首页> 外文会议>Offshore technology conference >Pore Pressure Prediction Before and During Drilling Applying the Four Zones Method
【24h】

Pore Pressure Prediction Before and During Drilling Applying the Four Zones Method

机译:应用四区法预测钻井前后的孔隙压力

获取原文

摘要

This method integrates the geological building blocks of sedimentation, dehydration to lithification and the formation water hydrodynamic forces associated with each of these phases. The current known conventional velocity - pore pressure transformation models are lacking this relationship. In the current widely used conventional methods, it is controversial to consider the shallow section as normally pressured and at the same time extract a compaction trend from its petrophysical properties. Moreover, there is confusion about which part of the subsurface section the Effective Stress theorem should be applied to. The novelty of dividing the subsurface into four zones using this new approach reduces the risk of predicting the pore pressure before drilling and the uncertainty of its correct calibration during drilling. This new pore pressure calculation is done separately in each zone based on the predominant formation-water dynamic. Normal hydrostatic pressure is only assigned to the loosely compacted very shallow section (A). Hydrodynamic zone B with upward formation water flow is associated with compaction and reduction of porosity due to sediments load. Petrophysical trends such as velocity, density, resistivity follows a compaction trend in this zone. As result of depositing shale seal in zone C, due to high stand sea level, fluid is prevented from permeating upward. This low permeable top seal is referred to as top of geopressure (TOG). The geopressured section of zone D below the pressure ramp in zone C follows a cascade outline where the pressure in permeable beds show linear trends and shale exhibits an exponential trend. The petrophysical properties of the deeper shale beds below the top seal represent several passive compaction trends. Pore pressure prediction in the deep geopressured section D is derived from calculating at the same depth the disparity between the extrapolated velocity compaction trend (CT) values and the measured ones. A unique mathematical calculation is introduced here to establish the compaction trend (CT) instead of the manual graphically extrapolated so called NCT. Before drilling seismic velocity, semblance is a key for defining the four zones. Velocity - pore-pressure transformation modeling is an important aspect of the drilling cost for a proposed location. Moreover, LWD's during drilling and conventional logs post drilling are the fine-tuning tools of calibrating the pre-drilling seismic-pressure model. The calibrated model is the backbone of any predicted pore pressure in future drilling locations in the same basin. The pore pressure prediction applying this method facilitates assigning the casing setting and mud programs at the appropriate depths before drilling. Furthermore, it reduces the non-productive time (NPT) and challenges by assessing the subsurface formation pressure including the shallow water flow (SWF), risk of kicks and loss of circulation along the proposed bore-hole trajectory before moving rig on location.
机译:该方法整合了沉积,脱水至岩化的地质构造块以及与这些阶段的每个阶段相关的地层水动力。当前已知的常规速度-孔隙压力转换模型缺乏这种关系。在当前广泛使用的常规方法中,将浅段视为常压并同时从其岩石物性中提取出压实趋势是有争议的。此外,对于应将有效应力定理应用于地下部分的哪个部分也存在困惑。使用这种新方法将地下划分为四个区域的新颖性降低了在钻探之前预测孔隙压力的风险,并降低了在钻探过程中正确校准的不确定性。这种新的孔隙压力计算是根据主要的地层水动力学在每个区域中分别进行的。正常的静水压力仅分配给松散压实的非常浅的部分(A)。地层水流向上的流体动力区B与压实作用有关,并由于沉积物负荷而降低了孔隙度。岩石物理趋势(例如速度,密度,电阻率)遵循该区域的压实趋势。由于页岩海豹在C区沉积,由于高的海平面,阻止了流体向上渗透。此低渗透性顶部密封称为地压顶部(TOG)。在区域C的压力斜坡下方的区域D的地压部分遵循级联轮廓,其中可渗透床中的压力呈线性趋势,而页岩呈指数趋势。顶部密封之下较深的页岩床的岩石物理特性代表了几种被动压实趋势。通过在相同深度计算外推速度压实趋势(CT)值与实测值之间的差异,可以得出深部地压部分D中的孔隙压力预测。这里引入了独特的数学计算来建立压实趋势(CT),而不是手动图形化外推的所谓NCT。在钻探地震速度之前,相似度是定义四个区域的关键。速度-孔隙压力转换模型是建议位置的钻井成本的重要方面。此外,随钻随钻和常规的原木随钻钻探是校准钻前地震压力模型的微调工具。校准后的模型是同一盆地未来钻探位置中任何预测的孔隙压力的基础。应用此方法进行的孔隙压力预测有助于在钻井之前在适当的深度分配套管设置和泥浆程序。此外,通过在移动钻机到位之前评估包括地下水流(SWF)的地下地层压力,踢动风险和沿建议的井眼轨迹的环流损失,它减少了非生产时间(NPT)和挑战。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号