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Comparison of Geostatistical Kriging Algorithms for Intertidal Surface Sediment Facies Mapping with Grain Size Data

机译:潮汐表层沉积物相与粒度数据地统计克里金法的比较

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摘要

This paper compares the predictive performance of different geostatistical kriging algorithms for intertidal surface sediment facies mapping using grain size data. Indicator kriging, which maps facies types from conditional probabilities of predefined facies types, is first considered. In the second approach, grain size fractions are first predicted using cokriging and the facies types are then mapped. As grain size fractions are compositional data, their characteristics should be considered during spatial prediction. For efficient prediction of compositional data, additive log-ratio transformation is applied before cokriging analysis. The predictive performance of cokriging of the transformed variables is compared with that of cokriging of raw fractions in terms of both prediction errors of fractions and facies mapping accuracy. From a case study of the Baramarae tidal flat, Korea, the mapping method based on cokriging of log-ratio transformation of fractions outperformed the one based on cokriging of untransformed fractions in the prediction of fractions and produced the best facies mapping accuracy. Indicator kriging that could not account for the variation of fractions within each facies type showed the worst mapping accuracy. These case study results indicate that the proper processing of grain size fractions as compositional data is important for reliable facies mapping.
机译:本文比较了使用粒度数据的不同地统计学克里金法对潮间带沉积物相图的预测性能。首先考虑指示器克里金法,其从预定义相类型的条件概率映射相类型。在第二种方法中,首先使用cokriging预测粒度分数,然后映射相类型。由于粒度分数是成分数据,因此在空间预测期间应考虑其特征。为了有效地预测成分数据,在进行协同克里金分析之前应用了对数比值变换。就分数的预测误差和相映射精度而言,将转换变量的协同克里金的预测性能与原始分数的协同克里金的预测性能进行了比较。从韩国Baramarae滩涂的案例研究来看,基于分数对数比率转换的协同克里格法的映射方法在基于分数的预测中优于基于未转化分数的协同克里格法的映射方法,并且产生了最佳的相图精度。不能解释每种相类型内分数变化的指标克里金法测绘精度最差。这些案例研究结果表明,正确处理晶粒度分数作为成分数据对于可靠的相图绘制很重要。

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  • 作者

    No-Wook Park; Dong-Ho Jang;

  • 作者单位
  • 年(卷),期 -1(2014),-1
  • 年度 -1
  • 页码 145824
  • 总页数 11
  • 原文格式 PDF
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