...
首页> 外文期刊>Energy Exploration & Exploitation >Probe material choice for nuclear magnetic resonance cryoporometry (NMRC) measurements of the nano-scale pore size distribution of unconventional reservoirs
【24h】

Probe material choice for nuclear magnetic resonance cryoporometry (NMRC) measurements of the nano-scale pore size distribution of unconventional reservoirs

机译:非常规储层纳米尺度孔径分布的核磁共振低温法(NMRC)测量的探针材料选择

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

Nuclear magnetic resonance cryoporometry is a newly developed technique that can characterize the pore size distribution of nano-scale porous materials. To date, this technique has scarcely been used for the testing of unconventional oil and gas reservoirs; thus, their micro- and nanoscale pore structures must still be investigated. The selection of the probe material for this technique has a key impact on the quality of the measurement results during the testing of geological samples. In this paper, we present details on the nuclear magnetic resonance cryoporometric procedure. Several types of probe materials were compared during the nuclear testing of standard nano-scale porous materials and unconventional reservoir geological samples from Sichuan Basin, Southwest China. Gas sorption experiments were also carried out on the same samples simultaneously. The K-GT values of the probe materials octamethylcyclotetrasiloxane and calcium chloride hexahydrate were calibrated using standard nano-scale porous materials to reveal respective values of 149.3 Knm and 184 Knm. Water did not successfully wet the pore surfaces of the standard controlled pore glass samples; moreover, water damaged the pore structures of the geological samples, which was confirmed during two freeze-melting tests. The complex phase transition during the melting of cyclohexane introduced a nuclear magnetic resonance signal in addition to that from liquid in the pores, which led to an imprecise characterization of the pore size distribution. Octamethylcyclotetrasiloxane and calcium chloride hexahydrate have been rarely employed as nuclear magnetic resonance cryoporometric probe materials for the testing of an unconventional reservoir. Both of these materials were able to characterize pore sizes up to 1 mu m, and they were more applicable than either water or cyclohexane.
机译:核磁共振超低温法是一项新开发的技术,可以表征纳米级多孔材料的孔径分布。迄今为止,该技术几乎没有用于非常规油气藏的测试。因此,它们的微孔和纳米孔结构仍必须进行研究。在地质样品测试过程中,用于该技术的探针材料的选择对测量结果的质量具有关键影响。在本文中,我们介绍了有关核磁共振低温计量程序的详细信息。在对来自中国西南四川盆地的标准纳米级多孔材料和非常规储层地质样品进行核试验期间,比较了几种探针材料。气体吸附实验也同时在相同的样品上进行。使用标准的纳米级多孔材料校准了探针材料八甲基环四硅氧烷和六水合氯化钙的K-GT值,以显示各自的值149.3 Knm和184 Knm。水不能成功地润湿标准受控孔玻璃样品的孔表面。此外,水破坏了地质样品的孔隙结构,这在两次冷冻融化试验中得到了证实。环己烷熔融过程中的复杂相变除了引入了孔中液体的信号以外,还引入了核磁共振信号,这导致了孔径分布的不精确表征。八甲基环四硅氧烷和六水合氯化钙很少用作核磁共振低温测温探针材料,用于测试非常规储层。这两种材料都能够表征最大1微米的孔径,并且比水或环己烷更适用。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号