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Modeling lateral gas transport in soil adjacent to old landfill

机译:模拟旧垃圾填埋场附近土壤中的横向气体传输

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Lateral migration of landfill gases in soils surrounding old (closed) municipal landfills can lead to explosion hazards and damage to vegetation. Landfill gas production and migration is controlled by microbial activity and soil physical properties such as gas lair) permeability, gas diffusivity, and atmospheric pressure variations. Gas diffusivity and air permeability were measured on undisturbed samples collected at an agricultural field adjacent to an old Danish municipal landfill. Empirical expressions for predicting gas diffusivity and air permeability from soil-water content were fitted to the data. An empirical expression for calculating methane oxidation rate as a function of soil temperature was developed using site-specific measurements of methane oxidation rate. The transport and degradation parameter expressions were incorporated into a numerical model for simulating landfill gas transport, using soil-water content, temperature, and soil organic matter content as measured input parameters (functions of time and soil depth). Previous measurements of landfill gas (CO, and CH,) concentrations and fluxes in the agricultural field soil conducted over a period of one year were used to calibrate the gas transport model using methane oxidation rate, landfill gas pressure, and wind-induced dispersion as fitting parameters. The model was subsequently tested against independent concentration and flux data (not used in the model calibration). This yielded a prediction accuracy similar to that found during the calibration. The model was used to evaluate the sensitivity of landfill gas concentration and flux with respect to a set of governing parameters. The results of the sensitivity analysis indicated that landfill gas migration in the field soil was most sensitive to air permeability and soil-water content. Methane oxidation rate and atmospheric pressure variations had some effects, especially on the gas Bur, whereas gas diffusion was not important. [References: 37]
机译:垃圾填埋气体在旧的(封闭的)市政垃圾填埋场周围土壤中的横向迁移会导致爆炸危险和对植被的破坏。垃圾填埋气体的产生和迁移受微生物活动和土壤物理特性(如气体巢穴的渗透性,气体扩散率和大气压力变化)的控制。气体扩散率和空气渗透率是在与丹麦老市政垃圾填埋场相邻的农田上采集的未扰动样品上测量的。从土壤含水量预测气体扩散率和空气渗透率的经验表达式与数据拟合。使用特定位置的甲烷氧化速率测量值,得出了计算甲烷氧化速率随土壤温度变化的经验表达式。使用土壤-水含量,温度和土壤有机质含量作为测得的输入参数(时间和土壤深度的函数),将运输和降解参数表达式合并到一个用于模拟垃圾填埋气运输的数值模型中。使用甲烷氧化速率,垃圾填埋气压力和风致散度作为测量标准,对过去一年中农田土壤中的垃圾填埋气(CO和CH)浓度和通量进行了先前的测量,以校准气体传输模型。拟合参数。随后针对独立的浓度和通量数据对模型进行了测试(模型校准中未使用)。这产生了与校准期间相似的预测精度。该模型用于评估填埋气体浓度和通量相对于一组控制参数的敏感性。敏感性分析的结果表明,填埋气体在田间土壤中的迁移对透气度和土壤水分最敏感。甲烷的氧化速率和大气压力的变化有一些影响,特别是对气体Bur的影响,而气体的扩散并不重要。 [参考:37]

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