首页> 外文会议>Workshop on Geothermal Reservoir Engineering >GEOTHERMAL BRINE INVASION IN OIL RESERVOIRS: A 3D GENERALIZATION OF THE BUCKLEY-LEVERETT MODEL USING NON-LINEAR FINITE ELEMENTS
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GEOTHERMAL BRINE INVASION IN OIL RESERVOIRS: A 3D GENERALIZATION OF THE BUCKLEY-LEVERETT MODEL USING NON-LINEAR FINITE ELEMENTS

机译:油藏地热盐水入侵:使用非线性有限元的斗出leverett模型的3D概括

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In the southern coast of the Gulf of Mexico some deep geothermal aquifers are associated to hydrocarbon reservoirs. Some of their wells are invaded by geothermal brine, producing a variable mixture of hot water and oil. This water, at temperatures of 150 deg C and having a density of 1150 kg/m~(3); flows vertically through a fault from the aquifer located 6000 m depth. The non isothermal conditions affect the effective saturations and the relative permeabilities of the immiscible phases. The relative permeability of oil is increased by the increase of temperature produced by the geothermal water. This effect reduces the residual saturation of heavy oils. At the same time the dynamic viscosities of water and oil are diminished, affecting the displacement of both fluids. Although the oil is extracted in wells finished upper the aquifer, the total volume of produced water, in some cases, equals or exceeds the oil production. The handling of this extra hot water becomes a practical serious problem. We introduce a numerical original model able to predict the critical oil rate for which the wells can be totally invaded by geothermal brine. For the construction of the model we apply classic laws and equations. We use standard published formulas for both relative permeabilities and capillary pressure. We obtain a single non - linear partial differential equation (PDE) which depends only on water saturation, space and time. This PDE is a 3D generalization of the classical 1D Buckley-Leverett model. To solve the new PDE we use non linear finite elements. The numeric simulation could reproduce the effect of water invasion: After some time elapsed, the original oil volume diminishes abruptly, displacing the boundary of the water-oil contact and the transition zone in the vertical direction. Our objective is to estimate the optimum mass rate for producing wells in order to minimize the production of water or to achieve a mixture oil-water extraction where oil always prevails.
机译:在墨西哥湾的南部海岸,一些深海地热含水层与碳氢化合物储层有关。他们的一些井被地质盐水侵入,产生了热水和油的可变混合物。这种水,在150℃的温度下,密度为1150 kg / m〜(3);通过位于6000米深度的含水层的故障垂直流动。非等温条件影响有效的饱和饱和和不加混阶段的相对渗透率。通过地热水产生的温度的增加,油的相对渗透率增加。这种效果降低了重油的残余饱和度。同时,水和油的动态粘度降低,影响了两种流体的位移。虽然油在井中提取完成的含水层,但在某些情况下,生产的水总量,等于或超过石油生产。这种额外的热水的处理成为一个实际的严重问题。我们介绍了一个能够预测地热盐水完全侵入井的临界石油速率的数值原始模型。为了建造模型,我们应用经典的法律和方程。我们使用标准发布的公式来进行相对渗透率和毛细血管压力。我们获得单个非线性偏微分方程(PDE),其仅取决于水饱和度,空间和时间。该PDE是古典1D Buckley-Leverett模型的3D概括。要解决新的PDE,我们使用非线性有限元。数值模拟可以再现水侵袭的影响:经过一段时间后,原油体积突然减少,沿垂直方向沿着水 - 油触点和过渡区移位的边界。我们的目的是估计生产井的最佳质量率,以最大限度地减少水的生产或实现油 - 水的混合物始终占上风。

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