录井工程 ›› 2023, Vol. 34 ›› Issue (2): 1-8.doi: 10.3969/j.issn.1672-9803.2023.02.001
• 工艺技术 • 下一篇
屈凯旋①, 李国良①, 于春勇②, 赵全国①, 段传丽①, 房金伟①
QU Kaixuan①, LI Guoliang①, YU Chunyong, ZHAO Quanguo①, DUAN Chuanli①, FANG Jinwei①
摘要: 利用核磁共振技术估算孔喉分布的关键在于准确确定弛豫时间与孔喉半径之间的转换方法,常规的线性关系转换方法拟合效果较差,而幂函数转换方法是经验公式,无法通过数学关系推导得出,两种方法都具有一定的缺陷。因此,基于Korringa-Seevers-Torrey模型,结合核磁共振原理推导出了弛豫时间T2谱与孔喉半径的理论关系,并建立了相应的计算模型,所有的模型参数都具有严格的物理意义。以南华北盆地太原组致密砂岩样品为例,对推导公式的准确性进行了验证。考虑到不同大小孔隙的表面弛豫率具有差异性,利用推导公式模型对致密砂岩的孔喉半径分布范围分段进行了拟合,结果显示,采用新方法拟合弛豫时间与孔喉半径数据的效果极佳,拟合决定系数均在0.89以上,说明新方法的准确性极高。此外,基于新方法获得了致密砂岩储层核磁共振孔喉半径分布,并确定了与可动流体分布对应的孔喉半径下限范围。该方法不仅有效提升了核磁共振孔喉半径分布的转换精度,也为利用核磁共振技术定量表征致密砂岩储层的孔隙结构特征提供了可靠的工具。
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