Issue |
E3S Web Conf.
Volume 218, 2020
2020 International Symposium on Energy, Environmental Science and Engineering (ISEESE 2020)
|
|
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Article Number | 02035 | |
Number of page(s) | 5 | |
Section | New Energy Development and Energy Sustainable Development Optimization | |
DOI | https://doi.org/10.1051/e3sconf/202021802035 | |
Published online | 11 December 2020 |
Analysis of the difference between the test and production in Well Z202-H1
1
Chongqing Shale Gas Exploration and Development Co., Ltd., Chongqing, China
2
State Key Lab Of Oil And Gas Reservoir Geology And Exploitation (Southwest Petroleum University), Chengdu, P.R. China
3
Geology Exploration and Development Research Institute, CNPC Chuanqing Drilling Engineering Co., Ltd., Chengdu, Sichuan 610051, China
4
Sichuan Changning Natural Gas Development Co., Ltd., Chengdu, Sichuan 610056, China
5
Sichuan Shale Gas Exploration and Development Co., Ltd., Chengdu, 610051, China
6
Key Laboratory of Seepage and Rock Mechanics of Oil and Gas Wells in Shanxi Province, Xian 710000, China
a* Corresponding author: 1298047301@qq.com
In recent years, shale gas in the Upper Ordovician Wufeng Formation and lower Silurian Longmaxi Formation is gradually developing into deep strata in Sichuan Basin. Well 202-H1 is a evaluation well deployed to evaluate the productivity of horizontal Wells in longmaxi Formation and Wufeng Formation in The West Chongqing block. The well type is horizontal well. The main reasons for the poor production effect of Well Z202-H1 are as follows: Reservoir pores are not developed; continuous thickness of thin reservoir; insufficient fracturing treatment; low flowback rate, large water production and wellbore fluid accumulation. This article not only obtained the reasons for the difference between the test and production of well Z202-H1, but also provided a new research idea for the test and production tracking analysis of deep shale gas static in The Western Chongqing block.
© The Authors, published by EDP Sciences, 2020
This is an Open Access article distributed under the terms of the Creative Commons Attribution License 4.0, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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