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PECULIARITIES OF HYDROCARBONS AND WATER BEHAVIOR AT TIGHT GAS RESERVOIRS

机译:紧汽藏储层碳氢化合物和水行为的特性

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The traditional development methods of tight reservoirs of so-called Achimovskoe formations (Urengoy oil-gas-condensate field) will cause of great losses of hydrocarbons. The main sources of the troubles that will be come up at the development of those reservoirs are the structure peculiarities of reservoir rocks and the composition peculiarities of hydrocarbon fluids. Our investigations showed that phase behavior of hydrocarbons and water trapped in a porous medium was transformed quantitatively and qualitatively. The larger a specific surface the stronger an effect. The low permeability (less than 10~(-15) m~2) and high porosity (16-18%) of Achimovskoe formations consisted of tight sands, clays and limestone indicate about a very large specific surface of these reservoirs. A spacious surface predetermines the phase behavior and the filtration nature of hydrocarbons and water. A hydrocarbon fluid of these formations contains a lot of condensate (250-500 g/m~3) and paraffins (greater than 5%). Molecules of these substances just as molecules of liquid crystals in a porous medium form the homeotropic oriented quasi-liquid-crystals structures. Molecular orientation of these structures in relation to a porous medium wall predetermines the filtration behavior of a hydrocarbon fluid in all. We believe that in case of selection of the tight reservoirs development methods it is necessary to take into consideration the peculiar phase behavior and therefore the filtration behavior of hydrocarbons and water saturating these tight reservoirs.
机译:所谓的Achimovskoe地层(Urengoy油气冷凝水)的紧身储层的传统发展方法将导致碳氢化合物的损失很大。在那些水库开发的麻烦的主要来源是水库岩石的结构特性和烃流体的组成特性。我们的研究表明,定量和定性地转化在多孔介质中捕获的烃和水的相行为。比表面越大,效果越强。低渗透率(小于10〜(-15)m〜2)和高孔隙率(16-18%)Achimovskoe地层由紧密的砂,粘土和石灰岩组成,表示这些储层的非常大的表面。宽敞的表面预先确定碳氢化合物和水的相行为和过滤性质。这些地层的烃流体含有大量冷凝物(250-500g / m〜3)和链烷烃(大于5%)。这些物质的分子作为多孔介质中的液晶分子形成垂直导向的准液晶结构。这些结构与多孔介质壁的分子取向预先确定了烃流体的过滤行为。我们认为,如果选择紧密水库的发展方法,有必要考虑特殊的阶段行为,从而考虑碳氢化合物的过滤行为和饱和这些紧的储层。

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