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Comparative studies of kriging, multiquadric-biharmonic and other methods for solving mineral resources problems

机译:克里金法,多二次谐波和其他方法解决矿产资源问题的比较研究

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摘要

The multiquadric (MQ) method was discovered by Rolland L. Hardy in the late 1960s. It is a true scattered data, grid-free scheme for mapping of surfaces and volumes. It is a physically deterministic process and is related to concepts of the potential. With proper constraints it satisfies equilibrium and minimum energy conditions. The geostatistical kriging (K) method, developed by matreron in the 1960s, is a stochastic process procedure based on the theory of regionalized variables. It is claimed to be different from classical Statistics and Probability;;This dissertation consists of two major research areas: a comparative study of both the MQ and K theories, and a comparative study of the application of both methods to directly or indirectly related mineral resources problems. The results of the research shows that the MQ method yields equal or better accuracy than the K method. The MQ method avoids the costly pre-processing steps which are required by the K method. The MQ variation varies with location but the K variance does not. Both methods were able to produce representations of isarithmic contours or surfaces for the variable under investigation (temperature, wind velocity, iron grade, manganese percent, simulated data, and Iowa coal thickness). However, the K method could not rigorously produce three dimensional maps for the cases in this research which involved non-simulated data;The K stochastic error prediction formula yields an overly optimistic result. This formula can be used for comparing relative accuracy among various theoretical variograms, but for error of prediction purposes cross validation should be used as with the MQ method;Research produced the following outcomes: the MQ system is found to yield an unbiased estimation, a formula for the equal weighting of data for semivariograms in the K method, a proof of positive definiteness of the Q[superscript] TQ matrix, methods of preventing ill conditioning in coefficient matrices, methods of preventing underflow and overflow in computation, vector data analysis, and multiplane plotting. This research was supported (in part) by the Iowa State Mining and Mineral Resource Institute through the Department of the Interior\u27s Mineral Institute program administered by the U.S. Bureau of Mines under allotment Grant G1164119 and G1174119.
机译:多二次方(MQ)方法是由Rolland L. Hardy在1960年代后期发现的。它是真正的分散数据,无网格方案,用于绘制表面和体积。这是一个物理确定性的过程,与潜力的概念有关。在适当的约束下,它满足平衡和最小能量条件。 Matreron在1960年代开发的地统计Kriging(K)方法是一种基于区域变量理论的随机过程。它被认为与经典的统计学和概率论不同;本论文包括两个主要研究领域:MQ和K理论的比较研究,以及两种方法直接或间接相关矿产资源应用的比较研究。问题。研究结果表明,MQ方法产生的准确性与K方法相等或更好。 MQ方法避免了K方法所需的昂贵的预处理步骤。 MQ的变化随位置而变化,但K的变化不随位置变化。两种方法都能够为所研究的变量(温度,风速,铁号,锰百分比,模拟数据和爱荷华州煤层厚度)生成等值线轮廓或表面表示。然而,对于本研究中涉及非模拟数据的案例,K方法无法严格生成三维图; K随机误差预测公式得出的结果过于乐观。该公式可用于比较各种理论变异函数之间的相对准确度,但出于预测误差的目的,应与MQ方法一样使用交叉验证;研究得出以下结果:发现MQ系统产生无偏估计,公式在K方法中对半变异函数的数据进行相等加权,证明Q [T] TQ矩阵为正定性,在系数矩阵中防止不良条件的方法,在计算中防止下溢和溢出的方法,矢量数据分析以及多平面绘图。这项研究得到爱荷华州州矿业和矿产资源研究所的支持(部分)是通过美国矿务局管理的内政部矿产研究所计划进行的,拨款为G1164119和G1174119。

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    Sirayanone, Supachai;

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  • 年度 1988
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  • 原文格式 PDF
  • 正文语种 en
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