, Pinus tabulaeformis Carr., forests in Shanxi Province, China:plantation young forests (AY,<20 year-old);plantation middle-aged forests (AM, 21-30 year-old); natural young forests (NY,<30 year-old); and natural middle-aged forests (NM, 31-50 year-old). The average C:N:P ratios calculated for tree, shrub, and herbaceous leaves, litter, and soil (0-100 cm) were generally higher in NY followed by NM, AM, and AY. C:N and C:P ratios were higher in litter than in leaves and soils, and reached higher values in the litter and leaves of young forests than in middle-aged forests;however, C:N and C:P ratios were higher in soils of mid-dle-aged forests than in young forests. N:P ratios were higher in leaves than in litter and soils regardless of stand age; the consistent N:P<14 values found in all forests indicated N limitations. With plant leaves, C:P ratios were highest in trees, followed by herbs and shrubs, indicating a higher efficiency in tree leaf formation. C:N ratios decreased with increasing soil depth, whereas there was no trend for C:P and N:P ratios. C:N:P stoichiometry of forest foliage did not exhibit a consistent variation according to stand age. Research on the relationships between N:P, and P, N nutrient limits and the characteristics of vegetation nutrient adaptation need to be continued.
机译:尽管碳(C),氮(N)和磷(P)的化学计量比被认为是营养物过量/限制以及生态系统健康的良好指标,但很少有报道讨论C:N的趋势和相互影响:植物凋落物-土壤系统中的化学计量。本研究分析了中国山西省油松森林四个年龄组的C:N:P比率:人工林(AY,<20岁);人工林中年森林(AM) ,21-30岁);天然幼林(纽约州,<30岁);和天然的中年森林(NM,31-50岁)。在纽约,NM,AM和AY之后,针对树木,灌木和草本叶,凋落物和土壤(0-100厘米)的平均C:N:P比值通常更高。凋落物中的C:N和C:P比值高于叶片和土壤,幼林的凋落物和树叶中的C:N和C:P值高于中年森林;而C:N和C:P的比例则高于中年森林。中等年龄森林的土壤比幼林的土壤多。不论林分年龄,叶片中N:P的比率均高于凋落物和土壤。在所有森林中发现的一致的N:P <14值表明存在N个限制。对于植物叶片,C:P比率在树木中最高,其次是草药和灌木,这表明在树木叶片形成中效率更高。 C:N比随土层深度的增加而降低,而C:P和N:P比值没有趋势。根据林分年龄,森林叶子的C:N:P化学计量没有表现出一致的变化。氮磷和磷,氮养分限量与植被养分适应特征之间关系的研究仍需继续。

著录项

  • 来源
    《林业研究(英文版)》 |2018年第6期|1665-1673|共9页
  • 作者单位

    College of Agronomy, Heilongjiang Bayi Agricultural University, Daqing 163319, Heilongjiang, People's Republic of China;

    Daqing Forestry Bureau, Daqing 163002, Heilongjiang, People's Republic of China;

    Soil and Water Conservation School, Beijing Forestry University, Beijing 100083, People's Republic of China;

    Soil and Water Conservation School, Beijing Forestry University, Beijing 100083, People's Republic of China;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 eng
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