Qianyou Wang

Dr. Qianyou Wang

University of Liverpool, Liverpool, UK
orcid

Research Focus & Metrics

Academic Career Length

9Years (2018-Present)

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

Representative Publications

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1 December 2018 in Marine and Petroleum Geology
Verified
Journal Article
Closed access
WYWei Yang
Wei Yang
RZRusi Zuo
Rusi Zuo
ZJZhenxue Jiang
Zhenxue Jiang
Dongxia ChenDongxia Chen
Dongxia Chen
YSYan Song
Yan Song
HZHongji Zhu
Hongji Zhu

1 August 2020 in Marine and Petroleum Geology
Verified
Journal Article
Closed access
WYWei Yang
Wei Yang
Qianyou WangQianyou Wang
Qianyou Wang
YWYaohua Wang
Yaohua Wang
ZJZhenxue Jiang
Zhenxue Jiang
YSYan Song
Yan Song
FZFan Zhang
Fan Zhang

Verified
Journal Article
Open access
PDF file
ZHZiqing Hong
Ziqing Hong
MMMianmo Meng
Mianmo Meng
KDKong Deng
Kong Deng
JBJingwen Bao
Jingwen Bao
Qianyou WangQianyou Wang
Qianyou Wang
XLXingchen Liu
Xingchen Liu
Pore connectivity and ultimate imbibed porosity are two important parameters used to assess the shale oil reservoir property, the proper appraising of which could facilitate the efficient flow of oil from the matrix and an improvement in recovery efficiency. In previous studies, the uncertainty in sample dimensions and the extra-long stable time during imbibition experiments exploring pore connectivity and ultimate imbibed porosity showed a lack of discussion, which influenced the accuracy and efficiency of the SI experiments. In this study, SI experiments with shale samples of different thicknesses are carried out to acquire the two parameters in a short period of time. As a result, the pore connectivity of sample D86-5 from the Qingshankou Formation (Fm) in the Songliao Basin fluctuates with the increase in thicknesses, with an average of 0.265. The water penetrates sample D86-5 of all thicknesses, so the ultimate imbibed porosity fluctuates around 3.7%, and the stable time increases with thicknesses. The pore connectivity of sample Y172 from the Shahejie Fm in the Bohaiwan Basin fluctuates around an average of 0.026, which is much smaller than that of D86-5. The ultimate imbibed porosity of Y172 decreases with thicknesses because the penetration depth is so small that the pores cannot be fully accessed, and the stable time increases before becoming stable with fluctuations. The method is examined using the samples from the Liushagang Fm in the Beibuwan Basin measuring around 400 μm: the ultimate imbibed porosity of BW1-1 and BW1-3 is 5.8% and 18.1%, respectively, the pore connectivity of BW1-1, BW1-2, and BW1-3 is 0.086, 0.117, and 0.142, respectively, and the results can be obtained within a day. In comparison, the average pore connectivity of the 400 μm samples from Qingshankou, Shahejie, and Liushagang Fms is 0.324, 0.033, and 0.097, respectively, and the average ultimate imbibed porosity of these Fms is 3.7%, 3.1%, and 12.0%, respectively. Based on the above results, a quick method for measuring the two parameters with thin samples by spontaneous imbibition is established, providing a fast solution for the evaluation of the sweet spot.

1 July 2019 in International Journal of Coal Geology
Verified
Journal Article
Closed access
WYWei Yang
Wei Yang
RZRusi Zuo
Rusi Zuo
DCDongxia Chen
Dongxia Chen
ZJZhenxue Jiang
Zhenxue Jiang
LGLishuang Guo
Lishuang Guo
CZChen Zhang
Chen Zhang

1 April 2019 in Ore Geology Reviews
Verified
Journal Article
Closed access
LYLiang Yue
Liang Yue
YJYangquan Jiao
Yangquan Jiao
LWLiqun Wu
Liqun Wu
HRHui Rong
Hui Rong
HXHuili Xie
Huili Xie
QYQianqian Yan
Qianqian Yan

12 April 2022 in Journal of Natural Gas Science and Engineering
Verified
Journal Article
Closed access
WYWei Yang
Wei Yang
YWYaohua Wang
Yaohua Wang
WDWei Du
Wei Du
YSYan Song
Yan Song
ZJZhenxue Jiang
Zhenxue Jiang
SXShuling Xiong
Shuling Xiong