Pang Liping, Goltz Mark, Close Murray
Institute of Environmental Science and Research Ltd., PO Box 29181, Christchurch, New Zealand.
J Contam Hydrol. 2003 Jan;60(1-2):123-34. doi: 10.1016/s0169-7722(02)00061-x.
In this note, we applied the temporal moment solutions of [Das and Kluitenberg, 1996. Soil Sci. Am. J. 60, 1724] for one-dimensional advective-dispersive solute transport with linear equilibrium sorption and first-order degradation for time pulse sources to analyse soil column experimental data. Unlike most other moment solutions, these solutions consider the interplay of degradation and sorption. This permits estimation of a first-order degradation rate constant using the zeroth moment of column breakthrough data, as well as estimation of the retardation factor or sorption distribution coefficient of a degrading solute using the first moment. The method of temporal moment (MOM) formulae was applied to analyse breakthrough data from a laboratory column study of atrazine, hexazinone and rhodamine WT transport in volcanic pumice sand, as well as experimental data from the literature. Transport and degradation parameters obtained using the MOM were compared to parameters obtained by fitting breakthrough data from an advective-dispersive transport model with equilibrium sorption and first-order degradation, using the nonlinear least-square curve-fitting program CXTFIT. The results derived from using the literature data were also compared with estimates reported in the literature using different equilibrium models. The good agreement suggests that the MOM could provide an additional useful means of parameter estimation for transport involving equilibrium sorption and first-order degradation. We found that the MOM fitted breakthrough curves with tailing better than curve fitting. However, the MOM analysis requires complete breakthrough curves and relatively frequent data collection to ensure the accuracy of the moments obtained from the breakthrough data.
在本论文中,我们应用了[Das和Kluitenberg,1996年。《土壤科学美国杂志》60,1724]中关于一维对流-弥散溶质运移的时间矩解,该运移涉及线性平衡吸附和一阶降解的时间脉冲源,以分析土柱实验数据。与大多数其他矩解不同,这些解考虑了降解和吸附的相互作用。这使得可以利用柱突破数据的零阶矩估计一阶降解速率常数,以及利用一阶矩估计降解溶质的阻滞因子或吸附分配系数。应用时间矩(MOM)公式法分析了实验室柱实验中阿特拉津、嗪草酮和若丹明WT在火山浮石砂中运移的突破数据,以及文献中的实验数据。将使用MOM获得的运移和降解参数与通过使用非线性最小二乘曲线拟合程序CXTFIT,对具有平衡吸附和一阶降解的对流-弥散运移模型的突破数据进行拟合得到的参数进行了比较。还将使用文献数据得出的结果与文献中使用不同平衡模型报告的估计值进行了比较。良好的一致性表明,MOM可为涉及平衡吸附和一阶降解的运移提供一种额外有用的参数估计方法。我们发现,MOM对有拖尾的突破曲线的拟合效果优于曲线拟合。然而,MOM分析需要完整的突破曲线和相对频繁的数据采集,以确保从突破数据中获得的矩的准确性。