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首页> 外文期刊>Soils and foundations >CHARACTERISTICS OF STRENGTH FOR HYDRAULIC FRACTURING OF BUFFER MATERIAL
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CHARACTERISTICS OF STRENGTH FOR HYDRAULIC FRACTURING OF BUFFER MATERIAL

机译:缓冲材料液压断裂的强度特征

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The fundamental characteristics of strength for the hydraulic fracturing of highly compacted bentonite were studied. Firstly, the constant pressurize rate tests were carried out for the material having various specifications. Secondly, the cyclic pressurize test was carried out to examine the self-sealing function as a buffer material. Thirdly, the constant pressure test was carried out to observe the change in strength during seepage. The observed phenomena were analytically examined. As a result, it was found that the strength for hydraulic fracturing of the buffer material increased with the increase of initial dry density, decrease of sand-mixture ratio and decrease of water content. The swelling pressure of the buffer material worked as a constraint stress for the strength for hydraulic fracturing. The fracture made by hydraulic fracturing was fixed through the supply of water. However a long period of low-pressure supply was needed to recover the strength at the failed parts. While the tensile failure was dominant, the specimen having a low dry density might be failed initially by the shear failure. When the water content became large during seepage, the strength for hydraulic fracturing reduced.
机译:研究了高密度膨润土水力压裂强度的基本特征。首先,对具有各种规格的材料进行恒压速率测试。其次,进行循环加压试验以检验自密封作为缓冲材料的功能。第三,进行恒压试验以观察渗透过程中强度的变化。分析观察到的现象。结果,发现缓冲材料的水力压裂强度随着初始干密度的增加,砂混合比的降低和水含量的降低而增加。缓冲材料的溶胀压力作为水力压裂强度的约束应力。水力压裂造成的裂缝通过供水来固定。但是,需要长时间的低压供应以恢复失效零件的强度。虽然拉伸破坏是主要的,但是具有低干密度的样品可能最初会由于剪切破坏而破坏。当渗水期间水含量变大时,水力压裂强度降低。

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