4.5 Article

Strain energy density distribution of a tight gas sandstone reservoir in a low-amplitude tectonic zone and its effect on gas well productivity: A 3D FEM study

Journal

JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING
Volume 170, Issue -, Pages 89-104

Publisher

ELSEVIER
DOI: 10.1016/j.petrol.2018.06.057

Keywords

Strain energy density; Tight gas sandstone; Paleotectonic stress field; Productivity

Funding

  1. National Science and Technology Major Project of China [2016ZX05050]
  2. Open Foundation of Shandong Provincial Laboratory of Depositional Mineralization AMP
  3. Sedimentary Mineral, Shandong University of Science and Technology [DMSM2017081]

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The tight gas sandstone reservoirs in the Paleozoic of the Sulige gas field in China are highly heterogeneous, and fractures are key factors for stable reservoir production. Low-amplitude folds or nose-like structures are widely developed in the Upper Paleozoic strata in this area. To effectively predict gas well productivity, in this paper, a 3D FEM numerical simulation based on the deformation and energy variation of the rock mass was used to predict the sweet spots of gas well productivity in a tight gas sandstone reservoir using the He8 segment of the Middle Permian Xiashihezi Formation in the Central Sulige block as an example. The paleotectonic stress field of the study area during the maximum episode of compression in the Yanshanian movement was restored, and the two rupture parameters of the integrated rupture rate (IF) and strain energy density (U) were constructed. The strain energy density distribution has a high correlation with gas well productivity, indicating that it can better predict the rock rupture degree in low-amplitude tectonic zones. A complex relationship exists between the strain energy density distribution and low-amplitude folds. The high strain energy density zones are mainly distributed among the high positions and wing areas of the low-amplitude fold zone, but the top area of the low-amplitude fold does not necessarily have a high strain energy density. Portions of the high strain energy density zones are located in the gentle tectonic zone, located near but outside the low-amplitude fold zone. The strain energy in these gentle tectonic zones with a high strain energy density value is relatively high, and the rock mass is prone to rupture. This study is of great value in enriching the prediction of sweet spots in tight gas sandstone reservoirs in low-amplitude tectonic zones worldwide.

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