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Experimental errors of measurements of vertical geomagnetic gradients in the stratosphere

机译:平流层垂直地磁梯度测量的实验误差

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摘要

The errors of measurements of vertical geomagnetic gradients at altitudes of 20-40 km, using a balloon magnetic gradiometer with a 6-km-long measuring base oriented along gravity, have been studied in the work. The errors related to the deviation of the measuring base position relative to the vertical have been studied during the real balloon flight with the help of the navigation GPS receivers. The deviations of the measuring base within 5 degrees, which can sometimes reach 15 degrees, have been obtained. This results in a decrease in the magnetic gradient measurement accuracy due to the errors introduced in the specification of the normal magnetic field used to detect magnetic anomalies. To eliminate this error, a GPS receiver was built in each magnetometer in order to observe magnetometers during synchronous measurements and to correct the measurements for the normal magnetic field. It has been indicated that the effect of deviations of the measuring base position on the results is not more than 2% of the measured value at such organization of a gradiometer.
机译:在工作中,研究了使用具有沿重力方向定位的6公里长的测量基座的气球式磁力梯度仪在20-40 km的高度上测量垂直地磁梯度的误差。在实际气球飞行过程中,借助导航GPS接收器研究了与测量基准位置相对于垂直方向的偏差有关的误差。已获得测量基准的偏差在5度以内,有时可以达到15度。由于用于检测磁异常的正常磁场规范中引入的误差,导致磁梯度测量精度下降。为了消除此错误,每个磁力计中都内置了GPS接收器,以便在同步测量期间观察磁力计并针对正常磁场校正测量值。已经表明,在这种梯度仪的结构上,测量基准位置的偏差对结果的影响不大于测量值的2%。

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