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Experiment and Numerical Simulation on Transportation of Ammonia Nitrogen in Saturated Soil Column with Steady Flow

机译:稳定流动饱和土柱氨氮运输的实验与数值模拟

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Ammonium nitrogen in groundwater is one of the nutrient elements in the key monitoring indexes during the infiltration of water. Our objective of this study is to understand the adsorption and transportation characteristic of NH3-N in the sandy loam. The calculated distribution coefficient (K_d) and retardation factor (R) of NH3-N in the sandy loam was determined using the batch and Freundlich adsorption isotherm. We also got the break through curve (BTC) of NH4~+ in saturated sandy loam by mixed displacement experiment. To verify the accuracy of the adsorption parameters, using the effluent data from a pulse change input miscible displacement experiments, by solving inverse problems of the equilibrium and chemical nonequilibrium convection-dispersion equation with the computer code (CXTFIT 2.0), we estimated the optimized values of the retardation factor. These results indicate that the adsorption parameters calculated by our experimental data are in agreement with those estimated by the empirical formula.
机译:铵氮在地下水是水的渗透过程中的关键监控指标的营养元素之一。我们这项研究的目的是了解在沙壤土的NH3-N的吸附和传递特性。在砂壤土所计算出的分配系数(K_D)和NH3-N延迟因子(R)用的是批次和Freundlich吸附等温线来确定。我们还通过曲线拿到了破发(BTC)的NH4〜+通过混合置换实验饱和砂质壤土。为了验证吸附参数的精度,使用流出物的数据从一个脉冲改变输入混溶位移的实验中,通过求解逆平衡和化学非平衡对流色散方程的计算机代码(CXTFIT 2.0)的问题,我们估计优化值的延迟因子。这些结果表明,通过我们的实验数据计算的吸附参数与那些由经验公式估计协议。

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