Wei Zhao

Dr. Wei Zhao

School of Emergency Management and Safety Engineering, China University of Mining & Technology, Beijing, China

Research Focus & Metrics

Academic Career Length

11Years (2016-Present)

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

Representative Publications

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23 September 2023 in International Journal of Heat and Mass Transfer
Verified
Journal Article
Closed access
Wei ZhaoWei Zhao
Wei Zhao
HDHuzi Dong
Huzi Dong
KWKai Wang
Kai Wang
SLShimin Liu
Shimin Liu
ZYZhida Yan
Zhida Yan



19 July 2021 in International Journal of Coal Science & Technology
Verified
Journal Article
Open access
PDF file
JLJianshe Linghu
Jianshe Linghu
Wei ZhaoWei Zhao
Wei Zhao
JZJianbin Zhou
Jianbin Zhou
ZYZhiming Yan
Zhiming Yan
KWKai Wang
Kai Wang
CSChuanwen Sun
Chuanwen Sun
The thermal effect caused by deep magma intrusion can not only accelerate the metamorphism of coal body, but also bring additional thermal field that changes the mechanical environment of coal seams, thereby affecting the permeability of coal seams. Different from shallow coal resources, deep coal resources are in a mechanical environment characterized by limited stress and strain. Thus, the thermal effect has a more significant influence on the distribution and permeability characteristics of deep coal seams. In this study, the evolution history of highly metamorphic coal seams in Yangquan mining area was analyzed, and the main effect of magmatic activity on coal seams was obtained. Based on the determined vitrinite reflectance data of typical mines in Yangquan mining area, the maximum paleotemperature was calculated by adopting the Barker’s method. Furthermore, the paleotemperature distribution in Yangquan mining area was summarized, and its relationship with the metamorphic degree was acquired. Then, a new permeability model considering the thermal strain was proposed to analyze the permeability evolution in deep coal seams at different ground temperatures. Finally, through a combination of the results of gas pressure and outburst number in Sijiazhuang Mine, Yangquan No. 5 Mine and Xinjing Mine, the influence of ground temperature on the gas outburst risk in Yangquan mining area was explored. The following conclusions were drawn: The maximum paleotemperature in Yangquan area can be 303 °C. In addition, the paleotemperature in the south is higher than that in the north of Yangquan mining area. The various temperatures at different depths bring about different degrees of thermal stress to different coal seams, leading to different strains. Under the fixed displacement boundary conditions in the deep, the coal seam folds and bends to varying degrees. Moreover, the difference in the ground temperature raises the a value of coal seams and lowers the permeability, which promotes the formation of gas-rich zones and increases the risk of coal seam outburst. The research results can help mines to make proper gas disaster prevention plan for different zones.

16 January 2022 in Geomechanics and Geophysics for Geo-Energy and Geo-Resources
Verified
Journal Article
Closed access
PDF file
WWWei Wang
Wei Wang
Gang WangGang Wang
Gang Wang
Wei ZhaoWei Zhao
Wei Zhao
LWLiang Wang
Liang Wang
ZFZhongkai Feng
Zhongkai Feng
FDFeng Du
Feng Du

10 January 2023 in Energy
Verified
Journal Article
Closed access
KWKai Wang
Kai Wang
HDHuzi Dong
Huzi Dong
LWLong Wang
Long Wang
Wei ZhaoWei Zhao
Wei Zhao
YWYanhai Wang
Yanhai Wang
XZXiaolei Zhang
Xiaolei Zhang