| 高压压汞与核磁共振技术在致密储层孔隙结构分析中的应用: 以鄂尔多斯盆地合水地区为例 |
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| 引用本文： | 卢振东,刘成林,臧起彪,吴育平,杨熙雅,阳宏,曾晓祥,李闻达.高压压汞与核磁共振技术在致密储层孔隙结构分析中的应用: 以鄂尔多斯盆地合水地区为例[J].地质科技通报,2022,41(3):300-310. |
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| 作者姓名： | 卢振东 刘成林 臧起彪 吴育平 杨熙雅 阳宏 曾晓祥 李闻达 |
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| 基金项目： | 国家自然科学基金项目41872127 |
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| 摘 要： | 孔隙结构制约着油气在储层中的储集能力和流动能力, 是研究致密砂岩储层的关键要素, 也是当前研究的重点和难点问题。以鄂尔多斯盆地合水地区上三叠统延长组长7致密储层为例, 结合高压压汞、核磁共振等分析技术, 对储层孔隙结构、可动流体参数之间的关系进行了深入研究, 主要取得以下认识: ①利用常规方法, 线性最小二乘法将核磁共振T2谱转换孔隙半径时, 这种通过线性关系得到的结果精度较低, 相关系数为(0.87~0.98)/0.92, 通过分形理论, 计算出压汞曲线对应的拐点, 进行分段换算出对应的T2, 以此为界限将核磁共振T2谱分段转换, 结果显示转化后曲线叠合程度高, 相关系数(0.97~0.99)/0.98;②通过分析流体可动性的影响因素, 岩石的物性具有直接的关系, 其中孔隙度更适合表征储层的储集空间大小, 相关性为0.9, 和可动流体饱和度的相关性更好; 孔隙结构特征参数与可动流体参数相关性较好, 致密的孔隙结构制约着流体的可动性。
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| 关 键 词： | 致密砂岩 核磁共振 高压压汞 压汞分形 孔隙结构 可动流体 |
| 收稿时间： | 2021-07-21 |
Application of high pressure mercury injection and nuclear magnetic resonance in analysis of the pore structure of dense sandstone: A case study of the Heshui area,Ordos Basin |
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| Abstract: | Pore structure restricts the reservoir capacity and flow capacity of oil and gas in the reservoir, which is the key factor of studying tight sandstone reservoir, and also the key and difficult problem of current research. Taking the Chang 7 tight reservoir of Upper Triassic Yanchang Formation in Heshui area of Ordos Basin as an example, the relationship between pore structure and movable fluid parameters was studied by combining high-pressure mercury injection and nuclear magnetic resonance (NMR) analysis techniques. The main results are as follows: ① when using the conventional method and linear least square method to convert the NMR T2 spectrum into pore radius, the pore structure can be divided into two parts, The correlation coefficient is (0.87-0.98)/0.92. The inflection point of the mercury injection curve is calculated by fractal theory, and the corresponding T2 is converted. The T2 spectrum is converted by segments. After the conversion, the curve has a high degree of overlap, and the number of phase relations is (0.97-0.99)/0.98. ② By analyzing the influencing factors of fluid mobility, it is found that there is a direct relationship between rock physical properties, in which porosity is more suitable to characterize the size of reservoir space, the correlation is 0.9, and the correlation with movable fluid saturation is better; The characteristic parameters of pore structure have a good correlation with the parameters of movable fluid, and the tight pore structure restricts the mobility of fluid. The proportion of dead pores is related to SMFS φ The negative correlation coefficients of MFS were 0.5371 and 0.3775, respectively φ MFS has little effect, but it has no effect φ MFS is more suitable to characterize the micro pore structure. |
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