天然气开发

塔里木盆地克拉2气田断裂地质力学活动性对水侵的影响

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  • 中国石油塔里木油田分公司,新疆 库尔勒 841000
江同文(1968-),男,四川绵阳人,教授级高级工程师,博士,主要从事石油地质研究及油气田开发科研与生产管理工作.E-mail:jiangtw_tlm@petrochina.com.cn.

收稿日期: 2017-06-21

  修回日期: 2017-09-07

  网络出版日期: 2017-11-10

基金资助

国家重大科技专项(编号:2011ZX05046);中国石油天然气股份有限公司重大科技专项(编号:2014E-2104)联合资助.

Effects of faults geomechanical activity on water invasion in Kela 2 Gasfield,Tarim Basin

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  • PetroChina Tarim Oilfield Company,Korla 841000,China

Received date: 2017-06-21

  Revised date: 2017-09-07

  Online published: 2017-11-10

摘要

中国陆相最大天然气田——克拉2气田经过10余年的高速开发后,目前面临气井快速见水和气水界面非均匀抬升等问题。为进一步明确复杂构造背景下的高压气田水侵机理,开展了气田内部基于断裂的地质力学活动性及其与气井见水之间的关联性研究。将气田四维地应力场建模和三维断裂力学分析相结合,建立了随气田开发的断裂力学活动性预测模型,研究了断裂活动性对气田水侵的影响。结果表明:①气井见水与井旁断裂力学特征变化有较好的关联性,随着气藏开采及现今地应力场的动态变化,断裂面受力状态也随之改变,从而使断裂带内部渗透性变强或变弱。②随气藏地层压力的下降,若井旁断层和裂缝活动性增加或保持较好,则气井见水较早,气水界面抬升较快。③由于气田内部应力场和断裂分布均较复杂,因此不同构造部位的断裂活动性差异较大,从而造成不同位置气水界面抬升不均匀且相差较大。研究进一步明确了克拉2气田的水侵机理,并利用断裂地质力学活动性指数将气藏划分为3个见水风险区,为气田开发方案优化提供依据。
 

本文引用格式

江同文,张辉,王海应,尹国庆,肖香姣 . 塔里木盆地克拉2气田断裂地质力学活动性对水侵的影响[J]. 天然气地球科学, 2017 , 28(11) : 1735 -1744 . DOI: 10.11764/j.issn.1672-1926.2017.09.003

Abstract

After more than ten years high-speed development,the most productive continental gasfield in China,Kela 2 Gasfield is now facing challenges associated with water breakthrough in gas well and heterogeneous water invasion in the field.To further understand the water invasion mechanism of the high pressure gasfield under complex tectonic setting,an investigation of faults geomechanical activity was conducted to investigate the relationship between variation of faults mechanical activity and water breakthrough of gas well.The faults geomechanical activity prediction model was established based on the combination of modeling of four dimensional stress field and 3D faults mechanical analysis to research its effects on water invasion in this field.The results are shown:(1)There is a good correlation between water breakthrough in gas well and faults mechanical characteristics.With the development of gas reservoir,dynamic variation of stress field led to change of stress state on faults’ planes,so that the permeability of the faults zone would be able to become stronger or weaker.(2)With the depletion of gas reservoir,the gas wells near the faults with higher geomechanical activity would produce water earlier and the gas-water interface would rise faster.(3)Because the distribution of stress field and faults in the reservoir are complex,there are great differences in the faults mechanical activity on different location of structure,which result in the uplift of gas-water interface being greatly different and inhomogeneous in the reservoir.The research further clarified the mechanism of water invasion in Kela 2 Gasfield,the gas reservoir is divided into three water breakthrough risk districts based on the prediction of faults geomechanical activity to do early warning for the areas and gas wells which has the high risk of water invasion.This research provides a basis for optimizing the development program of Kela 2 Gasfield.
 

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