Modeling of NO3 transport in gypsiferous soil under unsaturated flow

R. Shihab, Ahmed A. Fattah, Noor Aldeen M. Muhawish
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Abstract

"This study was conducted to determine the effect of gypsum content and depth of water head on displacement and transport of nitrate in gypsiferous soil under unsaturated flow conditions. Also, to predict the concentration of nitrate using convection dispersion model (CDE). Soil columns with 63, 97, 142, 180, and 236 g kg-1 of gypsum were prepared. 200 mg L-1 of potassium nitrate were added to the surface of each soil column. The soil columns were leached by intermittent ponding in 2 pore volumes of water. A constant head depth of 0.005, 0.01, and 0.015 m of water was kept on the top of soil column. Samples of effluent were collected for measuring nitrate concentration. The CDE model was analyzed to estimate the best fitting between measured and predicted nitrate concentration, and to calculate dispersion coefficient (D), the retardation factor (R), and Peclet number (P). Results showed that CDE can be used to predict nitrate concentration in soil. Good fit was observed to describe breakthrough curves (BTC's), and predict the transport of nitrates in the leachate of gypsum soil columns. D values increased with the increase in the content of soil gypsum and decrease with increase the water head. Its values ranged between 6.59-9.87 m 2h-1. P and pore water velocity (v) decreased with the increase in soil gypsum content. The R values were less than 1 for all treatments"
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非饱和流动条件下石膏质土壤NO3运移模拟
本研究旨在确定非饱和流动条件下石膏含量和水头深度对石膏土中硝酸盐位移和运移的影响。并利用对流弥散模型(CDE)对硝酸盐浓度进行了预测。分别制备了63,97,142,180和236 g kg-1石膏土柱。每个土柱表面加硝酸钾200 mg L-1。在2孔隙体积的水中,采用间歇池法对土柱进行浸出。土柱顶部的水头深度分别为0.005、0.01和0.015 m。采集污水样本,测定硝酸盐浓度。对CDE模型进行了分析,以估计硝酸盐浓度实测值与预测值之间的最佳拟合,并计算了分散系数(D)、延迟因子(R)和Peclet数(P)。结果表明,CDE模型可以用于预测土壤中硝酸盐浓度。对突破曲线进行了较好的拟合,预测了石膏土柱渗滤液中硝酸盐的迁移。D值随土壤石膏含量的增加而增大,随水头的增大而减小。其值为6.59 ~ 9.87 m 2h-1。磷和孔隙水流速(v)随土壤石膏含量的增加而减小。所有处理的R值均小于1。”
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