尼日利亚西南部典型基岩磁化率与力学性质经验关系的测定与建立

O. Akintorinwa, C. A. Ajayi, A. Oyedele
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引用次数: 1

摘要

在尼日利亚西南部的一个典型的基底复杂岩体中,岩石的磁化率和力学性质是相互关联的,目的是建立两个参数相关的经验方程,并评估与土木结构承载能力相关的参数。在整个地区的地质中总共采集了30个岩石样本,并进行了力学特性测定。对露头新鲜岩体进行了磁化率测量,磁化率范围为2.1 × 10-4 ~ 9.5 × 10-4。这表示岩石中的铁含量及其硬化程度。单轴抗压强度(UCS)、杨氏模量(E)、剪切模量(µ)、体积模量(K)和泊松比(Ѵ)的取值范围分别为49 ~ 107 MPa、1003 ~ 3321 MPa、416 ~ 1310 MPa、707 ~ 2728 MPa和0.232 ~ 0.316。力学参数与磁化率的交叉图表现出直接的线性关系。该关系与单轴抗压强度、体模量和泊松比的相关系数(R)在0.60 ~ 0.85之间具有良好的相关性。磁化率与剪切和杨氏模量的关系较弱,相关系数R分别为0.44和0.47。这意味着磁化率测量可能不可靠地适用于确定岩石的刚度和岩石对现行剪切载荷的阻力率。验证结果表明,利用所建立的经验方程,可以从磁化率测量中可靠地估计岩石的力学性质。关键词:磁性,磁化率,力学,性质,岩石
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Determination and establishment of empirical relationship between magnetic susceptibility and mechanical properties of typical basement rocks in Southwestern Nigeria
Magnetic susceptibility and mechanical properties of rocks in a typical basement complex Southwestern Nigeria were correlated with the aim of establishing empirical equations relating the two parameters and evaluate the parameters as related to its competency in hosting civil structures. A total of thirty rock samples were taken across the geology of the area and subjected to mechanical properties determinations. Magnetic susceptibility measurements were carried out on in-situ fresh rock outcrops and it ranges from 2.1 × 10-4 to 9.5 × 10-4. This signifies the amount of iron content in the rocks and its level of induration. The values of uniaxial compressive strength (UCS), Young’s modulus (E), shear modulus (µ), bulk modulus (K) and Poisson’s ratio (Ѵ) ranges from 49 - 107 MPa, 1003 - 3321 MPa, 416 - 1310 MPa, 707 - 2728 MPa and 0.232 - 0.316, respectively. The cross plots of the mechanical parameters with the magnetic susceptibility exhibit a direct linear relationship. The relationship shows a good correlation with coefficient of correlation (R) ranging from 0.60 to 0.85 for uniaxial compressive strength, bulk modulus and Poisson’s ratio. The magnetic susceptibility relationship with shear and Young’s Modulus are relatively weak with coeffecient of correlation (R) of 0.44 and 0.47, respectively. This implies that, magnetic susceptibility measurement may not be reliably applicable in determination of the stiffness of rocks and the rate of resistance of rocks to prevailing shearing loads. The validation results show that, reliable mechanical properties of rocks can be estimated from magnetic susceptibility measurements using the established empirical equations. Key words: Magnetic, susceptibility, mechanical, properties, rocks.
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来源期刊
International Journal of Physical Sciences
International Journal of Physical Sciences 综合性期刊-综合性期刊
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