The Effect of Slickwater on Shale Properties and Main Influencing Factors in Hydraulic Fracturing

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Geofluids Pub Date : 2023-12-18 DOI:10.1155/2023/6645245
Jiawei Liu, Xuefeng Yang, Shengxian Zhao, Yue Yang, Shan Huang, Lieyan Cao, Jiajun Li, Jian Zhang
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Abstract

As shale gas reservoirs have low porosity and low permeability, hydraulic fracturing is a necessary means for industrial exploitation of shale gas. In this study, aiming at the problem of reservoir damage in the process of hydraulic fracturing of shale gas reservoir, a physical simulation method of slickwater fracturing fluid flow in shale core has been established. The change laws of physical parameters of the shale were quantified after slickwater fracturing fluid filtrating into it. The main factors affecting physical parameters of shale matrix around fractures were found out in the process of fracturing, shut-in, and flowback of slickwater fracturing fluid. The results show that after treated by slickwater fracturing fluid, the wettability of shale becomes more uniform in distribution (the water contact angles from 43° to 48°). In the fracturing filtration zone, the damage rate of fracturing fluid to shale porosity is 6.4%-42.0%. Low differential pressure flowback can reduce the damage of the shale, and prolonging the time of shut-in has no obvious effect on the damage to porosity. After 0.3 d (imbibition stability time), the damage of fracturing fluid to shale permeability is basically stable (55.9%). Permeability damage is mainly caused by residue of the fracturing fluid in large pores and bound water in small pores. Analysis of weights of all fracturing parameters shows that flowback differential pressure has the largest influence weight on shale porosity (51.4%), and well shut-in time has the largest influence weight on shale permeability (62.7%). Therefore, in the production process, it is suggested to properly reduce the backflow differential pressure and moderately shorten the well shut-in time.
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泥浆水对页岩性质的影响及水力压裂的主要影响因素
由于页岩气储层孔隙度低、渗透率低,水力压裂是页岩气工业开采的必要手段。本研究针对页岩气藏水力压裂过程中的储层破坏问题,建立了页岩岩心滑油压裂液流动的物理模拟方法。研究定量分析了水力压裂液滤入页岩后页岩物理参数的变化规律。发现了在滑油压裂液压裂、关井和回流过程中影响裂缝周围页岩基质物理参数的主要因素。结果表明,经滑油压裂液处理后,页岩的润湿性分布更加均匀(水接触角从 43°到 48°)。在压裂过滤区,压裂液对页岩孔隙度的破坏率为 6.4%-42.0%。低压差回流可减轻对页岩的破坏,延长关井时间对孔隙度的破坏无明显影响。0.3 d(浸润稳定时间)后,压裂液对页岩渗透率的损害基本稳定(55.9%)。渗透率破坏主要是大孔隙中压裂液的残留和小孔隙中的结合水造成的。对所有压裂参数的权重分析表明,回流压差对页岩孔隙度的影响权重最大(51.4%),关井时间对页岩渗透率的影响权重最大(62.7%)。因此,在生产过程中,建议适当降低回流压差,适度缩短关井时间。
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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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