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Fire influences needle decomposition: Tipping point in Pinus radiata carbon chemistry and soil nitrogen transformations

机译:火灾影响针分解:Pinus radiata碳化学和土壤氮转化中的提示点

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As climate change proceeds, a change in the frequency and intensity of fire events is expected to affect soil organic matter (SOM) transformations within forestry systems. A likely consequence is the development of post-fire litter layers composed of thermally altered non-senescent materials that have fallen during a fire event. In this study, Pinus radiata needles were thermally altered to determine the effect of changes in carbon chemistry on needle decomposition and nitrogen cycling. Live needles were collected and dried at 40 degrees C before being further heated for 1 h in a muffle furnace at a range of temperatures > 40 degrees C (max. = 320 degrees C) to simulate a range of canopy temperatures that can occur during a fire, and then coarsely ground and screened (0.5-1.0 man fraction retained). These needles were characterised for carbon and nitrogen content, and carbon chemistry (solid-state C-13 NMR spectroscopy); they were also used in an incubation experiment (14 days) which was performed to assess the impact of heating on nitrogen transformations. Soil respiration and extractable nitrogen pools (mineral, potentially mineralizable, and microbial biomass) were measured throughout the incubation. During the incubation, cumulative respiration and nitrogen absorption capacity decreased with increasing thermal alteration. The results indicate a step change in the response of nitrogen pools to thermal alteration of pine needles, with a critical change occurring at or before 200 degrees C. This step change in nitrogen response may be due to the thermal degradation of light fraction organic matter, simple polysaccharides, or both. From this experiment it is clear that a post fire litter layer can have distinctly different effects on the soil environment depending on canopy temperature conditions during the fire with post fire litters composed of low temperature needles absorbing most mineral nitrogen that they contact. This will in turn affect post-fire plant recovery and therefore ecological succession.
机译:随着气候变化所得,预计消防事件频率和强度的变化将影响林业系统内的土壤有机物(SOM)转变。可能的后果是由在火灾事件中落下的热改变的无衰老材料组成的火灾后垃圾层的发展。在该研究中,热改变疙瘩辐射针针,以确定碳化学变化对针分解和氮循环的影响。收集活针并在40摄氏度下在40摄氏度下进一步加热1小时,在一个温度> 40摄氏度(最大。= 320℃)范围内,以模拟在A期间可能发生的冠层温度范围火灾,然后粗略地磨碎并筛选(保留0.5-1.0人级分)。这些针的特征在于碳和氮含量,以及碳化学(固态C-13 NMR光谱);它们也用于孵育实验(14天),以评估加热对氮转化的影响。在整个孵育过程中测量土壤呼吸和可提取的氮气池(矿物质,潜在的矿物和微生物生物量)。在孵育期间,随着热改变的增加而降低累积呼吸和氮吸收能力。结果表明氮气池对松针热改变的响应的步骤变化,在200摄氏度时或之前发生临界变化。氮响应的该步骤变化可能是由于光馏分有机物质的热降解,简单的多糖,或两者。从这个实验中,显然,根据冠部温度条件,消防窝组成的冠状动脉温度条件,由低温针构成的冠状窝,吸收最多的矿物氮气的冠部温度条件,消防垃圾层对土壤环境具有明显不同的影响。这反过来又会影响火药后植物恢复,从而影响生态继承。

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