无人飞行器对罗马什金斯克油气田的航磁勘测结果

B. M. Nasyrtdinov, A. V. Starovoytov, M. M. Khamiev
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引用次数: 0

摘要

本研究的目的是使用无人驾驶飞行器对 Romashkinskoye 油田(俄罗斯鞑靼斯坦共和国)68 km 320 m 剖面上的磁场感应进行勘测。勘测方案如下:任务路线包括三次平行飞行(主要剖面)和一次交叉飞行(横向剖面)。相邻平行飞行之间的距离为 100 米。每个野外考察日的飞行任务分配是为了使附近的飞行任务与剖面重叠至少 100 米,并使飞行轨迹与前一个飞行任务的轨迹相吻合。为优化流程,两个邻近的航班选择一个起飞/降落点。在一次 20-25 分钟的勘测过程中,无人飞行器覆盖的最大剖面为 1.25 公里。最大飞行距离(从起飞到降落)不超过 6-6.5 公里。即使在恶劣的天气条件下(下雨和 8-12 米/秒的阵风),文章中考虑的方法也能在较长的跨度内覆盖 45 公里的直线距离。勘测结果的均方根误差为 ±4.7 nT。通过这次勘测,可以在一个较长的断面上获得 3 个磁场感应幅值剖面图。航磁勘测和基底块体结构数据(根据地貌分析数据)与结晶基底的局部成分之间具有良好的相关性。阿尔图尼诺-舒纳克断层在磁场中明显表现为振幅≈60 nT的正异常。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Unmanned aerial vehicle aeromagnetic survey results on Romashkinskoye hydrocarbon field
The purpose of the study is to survey the magnetic field induction on the Romashkinskoye oil field (Republic of Tatarstan, Russia) using an unmanned aerial vehicle over the profile of 68 km 320 m. A DJI Matric 600Pro electric hexacopter was used as an unmanned aerial vehicle. The survey scheme was as follows: the mission route consisted of three parallel flights (main profiles) and one crossing flight (transverse profile). The distance between adjacent parallel flights was 100 m. The intersecting profile was necessary to connect the main profiles. The flight assignments of each field day were built to overlap the profiles by at least 100 m by the nearby flights and make the flight trajectory coincide with the one of the previous flight. To optimize the process one takeoff / landing point was selected for two nearby flights. During one 20-25 min survey the maximum profile covered by the unmanned aerial vehicle was 1.25 km. The maximum flight distance (from the takeoff moment to the landing) did not exceed 6–6.5 linear kilometers. The methodology considered in the article made it possible to cover 45 linear kilometers over a long span even in adverse weather conditions (rain and wind gusts of 8–12 m/s). The resulting root mean square error for this survey was ±4.7 nT. The survey conducted allowed to obtain 3 profiles with the magnetic field induction magnitude over an extended section. A good correlation was registered between the aeromagnetic survey and the data on the block structure of the basement (according to geomorphological analysis data) with the local component of the crystalline basement. Altunino-Shunak fault has clearly manifested itself in the magnetic field as a positive anomaly with an amplitude of ≈60 nT.
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