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Effects of compaction by heavy machine traffic on soil fluxes of methane and carbon dioxide in a temperate broadleaved forest

机译:重型机械交通压实对温带阔叶林土壤甲烷和二氧化碳通量的影响

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Soil compaction decreases soil aeration and water infiltration, lowering air-filled porosity, which may impact biological processes involved in soil fluxes of carbon dioxide (F-co2) and methane (F-cH4), and decrease the greenhouse gas emissions mitigation potential offered by the forestry sector. We recorded F-co2 and F-cH4 continuously for two years using automated chambers connected to a laser-based gas analyser in an experimental forest site on an acidic ruptic Luvisol that was established to assess the long-term impact of a loaded forwarder. Heavy machine traffic had considerably increased soil surface roughness. Air-filled porosity (AFP) in the first 0.1 m was lower in the trafficked plot especially in hollows than in the control almost all year long. The temperature sensitivity of F-co2 was higher for the control plot than for both mounds and hollows in the trafficked plot. Cumulative F-co2 was much higher in the control than in hollows and mounds of the trafficked plot. In contrast, annual F-cH4 did not significantly differ between the control plot and either the mounds or the hollows in the trafficked plot, but was significantly higher in mounds than in hollows. F-cH4 was negative all year round indicating a net uptake of CH4, except during winter when a net emission of CH4 was occasionally observed in the hollows on the trafficked plot. While seasonal variations of F-cH4 were well related to variations in AFP, the potential rate of methane uptake at optimal air-filled porosity was higher in the trafficked plot than in the control. (C) 2016 Elsevier B.V. All rights reserved.
机译:土壤压实减少了土壤的通气和水的渗透,降低了空气的孔隙度,这可能会影响涉及土壤通量的二氧化碳(F-co2)和甲烷(F-cH4)的生物过程,并降低温室气体减排潜力。林业部门。我们在酸性断裂性Luvisol上的实验林场中,使用连接到基于激光的气体分析仪的自动隔室,连续两年记录了F-co2和F-cH4,该酸性室被建立用来评估装载的货运代理的长期影响。繁忙的机器交通大大增加了土壤表面粗糙度。几乎全年,在被贩运的地块中,特别是在空心地带,头0.1 m处的空气孔隙度(AFP)都比对照组低。对照区的F-co2温度敏感性高于被贩运区的土丘和洼地。对照中的累积F-co2高于被贩运地块的凹陷和丘陵。相反,对照样地与被贩运样地的土丘或空洞之间的年F-cH4差异不明显,但土墩中的F-cH4明显高于空洞。 F-cH4全年都是负值,表明CH4的净吸收,除了在冬季,有时在贩运地块的空洞中会观察到CH4的净排放。尽管F-cH4的季节性变化与AFP的变化密切相关,但在最佳气孔孔隙度下,贩运地块中甲烷的潜在吸收速率要比对照高。 (C)2016 Elsevier B.V.保留所有权利。

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