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Net Nitrogen Mineralization and Nitrification in Three Subtropical Forests of Southwestern China

机译:西南三大亚热带森林的净氮矿化与硝化作用

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Nitrogen is a limiting nutrient for plant growth in many forest ecosystems; however, information on N mineralization and nitrification in subtropical forests is generally lacking. To determine the effect of forest site on N mineralization and nitrification and the key contributing factors under subtropical climate, we studied the seasonal patterns of soil N mineralization and nitrification with closed in situ core incubation method in a mixed evergreen broadleaf forest, a pure Chinese fir (Cunninghamia lanceolata (Lamb.) Hook) forest and a pure Zhennan (Phoebe zhennan S. Lee et F. N. Wei) forest in Dujiangyan, Sichuan province, southwestern China. Our results indicated that the rates and the seasonal patterns of net N mineralization and nitrification were similar among the three forest sites. The rates of both net N mineralization and nitrification were the highest in the winter season (December 2000 to April 2001), and negligible in spring and summer The variability in net N mineralization and nitrification and the specific environmental contributing factors, however, varied in different forest sites. The overall similarity in N mineralization and nitrification rates suggests that regional climate condition is the most dominant controlling factoron N mineralization and nitrification. At local scales, however, biodiversity may play an important role in patterns of N mineralization and nitrification; higher biodiversity could lead to higher and more stable N mineralization and nitrification.
机译:氮是许多森林生态系统中植物生长的限制性营养素;但是,通常缺乏有关亚热带森林中氮矿化和硝化的信息。为了确定亚热带气候下林地对氮矿化和硝化作用的影响以及主要的影响因素,我们采用封闭原位育种方法在纯常绿阔叶混交林中研究了土壤氮矿化和硝化的季节模式。 (Cunninghamia lanceolata(Lamb。)Hook)森林和中国西南部四川都江堰市的纯镇南(Phoebe zhennan S. Lee et FN Wei)森林。我们的结果表明,这三个林地之间净氮矿化和硝化的速率和季节模式相似。净氮矿化和硝化的比率在冬季(2000年12月至2001年4月)最高,而在春季和夏季可以忽略不计。但是,净氮矿化和硝化的变化以及具体的环境贡献因子因不同而有所不同。森林遗址。氮矿化和硝化速率的总体相似性表明,区域气候条件是氮矿化和硝化的最主要控制因素。然而,在地方尺度上,生物多样性可能在氮矿化和硝化的模式中起重要作用;更高的生物多样性可以导致更高和更稳定的氮矿化和硝化作用。

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