首页 | 官方网站   微博 | 高级检索  
     

致密含气砂岩核磁共振—声波速度联合实验
引用本文:邓少贵,牛云峰,赵岳,马明明,谢伟彪,庄东志.致密含气砂岩核磁共振—声波速度联合实验[J].石油学报,2016,37(6):768-776.
作者姓名:邓少贵  牛云峰  赵岳  马明明  谢伟彪  庄东志
作者单位:1. 中国石油大学地球科学与技术学院 山东青岛 266580; 2. 海洋国家实验室海洋矿产资源评价与探测技术功能实验室 山东青岛 266071; 3. 中国石油冀东油田公司勘探开发研究院 河北唐山 063004
基金项目:国家自然科学基金项目(No.41174099,No.41574118)和中国石油冀东油田公司重大专项(2013A02-04)资助。
摘    要:为研究致密含气砂岩有效储层划分、流体识别方法,选取了典型致密含气砂岩样品,开展核磁共振—声波速度联合实验。以核磁共振实验为基础,结合压汞曲线特征,研究了储层孔隙结构特征,分析了储层可储性;以岩石声学特性实验为基础,研究纵、横波速对储层含气性的敏感性;分析了核磁共振T2谱与横波速度对岩石孔隙特征的共性反映,得出了T2几何平均值(T2gm)与横波速度之间的关系,进而建立了核磁共振—声波速度联合含气性识别图版。研究表明,目标区致密砂岩储层有4种孔隙结构,孔隙发育尺度与粗—细小喉道交互配位关系,决定了4种孔隙结构储层的储集和渗透能力。致密含气砂岩纵波速度对含气性敏感,利用纵波时差与纵、横波速比交会识别含气性效果良好;核磁共振T2gm与横波速度呈幂函数关系,为利用核磁共振测井预测地层横波速度提供了帮助。进而将不同含气岩石纵波时差与核磁共振T2gm进行交会,显示该方法对致密砂岩储层含气性具有较好的识别效果。

关 键 词:孔隙结构  核磁共振  声波速度  T2几何平均值  含气性识别  
收稿时间:2015-11-03

Nuclear magnetic resonance-acoustic velocity joint experiment of tight gas sandstone
Deng Shaogui,Niu Yunfeng,Zhao Yue,Ma Mingming,Xie Weibiao,Zhuang Dongzhi.Nuclear magnetic resonance-acoustic velocity joint experiment of tight gas sandstone[J].Acta Petrolei Sinica,2016,37(6):768-776.
Authors:Deng Shaogui  Niu Yunfeng  Zhao Yue  Ma Mingming  Xie Weibiao  Zhuang Dongzhi
Affiliation:1. School of Geosciences, China University of Petroleum, Shandong Qingdao 266580, China; 2. Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Shandong Qingdao 266071, China; 3. Research Institute of Petroleum Exploration and Development, PetroChina Jidong Oilfield Company, Hebei Tangshan 063004, China
Abstract:To study the effective reservoir division and fluid identification methods of tight gas sandstone, the samples of typical tight gas sandstone were selected to carry out Nuclear Magnetic Resonance(NMR)-acoustic velocity joint experiment. Based on NMR experiments in combination with the characteristics of mercury injection curves, the pore structure characteristics and reservoir reserving availability of reservoirs were studied and analyzed. The sensibility of vp and vs to reservoir gas-bearing ability was studied on a basis of rock acoustic characteristic experiments. The common reflection of rock pore characteristics by NMR T2 spectrum and vs was analyzed to obtain the relationship between T2 geometric average (T2gm) and vs, based on which the NMR-acoustic velocity joint gas-bearing identification chart is established. Research results show that there are four kinds of pore structures in tight sandstone reservoirs of the target area, and the reserving and penetration abilities of such reservoirs is determined by the interacted coordination relationship between pore development scale and coarse-fine throat. The vp of tight gas sandstone is sensitive to gas-bearing property, and the P-wave transit time versus vp/vs cross-plot works well in identifying the gas-bearing property. There is a power function relationship between NMR T2gm and vs, helpful to predict reservoir vs with the use of NMR logging. Thus, P-wave transit time versus NMR T2gm of different gas-bearing rocks is cross-plotted to prove the favorable identification effect of this method on gas-bearing property of tight sandstone reservoirs.
Keywords:pore structures  nuclear magnetic resonance  acoustic velocity  T2 geometric mean  gas-bearing indentification  
本文献已被 CNKI 等数据库收录!
点击此处可从《石油学报》浏览原始摘要信息
点击此处可从《石油学报》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司    京ICP备09084417号-23

京公网安备 11010802026262号