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首页> 外文期刊>Forest Ecology and Management >Long-term effects of repeated urea fertilization in Douglas-fir stands on forest floor nitrogen pools and nitrogen mineralization
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Long-term effects of repeated urea fertilization in Douglas-fir stands on forest floor nitrogen pools and nitrogen mineralization

机译:道格拉斯冷杉林重复施肥对林地氮库和氮矿化的长期影响

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In six Douglas-fir [Pseudotsuga menziesii (Mirb.) Franco] stands in the Puget Sound Region in Western Washington/USA, forest floor C and N pools were quantified on control plots and on plots that had been fertilized repeatedly with urea 8-30 years ago (total amount of applied N 0.9-1.1 Mg ha(-1)). Additionally, net N mineralization and nitrification rates were assessed in field and laboratory incubation experiments. Forest floor C/N ratios were decreased on the fertilized plots of all sites compared to the respective control plots. The decreases were particularly strong at sites with initial C/N ratios larger than 30. On sites with low productivity (site index at age 50: <33 m), N fertilization resulted in considerable increases in forest floor N pools. Net N mineralization and nitrification during 12-week field incubation was negligible for the unfertilized and fertilized plots of all except one site (Pack Forest), where the stand had been clear-cut 2 years ago. The increases in N mineralization rates during 12-week laboratory incubation induced by repeated N fertilization showed an inverse relationship to the time elapsed since the last fertilizer application, and were generally larger at sites with initial forest floor C/N ratios >30. For the investigated sites, fertilization effects on net N mineralization sustained for at least 11 years after the last fertilizer application. Nitrification correlated strongly with the forest floor pH; significant formation of NO3- was observed only for 0 layers with a pH (H2O) higher than 4.5
机译:在美国华盛顿西部的普吉特海湾地区的六个道格拉斯冷杉[Pseudotsuga menziesii(Mirb。)Franco]中,对对照样地和已用尿素8-30反复施肥的样地中的林底C和N库进行了量化。年前(施用的N 0.9-1.1 Mg ha(-1)总量)。此外,在田间和实验室培养实验中评估了净氮矿化率和硝化率。与相应的对照地块相比,所有地点的施肥地块的林地碳氮比均降低。在初始C / N比大于30的地点,下降尤为明显。在生产力低下的地点(50岁时的地点指数:<33 m),施氮导致林地氮池大量增加。在12周的田间温育期间,净氮矿化和硝化作用对于除一个地点(帕克森林)以外的所有其他地区的未施肥和施肥的地块微不足道,该地点2年前已被砍伐。重复施氮导致12周实验室温育期间氮矿化速率的增加与自上次施肥以来所经过的时间成反比关系,并且通常在初始林底C / N比> 30的情况下更大。对于所调查的地点,在最后一次施肥后,施肥对净氮矿化的影响至少持续了11年。硝化作用与林地pH密切相关;仅在pH(H2O)高于4.5的0层中观察到明显的NO3-形成

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