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New characterization on the petrophysical characteristics of tight sandstone reservoirs in Yanchang Formation Ordos Basin China

机译:鄂尔多斯盆地延长组致密砂岩储层岩石物性新特征

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New characterization on petrophysical characteristics of tight sandstone reservoirs is of an important value to exploration and exploitation of oil and gas. In this paper, low-field nuclear magnetic resonance, combined with casting thin sections, laser scanning confocal microscopy, scanning electron microscopy and pressure-controlled porosimetry were applied to investigate the pore structure characteristics of nine tight sandstone samples of Yanchang Formation in the Upper Triassic Ordos Basin China. And then, based on the nuclear magnetic resonance T-2 spectrum distribution and previous theoretical models, a new model is proposed to predict permeability of tight sandstone reservoirs. Petrophysical characteristics are qualitatively-quantificationally analyzed by a combination of various experiments, which is considered to be a new method that will be widely used in future research. Results indicate that nuclear magnetic resonance T-2 spectrum distribution has a close relationship with characteristics of pore types and pore radius distribution. Three T-2 spectrum peaks are identified by the relaxation time at 0.1-10ms, 10-100ms and >100ms correspond to micropores (<0.2 mu m), mesopores (0.2-4.9 mu m) and macropores and fractures (>4.9 mu m), respectively, which is well consistent with results from casting thin sections, laser scanning confocal microscopy, scanning electron microscopy and pressure-controlled porosimetry. Compared with the existing several classical models, the new permeability model can better estimate the permeability of tight sandstone samples. The new characterization method and new model can accurately evaluate petrophysical characteristics of typical tight sandstone samples, which have a great value for nuclear magnetic well logging in the exploration and exploitation of tight sandstone reservoirs in the Ordos basin.
机译:致密砂岩储层岩石物性的新表征对油气勘探开发具有重要价值。本文采用低场核磁共振,结合铸件薄片,激光扫描共聚焦显微镜,扫描电子显微镜和压力控制孔隙率法,研究了上三叠统延长组9个致密砂岩样品的孔隙结构特征。鄂尔多斯盆地中国。然后,基于核磁共振T-2谱分布和先前的理论模型,提出了一种预测致密砂岩储层渗透率的新模型。通过结合各种实验对岩石物理特征进行定性定量分析,这被认为是一种将在未来研究中广泛使用的新方法。结果表明,核磁共振T-2谱分布与孔类型和孔半径分布特征密切相关。通过弛豫时间在0.1-10ms,10-100ms和> 100ms识别出三个T-2谱峰,分别​​对应于微孔(<0.2μm),中孔(0.2-4.9μm)和大孔和裂缝(> 4.9μm) ),分别与薄壁铸造,激光扫描共聚焦显微镜,扫描电子显微镜和压力控制孔隙率法的结果一致。与现有的几种经典模型相比,新的渗透率模型可以更好地估算致密砂岩样品的渗透率。新的表征方法和模型可以准确地评价典型致密砂岩样品的岩石物性,对于核磁测井在鄂尔多斯盆地致密砂岩油藏的勘探和开发中具有重要的价值。

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