首页> 外文期刊>Petrophysics: The SPWLA Journal of Formation Evaluation and Reservoir Description >Pore Network Simulation of Low-Field NMR Relaxometry under Conditions of Drainage and Imbibition: Effects of Pore Structure and Saturation History
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Pore Network Simulation of Low-Field NMR Relaxometry under Conditions of Drainage and Imbibition: Effects of Pore Structure and Saturation History

机译:排水和吸水条件下低场核磁共振弛豫的孔隙网络模拟:孔隙结构和饱和历史的影响

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摘要

Nuclear magnetic resonance (NMR) relaxometry tests, carried out on partially saturated porous media, convey information on the distribution of fluids within the pore space. Proper interpretation of this information requires a means to isolate the effects of pore structure (pore and throat shape and size distributions, spatial correlations, etc.) wettability and saturation history. A pore network simulator of NMR relaxation that can clarify the effect of these factors on observed T_2 distributions is developed in this work. The pore network model can be calibrated with pore structure parameters (pore volume and throat size distributions, pore connectivity) determined from analysis of stochastic 3D replicas of the pore space generated from thin-section image information. The presence of irregular, and possibly, fractal pore surfaces is accounted for through a "late pore filling" model calibrated to match mercury porosimetry data. The network model is then used to simulate the water distribution and proton magnetization decay under conditions of drainage and imbibition. The model can be used to examine: (a) conditions under which diffusive coupling between pores has a significant effect on the decay spectra; (b) contributions to the magnetization decay spectra from water trapped at the irregular pore surfaces; and (c) contributions to the magnetization decay spectra from water in large pores which are inaccessible by the non-wetting phase during drainage, and water in pores containing oil trapped during imbibition.
机译:在部分饱和的多孔介质上进行的核磁共振(NMR)弛豫法测试可传达有关孔隙空间内流体分布的信息。对这些信息的正确解释需要一种方法来隔离孔隙结构(孔和喉的形状和大小分布,空间相关性等)的影响,润湿性和饱和历史。在这项工作中,开发了核磁共振弛豫的孔隙网络模拟器,可以澄清这些因素对观察到的T_2分布的影响。可以使用孔隙结构参数(孔隙体积和喉道尺寸分布,孔隙连通性)对孔隙网络模型进行校准,该孔隙结构参数是根据由薄截面图像信息生成的孔隙空间的随机3D复制品的分析确定的。通过校准以匹配汞孔隙率数据的“晚期孔隙填充”模型,可以解决不规则的,可能存在的分形孔隙表面的问题。然后使用网络模型模拟排水和吸水条件下的水分布和质子磁化强度衰减。该模型可用于检查:(a)孔之间的扩散耦合对衰减谱有显着影响的条件; (b)滞留在不规则孔表面的水对磁化衰减谱的贡献; (c)排水过程中非润湿阶段无法进入的大孔隙中的水以及吸收过程中被困油的孔隙中的水对磁化衰减谱的贡献。

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