Characteristics of gas accumulation in a less efficient tight-gas reservoir, He 8 interval, Sulige gas field, Ordos Basin, China

被引:17
作者
Ding Xiaoqi [1 ]
Yang Peng [2 ,3 ]
Han Meimei [3 ]
Chen Yang [3 ,4 ]
Zhang Siyang [5 ]
Zhang Shaonan [2 ]
Liu Xuan [1 ]
Gong Yiming [1 ]
Nechval, A. M. [4 ]
机构
[1] Chengdu Univ Technol, State Key Lab Oil & Gas Reservoir Geol & Exploita, Chengdu 610059, Sichuan, Peoples R China
[2] Sinopec, Northwest Petr Bur, Xinjiang 830011, Peoples R China
[3] Southwest Petr Univ, State Key Lab Oil & Gas Reservoir Geol & Exploita, Chengdu 610500, Sichuan, Peoples R China
[4] Ufa State Petr Technol Univ, Teaching & Res Off Oil & Gas Engn, Ufa 450062, Russia
[5] Univ Regina, Dept Geol, Regina, SK S4S 3X3, Canada
基金
美国国家科学基金会;
关键词
tight gas; gas-water distribution; reservoir; heterogeneity; He; 8; interval; Sulige gas field; Ordos Basin; PORE-THROAT SIZES; RESOURCE-ASSESSMENT; SYSTEMS; MODEL; SANDSTONES; SHALES;
D O I
10.1016/j.rgg.2016.06.006
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Because of the lack of gas supply from source rocks and gas loss, inefficient tight-gas fields represent a high share of all gas reservoirs in China. These gas fields are characterized by low abundance and large gas reserves. Here, the He 8 tight-gas reservoirs in the western region of the Sulige gas field are used as an example to characterize gas distribution under conditions of less efficient charging. Results show the following characteristics. First, the sandstone densification process has a relatively large impact on the charging of gas. Litharenite was already subjected to densification at the time of large-scale gas charging, and this was not conducive to gas charging. On the contrary, for sublitharenite, although strong compaction has already occurred during gas generation, quartz overgrowth that leads to further densification of the gas reservoirs occurs simultaneously with large-scale gas charging. This facilitates gas charging and is characterized by concomitant densification and reservoir formation. Second, structure traps can control the accumulation of gas to a certain extent. In particular, when physical properties of sandstones within the structure traps are appropriate, gas saturation during gas charging can be increased by approximately 7%. Third, less efficient charging is the main cause of the complex gas and water distribution in the He 8 gas reservoirs. The strong heterogeneity of the reservoirs and the decline in the gas reservoir pressure caused by tectonic uplift in the Yanshan period further exacerbate the complexity of gas and water distribution. These factors ultimately caused the He 8 gas reservoirs to become a multireservoir gas field with several gas-water interfaces. The He 8 gas reservoirs are neither conventional gas nor continuous gas reservoirs. Rather, they are quasi-continuous gas reservoirs, and the accumulation of gas is controlled by both the top surface of sandstone and the physical properties of the reservoirs. Traps and high-quality reservoirs within the regional traps are beneficial for the gas accumulation. (C) 2016, V.S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:1064 / 1077
页数:14
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