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Effects of wood ash fertilization on forest floor greenhouse gas emissions and tree growth in nutrient poor drained peatland forests

机译:施肥对贫瘠的泥炭地森林的林地温室气体排放和树木生长的影响

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摘要

Wood ash (3.1, 3.3 or 6.6 tonnes dry weight ha~(-1)) was used to fertilize two drained and forested peatland sites in southern Sweden. The sites were chosen to represent the Swedish peatlands that are most suitable for ash fertilization, with respect to stand growth response. The fluxes of carbon dioxide (CO_2). methane (CH_4) and nitrous oxide (N_2O) from the forest floor, measured using opaque static chambers, were monitored at both sites during 2004 and 2005 and at one of the sites during the period 1 October 2007-1 October 2008. No significant (p>0.05) changes in forest floor greenhouse gas exchange were detected. The annual emissions of CO_2 from the sites varied between 6.4 and 15.4 tonnes ha~~(-1), while the CH_4 fluxes varied between 1.9 and 12.5 kg ha~~(-1). The emissions of N_2O were negligible. Ash fertilization increased soil pH at a depth of 0-0.05 m by up to 0.9 units (p<0.01) at one site, 5 years after application, and by 0.4 units (p<0.05) at the other site, 4 years after application. Over the first 5 years after fertilization, the mean annual tree stand basal area increment was significantly larger (p<0.05) at the highest ash dose plots compared with control plots (0.64 m~2 ha~(-1) year~(-1) and 0.52 m~2 ha~(-1) year~(-1), respectively). The stand biomass, which was calculated using tree biomass functions, was not significantly affected by the ash treatment. The groundwater levels during the 2008 growing season were lower in the high ash dose plots than in the corresponding control plots (p<0.05), indicating increased evapotranspiration as a result of increased tree growth. The larger basal area increment and the lowered groundwater levels in the high ash dose plots suggest that fertilization promoted tree growth, while not affecting greenhouse gas emissions.
机译:木灰(3.1、3.3或6.6吨干重ha〜(-1))被用于施肥瑞典南部的两个排水和林木的泥炭地。从林分生长反应的角度出发,选择这些地点来代表最适合灰烬施肥的瑞典泥炭地。二氧化碳通量(CO_2)。在2004年至2005年期间,在两个地点以及2007年10月1日至2008年10月1日至10月1日期间,对其中一个地点的森林地面甲烷,甲烷(CH_4)和一氧化二氮(N_2O)进行了监测。 p> 0.05)检测到林地温室气体交换量的变化。这些场所的CO_2年排放量在6.4至15.4吨ha ~~(-1)之间变化,而CH_4通量在1.9至12.5 kg ha ~~(-1)之间变化。 N_2O的排放可以忽略不计。施灰5年后,在一个地点施肥,灰分施肥可在0-0.05 m深度处将土壤pH值提高至0.9个单位(p <0.01),在施肥4年后,在另一个地点将土壤pH值提高0.4个单位(p <0.05)。 。施肥后的前5年,最高灰分剂量地块的年生林分基础面积的年均显着大于对照地块(0.64 m〜2 ha〜(-1)年〜(-1)(p <0.05) )和0.52 m〜2 ha〜(-1)年〜(-1))。使用树木生物量功能计算的林分生物量不受灰分处理的显着影响。在高灰分剂量区,2008年生长季的地下水水位低于相应的对照区(p <0.05),表明由于树木生长的增加,蒸散量增加了。在高灰分剂量图中更大的基础面积增加和较低的地下水位表明施肥促进了树木生长,同时不影响温室气体排放。

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  • 来源
    《Science of the total environment》 |2010年第20期|p.4580-4590|共11页
  • 作者单位

    Teagasc. Johnstown Castle Environment Research Centre, Wexford. Co. Wexford, Ireland;

    rnThe Forestry Research Institute of Sweden, Uppsala Science Park, SE-751 83 Uppsala, Sweden;

    rnDepartment of Forest Ecology and Management, Swedish University of Agricultural Sciences, SE-901 83 Umei, Sweden;

    rnDepartment of Plant and Environmental Sciences, University of Gothenburg, Box 461,SE-405 30 Gothenburg, Sweden;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    CO_2; CH_4; N_2O; biofuel wood ash; pinus sylvestris; bog;

    机译:CO_2;CH_4;N_2O;生物燃料木灰;樟子松;沼泽;

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