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A New Perspective to Shallow Water Flow (SWF) and Sinking Well-Head Preventions in Deep Water

机译:浅水流量(SWF)和深水中井头预防的新视角

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A new study integrating the seismic velocity profile with a proposed subsurface geopressure partition sheds light on one of the possible main causes of shallow water flow (SWF) and sinking well head in deep water. The Bureau of Ocean Energy Management (BOEM), previously known as the Minerals Management Service (MMS), reported 157 cases of SWF in the Gulf of Mexico. Most of these cases occurred in the Mississippi and Green Canyons areas where the late Pleistocene depositional fan was active. Occasionally, conductor casings and well heads sink and get lost in these areas as well. Study of the pressure gradients of sand vs. shale in the proposed subsurface zones (A, B, C, and D) points to a possible source of these two events. The fragile nature of the unconsolidated shallow hydrostatic zone A is mostly responsible for the loss of well head. This shallow zone gradually transforms to a compacted hydrodynamic system (zone B), associated with a dewatering process that can lead to SWF. Calculating the linear pressure gradient in the sand beds vs. the feasible formation pressure in the shale layers in zone B is the backbone of this shallow water flow study. The sand rapidly flows upward at a linear gradient (0.536 * z - 228) ranging from 0.53 to 0.59 psi/ft. On the other hand, slow compaction of shale and dewatering follows an exponential pressure gradient rate of 1.49 * ln(z - MLdepth) - a. During drilling, penetrating the interface between the shale and the underlying sand causes sand overflow that overcomes the mud pressure and SWF takes place due to the pressure differential between the sand and the shale. Mitigating these events should be attempted before drilling any wells in the deepwater. Seismic velocity, sequence stratigraphy and geopressure modeling can identify potentially problematic zones so that precautions can be taken to combat and avoid these challenges during drilling operation. Choosing the right depth for casings and adjusting the value of the mud up during drilling to avoid SWF are recommended in this article to avoid potential well abandonments.
机译:一种新的研究,将地震速度概况与拟议的地表地层分区脱落,揭示了浅水流量(SWF)的可能原因之一,深水中沉入井头。海洋能源管理局(博伊姆),以前称为矿物质管理服务(MMS),报告了墨西哥湾的157例SWF案件。这些案件中的大多数情况发生在密西西比和绿色峡谷领域,后期更新的沉积风扇活跃。偶尔,导体套管和头部头部也迷失在这些区域。在拟议的地下区(A,B,C和D)中的沙子与Shale的压力梯度研究这两个事件的可能源。未溶胀的浅水静压区A的脆弱性质主要负责井头的损失。这种浅区域逐渐变换为压实的流体动力系统(B区),与可导致SWF的脱水过程相关。计算砂床中的线性压力梯度与区域B区的页岩层中的可行形成压力是该浅水流动研究的骨干。沙子在线性梯度(0.536 * Z-228)的线性梯度(0.536 * Z-228)上快速流动,范围为0.53至0.59 psi / ft。另一方面,页岩和脱水的缓慢压实遵循指数压力梯度率为1.49 * ln(z - mldepth) - a。在钻孔期间,穿透页岩和下面的沙子之间的界面导致砂溢出克服泥浆压力,并且由于沙子和页岩之间的压差而发生SWF。在深水中的任何井钻井之前,应尝试减轻这些事件。地震速度,序列地层和地磁建模可以识别潜在的有问题的区域,以便在钻井操作期间可以采取预防措施来打击和避免这些挑战。在本文中建议在钻孔过程中选择壳体的正确深度并调节摩擦的值,以避免SWF,以避免潜在的放弃。

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