The formation young’s modulus and textural attributes of the Axx-field from southern Niger delta, Nigeria

Joseph Gordian ATAT, Emmanuel Bassey UMOREN, Akaninyene Okon AKANKPO, Joyce Ime ISAIAH
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Abstract

This research was carried out to determine the formation brittleness and textural attributes of an Axx-Field in the Niger Delta Basin. Data available for this study were obtained from three wells (A11, A22 and A33). They were analyzed using Microsoft Excel after spurious values were removed. Two techniques (John Fuller and Plumb Bradford) were used to determine static young's modulus but only one is reported because after statistical analysis on both, the one reported was adequate for accurate outcomes although both approaches have low variance. The results indicates that the highest values of static and dynamic young's modulus are 2.05 x 1025N/m2 and 1.93 x 1010N/m2 respectively. The lowest values are 1.1 x 1024N/m2 and 8.5 x 109N/m2 respectively for well A11. The average values are 1.024 x 1025N/m2 and 5.25 x 1023N/m2 for this well. For well A22, the highest and lowest values of dynamic young’s modulus are 1.5848 x 1010N/m2 and 1.5726 x 1010N/m2 while those of static are correspondingly 1.47 x 1025N/m2 and 9.01 x 1014N/m2. Their average values are 1.5787 x 1010N/m2 and 7.35 x 1024N/m2 for dynamic and static young's moduli respectively. Also, for well A33, dynamic has the lowest value as 3.28 x 1010 N/m2; static has 8.36 x 1014N/m2 and their highest correspond to 2.04 x 1010N/m2 and 7.08 x 1025N/m2. The average value for this well are 2.66 x 1010N/m2 and 3.54 x 1025 N/m2 for dynamic and static respectively. The static Young's modulus results define the formation as brittle, whose environment is extremely poorly sorted, very fine skewed and very leptokurtic with low energy for well A11, very poorly sorted, fine skewed and platykurtic for well A22, extremely poorly sorted, very fine skewed and mesokurtic for well A33.
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尼日利亚尼日尔三角洲南部 Axx 油田的地层青年模量和纹理属性
本研究旨在确定尼日尔三角洲盆地 Axx 油田的地层脆性和纹理属性。本研究的数据来自三口油井(A11、A22 和 A33)。在去除虚假值后,使用 Microsoft Excel 对数据进行了分析。使用了两种技术(John Fuller 和 Plumb Bradford)来确定静态青年模量,但只报告了其中一种,因为在对两种技术进行统计分析后,尽管两种方法的方差都很小,但报告的一种技术足以获得准确的结果。结果表明,静态和动态杨氏模量的最高值分别为 2.05 x 1025N/m2 和 1.93 x 1010N/m2。A11 井的最低值分别为 1.1 x 1024N/m2 和 8.5 x 109N/m2。该井的平均值分别为 1.024 x 1025N/m2 和 5.25 x 1023N/m2。在 A22 井中,动态青年模量的最高值和最低值分别为 1.5848 x 1010N/m2 和 1.5726 x 1010N/m2,而静态青年模量的最高值和最低值分别为 1.47 x 1025N/m2 和 9.01 x 1014N/m2。它们的平均值分别为 1.5787 x 1010N/m2 和 7.35 x 1024N/m2。此外,在 A33 井中,动态值最低,为 3.28 x 1010 N/m2;静态值为 8.36 x 1014 N/m2,它们的最高值分别为 2.04 x 1010 N/m2 和 7.08 x 1025N/m2。这口井的动态和静态平均值分别为 2.66 x 1010N/m2 和 3.54 x 1025N/m2。静态杨氏模量结果表明地层为脆性地层,A11 井的地层环境为极差分选、极细斜和低能量的极左曲地层;A22 井的地层环境为极差分选、细斜和板状曲地层;A33 井的地层环境为极差分选、极细斜和中曲地层。
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