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Tracer investigations at the research station 'Wagna' (Leibnitzer Feld, Austria) to detect the role of the unsaturated zone for groundwater protection

机译:研究站“WAGNA”(Leibnitzer Feld,奥地利)的示踪剂调查检测了不饱和区对地下水保护的作用

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Tracer investigation and numerical modelling of the movement of water and solids in the unsaturated and saturated zone of an aquifer enables to quantitatively predict the impact of different measures on the whole system. However, setting up a model and determining model parameters still calls for substantial research efforts. The results of tracing experiments in the unsaturated zone of a quaternary gravel fill were used to prove the measuring and sampling devices on their ability to detect transient transport phenomena of water and solutes, to illustrate the differences between hydraulic reaction of water content on infiltration events and the velocity of solute movement in the unsaturated zone, to estimate hydraulic parameters of soil horizons as a basis for the calibration of solute transport models in the unsaturated zone, to quantify different flow components using advection-dispersion transport modelling and to correct measured flow data of field lysimeters.
机译:在含水层的不饱和和饱和区中的水和固体运动的示踪剂调查和数值模型可以定量预测不同措施对整个系统的影响。但是,建立模型和确定模型参数仍需要大量的研究工作。使用季砾石填充的不饱和区中的追踪实验结果证明了测量和取样装置,以检测水和溶质的瞬态传输现象,以说明水含量对渗透事件的液压反应之间的差异不饱和区溶质运动的速度,以估计土壤液压参数作为不饱和区旋转溶质运输模型的基础,以使用平程分散传输建模量化不同流量分量,并校正测量的流量数据田间透明仪。

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