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首页> 外文期刊>Journal of Powder Technology >Correlation between Shear Wave Velocity and Porosity in Porous Solids and Rocks
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Correlation between Shear Wave Velocity and Porosity in Porous Solids and Rocks

机译:多孔固体和岩石中剪切波速度与孔隙率的相关性

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The shear wave velocity dependence on porosity was modelled using percolation theory model for the shear modulus porosity dependence. The obtained model is not a power law dependence (no simple scaling with porosity), but a more complex equation. Control parameters of this equation are shear wave velocity of bulk solid, percolation threshold of the material and the characteristic power law exponent for shear modulus porosity dependence. This model is suitable for all porous materials, mortars and porous rocks filled with liquid or gas. In the case of pores filled with gas the model can be further simplified: The term for the ratio of the gas density to the density of solid material can be omitted in the denominator (the ratio is usually in the range of (10−4, 10−3) for all solids). This simplified equation was then tested on the experimental data set for porous ZnO filled with air. Due to lack of reasonable data the scientists are encouraged to test the validity of proposed model using their experimental data.
机译:利用渗流理论模型对剪切波速度对孔隙度的依赖性进行了建模,以求出剪切模量对孔隙度的依赖性。所获得的模型不是幂律相关性(没有简单的孔隙率定标),而是更复杂的方程式。该方程的控制参数是块状固体的剪切波速度,材料的渗滤阈值以及与剪切模量孔隙率相关的特征幂律指数。该模型适用于所有充满液体或气体的多孔材料,砂浆和多孔岩石。对于充满气体的孔隙,可以进一步简化模型:分母中可以省略气体密度与固体物质密度之比的术语(该比率通常在(10−4, 10-3)(对于所有固体)。然后在充有空气的多孔ZnO的实验数据集上测试了该简化方程。由于缺乏合理的数据,鼓励科学家使用他们的实验数据来检验所提出模型的有效性。

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