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Methodology for predicting reservoir breakdown pressure and fracture opening pressure in low-permeability reservoirs based on an in situ stress simulation

机译:基于原位应力模拟预测储层储存器中储层击穿压力和断裂开口压力的方法。

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Using numerical simulations of the paleostress field during the time of fracture formation, we predict the occurrence of fractures in the reservoirs of the second member of the Funing Formation in the Tongcheng fault zone, Subei basin, East China. We use sonic velocity measurements from rock cores and microseismic monitoring to determine the in situ stress, which is combined with fracture data to calculate the magnitude of the in situ stress at the well site. By determining the mechanical parameters of the rock, we use the finite element method (FEM) to develop a geomechanical model and conduct numerical simulations of the in situ stress field. Based on the occurrence of fractures and the numerical simulation results of the in situ stress field, we predict the opening pressure and opening sequence of natural fractures in the reservoirs. The results indicate that the maximum horizontal principal stress in the second member of the Funing Formation in the Tongcheng fault zone is oriented ENE. During the injection process, the ENE-trending fractures open first, and the ESE-trending fractures open later. The opening pressure of the fractures increases as the angle between the fracture strike and the maximum horizontal principal stress increases, and the burial depth of the fractures also has a relatively positive correlation with the opening pressure. At the structurally high site (1850 m-2350 m), the opening pressure of the fractures is in the range of 25 MPa-50 MPa, and at the structurally low site (3300 m-4000 m), the opening pressure of the fractures is in the range of 45 MPa-75 MPa. By calculating the actual fracture pressure of the reservoirs, we propose using different injection pressures in different blocks to ensure the high and stable production of oil from wells.
机译:在骨折形成期间使用古聚会场的数值模拟,我们预测桐中国县桐城盆地桐城断裂带第二成员水库骨折的发生。我们使用岩石芯和微震监测的声速测量来确定原位应力,与骨折数据相结合,以计算井场的原位应力的大小。通过确定岩石的机械参数,我们使用有限元方法(FEM)来开发地质力学模型并进行原位应力场的数值模拟。基于裂缝的发生和原位应力场的数值模拟结果,我们预测了储层中自然骨折的开口压力和开口序列。结果表明,桐城断裂区磁力形成第二成员的最大水平主应力是面向埃涅。在注射过程中,肌肉趋势裂缝首先开放,并且在后面开放的ESE趋势裂缝。由于断裂撞击和最大水平主应力之间的角度增加,裂缝的开口压力增加,并且裂缝的粗糙深度也具有与开口压力的相对正相关的相关性。在结构高位(1850 m-2350 m),裂缝的开口压力在25mPa-50MPa的范围内,并且在结构低位(3300 m-4000 m),裂缝的开口压力在45 MPa-75 MPa的范围内。通过计算储层的实际断裂压力,我们建议在不同块中使用不同的注射压力,以确保来自孔的高稳定的油。

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