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首页> 外文期刊>International Journal of Heat and Mass Transfer >Heat and mass transfer in landfills: Simulation of the pile self-heating and of the soil contamination
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Heat and mass transfer in landfills: Simulation of the pile self-heating and of the soil contamination

机译:垃圾填埋场的传热传质:桩自热和土壤污染的模拟

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The unsteady 2D heat and mass transfer of waste piles in landfill sites in which self-heating of piped material occurs and the effect on the soil below them are studied. A simplified mathematical model that includes temperature, water content, oxygen and solute (ammonium) concentration is proposed. Inside the pile, the biological and chemical reactions increase the temperature whilst consuming oxygen. Here the solute and water content are not solved for. In the soil, ammonium leaching from the landfill site into the surrounding soil is considered. Therefore, a diffusion partial differential equation (PDE) system without cellulose consumption and with source terms is considered and only temperature, oxygen and solute concentration are solved for. An Arrhenius equation is used to calculate the effect of temperature on the solute hydrodynamic parameters of the soil. The mathematical model is solved for the ammonium, oxygen concentration and temperature in thesoil by means of the finite volume method. In the soil the water content is considered to be in steady state. Comparisons between analytical and numerical results for the 2D solute equation allow the algorithm to be validated. A mesh study is carried out in order to verify the algorithms convergence and to decrease the simulation time. The effect of the soil type on energy generation and mass transfer in the pile and the soil hollow depth in which the waste pile is placed are analyzed. When the soil thermal diffusion is lower, the time over which self-heating inside the pile takes place is so shorter, as expected. The hollow depth where the waste pile is placed may be related with the solute concentration near the interface air/soil and infiltration depth in the soil. In all cases, the ammonium concentration infiltrated through the hole located in the landfill base, at the interface air/soil, on both sides, has not increased.
机译:研究了垃圾堆填埋场中管道材料自热发生的非稳态二维传热和传质,以及它们对下方土壤的影响。提出了一个简化的数学模型,该模型包括温度,水含量,氧气和溶质(铵)浓度。在堆内部,生物和化学反应会在消耗氧气的同时提高温度。在这里溶质和水含量无法解决。在土壤中,考虑了铵从填埋场浸出到周围土壤中的情况。因此,考虑了没有纤维素消耗和带有源项的扩散偏微分方程(PDE)系统,并且仅求解了温度,氧气和溶质浓度。 Arrhenius方程用于计算温度对土壤溶质水动力参数的影响。通过有限体积法求解了土壤中​​铵,氧浓度和温度的数学模型。在土壤中,水分被认为处于稳定状态。二维溶质方程的分析结果与数值结果之间的比较使该算法得以验证。进行网格研究是为了验证算法的收敛性并减少仿真时间。分析了土壤类型对堆中能量产生和传质的影响以及放置废桩的土壤中空深度。当土壤的热扩散较低时,如预期的那样,桩内部发生自热的时间将缩短。放置废料堆的中空深度可能与空气/土壤界面附近的溶质浓度和土壤中的渗透深度有关。在所有情况下,从位于垃圾填埋场底部两侧的空气/土壤界面的孔渗入的铵浓度并未增加。

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