吕端川,吕延防,王岐,王万军
L Duanchuan,L Yanfang,WANG Qi,WANG Wanjun

• 1:东北石油大学地球科学学院
• 2:油气藏形成机理与资源评价黑龙江省重点实验室
• 3:大庆油田有限责任公司第二采油厂
• 4:大庆钻探工程公司钻技一公司

摘要(Abstract)：

在断层型油藏的注水开发过程中,过大的注水压力可能导致控圈断裂活化。为了保证生产安全,需要根据断裂的最大静摩擦力调整注水压力,而断层泥的摩擦系数是断裂活化条件下发生摩擦滑移时重要的物理参数。通过对岩石样品所夹断层泥的摩擦实验发现,在断层活化条件下断层泥的摩擦系数随正应力、断层泥含量及黏土成分、温度、含水量等的增加而降低。因此,在正应力大、泥质含量高、黏土成分富集、温度高、含水率高时控圈断裂的摩擦系数低,稳定性较差,断裂在注水压力变化时易滑动。
During the process of the waterflooding in the fault-type reservoir,the excessive water injection pressure may lead to the fracture activation that controls the trap.In order to ensure the operation and production safety,the water injection pressure must be adjusted according to the maximum static friction of the fracture,and the friction coefficient of the fault gouge is one of the important physical parameters in the process of the frictiorl and sliding of the activated fracture.Through the experiment of the fault clay/pug friction between the rock samples discovers that under the conditions of the above activation,the friction coefficient of the fault gouge drops with the increase of the normal stress,fault gouge content and composition,temperature and water content and so on.So in the places of higher normal stress,larger shale content and clay composition,higher temperature and water content,the friction coefficient of the faults that control the trap is lower,its stability is rather poorer,the fractures are prone to slip under the change of the water injection pressure.

关键词(KeyWords)： 断裂;摩擦系数;影响因素;断层型油藏;注水开发
fault;friction coefficient;influencing factor;fault-type oil reservoir;waterflooding development

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金项目(41372154);; 中国石油科技创新基金项目(2012D-5006-0110);; 东北石油大学校青年科学基金项目(2013NQ1270)

