首页> 外文会议>International Symposium of the Society of Core Analysts >CHARACTERIZATION OF MICRO-PORES IN ORGANICRICH UNCONVENTIONAL RESERVOIR ROCKS
【24h】

CHARACTERIZATION OF MICRO-PORES IN ORGANICRICH UNCONVENTIONAL RESERVOIR ROCKS

机译:有机性非传蓄水库岩石中微孔的特征

获取原文

摘要

Physical measurements of pore-size distributions in many unconventional reservoir rocks are hampered by a combination of very small features that push the limits of many measurement techniques and the challenges associated with removing residual liquids from the pores. Organic-rich reservoir rocks that act both as source and producer are especially difficult to analyze because of the residual liquids,hydrocarbons and formation water that are trapped in the smallest pores. A combination of low-pressure gas adsorption and differential thermal analysis measurements are used to quantify the proportion and distribution of pores in the micro-scale(less than 5 nm). Pore-size estimation with conventional low-pressure gas adsorption using N2 has a lower limit of several nanometers,but is severely affected by the presence of organic carbon. The use of CO2 as the absorbent gas improves the size range down to 0.5 nm. Solvent extraction on small chips of sample was successful in removing small amounts of residual water and hydrocarbon that increased the total pore volume by approximately 10-20% compared to as-received samples. That volume increase was dominated by the very smallest pores,less than 5 nm,as measured with CO2 adsorption. Thermal analysis measurements verified the loss of water and light hydrocarbons from the extracted samples,while the more complex kerogen that decomposed at higher temperatures was less affected by the extraction. The solvent extraction step removed oil from the solid organic matter and opened very small pores in the sample. The combination of results indicated that a majority of pores in these organicrich samples fell in the 100-500 nm range and that only a small proportion were true micropores. While extraction of residual hydrocarbons opened up a number of very small pores,their contribution to the overall pore volume was small.
机译:许多非常规储层岩石中的孔径分布的物理测量由非常小的特征的组合阻碍了许多测量技术的限制和与从孔中除去残留液体相关的挑战。由于残留的液体,碳氢化合物和形成水陷入最小的孔隙,富含有机富含水库岩石的岩石是源和生产者的岩石尤其难以分析。低压气体吸附和差分热分析测量的组合用于量化微尺度(小于5nm)的孔的比例和分布。使用N2的常规低压气体吸附的孔径估计具有几纳米的下限,但受到有机碳的存在严重影响。使用CO2作为吸收气体的尺寸范围降至0.5nm。与接受的样品相比,样品小芯片上的溶剂萃取成功地除去少量的残留水和碳氢化合物,使总孔体积增加约10-20%。随着CO 2吸附测量的,该体积增加由小于5nm的最小孔径,小于5nm。热分析测量验证了从提取的样品中损失水和轻质烃,而在较高温度下分解的更复杂的基因因子受到萃取的影响。溶剂萃取步骤从固体有机物质中除去油,并在样品中打开非常小的孔隙。结果的组合表明,这些有机辛样品中的大部分孔隙在100-500nm范围内下降,只有小比例是真正的微孔。虽然萃取残留的碳氢化合物突出了一些非常小的毛孔,但它们对整体孔体积的贡献很小。

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