页岩气生产过程中规模管理模拟研究

Xu Wang, E. Mackay
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引用次数: 0

摘要

用于页岩气生产的水力压裂需要泵送大量的水;因此,为了可持续地开采页岩气,采出水管理是一个重要的问题。有充分的证据表明,只有大约10-40%的泵送流体会被送回地面,并且在此过程中,返排水中各种离子的浓度会增加。这种返排水具有高总溶解固体和高浓度的某些离子,具有显著的矿物结垢风险(Blauch, 2009)。一般来说,由于地层水的样品很难获得,因此识别页岩储层的地层水成分是非常具有挑战性的。它们可能在钻井过程中被污染,可能由于注入流体与地层水之间的流体混合而发生反应,或者只是它们可能没有得到适当的保存(Pan, 2017)。有些地层水成分的计算需要在观测到的成分数据基础上进行;然后,通过与观测到的总溶解固体(TDS)数据的比较,验证了预测的地层水成分。开发了一个包含水力裂缝和页岩储层性质的两相三维数值流动模型。(该模型假设水力裂缝已经建立,即计算包括耦合流动和组分输运,但不考虑地质力学)。它用于模拟页岩系统内的流体输送机制,并解决导致页岩储层中压裂液大量滞留的原因。为了与加拿大西部盆地(合恩河盆地)的反排水观测数据相匹配,进行了一系列模拟。开发了进一步的两相三维流动模型,以检查由于井生命周期内产出的盐水成分不断变化而导致的结垢趋势。它是基于以前的历史匹配模型,包括裂缝流体和地层水组成来预测矿物的沉淀。最后,模拟注入阻垢剂,以检验阻垢剂滞留对油井保护的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Simulation Study for Scale Management During Shale Gas Production
Hydraulic fracturing for shale gas production involves pumping large volumes of water; as a consequence of this, produced water management is an important topic to address in order to sustainably produce shale gas. It has been well documented that only approximately 10-40% of the pumped fluids will be produced back to the surface, and that there will be increased concentrations of various ions in the flowback water during this process. This flowback water, with high total dissolved solids and high concentrations of certain ions, presents a significant risk of mineral scaling (Blauch, 2009). In general, it can be very challenging to identify the in situ formation water composition in shale reservoirs since samples of the formation water can be difficult to obtain. They may have been contaminated during the drilling process, reactions may have taken place due to fluid mixing between the injected fluid and the formation water, or simply they may not have been preserved appropriately (Pan, 2017). Some calculations of formation water compositions require to be preceded based on the observed compositional data; thereafter, the predicted formation water compositions are validated by comparison with the observed total dissolved solids (TDS) data. A two-phase 3D numerical flow model has been developed that includes a hydraulic fracture and is populated with shale reservoir properties. (This model assumes the hydraulic fracture is already established – i.e. the calculations include coupled flow and component transport, but the geomechanics are not considered). It is used to simulate fluid transport mechanisms within the shale system and to address the question – what causes the significant retention of fracture fluid in shale reservoirs. A series of simulations was performed to achieve a history match with observed flowback water data in a western Canadian basin (the Horn River Basin). A further two-phase 3D flow model was developed to examine the scaling tendency due to the evolving produced brine composition over the lifetime of the well. It is based on the previously history matched model and includes the fracture fluid and formation water compositions to predict precipitation of minerals. Finally, scale inhibitor injection was simulated to examine the impact of inhibitor retention on well protection.
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