Gini系数在镜质体反射率量测分析上之应用

孙立中; 杨宗霖; 蔡龙珆

doi:10.11781/sysydz200103338

Gini系数在镜质体反射率量测分析上之应用

doi: 10.11781/sysydz200103338

1.
中央大学地球物理所环境研究中心台湾中坜南开技术学院电机系, 台湾南投
2. 中央大学应用地质所, 台湾中坜

详细信息

作者简介:
孙立中(1962- ),男,博士,主要从事煤岩学方面的研究工作.

中图分类号: TE135
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出版历程
- 收稿日期: 2001-04-09
- 刊出日期: 2001-07-25

APPLICATION OF GINI COEFFICIENT ON THE ANALYSIS OF VITRINITE REFLECTANCE MEASUREMENT

1.
Center of Environmental Studies, Institute of Geophysics, National Central University, Zhongli, Taiwan, China
2. Department of Electrical Engineering, Nankai College of Technology & Commerce, Nantou, Taiwan, China

摘要

摘要: 该研究主要利用Gini系数来探讨镜质体反射率量测上不均性的结果,由单一煤样之水洗样(Y₂)及富集壳质组之样品(Y₃),与原始样(Y₁)作Gini系数的比较。分析显示水洗样Y₂之镜质体反射率有向平均值集中的情形,而富集样Y₃之Gini系数则有向平均值两端分布的趋势;向高值端的部分系受水洗的影响,而向低值端的发展,系受壳质组富集的影响。由Gini系数特性的研究可推广至已知再沉积材料之镜质体反射率的量测上,以取得一个可靠之Gini系数分布范围,作为将来分析样品时的参考。
- 量测分析 /
- 镜质体反射率 /
- Gini系数
Abstract: In order to evaluate the distribution of measured vitrinite reflectance data,Gini coefficient was applied in this study.Three groups of coal samples were prepared for the measurement of vitrinite reflectance,namely the original sample(Y₁),water washed sample (Y₂) and exinite enriched sample(Y₃) after denstty centrifuge separation.Gini coefficients were calculated and compared among them afterwards. The smaller Gini coefficient of Y₂ indicates a better kurtosis in the distribution of vitrinite reflectance,which can be explained by the effect of washing.On the other hand,the larger Gini coefficient of Y₃,a worse kurtosis in reflectance distribution,can be explained by both water-washing (right shift) and exinite enrichment (left shift).The Gini coefficient is expected to be applied further to sedimentary source and provenance studies in the future.
- measurement and analysis /
- vitrinite reflectance /
- Gini coefficient

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参考文献(12)

[1]	Stach E,Mackowsky M-Th,Teichmuller M,Taylor G H,Chandra D,Teichmuller R. Stach's Textbook of Coal Petrology (3rd ed)[M].Berlin Stuttgar:Gebruder Borntraeger,1982.535.
[2]	Tissot B P,Welte D H. Petroleum formation and occurrence:a new approach to oil gas exploration[M].Berlin:Springer-Verlag,NewYork:Heidelberg,1984.699.
[3]	Davis A.The reflectance of coal[A]. Karr C Jr. Analytical Methods for Coal and Coal Products[M].New York:Academic Press Inc,1978.27-81.
[4]	Ting F T C. Petrographic techniques in coal analysis[A].Karr C Jr. Analytical Methods for Coal and Coal Products[M].New York: Academic Press Inc,1978.3-26.
[5]	Sitler J A.Effects of source material on vitrinite reflectance[D].West Virginia University,1979,103.
[6]	ASTM.Standard D-2797[S]. ASTM Standard Manual (Part 26), 1975.350-354.
[7]	郭政隆.镜质体反光率在台湾西部油气探勘的应用.国立台湾大学地质学研究所博士论文,1997.
[8]	Lorenz M C.Methods of measuring the concentrations of wealth[M].Publications of American statistical association,1905,9.高叔康.经济学新辞典[M].三民书局出版,1983.
[9]	孙立中.抑制镜质体反射率之量测成因——以分离台湾裕峰煤为例.国立中央大学地球物理研究所博士论文,2000.
[10]	孙立中.台湾竹苗地区之煤岩学及油气生成研究.国立中央大学地球物理研究所硕士论文,1992.
[11]	Hutton A C,Cook A C.Influence of alginite on the reflectance of vitrinite from Joadja,NSW,and some other coals and oil shales containing alginite[J].Fuel, 1980,59:711-714.
[12]	孙立中,蔡龙王台,杨宗霖.镜质体反射率受抑制的量测问题.1989年度中国地质学会年会,2000.