首页> 外文会议>SPWLA Annual Logging Symposium >MAGNETIC INTERFERENCE EFFECTS ON ACCELEROMETER AND MAGNETOMETER DATA:DETECTION,QUALITY CONTROL AND CORRECTION
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MAGNETIC INTERFERENCE EFFECTS ON ACCELEROMETER AND MAGNETOMETER DATA:DETECTION,QUALITY CONTROL AND CORRECTION

机译:加速度计和磁力计数据的磁干扰效应:检测,质量控制和校正

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Accurate orientation is required for both hole trajectory determination and for information gleaned from borehole images,acoustic waveforms and other azimuthally acquired data.Orientation quality depends on high quality acquisition of accelerometer and magnetometer information.Anomalous magnetization within the wellbore and formation can influence accelerometer and magnetometer measurements. Detection and proper correction for these magnetic anomalies is important to maintain the integrity of the orientation data and consequently the results derived from the data.Using a fast robust method,quality control and corrections for these magnetic field disturbances has improved the quality of the directional components. At least four different sources of well magnetic anomalies have been observed:1)geological remnant magnetization,2)magnetic materials near,but not in the well,3)magnetic field below the casing shoe and 4) magnetic debris in the well.Geologic remnant magnetization and magnetic materials near the well are of interest to geologists and drillers,e.g. paleomagnetism and collision avoidance,respectively. Repeated multiple log passes from a test well provides proof that the orientation module is sensitive enough to detect and correct certain magnetic sources. Comparisons to gyro data have further provided verification of results in several wells. Several data sets are illustrated that suffer from both accelerometer and magnetometer bias and tool string magnetization.Corrections have been applied to remove the accelerometer and magnetic biases and tool string magnetization effects.Additional processing has been applied to extract(and correct for)the local magnetic anomalies.These local anomalies are described by three curves containing the anomalous magnetic field strength,its inclination and azimuth. Example data was diverse and varied from conventional sediments to geothermal volcanics along with anomalies from tool string magnetization to remnant magnetic fields. Data with a high rotation rate were also tested,analyzed and corrected.The limitations of the orientation module,the acquisition system and processing are summarized.
机译:孔轨迹确定需要精确的方向,并且从钻孔图像中收集信息,声波形状和其他方位角获取的数据。机构质量取决于加速度计和磁力计信息的高质量获取。井筒内的磁化,形成加速度计和磁力计可以影响加速度计和磁力计测量。对这些磁异常的检测和适当的校正对于保持方向数据的完整性以及因此源自数据的结果是重要的。对于这些磁场干扰的快速鲁棒方法,质量控制和校正具有改善了方向部件的质量。已经观察到至少四种不同的井磁性异常来源:1)地质残余磁化,2)磁性材料靠近,但不在井中,3)磁场下方鞋面鞋下方和4)磁性碎片在井中。地理残余物井附近的磁化和磁性材料对地质学家和钻孔者感到兴趣,例如古磁体分别和碰撞避免。重复的多个日志从测试井通过提供证明方向模块足够敏感以检测和纠正某些磁源。陀螺数据的比较还提供了几个井中的结果验证。示出了几种数据集,其遭受加速度计和磁力计偏置和刀具串磁化。已施加粗校以除去加速度计和磁偏置,刀具磁化效果。已应用于提取(并校正)局部磁的加工异常。这些局部异常由含有异常磁场强度的三条曲线,其倾斜和方位角描述。示例数据多样化,并从常规沉积物与地热火山的变化以及从工具串磁化到残余磁场的异常。还测试了具有高旋转速率的数据,分析和校正。总结了方向模块,采集系统和处理的局限性。

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