Please use this identifier to cite or link to this item: http://earchive.tpu.ru/handle/11683/35167
Title: Changes in composition and pore space of sand rocks in the oil water contact zone (section YU[1] {3-4}, Klyuchevskaya area, Tomsk region)
Authors: Nedolivko, Nataliya Mikhailovna
Perevertaylo (Perevertailo), Tatyana Gennadievna
Pavlovec, T.
Keywords: поровое пространство; песчаные породы; водонефтяные зоны; Томская область; низкоомные коллекторы; породы-коллекторы; водонефтяные контакты
Issue Date: 2016
Publisher: IOP Publishing
Citation: Nedolivko N. M. Changes in composition and pore space of sand rocks in the oil water contact zone (section YU[1] {3-4}, Klyuchevskaya area, Tomsk region) / N. M. Nedolivko, T. G. Perevertaylo (Perevertailo), T. Pavlovec // IOP Conference Series: Earth and Environmental Science. — 2016. — Vol. 43 : Problems of Geology and Subsurface Development : XX International Scientific Symposium of Students, Postgraduates and Young Scientists, 4–8 April 2016, Tomsk, Russia. — [012058, 6 p.].
Abstract: The article provides an analysis of specific features in changes of rocks in the oil water contact zone. The object of study is the formation YU[1] {3-4} (J[3]o[1]) of Klyuchevskaya oil deposit (West Siberian oil-gas province, Tomsk region). The research data allow the authors to determine vertical zoning of the surface structure and identify the following zones: oil saturation (weak alteration), bitumen-content dissolution, non-bitumen-content dissolution, cementation, including rocks not affected by hydrocarbon deposit. The rocks under investigation are characterized by different changes in composition, pore space, as well as reservoir filtration and volumetric parameters. Detection of irregularity in distribution of void- pore space in oil-water contact zones is of great practical importance. It helps to avoid the errors in differential pressure drawdown and explain the origin of low-resistivity collectors.
URI: http://earchive.tpu.ru/handle/11683/35167
Appears in Collections:Материалы конференций

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