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首页> 外文期刊>Journal of Geoscience and Environment Protection >An Experimental Study on Measurement Methods of Bulk Density and Porosity of Rock Samples
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An Experimental Study on Measurement Methods of Bulk Density and Porosity of Rock Samples

机译:岩石样品体积密度和孔隙率测量方法的实验研究

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Density and porosity are fundamental andimportant physical properties of rocks in various geological problems, andaffect the other physical properties. Therefore, measurements of density andporosity of rock samples are important investigation items in both geo-scienceand geo-engineering areas. Several measurement techniques of the density andporosity are available and being applied currently. To ensure the data qualityand to conduct its quality assessment, comparison of measurement results bydifferent measurement techniques is necessary since the techniques are based ondifferent principles and test procedures. In this study, we collected eighttypes of rock samples including a gabbro, a granite, four sandstones, a weldedtuff and a mudstone as study materials, and also prepared several metalspecimens for the experimental comparison. The porosities of the eight rockscovered a very wide range from 0.3% to 50% approximately. We employed threemethods (caliper, buoyancy and helium-displacement pycnometer) to measurevolumes of regularly-shaped specimens and to determine their bulk densities andporosities. As a result, the three techniques yielded almost same bulkdensities and porosities for all the specimens. In addition, we also appliedmercury intrusion porosimetry to measure density and porosity as well as todetermine pore size distribution of the rock samples. Porosity values obtainedby the porosimetry method were underestimated in the case of high-porosity(soft) rock samples and overestimated for the very low-porosity rock samples.Ability to determine pore size distribution, however, is a very importantadvantage of the porosimetry method.
机译:密度和孔隙率是岩石在各种地质问题中的基本和重要的物理性质,并影响其他物理性质。因此,岩石样品的密度和孔隙率的测量在地球科学和地球工程领域都是重要的研究项目。目前有几种密度和孔隙率的测量技术可以应用。为了确保数据质量并进行质量评估,必须使用不同的测量技术对测量结果进行比较,因为这些技术基于不同的原理和测试程序。在这项研究中,我们收集了八种类型的岩石样品,包括辉长岩,花岗岩,四块砂岩,焊接的凝灰岩和泥岩作为研究材料,并准备了几种金属样品进行实验比较。八块岩石的孔隙度大约在0.3%至50%的范围内。我们采用了三种方法(卡尺,浮力和氦置换比重瓶)来测量规则形状的标本的体积,并确定其体积密度和孔隙率。结果,三种技术对所有样品产生的堆积密度和孔隙率几乎相同。此外,我们还采用了压汞法测量岩石的密度和孔隙率,并确定岩石样品的孔径分布。对于高孔隙度(软)岩石样品,低估了通过孔隙率法获得的孔隙率值,而对于极低孔隙率的岩石样品则高估了孔隙率值,但是确定孔径分布的能力是孔隙率法的一个非常重要的优势。

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