Exploring in-situ combustion effects on reservoir properties of heavy oil carbonate reservoir

被引:1
|
作者
Mukhametdinova, Aliya [1 ]
Karamov, Tagir [1 ]
Markovic, Strahinja [1 ]
Morkovkin, Andrey [1 ]
Burukhin, Aleksander [1 ]
Popov, Evgeny [1 ]
Sun, Zi-Qi [2 ]
Zhao, Ren-Bao [2 ]
Cheremisin, Alexey [1 ]
机构
[1] Skolkovo Inst Sci & Technol Skoltech, Sikorskogo 11, Moscow 121205, Russia
[2] China Univ Petr, State Key Lab Petr Resources & Engn, Beijing 102249, Peoples R China
关键词
In-situ combustion; Thermal EOR; Carbonates; Porosity and pore size; MicroCT; NMR; SEM; CO; 2; storage; HIGH-TEMPERATURE; THERMAL-DECOMPOSITION; WETTABILITY; STORAGE;
D O I
10.1016/j.petsci.2024.04.014
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
Laboratory modeling of in-situ combustion is crucial for understanding the potential success of field trials in thermal enhanced oil recovery (EOR) and is a vital precursor to scaling the technology for field applications. The high combustion temperatures, reaching up to 480 degrees C, induce significant petrophysical alterations of the rock, an often overlooked aspect in thermal EOR projects. Quantifying these changes is essential for potentially repurposing thermally treated, depleted reservoirs for CO2 storage. In this study, we depart from conventional combustion experiments that use crushed core, opting instead to analyze the thermal effects on reservoir properties of carbonate rocks using consolidated samples. This technique maintains the intrinsic porosity and permeability, revealing combustion's impact on porosity and mineralogical alterations, with a comparative analysis of these properties pre- and postcombustion. We characterize porosity and pore geometry evolution using low-field nuclear magnetic resonance, X-ray micro-computed tomography, and low-temperature nitrogen adsorption. Mineral composition of the rock and grain-pore scale alterations are analyzed by scanning electron microscopy and X-ray diffraction. The analysis shows a significant increase in carbonate rocks' porosity, pore size and mineral alterations, and a transition from mixed-wet to a strongly water-wet state. Total porosity of rock samples increased in average for 15%e20%, and formation of new pores is registered at the scale of 1e30 mm size. High-temperature exposure results in the calcite and dolomite decomposition, calcite dissolution and formation of new mineralsdanhydrite and fluorite. Increased microporosity and the shift to strongly water-wet rock state improve the prospects for capillary and residual CO2 trapping with greater capacity. Consequently, these findings highlight the importance of laboratory in-situ combustion modeling on consolidated rock over tests that use crushed core, and indicate that depleted combustion stimulated reservoirs may prove to be viable candidates for CO2 storage. (c) 2024 The Authors. Publishing services by Elsevier B.V. on behalf of KeAi Communications Co. Ltd. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).
引用
收藏
页码:3363 / 3378
页数:16
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