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首页> 外文期刊>Journal of forest research >Temporal changes in litterfall, litter decomposition and their chemical composition in Sasa dwarf bamboo in a natural forest ecosystem of northern Japan
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Temporal changes in litterfall, litter decomposition and their chemical composition in Sasa dwarf bamboo in a natural forest ecosystem of northern Japan

机译:日本北部天然森林生态系统中Sasa矮竹的凋落物,凋落物分解及其化学成分的时间变化

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摘要

We investigated the dynamics of litterfall and litter decomposition of Sasa dwarf bamboo (Sasa senanensis) and trees to clarify the characteristics of organic matter and nitrogen cycling between plant and soil in a natural cool-temperate mixed forest ecosystem dominated by an understory vegetation of Sasa. Mean annual Sasa litterfall over the 3-year study period was 164 g m(-2) year(-1), which accounted for approximately 29% of total litterfall. Litter decomposition of Sasa leaf and Sasa culm was significantly slower than that of tree leaf during first and second years. The slow decomposition rates of both Sasa litter types were caused by a significantly higher silicate than in tree leaf. Nitrogen concentration in litter increased as decomposition progressed, especially in Sasa leaf and tree leaf. As a result of the slow decomposition of both Sasa litter types, 111 and 73% of nitrogen to the initial amounts were retained in Sasa leaf and Sasa culm after 3 years, respectively. The amounts of retained nitrogen in Sasa leaf, Sasa culm, and tree leaf after 3 years were 1.29, 0.47, and 3.92 g N m(-2), respectively, indicating that the differences of litter decomposition rates among the litter types influence on the nitrogen cycling in forest ecosystem through the differences of the nitrogen release from litter.
机译:我们调查了Sasa矮竹(Sasa senanensis)和树木的凋落物和凋落物分解的动力学,以阐明在以Sasa底层植被为主导的自然凉爽的混交林生态系统中,植物与土壤之间有机质和氮循环的特征。在3年的研究期内,平均Sasa凋落物为164 g m(-2)年(-1),约占总凋落物的29%。在第一年和第二年,Sasa叶和Sasa茎的凋落物分解明显慢于叶片。两种Sasa凋落物的分解速度较慢,其原因是硅酸盐的含量明显高于树叶。分解过程中,凋落物中的氮浓度增加,特别是在莎莎叶和树叶中。由于两种Sasa凋落物的缓慢分解,三年后分别在Sasa叶片和Sasa茎秆中保留了111%和73%的氮至初始量。 3年后,Sasa叶片,Sasa茎秆和树木叶片中的残留氮量分别为1.29、0.47和3.92 g N m(-2),表明不同凋落物类型之间的凋落物分解速率的差异会影响氮素的吸收。森林生态系统中氮的循环是通过凋落物中氮释放的差异来实现的。

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