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Sensitivity of the pressure decline curve during the hydraulic fracturing to poroelastic effects Научная публикация

Журнал Сибирские электронные математические известия / Siberian Electronic Mathematical Reports
ISSN: 1813-3304
Вых. Данные Год: 2018, Том: 15, Страницы: 1735-1742 Страниц : 8 DOI: 10.33048/semi.2018.15.143
Ключевые слова HYDRAULIC FRACTURE, MATHEMATICAL MODELING, PRESSURE DECLINE CURVE, POROELASTIC EFFECTS, ГИДРОРАЗРЫВ ПЛАСТА, МАТЕМАТИЧЕСКОЕ МОДЕЛИРОВАНИЕ, КРИВАЯ ПАДЕНИЯ ДАВЛЕНИЯ, ПОРОУПРУГИЙ ЭФФЕКТ
Авторы Lgotina E.V. 1,2 , Baykin A.N. 1,2 , Golovin S.V. 1,2 , Krivtsov A.M. 3
Организации
1 Lavrenyev Institute of Hydrodynamics
2 Novosibirsk State University
3 Peter the Great St.Petersburg Polytechnic University

Реферат: Computer simulators of hydraulic fracturing rely on known physical properties of the reservoir, in particular, the leak-off coefficient and the confining in situ stress. This information can be obtained from the solution of the inverse problem by analyzing of the pressure decline curve (PDC) in pump-in/shut-in tests. The goal of the present work is to demonstrate that poroelastic effect can have significant influence on the behavior of the PDC and, hence, to results of its analysis. For computer simulations we use the mathematical model of the hydraulic fracture in poroelastic medium developed in [6]. We investigate the dependence of the PDC on the closure stress and of the rock permeability. It is shown that classical methods for interpretation of PDC can lead to a significant error, in particular, in estimation of the minimal in situ confining stress.
Библиографическая ссылка: Lgotina E.V. , Baykin A.N. , Golovin S.V. , Krivtsov A.M.
Sensitivity of the pressure decline curve during the hydraulic fracturing to poroelastic effects
Сибирские электронные математические известия / Siberian Electronic Mathematical Reports. 2018. V.15. P.1735-1742. DOI: 10.33048/semi.2018.15.143 WOS Scopus РИНЦ OpenAlex
Даты:
Поступила в редакцию: 28 окт. 2018 г.
Опубликована в печати: 26 дек. 2018 г.
Идентификаторы БД:
Web of science: WOS:000454860200083
Scopus: 2-s2.0-85064390214
РИНЦ: 36998752
OpenAlex: W3016029171
Цитирование в БД:
БД Цитирований
РИНЦ 1
Scopus 1
Web of science 1
OpenAlex 1
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