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Investigation of Interactive Effects on Water Flow and Solute Transport in Sandy Loam Soil Using Time Domain Reflectometry

机译:时域反射法研究砂壤土中水和溶质运移的相互作用

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摘要

Surface-applied chemicals move through the unsaturated zone with complex flow and transport processes due to soil heterogeneity and reach the saturated zone, resulting in groundwater contamination. Such complex processes need to be studied by advanced measurement and modeling techniques to protect soil and water resources from contamination. In this study, the interactive effects of factors like soil structure, initial soil water content (SWC), and application rate on preferential flow and transport were studied in a sandy loam field soil using measurement (by time domain reflectometry (TDR)) and modeling (by MACRO and VS2DTI) techniques. In addition, statistical analyses were performed to compare the means of the measured and modeled SWC and EC, and solute transport parameters (pore water velocity and dispersion coefficient) in 12 treatments. Research results showed that even though the effects of soil structural conditions on water and solute transport were not so clear, the applied solution moved lower depths in the profiles of wet versus dry initial SWC and high application rate versus low application rates. The effects of soil structure and initial SWC on water and solute movement could be differentiated under the interactive conditions, but the effects of the application rates were difficult to differentiate under different soil structural and initial SWC conditions. Modeling results showed that MACRO had somewhat better performance than VS2DTI in the estimation of SWC and EC with space and time, but overall both models had relatively low performances. The means of SWC, EC, and solute transport parameters of the 12 treatments were divided into some groups based on the statistical analyses, indicating different flow and transport characteristics or a certain degree nonuniform or preferential flow and transport in the soil. Conducting field experiments with more interactive factors and applying the models with different approaches may allow better understanding of flow and transport processes in addition to the simulations of them in the unsaturated zone.
机译:由于土壤异质性,表面施用的化学物质流经具有复杂流动和运输过程的非饱和区,并到达饱和区,导致地下水污染。需要通过先进的测量和建模技术来研究这种复杂的过程,以保护土壤和水资源免受污染。在这项研究中,使用测量(通过时域反射法(TDR))和建模研究了沙质壤土土壤中土壤结构,初始土壤含水量(SWC)和施用量对优先流量和运输等因素的交互作用。 (通过MACRO和VS2DTI)技术。此外,进行统​​计分析以比较12种处理方法中测得的和建模的SWC和EC的平均值以及溶质运移参数(孔隙水速度和弥散系数)。研究结果表明,即使土壤结构条件对水和溶质运移的影响还不是很清楚,但施用的溶液在湿对干SWC与干初始SWC曲线中的移动深度较小,而高施用量与低施用量的迁移速率相对较低。在相互作用条件下,可以区分土壤结构和初始SWC对水和溶质运动的影响,但在不同的土壤结构和初始SWC条件下,难以区分施用量的影响。建模结果表明,在随时间和空间估算SWC和EC方面,MACRO比VS2DTI具有更好的性能,但总体而言,这两种模型的性能都相对较低。根据统计分析,将12种处理方法的SWC,EC和溶质运移参数的方法分为几类,表明土壤中不同的流动和运输特性或一定程度的不均匀或优先流动和运输。进行具有更多交互因素的现场实验,并以不同的方法应用模型,除了对非饱和区的流动和传输过程进行模拟外,还可以更好地理解流动和传输过程。

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