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A shaly look at brittleness

机译:谢利看脆弱性

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Brittleness is considered a key parameter for hydraulic fracturing initiation and propagation in low permeability rock, like gas shale. Plasticity, which in general increases with reduced brittleness, plays an important role in assessment of the mud weight window for borehole stability during drilling in shale. There is no unique definition of brittleness, rather a variety of index parameters that can be obtained from laboratory or field data, and which do not necessarily represent a coherent picture. This is digested here by analysis of rock mechanical test data mainly on high porosity, high clay content North Sea shale. Brittleness, defined by the amount of linear strain as part of the total strain before failure, and as the stress drop relative to peak stress after failure, was found to decrease with increasing stress level (as expected). Brittleness was also found to decrease with increasing temperature and with exposure to brine containing KC1. Experiments furthermore demonstrate that pore pressure evolution contributes strongly to undrained plasticity, whereas the drained shale response is largely brittle. In practical field situations, one needs to address the situation closely to find which definition of brittleness that is the most appropriate.
机译:脆性被认为是液压压裂启动和低渗透岩石繁殖的关键参数,如气体页岩。可塑性,这通常随着脆性降低而增加,在页岩钻井期间评估泥浆稳定性的泥浆重量窗口中起重要作用。没有独特的脆性定义,而是可以从实验室或现场数据获得的各种索引参数,并且不一定表示相干图片。这里通过分析主要用于高孔隙度,高粘土含量北海页岩来消化这一点。脆性,由线性菌株的量定义为失败前的总菌株的一部分,并且由于在失败后的应力下降相对于峰值应力,因此随着应力水平的增加而减少(如预期的)。还发现脆性随着温度的增加和暴露于含有KC1的盐水而降低。实验还表明孔隙压力进化有助于不可培养的可塑性,而排出的页岩响应大大脆弱。在实际场地的情况下,人们需要密切地解决这种情况,以找到最合适的脆性的定义。

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