Zhao Hui Hui Zhao

Ms. Zhao Hui Hui Zhao


Research Focus & Metrics

Academic Career Length

3Years (2024-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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3 June 2025
Verified
Book Chapter
Closed access
PDF file
ZZZhao Hui Hui Zhao
Zhao Hui Hui Zhao
ZRZong-Xiao Ren
Zong-Xiao Ren
CZChen-Yu Zhang
Chen-Yu Zhang
YRYan-Fei Ren
Yan-Fei Ren

16 December 2024 in Processes
Verified
Journal Article
Open access
PDF file
JWJialin Wang
Jialin Wang
JXJianping ren Xu
Jianping ren Xu
XLXinwei Liu
Xinwei Liu
铭李铭宇 李
铭宇 李
ZFZhaoyang Fan
Zhaoyang Fan
ZZZhao Hui Hui Zhao
Zhao Hui Hui Zhao
As one of the main numerical methods, the boundary element method boasts the advantages of fast computation speed and high accuracy. Based on the considerations of the influence of pressure drop, perforation height, skin coefficient, reservoir coefficient, and reservoir radius on the seepage law, a novel three-dimensional seepage model for vertical wells was established using the Laplace transform method and Stehfest numerical inversion method. The model was utilized to examine the velocity of pressure propagation and drop amplitude, revealing that the near-well area experienced faster propagation and drop than the far-well area. During dimensional analysis, it was observed that neglecting the effects of formation pressure change could lead to a substantial increase in the dimensional error of bottom hole pressure, with a maximum error of 9.45% recorded in this study. Additionally, a sensitivity analysis was conducted on perforation length, wellbore reservoir coefficient, skin coefficient, and reservoir radius to further elucidate the seepage law of vertical wells. This study provides theoretical guidance for oil and gas production. The original contribution of this research lies in the incorporation of formation pressure changes into the three-dimensional seepage model of vertical wells for the first time, which significantly enhances the model’s accuracy and practicality.