Ying Mu

Dr. Ying Mu

orcid

Research Focus & Metrics

Academic Career Length

6Years (2021-Present)

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

Representative Publications

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1 June 2021 in Marine and Petroleum Geology
Verified
Journal Article
Closed access
YLYanran Li
Yanran Li
ZHZhiming Hu
Zhiming Hu
CCChanghong Cai
Changhong Cai
XLXiangui Liu
Xiangui Liu
XDXianggang Duan
Xianggang Duan
JGJingshu Guo
Jingshu Guo

17 May 2024 in International Journal of Hydrogen Energy
Verified
Journal Article
Closed access
YMYing Mu
Ying Mu
CZCaineng Zou
Caineng Zou
ZHZhiming Hu
Zhiming Hu
SPSongqi Pan
Songqi Pan
XDXianggang Duan
Xianggang Duan
YTYongbing Tang
Yongbing Tang

31 December 2021 in Energy & Fuels
Verified
Journal Article
Closed access
YMYing Mu
Ying Mu
ZHZhiming Hu
Zhiming Hu
RSRui Shen
Rui Shen
JCJin Chang
Jin Chang
XDXianggang Duan
Xianggang Duan
Qiulei GuoQiulei Guo
Qiulei Guo

6 July 2025 in Advances in Geo-Energy Research
Verified
Journal Article
Open access
PDF file
YMYing Mu
Ying Mu
CZCaineng Zou
Caineng Zou
ZHZhiming Hu
Zhiming Hu
XDXianggang Duan
Xianggang Duan
QGQiulei Guo
Qiulei Guo
ZJZhenhua Jing
Zhenhua Jing
Water-rock interaction triggered by drilling and fracturing fluid retention in shale gas reservoirs induces secondary processes and the subsequent alteration of rock physical properties, critically modulating reservoir productivity. In this study, X-ray diffraction, nanoindentation, focused ion beam-scanning electron microscopy, and micro-computed tomography were utilized to characterize and analyze the mineral alteration, mechanical weakening and pore-fracture evolution of marine shale in the Longmaxi Formation, Sichuan Basin. The results reveal that the water-rock interaction preferentially dissolves clay minerals (mainly illite), feldspars and pyrite via hydration and redox reactions while promoting quartz and carbonate mineral recrystallization. The hydration-dissolution precipitation process significantly weakens the rock mass by reducing cohesion and the friction angle. This mechanical degradation is evidenced by a substantial decrease in elastic modulus, exhibiting pronounced anisotropy relative to stratifications. The resultant hetero-geneous stress fields initiate and propagate secondary pores and fractures, dramatically increasing the number, volume and surface area of pores. These newly formed structures integrate with pre-existing pore-fracture networks, markedly elevating overall porosity and enhancing interconnectivity, which consequently amplifies permeability by orders of magnitude. Additionally, water preferentially enters the reservoir through stratification, and the associated difference in water-rock interaction strength further enhances the heterogeneity of structural and mechanical heterogeneity. These findings link micro-scale physical-chemical reactions with the meso-scale mechanical properties and macro-scale pore-fracture structures, emphasize the key role of water-rock interaction in reshaping reservoir characteristics, and provide important insights for optimizing hydraulic fracturing strategies and improving shale gas recovery. Document Type: Original article Cited as: Mu, Y., Zou, C., Hu, Z., Duan, X., Guo, Q., Jing, Z. Impacts of multi-scale water-rock interaction on mineral alteration, mechanical weakening and pore-fracture evolution in marine shales. Advances in Geo-Energy Research, 2025, 17(1): 68-81. https://doi.org/10.46690/ager.2025.07.06

17 March 2023 in Energy & Fuels
Verified
Journal Article
Closed access
YMYing Mu
Ying Mu
ZHZhiming Hu
Zhiming Hu
Qiulei GuoQiulei Guo
Qiulei Guo
XDXianggang Duan
Xianggang Duan
JCJin Chang
Jin Chang
ZWZhenkai Wu
Zhenkai Wu

2 February 2024 in Energy & Fuels
Verified
Journal Article
Closed access
YMYing Mu
Ying Mu
ZHZhiming Hu
Zhiming Hu
Qiulei GuoQiulei Guo
Qiulei Guo
XDXianggang Duan
Xianggang Duan
JCJin Chang
Jin Chang