特低渗透砂岩储层可动流体变化特征与差异性成因
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国家重点基础研究发展计划(973计划),长江学者和创新团队发展计划(编号IRT0559)资助


Movable fluid variation characteristics and diversity origin of ultra-low permeability sandstone reservoir
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    摘要:

    特低渗透砂岩储层微观孔隙结构复杂,流体赋存状态不同于常规储层,利用核磁共振技术对鄂尔多斯盆地延长组3个层位样品的可动流体变化特征与差异性成因进行了分析,结果表明,样品 谱分布形态不同、 截止值中等—偏高,可动流体参数变化幅度较大、各层位的可动流体参数存在差异;渗透率较小时,可动流体参数的变化幅度大,当渗透率增大到一定程度后,可动流体参数数据点收敛,变化幅度减小;储层物性、孔隙(尤其是次生孔隙)发育连通程度、微裂缝的发育程度、黏土矿物的存在形式及其对孔隙的充填程度等微观孔隙结构特征变化是可动流体参数差异性产生的主要原因。可动流体参数本身就是储层诸多微观特征参数的综合反映,应在储层评价中予以考虑。

    Abstract:

    Micro-pore structure is complex of ultra-low permeability sandstone reservoir, and occurrence condition of fluid is different from conventional reservoir. Movable fluid variation characteristics and diversity origin of samples in Yanchang group of Ordos basin are analyzed through NMR technology. The results show that pattern distributions are various, cutoff value of is moderate—high,parameters of movable fluid change greatly, movable fluid parameters of every formation present difference. Variation range of movable fluid parameters is large when permeability of sample is minor. The data points of movable fluid parameters converge and Variation range decrease with the increasing permeability. Physical property, pore (especially secondary pore) development and communication degree, microcrack development degree and occurrence mode and filling degree to pore of clay mineral are the main reason to cause deviation of movable fluid parameters. Parameters of movable fluid which are the integrated reflection on micro-feature parameters should be considered in the reservoir evaluation.

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高辉,孙卫.2010.特低渗透砂岩储层可动流体变化特征与差异性成因[J].地质学报,84(8):1223-1230.
gaohui, sunwei.2010. Movable fluid variation characteristics and diversity origin of ultra-low permeability sandstone reservoir[J]. Acta Geologica Sinica,84(8):1223-1230.

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历史
  • 收稿日期:2009-07-20
  • 最后修改日期:2009-11-05
  • 录用日期:2010-01-05
  • 在线发布日期: 2010-07-28