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非饱和土壤条件下有机碳和硝酸盐化合物的迁移与生物转化

Transport and biotransformation of organic carbon and nitrate compounds in unsaturated soil conditions.

作者信息

Bunsri Thidarat, Sivakumar Muttucumaru, Hagare Dharmappa

机构信息

Department of Environmental Engineering, Faculty of Engineering, National Center of Excellence for Environmental and Hazardous Waste Management (NCE-EHWM), King Mongkut's University of Technology Thonburi, Bangkok, 10140, Thailand.

出版信息

Water Sci Technol. 2008;58(11):2143-53. doi: 10.2166/wst.2008.805.

Abstract

The lack of drinking water was one of the hot environmental issues that focused on the contaminants released from the failure of sanitary systems. Organic carbon and nitrate compounds were concerned since they represented a potential risk to human health and environment. Mathematical modelling was an effective tool for understanding and estimating the fate and transport of contaminants. An organic carbon and nitrate compounds transport model was developed using the mass balance concept. Richards and multiplicative Monod equations supported the estimating of advection-dispersion transport and biodegradation processes, respectively. The numerical solutions were obtained using the MATLAB programme. The model capability was evaluated using pilot scale experimental data. The depth-averaged time series of pressure head and contaminants concentration profiles were measured several times a week during 91 days. Simulations were found to provide reasonable agreement with the observed data. The aerobic biodegradation zone was observed within 15 cm depth of soil column. Even though the column was operated for 91 days, soil microbes were enough to retard these contaminants. This confirmed that the developed model could be applied to simulate the transport of the contaminants under real time boundary conditions.

摘要

饮用水短缺是备受关注的热点环境问题之一,该问题聚焦于卫生系统故障所释放的污染物。有机碳和硝酸盐化合物受到关注,因为它们对人类健康和环境构成潜在风险。数学建模是理解和估算污染物归宿与迁移的有效工具。利用质量平衡概念建立了有机碳和硝酸盐化合物迁移模型。理查兹方程和乘性莫诺德方程分别用于支持对流 - 弥散迁移和生物降解过程的估算。使用MATLAB程序获得数值解。利用中试规模实验数据评估模型性能。在91天内,每周多次测量压力水头的深度平均时间序列和污染物浓度剖面。结果发现模拟值与观测数据吻合良好。在土柱15厘米深度范围内观察到好氧生物降解区。尽管土柱运行了91天,但土壤微生物足以阻滞这些污染物。这证实了所开发的模型可用于模拟实时边界条件下污染物的迁移。

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