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应用地质统计学高斯模拟设计和解释土壤表面磁化率测量

Using Geostatistical Gaussian Simulation for Designing and Interpreting Soil Surface Magnetic Susceptibility Measurements.

机构信息

Warsaw University of Technology, Faculty of Building Services, Hydro and Environmental Engineering, Nowowiejska 20, 00-661 Warszawa, Poland.

出版信息

Int J Environ Res Public Health. 2019 Sep 19;16(18):3497. doi: 10.3390/ijerph16183497.

Abstract

This paper presents a new approach to the assessment of the uncertainty of using geostatistical Gaussian simulation in soil magnetometry. In the study area, numerous measurements of soil magnetic susceptibility were made, and spatial distributions of soil magnetic susceptibility were simulated. The parameters of variograms of soil magnetic susceptibility measured in the study area were determined and compared with those of simulated soil magnetic susceptibility. Regardless of the measurement scheme used, reproducibility of the original semivariograms of soil magnetic susceptibility was satisfactorily achieved when applying simulated values. A nugget effect, a sill, and a range of correlations of variograms of simulated values of soil magnetic susceptibility were similar to those of measured values. When the input data for the geostatistical simulation were averaged, the measured values of soil magnetic susceptibility and simulated spatial distributions were characterized by slightly lower standard deviations in comparison with the result of simulations based on the non-averaged, measured ones. At the same time, however, local variability of soil magnetic susceptibility was reproduced less. The accuracy of the calculations of point parameters and spatial distributions-based on the averaged values of soil magnetic susceptibility-were satisfactory, but when using geostatistical methods, it is recommended to use non-averaged magnetic susceptibility measurements.

摘要

本文提出了一种评估地质统计学高斯模拟在土壤磁测中不确定性的新方法。在研究区域内进行了大量的土壤磁化率测量,并对土壤磁化率的空间分布进行了模拟。确定了在研究区域内测量的土壤磁化率变异函数的参数,并将其与模拟的土壤磁化率进行了比较。无论使用哪种测量方案,当应用模拟值时,原始土壤磁化率半变异函数的可重复性都得到了令人满意的实现。模拟值的土壤磁化率变异函数的块金效应、基台值和相关范围与实测值相似。当地质统计学模拟的输入数据进行平均时,与基于非平均实测值的模拟结果相比,土壤磁化率的实测值和模拟的空间分布具有稍低的标准偏差。然而,与此同时,土壤磁化率的局部变异性再现性较差。基于土壤磁化率平均值的点参数和空间分布计算的准确性令人满意,但在使用地质统计学方法时,建议使用非平均的磁化率测量值。

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