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Effect of forest thinning on soil net nitrogen mineralization and nitrifi-cation in a Cryptomeria japonica plantation in Taiwan

机译:林间伐对台湾柳杉人工林土壤净氮矿化和硝化作用的影响

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摘要

We investigated the effect of forest thinning on soil nitrogen mineralization, nitrification and transformation in a Cryptomeria japoni-ca plantation at high elevation to provide basic data for forest manage-ment. We chose four study plots for control, light, medium and heavy thinning treatment, and three sub-plots for buried bag studies at similar elevations in each treatment plot to measure the net N mineralization and nitrification rates in situ. The contents of soil inorganic N (ammonium and nitrate) were similar between treatments, but all varied with season, reaching maxima in September 2003 and 2004. The seasonal maximum net Nmin rates after four treatments were 0.182, 0.246, 0.303 and 0.560 mg⋅kg-1⋅d-1 in 2003, and 0.242,0.258,0.411 and 0.671 mg⋅kg-1⋅d-1in 2004, respectively. These estimates are approximate with the lower annual rates of N mineralization for this region. Forest thinning can enhance net N mineralization and microbial biomass carbon. The percentage of annual rates of Nmin for different levels of forest thinning compared with the control plot were 13.4%, 59.8%and 154.2%in 2003, and 0.1%, 58.8%and 157.7%in 2004 for light, medium, and heavy thinning, respectively. These differences were related to soil moisture, temperature, precipita-tion, and soil and vegetation types. Well-planned multi-site comparisons, both located within Taiwan and the East-Asia region, could greatly im-prove our knowledge of regional patterns in nitrogen cycling.
机译:我们调查了森林抚育对高海拔柳杉人工林土壤氮矿化,硝化和转化的影响,为森林管理提供了基础数据。我们选择了四个研究样地进行控制,轻,中和重稀疏处理,并在每个处理样地中以相似的海拔高度选择了三个子图进行埋袋研究,以现场测量净氮矿化和硝化率。不同处理之间土壤无机氮(铵和硝酸盐)含量相似,但随季节变化,在2003年9月和2004年达到最大值。四种处理后的季节最大净Nmin率为0.182、0.246、0.303和0.560 mg·kg 2003年为-1⋅d-1,2004年分别为0.242、0.258、0.411和0.671 mg·kg-1·d-1。这些估算值与该地区较低的年度N矿化率近似。森林间伐可以增强净氮矿化和微生物生物量碳。与对照样地相比,不同森林间伐水平的Nmin年率百分比分别为2003年的13.4%,59.8%和154.2%; 2004年轻,中,重度间伐的Nmin的年率分别为0.1%,58.8%和157.7%,分别。这些差异与土壤湿度,温度,降水以及土壤和植被类型有关。在台湾和东亚地区进行精心策划的多站点比较,可以大大提高我们对氮循环区域模式的了解。

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  • 来源
    《林业研究(英文版)》 |2014年第3期|571-578|共8页
  • 作者单位

    Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China;

    Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China;

    Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China;

    Fujian Academy of Agricultural Sciences, Fuzhou 350003, 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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