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Please use this identifier to cite or link to this item: http://elar.nung.edu.ua/handle/123456789/3507
Title: Interaction of silicate rocks with acid-cut clay muds under pt conditions in the reservoir. Part 2. The mechanism of formation component dissolution
Authors: Rudyi, S. M.
Kachmar, Yu. D.
Rudyi, M. I.
Issue Date: 2013
Publisher: Нафтогаз України
Citation: Рудий, С. М. Взаємодія силікатних порід із глинокислотними розчинами в термобаричних умовах пласта. Ч. ІІ. механізм розчинення компонентів породи / С. М. Рудий, Ю. Д. Качмар, М. І. Рудий // Нафтогазова галузь України. - 2013. - № 4. - С. 19-24.
Abstract: It was established that in case of excess rock to acid-cut clay mud at increase of interaction pressure the selectiveness of dissolution of oxides within Bentonite Clay disappears. In case of excess rock the mechanism of dissolution of these oxides at high pressures is unchanged. Increasing pressure from 0.1 to 15 MPa leads to decreasing Horodyshche gel powder dissolution at higher specific consumption of acid for its dissolution, which is associated with the occurrence of secondary reactions of newly produced neutralizing products.
URI: http://elar.nung.edu.ua/handle/123456789/3507
ISSN: 0548-1414
Appears in Collections:Oil & gas industry of Ukraine - 2013. - , № 4

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