作者(Author): 吕端川,吕延防,王岐,王万军
L Duanchuan,L Yanfang,WANG Qi,WANG Wanjun

参考文献(References)：

• [1]王连捷,崔军文,周春景,等.汶川5.12地震发震机理的数值模拟[J].地质力学学报,2009,15(2):105-113.
• [2]马瑾,马胜利,刘力强,等.断层相互作用型式的实验研究[J].自然科学进展,2002,12(5):503-508.
• [3]卜万奎,茅献彪.断层倾角对断层活化及底板突水的影响研究[J].岩石力学与工程学报,2009,28(2):386-394.
• [4]石娜.断层因压差作用滑移机理及引发套损分析[J].油气田地面工程,2010,29(5):23-24.
• [5]高志华,翟香云,王建东.大庆油田注水开发后异常地层压力分布规律研究[J].大庆石油地质与开发,2005,24(1):51-53.
• [6]刘云彬,李永伏.高含水后期周期注水应用的一个实例[J].大庆石油地质与开发,2005,24(5):44-45.
• [7]肖勇,母长河.水驱典型区块综合治理及效果分析[J].大庆石油地质与开发,2004,23(3):54-56.
• [8]白长琦,李德儒,刘评,等.河南油田普通稠油注水开发深部调剖技术研究应用[J].石油地质与工程,2008,22(6):17-23.
• [9]宋子齐,王艳,王宏,等.克拉玛依油田砾岩油藏剩余油分布与挖潜方向[J].大庆石油地质与开发,2008,27(3):44-47.
• [10]赵晓丹,范玉平.欧31块高效开发实践与认识[J].大庆石油地质与开发,2008,27(4):70-72.
• [11]陈子光.岩石力学性质与构造应力场[M].北京:地质出版社,1986.
• [12]马瑾.构造物理学概论[M].北京:地震出版社,1987.
• [13]王仁,丁中一,殷有泉.固体力学基础[M].北京:地质出版社,1979.
• [14]Byerlee J.Friction of rocks[J].Pageoph,1978,116(4):615-626.
• [15]王泽利,何昌荣,周永胜,等.断层摩擦实验中的应力状态及摩擦强度[J].岩石力学与工程学报,2004,23(23):4079-4083.
• [16]刘晓红,方亚如,蔡戴恩,等.海原断层带断层泥摩擦特性的研究[J].西北地震学报,1986,8(3):50-54.
• [17]Saffer D M,Marone C.Comparison of smectite-and illite-rich gouge frictional properties:application to the updip limit of the seismogenie zone along subduction megathrusts[J].Earth and Planetary Science Letters,2003,215(1):219-235.
• [18]付晓飞,付广,赵平伟.断层封闭机理及主要影响因素研究[J].天然气地球科学,1999,10(3):54-62
• [19]周庆华,从断裂带内部结构探讨断层封闭性[J].大庆石油地质与开发,2005,24(6):1-3.
• [20]付晓飞,方德庆,吕延防,等.从断裂内部结构出发评价断层垂向封闭性的方法[J].地球科学——中国地质大学学报,2005,30(3):328-336.
• [21]吕延防,李国会.断层封闭性的定量研究方法[J].石油学报,1996,17(3):39-45.
• [22]耿乃光,郝晋舁,李纪汉,等.断层泥力学性质与含水量关系初探[J].地震地质,1986,8(3):56-60.
• [23]耿乃光.地学领域的摩擦试验研究[J].润滑与密封,1987,(6):21-26.
• [24]Murrell S A F,Ismail I A H.The effects of decomposition of hidrous minerals on the mechanical properties of rocks at high pressure and temperatures[J].Tectonophysics,1976,31(3):207-258.
• [25]吴诗勇,李自安,方亮.高压注水条件下泥岩蠕变的数值模拟研究——以大庆喇嘛甸油田北部背斜构造带SI顶泥岩为例[J].岩性油气藏,2009,21(2):110-112.
• [26]黄小兰,杨春和,刘建军,等.不同含水情况下的泥岩蠕变试验及其对油田套损影响研究[J].岩石力学与工程学报,2008,27(2):3477-3482.
• [27]王华林,耿杰.沂沐断裂带及其附近断裂的断层泥分形特征及其地震地质意义[J].中国地震,1996,12(3):307-315.
• [28]付晓飞,尚小钰,孟令东.低孔隙岩石中断裂带内部结构及与油气成藏[J].中南大学学报:自然科学版,2013,44(6):2428-2438.
• [29]孟元林,黄文彪,王粤川,等.超压背景下黏土矿物转化的化学动力学模型及应用[J].沉积学报,2006,24(4):461-467.
• [30]Stesky R M.Rock friction-effect of confining pressure,temperature and pore pressure[J].Pure and Applied Geophysics,1978,116(4):690-704.
• [31]马瑾,Moore D E,Summers R,等.温度压力孔隙压力对断层泥强度及滑动性质的影响[J].地震地质,1985,7(1):15-24.
• [32]何昌荣,Verberne B A,Spiers C J.龙门山断裂带沉积岩和天然断层泥的摩擦滑动性质与启示[J].岩石力学与工程学报,2011,30(1):113-131
• [33]Giger S B,Cox S F,Tenthorey E.Slip localization and fault weakening as a consequence of fault gouge strengthening—Insights from laboratory experiment[J].Earth and Planetary Science Letters,2008,276(1):73-84.
• [34]He Changrong,Yao Wenming,Wang Zeli,et al.Strength and stability of frictional sliding of gabbro gouge at elevated temperatures[J].Tectonophysics,2006,427(1):217-229.
• [35]Kazuo M,Eiichi F,Keigo K,et al.Depth dependent strength of the fault gouge at the Atotsugawa fault,central Japan:A possible mechanism for its creeping motion[J].Physics of the Earth and Planetary Interiors,2007,161(1):115-125.
• [36]He Changrong,Wang Zeli,Yao Wenming.Frictional sliding of gabbro gouge under hydrothermal conditions[J],Tectonophysics,2007,445(3):353-362.
• [37]Niemeijer A R,Spiers C J,Peach C J.Frictional behaviour of simulated quartz fault gouges under hydrothermal conditions;Results from ultra-high strain rotary shear experiments[J].Teetonophysics,2008,460(1):288-303.
• [38]韩文梅,康天合,王东,等.矿物成分对抛光岩石表面摩擦特性影响的试验研究[J].岩土工程学报,2011,33(8):1211-1215.
• [39]黄建国,张流.水对岩石磨擦滑动若干特性的影响[C]//面向国民经济可持续发展战略的岩石力学与岩石工程——中国岩石力学与工程学会第五次学术大会论文集,1998.
• [40]周瑞光,成彬芳,周玉生,等.断层泥蠕变特性与含水量的关系研究[J].工程地质学报,1998,6(3):217-222.
• [41]吕延防,张发强,吴春霞,等.断层涂抹层分布规律的物理模拟试验研究[J].石油勘探与开发,2001,28(1):30-32.
• [42]Morrow C A,Lockner D.A.,Moore D.E.The effect of mineral bond strength and adsorbed water on fault gouge frictional strength[J].Geophysical Research Letters,2000,27(6):815-818.
• [43]胡涛,任光明,聂德新,等.沉积型软弱夹层成因分类及强度特征[J].中国地质灾害与防治学报,2004,15(1):124-128.
• [44]宋丙辉,谌文物,吴玮江,等.甘肃舟曲泄流坡滑坡滑带土的抗剪强度特性[J].兰州大学学报:自然科学版,2011,47(6):7-12.