探测和考虑相对潮汐重力仪漂移

Q4 Earth and Planetary Sciences
E.A. Chistiakova
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引用次数: 0

摘要

在进行任何测量之前,必须对设备进行彻底研究。相对潮汐重力仪是一种复杂的技术装置;它们能够以高精度(1μGal)测量重力时间变化。系统误差的主要来源是仪器漂移。每个单元的漂移值和非线性是单独的。有很多考虑的方法;他们依赖物质和技术机会。最简单且资源消耗较少的算法是使用分段线性近似技术将漂移考虑在内。本研究涉及使用指定方法评估gPhoneX#117(Micro-g LaCoste,USA)潮汐重力仪仪器漂移的准确性。为此,通过一阶多项式和二阶多项式的近似获得漂移,并与参考(绝对)观测结果进行比较。结果表明,分段线性近似方法只能用于拒绝质量较差的测量。建议通过将测量值与定期绝对监测的数据进行比较来识别、控制和核算仪器漂移。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Detecting and considering a relative tidal gravimeter drift
Thorough study of the equipment is essential before any measurements are made. Relative tidal gravimeters are complex technical devices; they enable measuring gravity time variations with high accuracy (1 μGal). The main source of systematic errors is their instrumental drift. Value and nonlinearity of the drift for each unit is individual. There are plenty of considering methods; they depend on material and technical opportunities. The simplest and less resource-consuming algorithm is to take the drift into account using the piecewise linear approximation technique. This research deals with assessing the accuracy of accounting the instrumental drift of the gPhoneX#117 (Micro-g LaCoste, USA) tidal gravimeter using the specified means. For this purpose, the drift was obtained through approximation by polynomials of the first and second degree was estimated in comparison with the results of reference (absolute) observations. It is concluded that the method of piecewise linear approximation can only be used for rejecting poor quality measurements. It is recommended to identify, control and accounting the instrumental drift by comparing measurements with the data of regular absolute monitoring.
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来源期刊
Geodeziya i Kartografiya
Geodeziya i Kartografiya Earth and Planetary Sciences-Earth-Surface Processes
CiteScore
0.60
自引率
0.00%
发文量
73
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