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Chemical Transport in Undisturbed Soils Estimated Using Transfer Function Models

机译:用传递函数模型估算原状土中的化学迁移

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Assessment of chemical transport in vadose zone environments is critical for conserving the quality of groundwater. This project evaluated lognormal and convection-dispersion transfer function models with a conservative tracer through soil columns with silt loam soil material. The soil cores were sampled with minimal disturbance to maintain the inherent soil structure prior to running breakthrough curves with computed tomography (CT) imaging. Estimation of transport parameters for these undisturbed, heterogeneous silt loam cores were not significantly improved with group-pixel averages. This was due to transport through the macropores present in the sample cores. With more homogeneous cores, group-pixel averages of 1.0 × 1.0 mm or 2.0 × 2.0 mm were adequate to reduce fluctuations of CT image numbers. When using resident concentration estimates, the estimations improved since most of the chemical moved through the macropores. Applications of transfer function models were used in undisturbed soil columns with a conservative tracer. Assessment of chemicals with adsorption properties may be evaluated in the future.
机译:包气带环境中化学迁移的评估对于保护地下水质量至关重要。该项目评估了对数正态分布和对流扩散传递函数模型,并使用保守的示踪剂通过含粉砂壤土材料的土柱进行了追踪。在使用计算机断层扫描(CT)成像运行穿透曲线之前,以最小干扰对土芯进行取样,以保持固有的土壤结构。这些未受干扰的非均质粉砂壤土岩芯的输运参数估计与组像素平均值相比没有显著改善。这是由于通过样本岩芯中存在的大孔隙进行运输。对于更均匀的核心,1.0×1.0 mm或2.0×2.0 mm的组像素平均值足以减少CT图像数量的波动。当使用居民浓度估计值时,由于大多数化学物质通过大孔隙,估计值有所改善。传递函数模型应用于具有保守示踪剂的原状土柱。将来可能会对具有吸附特性的化学品进行评估。

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