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Global inversion of GPR traveltimes to assess uncertainties in CMP velocity models

机译:GPR行进时间的全球反演以评估CMP速度模型中的不确定性

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摘要

Velocity models are essential to process two- and three-dimensional ground-penetrating radar (GPR) data. Furthermore, velocity information aids the interpretation of such data sets because velocity variations reflect important material properties such as water content. In many GPR applications, common midpoint (CMP) surveys are routinely collected to determine one-dimensional velocity models at selected locations. To analyse CMP data gathers, spectral velocity analyses relying on the normal-moveout (NMO) model are commonly employed. Using Dix's formula, the derived NMO velocities can be further converted to interval velocities which are needed for processing and interpretation. Because of the inherent assumptions and limitations of such approaches, we investigate and propose an alternative procedure based on the global inversion of reflection travel-times. We use a finite-difference solver of the Eikonal equation to accurately solve the forward problem in combination with particle swarm optimization (PSO) to find one-dimensional GPR velocity models explaining our data. Because PSO is a robust and efficient global optimization tool, our inversion approach includes generating an ensemble of representative solutions that allows us to analyse uncertainties in the model space. Using synthetic data examples, we test and evaluate our inversion approach to analyse CMP data collected across typical near-surface environments. Application to a field data set recorded at a well-constrained test site including a comparison to independent borehole and direct-push data, further illustrates the potential of the proposed approach, which includes a straightforward and understandable appraisal of non-uniqueness and uncertainty issues, respectively. We conclude that our methodology is a feasible and powerful tool to analyse GPR CMP data and allows practitioners and researchers to evaluate the reliability of CMP derived velocity models.
机译:速度模型对于处理二维和三维探地雷达(GPR)数据至关重要。此外,速度信息有助于解释此类数据集,因为速度变化会反映出重要的材料特性(例如水含量)。在许多GPR应用中,通常会收集公共中点(CMP)测量值以确定在选定位置处的一维速度模型。为了分析CMP数据收集,通常采用依赖于法向运动(NMO)模型的光谱速度分析。使用Dix公式,可以将导出的NMO速度进一步转换为处理和解释所需的区间速度。由于这种方法的固有假设和局限性,我们研究并提出了一种基于反射旅行时间全球反演的替代程序。我们使用Eikonal方程的有限差分求解器结合粒子群优化(PSO)来精确解决正向问题,从而找到一维GPR速度模型来解释我们的数据。由于PSO是强大而有效的全局优化工具,因此我们的反演方法包括生成代表解决方案的整体,使我们能够分析模型空间中的不确定性。使用合成数据示例,我们测试和评估我们的反演方法,以分析跨典型近地表环境收集的CMP数据。将其应用于在严格限制的测试现场记录的现场数据集(包括与独立井眼数据和直接推力数据的比较),进一步说明了该方法的潜力,其中包括对非唯一性和不确定性问题的直接且易于理解的评估,分别。我们得出的结论是,我们的方法学是分析GPR CMP数据的可行且强大的工具,并允许从业人员和研究人员评估CMP衍生的速度模型的可靠性。

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