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    超高温高压岩石物理实验研究

    Experimental study of rock physics under ultrahigh temperature and high pressure conditions

    • 摘要: 随着石油勘探与开发技术的进步,尤其是材料、控制等技术的进步,岩石物理实验研究逐渐向超高温高压的地表深层原位发展。提出了一套适用于地表深层原位实验研究的超高温高压岩石地震弹性参数测量系统。该系统利用传统压机和石墨管实现了对温压的控制,具备了快速加载超高温高压的能力,可用于超高温高压条件下的岩石物理实验研究。利用所提出的岩石弹性参数测量系统对10块岩石样品进行了测试,获得了超深层储层条件(温度:~250 ℃,围压:~300 MPa)下岩石样品的纵横波速度。同时,在较大范围的压力、温度域上拟合了实验数据,分析了弹性波速度的温度和压力依赖性,刻画了速度−温压的协变关系。结果表明,速度随着温度和压力的增高分别呈现对数减小和对数增加,且纵波拟合系数对孔隙类型具有明显的指向性。

       

      Abstract: With the advancement of petroleum exploration and development technologies, especially with respect to materials and control, the experimental study of rock physics is moving towards in-situ deep surface layers under ultrahigh temperature and high pressure. This paper presents a seismic elastic parameter measurement system for ultrahigh-temperature and high-pressure rocks. This system utilizes traditional presses and graphite tubes to achieve temperature and pressure control, and has the ability to quickly load ultrahigh temperature and high pressure, so it can be used for experimental study of rock physics under ultrahigh temperature and high pressure conditions. With this system, 10 rock samples were tested to obtain the elastic parameters such as acoustic velocity under ultradeep reservoir conditions (temperature ~250 ℃, pressure ~300 MPa). Moreover, the experimental data were fitted over a wide range of pressure and temperature domains, the temperature-pressure dependence of elastic wave velocity was analyzed, and the covariant relationship between velocity and temperature-pressure was characterized. The results indicate that the velocity decreases and increases logarithmically with the increase of temperature and pressure respectively, and the longitudinal wave fitting coefficient has a clear directional effect on the pore type.

       

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