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Novel Mathematical Simulation of NOM (Natural Organic Matter) Motion in Bottom Sediment

机译:底泥中NOM(天然有机物)运动的新型数学模拟

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Approach of organic material anaerobic biodegradation and species of organic matter in sediment were discussed, then a classifying method of the species was proposed on a new viewpoint. Based on the proposed method, a pore water COD numerical model in bottom sediment system was derived originally, which differs from other ADS model in adding a COD-creating term. The model was validated via microcosm experiment. Then the model was used to mathematically simulate COD concentration of pore water in bottom sediment in order to analyze sensitivity of parameters in the model. The results indicated that COD-creating factor at beginning stage, pore water COD-attenuating factor in bottom sediment are the most important coefficients in the new model, which should be estimated accurately. Results also show that, because of the assumption of sorption/desorption equilibrium, the new model is valid only when vertical velocity of pore water is less than 5 m/d.
机译:讨论了有机物厌氧降解的方法和沉积物中有机物的种类,然后提出了一种新的分类方法。在此基础上,首次推导了底泥系统孔隙水COD数值模型,该模型与其他ADS模型的区别在于增加了COD生成项。该模型已通过微观实验验证。然后使用该模型数学模拟底部沉积物中孔隙水的COD浓度,以分析模型中参​​数的敏感性。结果表明,在新模型中,初始阶段的COD产生因子,底部沉积物中的孔隙水COD衰减因子是新模型中最重要的系数,应准确估算。结果还表明,由于吸附/解吸平衡的假设,新模型仅在孔隙水的垂直速度小于5 m / d时才有效。

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