Moradi A, Abbaspour K C, Afyuni M
Institute of Terrestrial Ecology, Swiss Federal Institute of Technology (ETH), Schlieren.
J Contam Hydrol. 2005 Oct;79(3-4):187-206. doi: 10.1016/j.jconhyd.2005.07.005.
Addition of trace metals such as cadmium to soils in metal-rich sewage sludge may result in contamination of soil and groundwater. This study addresses the plot-scale transport of Cd derived from sewage sludge in a layered clay soil in an arid region of central Iran. Sewage sludge was enriched by Cd at rates of 38 and 80 mg kg(-1) and applied to experimental soil plots using a complete random block design with three replicates. Cadmium concentration was measured as a function of depth after 185 and 617 days. HYDRUS-1D and MACRO codes were calibrated for Cd transport in the site treated with 80 mg kg(-1) sewage sludge. Model parameters were estimated by inverse modelling using the SUFI-2 procedure. The site treated with 38 mg kg(-1) cadmium was used to test the calibrated models. Both convection-dispersion equation (CDE) and non-equilibrium CDE in HYDRUS-1D produced reasonable calibration results. However, the estimated Freundlich sorption constants were significantly smaller than those measured in a batch study. A site tracer experiment revealed the existence of substantial macropore flow. For this reason we applied MACRO to account for this process. The calibration and test results with MACRO were as good as those obtained by HYDRUS-1D with the difference that adsorption constants were much closer to the measured ones. This indicates that in HYDRUS-1D, the adsorption parameters were underestimated in order to allow a deeper transport of Cd which had actually occurred due to macropore flow. A 20-year simulation scenario depicting the long-term effect of sludge application indicated small risk of groundwater contamination. However, high concentration of Cd near the soil surface raises a concern about the crop Cd uptake which should be further investigated.
在富含金属的污水污泥中向土壤添加镉等痕量金属可能会导致土壤和地下水污染。本研究探讨了伊朗中部干旱地区层状黏土中源自污水污泥的镉在地块尺度上的运移情况。以38和80 mg kg⁻¹的速率用镉对污水污泥进行富集,并采用完全随机区组设计将其施用于实验土壤地块,重复三次。在185天和617天后测量镉浓度随深度的变化。针对用80 mg kg⁻¹污水污泥处理的场地,对HYDRUS - 1D和MACRO代码进行了镉运移校准。使用SUFI - 2程序通过反演建模估算模型参数。用38 mg kg⁻¹镉处理的场地用于测试校准后的模型。HYDRUS - 1D中的对流 - 弥散方程(CDE)和非平衡CDE均产生了合理的校准结果。然而,估算的弗伦德利希吸附常数明显小于批量研究中测得的常数。一项场地示踪实验揭示了存在大量大孔隙流。因此,我们应用MACRO来考虑这一过程。MACRO的校准和测试结果与HYDRUS - 1D获得的结果一样好,不同之处在于吸附常数更接近实测值。这表明在HYDRUS - 1D中,为了使镉能够因大孔隙流而实际发生更深的运移,吸附参数被低估了。一个描述污泥施用长期影响的20年模拟情景表明,地下水污染风险较小。然而,土壤表层附近的高镉浓度引发了对作物吸收镉的担忧,对此应进一步研究。