Experimental Simulation of Proppant Migration for Slick Water With Variable Viscosity During Fracturing

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Geofluids Pub Date : 2024-11-11 DOI:10.1155/2024/7754256
Guiquan Wang, Jingyuan Zhao, Yuxue Sun, Anqi Shen
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Abstract

The migration law of proppants in slick water during fracturing is of great significance for field fracturing. A large-scale visualized experimental device was utilized to test sand patterns for varying injection parameter combinations, and sensitivity parameters of proppant settlement are analyzed. Experimental results showed that when the viscosity of fluid is 5 mPa.s, proppants with 70–140 mesh and 8% sand ratio were used, the slick water for fracture initiation had a good sand-carrying capacity, and there was no sand bank formed at the entrance of the fracture but the spreading of sands in fractures was insufficient. When slick water with a lower viscosity of 10 mPa.s, the proppant of 40–70 mesh and 10% sand ratio were used, massive proppants were filled within the fractures, and a high sand bank was formed in the deep of the fracture, while a poor-filling effect appeared at the entrance of fracture. When the higher viscosity slick water of 20 mPa.s, proppants with 20–40 mesh and 20% sand ratio were used; with the growth of pump-in rate, the distance between the sand front and fracture entrance increased, the height of the bank is lower, and the balance height stayed the same for various fracturing fluid and proppant combination. The injection parameters affected the sand bank patterns and made diverse bank shapes, which made it essential to modify the fracturing fluid and proppant combination in the field to improve the conductivity at the entrance of the fracture.

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压裂过程中粘度可变泥浆水支撑剂迁移的实验模拟
压裂过程中支撑剂在滑水中的迁移规律对现场压裂具有重要意义。利用大型可视化实验装置测试了不同注入参数组合的砂型,分析了支撑剂沉降的敏感性参数。实验结果表明,当流体粘度为 5 mPa.s、使用 70-140 目、砂率为 8%的支撑剂时,用于压裂起始的浮水具有良好的携砂能力,压裂入口处没有形成砂库,但压裂中的砂子铺展不足。当使用粘度较低的 10 mPa.s 漂浮水、40-70 目支撑剂和 10%的砂比时,大量支撑剂被填充在裂缝内,在裂缝深处形成了较高的砂库,而在裂缝入口处填充效果较差。当使用粘度较高的20 mPa.s滑水、20-40目、砂率20%的支撑剂时,随着泵入速度的增加,砂前与裂缝入口的距离增大,砂库高度降低,不同压裂液和支撑剂组合的平衡高度保持不变。注入参数影响了砂岸形态,使砂岸形状多样化,因此在现场有必要改变压裂液和支撑剂的组合,以提高裂缝入口处的电导率。
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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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