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Lower limits of petrophysical parameters allowing tight oil accumulation in the Lucaogou Formation, Jimusaer Depression, Junggar Basin, Western China

机译:岩石物理参数下限,允许卢卡楼山区的油积累,Jimusaer Despress,Jumusaer Des,Junggar Basin,中国西部

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摘要

In this study, we investigate the petrophysical parameter values above which oil can accumulate, using a tight oil reservoir in the Jimusaer Depression, Junggar Basin, as an example. Statistical analysis of well-drilling data and effective porosity measurements is integrated with numerical simulations of force balance to illuminate the mechanisms that place a lower limit on the petrophysical parameters of tight hydrocarbon reservoirs. Further, we discuss the factors that influence these limits. The results show that when porosity is observed to be less than 5%, corresponding to a pore-throat radius of more than 0.2 mu m, exploratory wells reach reservoirs comprising only water layers. The lower limit for oil accumulation is reached when irreducible water saturation reaches 100% and porosity is approximately 5%. This fits well with the values arrived at by modeling the force balance. In the reservoirs under consideration, oil charging is driven by excess pressure resulting from hydrocarbon generation and is resisted by capillary force. When the pore-throat radius is larger than 0.2 mu m, the capillary force will be greater than the driving force, and tight reservoirs cannot be charged with oil. This corresponds to a porosity of approximately 5%, matching the results derived from observations. The values of these lower limits depend on many factors, such as source rock quality, depth, temperature, hydrocarbon-generation kinetics, and interfacial tension, and hence vary under different geological conditions. Thus, in lacustrine basins in China with type I kerogen-dominated source rocks, the lower limits are smaller than in those where other types dominate. Differences in the geothermal gradient mean that, at similar hydrocarbon-generation temperatures, the lower limits for reservoirs in Western China are smaller than for those in the east. There is also a smaller lower limitation porosity in tight gas reservoirs than in tight oil reservoirs due to the difference in interfacial tension.
机译:在这项研究中,我们研究了在Jimusaer Despression,Junggar盆地中的毛芦缸可以积聚的岩石物理参数值,Junggar盆地的蓄水器。钻孔良好的数据和有效孔隙率测量的统计分析与力平衡的数值模拟相结合,以照亮对紧碳氢化合物储层的岩石物理参数下限的机制。此外,我们讨论影响这些限制的因素。结果表明,当观察到孔隙率小于5%时,对应于大于0.2μm的孔径半径,探索性井到仅包含水层的储层。当不可缩续的水饱和度达到100%而孔隙率约为5%时,达到了油积聚的下限。这与通过建模力平衡来达到的值很好。在所考虑的储层中,油充电由烃产生产生的过量的压力驱动,并通过毛细力抵抗毛细管。当孔径半径大于0.2μm时,毛细力将大于驱动力,并且不能用油充电粘力。这对应于约5%的孔隙率,匹配从观察结果的结果匹配。这些较低限度的值取决于许多因素,例如源岩质量,深度,温度,碳氢化合物动力学和界面张力,因此在不同的地质条件下变化。因此,在中国的Lapustine盆地,具有I型Kerogen-占主导地位的源岩,下限比其他类型占主导地位的底部。地热梯度的差异意味着,在类似的碳氢化合物 - 产生温度下,中国西部储层的较低限度小于东方的水库。由于界面张力差异,在狭窄的气体储层中也存在较小的储蓄孔隙率较小。

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