首页> 外文期刊>Journal of natural gas science and engineering >Experimental study on physical structure properties and anisotropic cleat permeability estimation on coal cores from China
【24h】

Experimental study on physical structure properties and anisotropic cleat permeability estimation on coal cores from China

机译:中国煤芯物理结构性质及各向异性割理渗透率估算的试验研究

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

Knowledge of the natural structure properties of coal seams is essential for the coal bed methane (CBM) production because of their great influence on the inner flow characteristics and permeability features of hydrocarbons and water. In this paper, a series of laboratory tests, including nondestructive low-field nuclear magnetic resonance (NMR), scanning electron microscopy (SEM), X-ray computed tomography (CT) and core tests were carried out to characterize the physical structure properties of coal. The pore size distribution, pore type, morphological features and three-dimensional rendering of coal cleat structures are presented. The permeability changes of 7 cylindrical coal cores investigated under a varying effective stress range (0-35Mpa) reveal that coal porosity decreased linearly and coal permeability declined exponentially with the rise of stress; while under higher stress conditions, the occurrence of internal crushing and mechanical damage will result in irreversible change for porosity and permeability. Through the comprehensive analysis based on linking permeability to porosity and CT result, a basic estimation on directional cleat permeability is also realized. This method provides a preliminary but satisfactory estimation for local directional cleat permeability, which reflects that both bedding and non bedding direction permeability owns great heterogeneity for an individual sample; but face cleat permeability always found to be the largest, and the mean bedding plane permeability value is found usually 3.01-11.68 times lower than face and butt cleat permeability. (C) 2016 Elsevier B.V. All rights reserved.
机译:煤层的自然结构特性的知识对于煤层气(CBM)的生产至关重要,因为它们对碳氢化合物和水的内部流动特性和渗透特性有很大的影响。在本文中,进行了一系列实验室测试,包括无损低场核磁共振(NMR),扫描电子显微镜(SEM),X射线计算机断层扫描(CT)和岩心测试,以表征铁氧体的物理结构特性。煤炭。给出了煤夹层结构的孔隙分布,孔隙类型,形态特征和三维绘制。在变化的有效应力范围(0-35Mpa)下对7个圆柱状煤芯的渗透率变化进行了研究,结果表明,随着应力的增加,煤的孔隙度呈线性下降,渗透率呈指数下降。在较高的应力条件下,内部压碎和机械损伤的发生将导致孔隙率和渗透率发生不可逆的变化。通过将渗透率与孔隙度联系起来的综合分析和CT结果,也可以实现对方向性固溶性渗透率的基本估算。这种方法提供了一个初步的但令人满意的局部方向钉渗透率的估计,这反映了层理方向和非层理方向渗透率对于单个样品都具有很大的异质性。但是,总是发现面部防滑钉的渗透率最大,通常发现铺垫平面的平均渗透率值比面部和对接楔的渗透率低3.01-11.68倍。 (C)2016 Elsevier B.V.保留所有权利。

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