2019
DOI: 10.1155/2019/6537571
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An Experimental Study of Seepage Properties in Crushed Sandstone and Mudstone

Abstract: To study the effects of compression rate and weight ratio of sandstone to mudstone on permeability, water flow tests were performed on crushed rocks using an in-house designed and built water flow apparatus. Seepage properties of sandstone and mudstone were tested on specimens under six axial displacement levels. e weight ratios of the six specimens of sandstone to mudstone were set to 1 : 0, 4 : 1, 3 : 2, 2 : 3, 1 : 4, and 0 : 1. A non-Darcy law was adopted to calculate the permeability in the experiments bas… Show more

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Cited by 3 publications
(2 citation statements)
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“…At present, relevant reports of crushed gangue's bearing compression characteristics mainly focus on the particle size distribution, stress level, and macroscopic deformation. In addition, the final crushing ratio of crushed gangue samples is mainly obtained by screening the samples after the experiment [30][31][32][33][34][35][36][37][38][39][40][41][42]. However, there is no research on particle crushing characteristics during the loading process, especially under the compression condition of different loading rates.…”
Section: A Comparative Discussion With Existing Studiesmentioning
confidence: 99%
“…At present, relevant reports of crushed gangue's bearing compression characteristics mainly focus on the particle size distribution, stress level, and macroscopic deformation. In addition, the final crushing ratio of crushed gangue samples is mainly obtained by screening the samples after the experiment [30][31][32][33][34][35][36][37][38][39][40][41][42]. However, there is no research on particle crushing characteristics during the loading process, especially under the compression condition of different loading rates.…”
Section: A Comparative Discussion With Existing Studiesmentioning
confidence: 99%
“…With the change of borehole azimuth and inclination angles, the included angle between the radial direction of borehole wall and the direction of the bedding fracture changes constantly, so the radial seepage capacity of the borehole wall also changes. As there is a difference on the radial seepage capacity of the borehole wall rock, it is inevitable that there are differences in the seepage capacities between the borehole and formation under a bottomhole pressure environment and its influence on the pore pressure distribution and effective stress field near the borehole wall. It is assumed that there are horizontal fractures at the lithologic interface of the sand–mud interbedding, and the azimuth angle of the well track is 90°; the variation law of radial seepage capacity of the borehole wall is evaluated and analyzed, as shown in Figure . Figure shows the geometric relationship between the angles.…”
Section: Calculationsmentioning
confidence: 99%