Циклические нагрузки и фильтрационные свойства пористых горных пород: экспериментальные исследования

Кожевников, Е.В.; Гладких, Е.А.; Гузев, М.А.; Ци, Чэнчжи; Пантелеева, А.Е.; Иванов, З.Г.; Щербаков, А.А.

doi:10.15593/2712-8008/2025.1.4

Циклические нагрузки и фильтрационные свойства пористых горных пород: экспериментальные исследования

Е.В. Кожевников, Е.А. Гладких, М.А. Гузев, Чэнчжи Ци, А.Е. Пантелеева, З.Г. Иванов, А.А. Щербаков

Сведения об авторах

Е.В. Кожевников
Пермский национальный исследовательский политехнический университет, Пермь, Российская Федерация
Е.А. Гладких
Пермский национальный исследовательский политехнический университет, Пермь, Российская Федерация
М.А. Гузев
Пермский национальный исследовательский политехнический университет, Пермь, Российская Федерация
Чэнчжи Ци
Пекинский университет гражданского строительства и архитектуры, Пекин, Китай
А.Е. Пантелеева
Пермский национальный исследовательский политехнический университет, Пермь, Российская Федерация
З.Г. Иванов
Пермский национальный исследовательский политехнический университет, Пермь, Российская Федерация
А.А. Щербаков
Пермский национальный исследовательский политехнический университет, Пермь, Российская Федерация

https://doi.org/10.15593/2712-8008/2025.1.4

Изучение фильтрационных свойств пористых пород при циклическом нагружении важно для прогнозирования использования подземных резервуаров для хранения природного газа или водорода, в которых поровое давление колеблется в процессе сезонной добычи или заполнения. При циклическом нагружении проницаемость пород необратимо уменьшается, однако, несмотря на значительный объем исследований, существует пробел в понимании истинных причин этого снижения. В работе представлены результаты экспериментальных исследований влияния циклического нагружения на проницаемость пористых известняков и песчаников. Выявлен механизм гистерезиса проницаемости. Неполное восстановление проницаемости при разгрузке обусловлено наличием порога раскрытия микротрещин в породах. Также установлено влияние миграции коллоидов и мелкодисперсных частиц при измерении проницаемости образцов. Величина изменения проницаемости при циклическом всестороннем давлении обнаруживает сильную корреляцию с начальной проницаемостью. Результаты исследований показывают, что в пористых песчаниках и известняках с начальной проницаемостью ниже 50 мД ухудшение проницаемости в первую очередь связано с закрытием микротрещин. Влияние миграции коллоидов менее очевидно в менее проницаемых породах, вероятно, из-за сниженной подвижности коллоидов. Однако для пород с начальной проницаемостью более 50 мД как уплотнение, так и миграция коллоидов и мелких частиц способствуют снижению проницаемости. В более проницаемых породах подвижность коллоидов выше, что потенциально приводит к значительному снижению проницаемости до 60 %.

Ключевые слова

проницаемостьциклическое нагружениемиграция коллоидовмикротрещиныпористые породыфильтрационные свойствапесчаникиизвестнякиобразцы горных пород

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Опубликована: 24.02.2025
В выпуске: 24.02.2025
Выпуск: Том 25, № 1 (2025)

Циклические нагрузки и фильтрационные свойства пористых горных пород: экспериментальные исследования

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Cyclic Loading and Transport Properties of Porous Rocks: Experimental Studies

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Циклические нагрузки и фильтрационные свойства пористых горных пород: экспериментальные исследования

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Cyclic Loading and Transport Properties of Porous Rocks: Experimental Studies

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