西南石油大学学报(自然科学版) ›› 2017, Vol. 39 ›› Issue (3): 97-102.DOI: 10.11885/j.issn.1674-5086.2015.08.14.02

• 地质勘探 • 上一篇    下一篇

挤压作用形成异常高压的定量研究

周鹏高1, 李亚双2, 刘燕3   

  1. 1. 克拉玛依职业技术学院, 新疆 克拉玛依 834000;
    2. 中国石油新疆油田分公司采油一厂, 新疆 克拉玛依 834000;
    3. 中国石油新疆油田分公司新疆技师学院, 新疆 克拉玛依 834000
  • 收稿日期:2015-08-14 出版日期:2017-06-01 发布日期:2017-06-01
  • 通讯作者: 周鹏高,E-mail:1353443828@qq.com
  • 作者简介:周鹏高,1981年生,男,汉族,湖北天门人,讲师,硕士,主要从事石油工程岩石力学研究。E-mail:1353443828@qq.com;李亚双,1981年生,女,汉族,河北丰润人,工程师,主要从事采油工程方面的研究。E-mail:371671688@qq.com;刘燕,1982年生,女,汉族,新疆呼图壁人,讲师,主要从事采油工程方面的教学工作。E-mail:liuyan8211@163.com
  • 基金资助:
    中国石油“新疆大庆”重大专项(2012E-31-13)

Quantitative Study on Abnormal High Pressure by Extrusion Effect

ZHOU Penggao1, LI Yashuang2, LIU Yan3   

  1. 1. Karamay Vocational & Technical College, Karamay, Xinjiang 834000, China;
    2. NO.1 Oil Production Plant, Xinjing Oilfield Company, PetroChina, Karamay, Xinjiang 834000, China;
    3. Institute of Xinjiang Technicians, Xinjing Oilfield Company, PetroChina, Karamay, Xinjiang 834000, China
  • Received:2015-08-14 Online:2017-06-01 Published:2017-06-01

摘要: 封闭地层受挤压后孔隙体积变小,孔隙中的流体受到压缩却无法排出引起压力升高。基于这一理解,许多文献认为构造挤压作用是形成异常高压的主要原因之一,但目前的研究均只是定性分析,未进行定量计算。以双重有效应力理论和多孔介质弹性力学理论为基础,通过缜密的推导,对挤压作用导致的地层弹性压缩量进行了研究,得到了孔隙压力系数增量的理论计算公式。定量计算结果表明,在特定地质条件下,封闭地层受挤压作用后能使孔隙压力小幅度增大,产生轻微的压力异常,挤压作用导致的孔隙压力系数增量十分有限;挤压作用形成异常高压的条件极为苛刻,只有当地层埋藏较深、强度足够大、围岩的密封性能好、挤压作用发生在最小水平主应力方向、且外挤压力足够大,这些条件同时满足时,才可能产生较大的异常高压;挤压作用难以形成异常高压,一般不是异常高压形成的主要原因。

关键词: 挤压作用, 孔隙压力, 异常高压, 地应力, 有效应力

Abstract: Pore volume in closed formation reduces when it is squeezed, and the compressed fluid that cannot be discharged in the pores causes the pressure to rise. A number of previous studies have argued that the tectonic compression effect is one of the main factors that lead to abnormal pressure. However, instead of a quantitative analysis, current studies have paid attention solely to qualitative analysis. In this study, stratum elastic compression caused by extrusion effect was investigated by close reasoning based on the double effective stress theory and the poroelasticity theory, by which the theoretical calculation formula of pore pressure coefficient increment was calculated. Quantitative calculation suggest that, under certain geological conditions, squeezed closed formation leads to a small increase in pore pressure and a slight pressure abnormality, with a limited increment of pore pressure coefficient. It was possible to cause abnormal high pressure by the extrusion effect only when the following occurred simultaneously:stratigraphic burial was sufficiently deep, the strength was sufficiently high, the sealing property of the surrounding rocks was excellent, extrusion occurred in the direction of minimum horizontal stress, and the external extrusion was sufficiently high. The extrusion effect could not generate abnormal high pressure, nor did it serve as the main cause.

Key words: extrusion effect, pore pressure, abnormal high pressure, crustal stress, effective stress

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