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Observing the effects of transition zone properties on fracture vertical propagation behavior for coal measure strata

机译:观察过渡带特性对煤系地层裂缝垂直传播特性的影响

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摘要

The transition zone is a typical interface with enough thickness and high heterogeneity between the sandstone and coal and has a great effect on the fracture propagation in coal measure strata. In the study, the true tri-axial experiments were conducted with the combination of sandstone, coal and limestone outcrops. The effect of cementing strength and thickness of the transition zone was mainly studied. Three types of hydraulic fracture initiation positions were used to simulate three fracturing situations in the field. The results showed that the effect of the transition zone on the fracture vertical extension could be concluded: the fracture was easy to cross or slip with low cementing strength and turned inside the transition zone with high cementing strength; the fracture tended to branch or be blocked by the thick transition zone. The horizontal flow through face cleats and natural fracture activation in coal contributed to a more developed fracture network. The characters of pumping curve pressure "increasing - fluctuation - dropping", and the "fluctuation pressure more than initiation pressure" indicated the interface crossing. The results of experiments agreed with the previous numerical simulation and helped to optimize the fracturing design in layered coal strata.
机译:过渡带是典型的界面,在砂岩和煤之间具有足够的厚度和高度的非均质性,对煤系地层的裂缝扩展具有很大的影响。在研究中,真实的三轴实验是结合砂岩,煤和石灰岩露头进行的。主要研究了固结强度和过渡区厚度的影响。三种类型的水力压裂起始位置用于模拟现场的三种压裂情况。结果表明,过渡区对断口垂直延伸的影响可以归纳为:低固结强度的裂缝易于穿越或滑移,高固结强度的裂缝易在过渡区内部转折。裂缝倾向于分支或被较厚的过渡带阻塞。穿过煤层的水平流和煤中的自然裂缝活化作用促使裂缝网络更加发达。泵送曲线压力“增加-波动-下降”和“波动压力大于初始压力”的特征表示界面交叉。实验结果与以前的数值模拟吻合,有助于优化分层煤层的压裂设计。

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