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Reasons for the low flowback rates of fracturing fluids in marine shale

机译:海相页岩压裂液返排率低的原因

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In this paper, marine shale cores taken from Zhaotong, Changning and Weiyuan Blocks in South China were used as samples to investigate the interaction between fracturing fluids and shale and the retention mechanisms. Firstly, adsorption, swelling, dissolution pore, dissolution fluid mineralization degree and ionic composition were experimentally studied to reveal the occurrence of water in shale and the reason for a high mineralization degree. Then, the mechanisms of water retention and mineralization degree increase were simulated and calculated. The scanning electron microscopy (SEM) analysis shows that there are a large number of micro fractures originated from clay minerals in the shale. Mineral dissolution rates of shale immersed in ultrasonic is around 0.5–0.7%. The ionic composition is in accordance with that of formation water. The clay minerals in core samples are mainly composed of chlorites and illites with a small amount of illites/smectites, but no montmorillonites (SS), and its content is between 18% and 20%. It is verified by XRD and infrared spectroscopy that the fracturing fluid doesn't flow into the space between clay mineral layers, so it can't lead to shale swelling. Thus, the retention of fracturing fluids is mainly caused by the adsorption at the surface of the newly fractured micro fractures in shale in a mode of successive permeation, and its adsorptive saturation rates is proportional to the pore diameters. It is concluded that the step-by-step extraction of fracturing fluids to shale and the repulsion of nano-cracks to ion are the main reasons for the abrupt increase of mineralization degree in the late stage of flowing back. In addition, the liquid carrying effect of methane during the formation of a gas reservoir is also a possible reason. Based on the experimental and field data, fracturing fluid flowback rates and gas production rates of 9 wells were analyzed. It is indicated that the same block follows an overall trend, namely, the lower the flowback rates, the more developed the micro fractures, the better the volume simulation effect and the higher the gas production rates.
机译:本文以华南昭通,长宁和威远区块的海相页岩岩心为样本,研究了压裂液与页岩的相互作用及固结机理。首先,通过实验研究了吸附,溶胀,溶解孔隙,溶解液的矿化度和离子组成,揭示了页岩中水的存在以及矿化度高的原因。然后,模拟并计算了保水率和矿化度增加的机理。扫描电子显微镜(SEM)分析表明,页岩中存在大量的微裂缝,这些裂缝来自粘土矿物。浸在超声波中的页岩的矿物溶解率约为0.5-0.7%。离子组成与地层水一致。岩心样品中的粘土矿物主要由绿泥石和伊利石组成,少量的伊利石/蒙脱石,但不含蒙脱石(SS),含量在18%至20%之间。 X射线衍射和红外光谱证实,压裂液不会流入粘土矿物层之间的空间,因此不会导致页岩溶胀。因此,压裂液的保留主要是由于页岩中新破裂的微裂缝表面以连续渗透的方式吸附而引起的,其吸附饱和率与孔径成正比。结论是,压裂液逐步提取到页岩中,纳米裂缝被离子排斥,是造成返矿后期矿化度急剧增加的主要原因。另外,在储气罐形成期间甲烷的液体携带作用也是可能的原因。根据实验和现场数据,分析了9口井的压裂液返排率和产气率。结果表明,同一区块遵循总体趋势,即返排率越低,微裂缝越发育,模拟效果越好,产气率越高。

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