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Application of differential effective medium, magnetic pore fabric analysis, and X-ray microtomography to calculate elastic properties of porous and anisotropic rock aggregates

机译:应用微分有效介质,磁性孔隙结构分析和X射线显微断层摄影术来计算多孔和各向异性岩石聚集体的弹性

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摘要

A differential effective medium (DEM) model is used to predict elastic properties for a set of porous and anisotropic aggregates, comprised of mixtures of calcite and muscovite. The DEM takes into consideration an anisotropic background medium with triclinic or higher symmetry, in which inclusions of idealized ellipsoidal shape are added incrementally. In general, the calculated elastic properties of a solid that contains inclusions representing "dry" pores/cracks are strongly dependent on the orientation and aspect ratio of the inclusions. Aspect ratios of inclusions in the synthetic aggregates, which consist of air-filled pores, are estimated from anisotropy of magnetic susceptibility (AMS) of samples whose pore space has been impregnated with a colloidal ferrofluid. The AMS derived pore shape geometry is used as an input value for inclusions in the DEM. Modeling results are compared with laboratory determined elastic properties, measured with ultrasonic waves. Calculated shear wave velocities agree in general well with laboratory measured S wave velocities, whereas calculated P wave velocities are typically 0.5-1.1 km/s higher than measured values. Differences between calculated and measured P wave velocities are attributed mainly to incomplete and biased ferrofluid saturation of pores. Spherical pores are preferably filled during imbibition, in comparison to thin cracks, which leads to overprediction of the calculated P wave velocities. The amount of ferrofluid that fills the pore space is dependent on the ratio of calcite to muscovite and the load used for compaction during sample synthesis. The permeability decreases with increasing muscovite content and increasing compaction load. Incomplete saturation of samples with high-muscovite content is confirmed by X-ray microtomography density contrast imaging of dry and ferrofluid saturated specimens.
机译:使用差分有效介质(DEM)模型来预测一组方解石和白云母混合物组成的多孔和各向异性聚集体的弹性。 DEM考虑到具有三斜或更高对称性的各向异性背景介质,其中理想化椭圆形形状的内含物逐渐增加。通常,所计算的包含表示“干燥”孔隙/裂纹的夹杂物的固体的弹性性能在很大程度上取决于夹杂物的取向和纵横比。合成聚集体中由空气填充的孔隙组成的夹杂物的纵横比,是根据孔隙空间已被胶态铁磁流体浸渍的样品的磁化率(AMS)的各向异性估计的。 AMS得出的孔的几何形状用作DEM中夹杂物的输入值。将建模结果与实验室确定的弹性特性(通过超声波测量)进行比较。计算出的剪切波速度通常与实验室测得的S波速度基本吻合,而计算出的P波速度通常比测量值高0.5-1.1 km / s。计算和测得的P波速度之间的差异主要归因于孔的铁磁流体饱和度不完全和偏向。与细裂缝相比,球形孔优选在吸收过程中被填充,这导致对所计算的P波速度的过高预测。填充孔空间的铁磁流体的数量取决于方解石与白云母的比例以及样品合成过程中用于压实的载荷。渗透率随着白云母含量的增加和压实载荷的增加而降低。具有干白云母含量的样品的不完全饱和通过干燥和铁磁流体饱和样品的X射线显微断层扫描密度对比成像得以确认。

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