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AN INTEGRATED NUMERICAL AND MINERALOGICAL STUDY OF A HIGH PRESSURE HIGH TEMPERATURE WELL

机译:高压高温井的数值和矿物学综合研究

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Predicting drilling risks in advance is a major challenge in areas that lack drilling experience, and even when information from offset wells is available. Large overpressure was found at TD of an offshore exploratory well drilled mainly through shale. None of the other two previously drilled offset wells in the area had shown any sign of such a high overpressure. This study presents two complementary approaches to gain insight on the overpressure generation mechanisms. The effect of chemical compaction is first evaluated in terms of well cuttings analysis, including sample washing, high-resolution photo catalog, automated mineralogy and X-ray diffraction clay mineralogy analysis. The obtained mineralogical results confirm the presence of the dehydration diagenetic process involving the transformation of smectite to illite. Consequently, a numerical model is presented which combines the effect of mechanical and chemical compaction to predict pore pressure values very close to the overpressure observed during drilling. The model reproduces the depositional history of the lithological column by coupling mechanical and chemical compaction with fluid flow over geological time, and it allows predicting stress, porosity and pore pressure evolution at different geological ages. Calibration and verification of the results of the pore pressure model is done by comparison to drilling experience and logs (post-drill pore pressure profile, geology tops and density/porosity logs).
机译:在缺乏钻井经验的地区,即使有偏移井的信息可用,提前预测钻井风险也是一项重大挑战。在主要通过页岩钻探的海上探井的TD处发现了较大的超压。该地区其他两个先前钻的偏移井中没有一个显示出如此高的超压迹象。这项研究提出了两种互补的方法来获得有关超压产生机理的见解。首先根据油井钻屑分析评估化学压实的效果,包括样品清洗,高分辨率照片目录,自动矿物学和X射线衍射粘土矿物学分析。所获得的矿物学结果证实了脱水成岩过程的存在,该过程涉及蒙脱石向伊利石的转变。因此,提出了一个数值模型,该模型结合了机械和化学压实的作用,可以预测非常接近钻井过程中观察到的超压的孔隙压力值。该模型通过将机械和化学压实作用与地质时间段内的流体流动结合起来,再现了岩性柱的沉积历史,并且可以预测不同地质年龄下的应力,孔隙度和孔隙压力演变。孔隙压力模型结果的校准和验证是通过与钻探经验和测井结果(钻后孔隙压力分布,地质顶部和密度/孔隙度测井结果)进行比较来完成的。

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