...
首页> 外文期刊>International Journal of Coal Geology >Statistical analysis of vitrinite reflectance data―a new approach
【24h】

Statistical analysis of vitrinite reflectance data―a new approach

机译:镜质反射率数据的统计分析-一种新方法

获取原文
获取原文并翻译 | 示例

摘要

The reflectance of vitrinite (collotelinite) particles is a widely used parameter as a geothermometer for the estimation of the thermal maturity of organic matter enclosed in rocks. However, several problems have occurred during the last decades, which can he traced back to basically three causes: human mistakes, technical problems, and problems associated with the structural and compositional inhomogeneity of organic matter. Whilst in most cases the first two types of uncertainties can be handled by standardization, the third can cause significant problems during interpretation due to its generally inestimable character. The suppression of vitrinite reflectance and statistical problems originated from small sample size, and outliers belong to this latter type. International standards, such as the ASTM and the ISO, define the vitrinite reflectance parameter as a statistical average of measured data, disregarding the fact that the average is an unresisting and unrobust statistical parameter. In other words, the average is very sensitive to outliers and distribution. The aim of this research was to find and test a better, more resistant, and robust statistical parameter used by traditional parametric and nonparametric statistics, which can be applied in practice instead of the average. Three categories of statistical problems were studied on coal and disperse organic matter (DOM) samples: the distribution of measured values, the effect of data number, and the effect of outliers on statistical parameters. The statistical experiments carried out on numerous original and generated sample sets show that the median (med) and the most frequent value (Mn), a special weighted average, are better parameters to estimate the thermal maturity of organic matter especially above 1% reflectance value.
机译:镜质(软沸石)颗粒的反射率是作为地热仪广泛使用的参数,用于估算围岩中有机物的热成熟度。但是,在过去的几十年中发生了一些问题,他可以追溯到基本上三个原因:人为错误,技术问题以及与有机物的结构和组成不均匀性相关的问题。尽管在大多数情况下,前两种不确定性可以通过标准化处理,但第三种不确定性通常由于其不可估量的特性而在解释时会引起重大问题。镜质体反射率的抑制和统计问题源于小样本量,离群值属于后一种类型。国际标准(例如ASTM和ISO)将镜质体反射率参数定义为测量数据的统计平均值,而忽略了该平均值是不可抗拒且不强健的统计参数这一事实。换句话说,平均值对异常值和分布非常敏感。这项研究的目的是找到并测试传统参数和非参数统计使用的更好,更具抵抗性和鲁棒性的统计参数,该参数可在实践中代替平均使用。研究了煤和分散有机物(DOM)样本的三类统计问题:测量值的分布,数据数的影响以及离群值对统计参数的影响。对大量原始和生成的样本集进行的统计实验表明,中值(med)和最频繁的值(Mn)(特殊的加权平均值)是更好的参数,可用来估计有机物的热成熟度,尤其是高于1%的反射率值。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号