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Lithof acies and petrophysical properties of Portland Base Bed and Portland Whit Bed limestone as related to durability

机译:波特兰基床和波特兰惠特床石灰石的岩性和岩石物理性质与耐久性的关系

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This study focuses on the differences in lithofacies and petrophysical properties of Base Bed and Whit Bed Portland limestone and the presumed relationships between these characteristics and the durability of this building stone. As Portland limestone probably will be used as a stone for several restoration projects in the Netherlands in the near future, it is of great importance to know the weathering behaviour, especially its resistance against freeze/thaw decay. Samples of Portland limestone were analyzed by means of thin section microscopy, X-Ray fluorescence spectroscopy, and measurements of petrophysical properties such as watersaturation, porosity, permeability and specific surface area. Distribution of pore throat diameters were analyzed by mercury porosimetry. Results of a freeze/thaw test performed on Whit Bed limestone were also taken in account. The Whit Bed consists of a medium grained, fine to coarse bioclastic oolitic limestone (oobiosparite; oolitic grainstone). Generally the fabric is grain supported showing a large amount of open inter-particle pores. High effective porosity combined with high permeability (1000 - 1400 milliDarcy), predominantly reflect the open interparticle porosity. The Base Bed is also a coarse bioclastic oolitic grainstone, but the oolitic fabric shows a tighter, matrix-rich compacted texture. Samples from the Base Bed show differences in primary matrix contents compared to the Whit Bed and differences in diagenesis, resulting in different physical properties. For example, a lower effective porosity (15.11 - 15.99 vol.%) and a lower permeability (35.0 - 80.1 milliDarcy). It is concluded that a thorough study of lithofacies (especially microfacies) and analysis of microporosity reveal basic data for selecting the most durable type of limestone. In this particular case, using only samples from one quarry, the Whit Bed samples are thought to be the most durable ones.
机译:这项研究的重点是基床和惠特床波特兰石灰石的岩相和岩石物理性质的差异,以及这些特征与这种建筑石材的耐久性之间的假定关系。由于波特兰石灰石可能会在不久的将来用作荷兰多个修复项目的石头,因此了解风化行为,尤其是其抗冻融性的重要性非常重要。通过薄层显微镜,X射线荧光光谱法和岩石物理性质(如水饱和度,孔隙度,渗透率和比表面积)的测量来分析波特兰石灰石样品。通过水银孔率法分析孔喉直径的分布。还考虑了在惠特床石灰石上进行的冻融测试结果。惠特床由中等粒度,细到粗的生物碎屑橄榄岩石灰岩(卵生物碎屑岩;橄榄石粒岩)组成。通常,织物是颗粒支撑的,显示出大量的开放的颗粒间孔。高效孔隙率与高渗透率(1000-1400毫达西)相结合,主要反映了开放的颗粒间孔隙率。基床也是一种粗碎屑的生物碎屑质橄榄石花岗岩,但该橄榄质织物显示出更紧密,富含基质的压实纹理。与惠特床相比,来自基础床的样品显示出原始基质含量的差异以及成岩作用的差异,从而导致了不同的物理性质。例如,较低的有效孔隙率(15.11-15.99体积%)和较低的渗透率(35.0-80.1毫达西)。结论是,对岩相(尤其是微相)的透彻研究和对微孔性的分析揭示了选择最耐用类型的石灰岩的基本数据。在这种特殊情况下,仅使用一个采石场的样品,Whit床样品被认为是最耐用的样品。

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