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作 者:赵永芬[1] 黄蔚北[1] 赵学敏[1] 程安龙[1] 周锦屏[1]
机构地区:[1]国家地震局地球物理研究所
出 处:《地震地磁观测与研究》1997年第6期80-84,共5页Seismological and Geomagnetic Observation and Research
基 金:地震科学基金会
摘 要:精密测定地磁台观测室内的墩位差,它对于统一标准、仪器比较、验收仪器,实现观测工作正常化,标准化至关重要。地磁组于1993~1996年在北京台3#与5#观测墩上,连续4年使用G856质子旋进式磁力仪测定地磁总强度F21次,笔者对774个数据进行了统计,其结果是,3#与5#墩之差值ΔFB(3-5)=-3.57nT,标准偏差SF=±0.45nT。并对墩差的测量方法、复测次数、以及数列与数据组的选择进行了有益的讨论。It is very important accurately to determine the geomagnetic field difference at different piers in the absolute observation house at a geomagnetic observatory. It will help us to establish a standard, to make instrumental comparison, to check new instrument before acceptance, and even more to bring about normalization and standardization in observation works. The measurement of geomagnetic total intensity F was made 21 times from the year 1993 to the year 1996 at the piers No.3 and No.5 in the absolute observation house at Beijing Geomagnetic Observatory with the proton precession magnetometer of G856 by the Technological Leading Group of the Chinese Geomagnetic Observatory Network. The statistical analysis on the 774 data points revealed that the geomagnetic field difference at the two piers is Δ F B (3-5) =-3.57 nT with the standard deviation of S F =±0.45 nT. More useful discussion was made on the observation method and on how many times to measure and how to choose the useful data points.
分 类 号:P318.6[天文地球—固体地球物理学]
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