南极维尔纳德斯基院士站阿根廷岛磁体间天文台的升级

A. Marusenkov, Ssau, M. Leonov, V. Korepanov, S. Leonov, A. Koloskov, Ye. Nakalov, Y. Otruba
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引用次数: 1

摘要

本文介绍了2019年1 - 4月在乌克兰南极维尔纳德斯基科考站地磁观测站(代码AIA)对基于LEMI-025变差仪的磁测综合体进行升级改造的主要特点。天文台的旧磁强计由两台LEMI-008(02号和16号)变差计和一台POS-1标量磁强计组成。LEMI-008和POS-1的测量没有相互同步,这是主要问题之一。每个测量仪器单独作为整个磁强计配合物的一个组成部分,具有良好的单独性能。然而,总的来说,该复合体作为一个整体系统的性能下降,主要是由于缺乏测量的相互同步。并给出了一些初步的试验结果。的主要目标。升级AIA天文台的主要任务之一是安装一个与1秒INTERMAGNET数据标准要求兼容的新变差计。二十年来,在Akademik Vernadsky站的旧LEMI-008变换器显示出很高的基线稳定性,符合INTERMAGNET的要求。不幸的是,旧变量计的噪声特性,与UTC同步的精度,以及分辨率不再满足当前INTERMAGNET对产生1秒数据的设备的要求。LEMI-008型变差仪与POS-1型标量磁强计测量结果不同步。由于缺乏可靠的相互同步,由变差计间接计算的场矢量模块与用标量磁强计直接测量的场矢量模块之间的差异会发生变化,可能不可靠。由于强烈的地磁干扰,这降低了磁测复合体作为一个整体测量系统的总体精度,尽管该复合体由高精度仪器组成。LEMI-008变差仪中只有一台配备了GPS同步。这使得数据处理变得困难。因此,关键的升级任务之一是创建一个系统,以相互同步的测量由变差计LEMI-025和标量磁强计pos1提供的精度约0.1秒(但不低于1秒)使用控制计算机。方法。利用控制计算机对POS-1时钟进行周期性调整,以给定的时间提前开始测量周期,解决了LEMI-025变差计与POS-1标量磁强计(整个磁强计系统升级阶段)测量相互同步的问题。在LEMI-025磁强计测试模式下,获得了新的数据阵列。利用巴特利特方法和谱谐波平均法,估计了地磁平静日磁力计的噪声水平。对两种方法定期在天文台进行的地磁场分量绝对测量结果进行了分析,并估计了LEMI-025磁力计的基线值。对用pos1型标量磁强计直接测量得到的地磁场强度记录和由LEMI-025变差计基线调整分量计算得到的地磁场强度记录进行了对比分析。利用获得的基线值和总场差信号,证实了新变差仪具有较高的标定精度,并估计了其敏感轴在地理坐标系中的定位误差。结论。我们的初步结果证实,新的LEMI-025变差计的特性符合INTERMAGNET的要求。LEMI-025传感器的定位误差不超过5角分。基线是相当稳定的。其所有分量在±2nt范围内均有色散,没有明显的时间漂移。LEMI-025变差仪的测试结果表明,AIA天文台测量馆内所有磁强计的特性在电磁兼容性方面应该是相互一致的。
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Upgrade of the Argentine Islands INTERMAGNET observatory at Akademik Vernadsky station, Antarctica
The article describes the main features of upgrading the magnetometric complex based on the LEMI-025 variometer in January-April 2019 at the geomagnetic observatory (code AIA) of the Ukrainian Antarctic Akademik Vernadsky station. The observatory’s old magnetometric complex consisted of two LEMI-008 (No. 02 and No. 16) variometers and one POS-1 scalar magnetometer. The measurements of LEMI-008 and POS-1 were not mutually synchronized and this was one of the main problem. Every measuring instrument taken individually as a component of the whole magnetometric complex had good individual properties. However, in general, the complex as an entire system had reduced performance, mainly due to the lack of mutual synchronization of measurements. Some preliminary test results are also presented. Main objective. One of the main task of upgrading the AIA observatory was to install a new variometer that is compatible with the requirements of the 1-second INTERMAGNET data standard. For two decades, old LEMI-008 variometers at Akademik Vernadsky station have shown high baseline stability, which meets INTERMAGNET requirements. Unfortunately, the noise characteristics of old variometers, the accuracy of synchronization with UTC, and the resolution do not longer meet the current INTERMAGNET requirements for devices that produce 1-second data. Measurements of LEMI-008 variometers and POS-1 scalar magnetometer were not mutually  synchronized. Due to lack of reliable mutual synchronization, the differences between the field vector modules, calculated indirectly from the variometer measurements and measured directly with the scalar magnetometer, varied and could be unreliable. With strong geomagnetic disturbances, this reduced the overall accuracy of the magnetometric complex as an integral measuring system, although the complex consisted of high-precision instruments. Only one of LEMI-008 variometers was equipped with GPS synchronization. This made data processing difficult. Therefore, one of the crucial upgrading tasks was creation of a system for mutual synchronization of measurements provided by the variometer LEMI-025 and the scalar magnetometer POS-1 with an accuracy of approximately 0.1 s (but not worse than 1 s) using control computer. Methods. The problem of mutual synchronization of the measurements of the LEMI-025 variometer and the POS-1 scalar magnetometer (at the stage of upgrading the magnetometric complex as a whole system) was solved using a control computer by periodical adjusting the POS-1 clock and starting its measurement cycles with a given timing advance. New data arrays were obtained while the LEMI-025 magnetometer was operated in test mode. Using the Bartlett’s method and spectral harmonics averaging, the noise level of the magnetometers during a geomagnetically quiet day was estimated. The results of absolute measurements of the geomagnetic field components, regularly carried out in the observatory by two methods, were analyzed and the baselines values of the LEMI-025 magnetometer were estimated. The comparative analysis of the records of the Earth magnetic field intensity, obtained by direct measurements with a scalar magnetometer POS-1 and calculated from the baseline-adjusted components of the LEMI-025 variometer, was performed. Using the obtained baseline values and the total field difference signals the high calibration accuracy of the new variometer was confirmed and the orientation errors of its sensitivity axes in the geographical coordinate frame were estimated. Conclusions. Our preliminary results confirm that the characteristics of new LEMI-025 variometer meet the INTERMAGNET requirements. The orientation errors of LEMI-025 sensor do not exceed 5 arc minutes. The base line is quite stable. All its components have dispersion within ±2 nT, without pronounced temporal drift. The test results of LEMI-025 variometer showed that the characteristics of all magnetometric instruments in the measuring pavilion of the AIA observatory should be mutually agreed in terms of electromagnetic compatibility.
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