韩学辉^1,,
徐登辉^1,,,
郭俊鑫²,
杨龙³,
王振林⁴,
张达⁵,
罗兴平⁴,
聂俊光¹,
李昊¹,
江佳洋¹
1. 中国石油大学(华东)地球科学与技术学院, 山东青岛 266580
2. 南方科技大学地球与空间科学系, 广东深圳 518055
3. 新疆砾岩油藏实验室, 新疆克拉玛依 833400
4. 新疆油田公司勘探开发研究院, 新疆克拉玛依 834000
5. 中石化东北油气分公司储层及含油气性预测攻关项目团队, 长春 130062

基金项目: 国家自然基金（U1562108）、国家科技重大专项（2017ZX05009001）和"十三五"专项（2016ZX05011）联合资助


详细信息

作者简介: 韩学辉, 男, 1974年生, 辽宁盘锦人, 博士, 副教授, 主要研究方向为岩石物理.E-mail:hanxuehui@upc.edu.cn

通讯作者: 徐登辉, 男, 1992年生, 山东青岛人, 博士在读, 主要研究方向为岩石物理.E-mail:b18010031@s.upc.edu.cn

中图分类号: P631

收稿日期:2018-04-06
修回日期:2018-11-27
上线日期:2018-12-05

Rock physics modelling for acoustic velocities of sandstone considering effects of cementation and compaction

HAN XueHui^1,,
XU DengHui^1,,,
GUO JunXin²,
YANG Long³,
WANG ZhenLin⁴,
ZHANG Da⁵,
LUO XingPing⁴,
NIE JunGuang¹,
LI Hao¹,
JIANG JiaYang¹
1. School of Geoscience, China University of Petroleum(East China), Shandong Qingdao 266580, China
2. Department of Earth and Space Sciences, Southern University of Science and Technology, Guangdong Shenzhen 518055, China
3. Laboratory of Petroleum Reserve in Conglomerate, Xinjiang Karamay 834000, China
4. Research Institute of Petroleum Exploration and Development, Xinjiang Oilfield Company, PetroChina, Xinjiang Karamay 834000, China
5. Reservoir and Fluid Prediction Group, Northeast Oil and Gas Branch, SINOPEC, Changchun 130062, China


More Information

Corresponding author: XU DengHui,E-mail:b18010031@s.upc.edu.cn

MSC: P631

--> Received Date: 06 April 2018
Revised Date: 27 November 2018
Available Online: 05 December 2018


摘要
摘要:成岩作用是影响砂岩声波速度的地质因素之一，定量表征压实和胶结作用的砂岩声波速度岩石物理模型具有重要的理论和实践应用意义.选取视压实率和视胶结率定量表征砂岩成岩作用，通过建立视压实率与颗粒配位数的关系将压实作用的影响引入修正的定量表征胶结作用的CCT模型，最终建立了一种能够定量表征压实和胶结作用对砂岩声波速度影响的岩石物理模型.理论考察发现，随胶结率的增大，岩石声波速度首先迅速增大，随后趋于稳定；随视压实率增大，岩石声波速度同样逐渐增大，当胶结率较大时声波速度变化更为明显.为了验证该声波速度模型，分别对人造砂岩和天然样品进行了声波速度实验观测，结果表明：实验结果与理论分析的趋势吻合良好.该模型易于使用，能够为应用地震和测井资料识别有利储层、定量评价孔隙度以及开展横波速度预测等应用提供理论基础.
关键词: 砂岩/
声波速度/
压实作用/
胶结作用/
岩石物理

Abstract:Diagenesis plays an important role in controlling the acoustic velocities of sandstone. Hence, it is of great importance to develop the rock physics model to quantify the effects of compaction and cementation on the acoustic velocities of sandstone for both the theory and application. Using the apparent compaction and cementation rates, we can quantify the diagenesis degree of the sandstone. The model is then developed based on the modified Contact Cement Theory (CCT), which quantifies the effects of cementation on sandstone elastic moduli. By relating the apparent compaction rate to the grain coordination number, the effects of compaction can be incorporated into the modified CCT. To illustrate these effects, a numerical example is given. The results show that the elastic wave velocities increase rapidly with the cementation rate initially, then keep nearly constant. Meanwhile, the velocities also increase with the compaction rate. which is more obvious under the high cementation rate. To validate our model, the theoretical predictions are compared with the ultrasonic measurements on both the synthetic and natural sandstone samples, which show good agreement between them. The proposed model is easy to use and provides the theoretical basis for identifying the good formations, quantifying the porosity, and predicting the shear wave velocities through the seismic or logging data.
Key words:Sandstone/
Acoustic velocity/
Compaction effects/
Cementation effects/
Rock physics



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