Please use this identifier to cite or link to this item: https://dspace.ncfu.ru/handle/20.500.12258/15903
Title: Technology of testing shale reservoirs of Paleogene age on the territory of the Eastern Ciscaucasia
Authors: Saltanova, A. G.
Салтанова, А. Г.
Vasilyev, V. A.
Васильев, В. А.
Kerimova, E. G.
Керимова, Е. Г.
Kramarenko, V. S.
Крамаренко, В. С.
Keywords: Depression;Shale reservoirs;Test;Packer
Issue Date: 2021
Publisher: IOP Publishing Ltd
Citation: Saltanova A.G., Vasiliev V.A., Kerimova E.G., Kramarenko V.S., Sova V.E. Technology of testing shale reservoirs of Paleogene age on the territory of the Eastern Ciscaucasia // IOP Conference Series: Earth and Environmental Science. 2021. - Том 745. - Выпуск 119. - Номер статьи 012025
Series/Report no.: IOP Conference Series: Earth and Environmental Science
Abstract: The article demonstrates the technology of testing reservoir layers represented by fractured clay-carbonate rocks in the Eastern Ciscaucasia. Practice shows that if the saturation of permeable rocks is uniform, the reliability of the tests can be ensured if the tested interval does not exceed 25 m. The probability of obtaining an inflow during tests significantly decreases with the increase in the amount of repression of the washing liquid and the duration of its impact on the reservoir. This is caused by clogging of the near-well zone of the reservoir, which results in the hydrodynamic connection of the reservoir with the well deteriorates. Test results are the most reliable if they are performed no later than 3-5 days after opening the reservoir, however, even in this case, the reservoir may be contaminated. For high-quality testing of reservoir layers represented by fractured clay-carbonate rocks, the following processes are required: to make an individual selection of the depression on the formation, to have a priori accurate information about the strength characteristics of the well walls
URI: http://hdl.handle.net/20.500.12258/15903
Appears in Collections:Статьи, проиндексированные в SCOPUS, WOS

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