Deriving hydrological parameters from VRP data: accounting for uncertainties in inverted velocities and petrophysical models

J. Tronicke, G. Hamann
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Abstract

Today, vertical radar profiling (VRP) is mainly used to derive 1D velocity models in the vicinity of a borehole by inverting direct arrival traveltimes. In hydrological applications, the resulting velocity models are often used to estimate hydrological material properties such as soil water content or porosity. However, uncertainties in the inverted velocity and in the employed petrophysical models are typically ignored. We present a workflow to appraise uncertainty and nonuniqueness issues inherent to VRP traveltime inversion and to quantify the influence of these issues on the following petrophysical translation. Our strategy relies on an efficient global inversion approach, which results in an ensemble of velocity models explaining the data equally well. For estimating water content and porosity, we use the entire ensemble of velocity models which results in an ensemble of possible petrophysical parameter distributions. In addition, this Monte-Carlo procedure allows us to investigate the impact of uncertainties in the employed petrophysical model by using a variety of appropriate translations. Using synthetic VRP data and a field example, we demonstrate the applicability and the potential of the proposed workflow.
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从VRP数据推导水文参数:考虑反向速度和岩石物理模型的不确定性
目前,垂直雷达剖面(VRP)主要用于反演井眼附近的直接到达行程时间,从而获得一维速度模型。在水文应用中,得到的速度模型通常用于估计水文物质的性质,如土壤含水量或孔隙度。然而,反转速度和所用岩石物理模型中的不确定性通常被忽略。我们提出了一个工作流程来评估VRP走时反演固有的不确定性和非唯一性问题,并量化这些问题对后续岩石物理转换的影响。我们的策略依赖于一种有效的全局反演方法,这导致速度模型的集合同样很好地解释了数据。为了估计含水率和孔隙度,我们使用了整个速度模型集合,从而得到了可能的岩石物理参数分布集合。此外,这种蒙特卡罗程序允许我们通过使用各种适当的转换来研究所采用的岩石物理模型中不确定性的影响。通过综合VRP数据和现场实例,我们证明了该工作流的适用性和潜力。
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