Modeling and analysis of gravity and gravity gradient based on terrain anomaly

Yuanwei Guo, Ling Xiong, Xiang Cheng
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引用次数: 2

Abstract

Gravity map or gravity gradient map is one of three elements of aided navigation based on the gravity field. The characteristics of the gravity map or gravity gradient map is one of the keys to gravity field aided navigation. In this paper, the integral range is determined under the condition of guaranteeing accuracy, the gravity map and gravity gradient map are calculated by the terrain anomaly body, and the statistical characteristics of gravity map and gravity gradient map at different grid spacing are analyzed. The simulation results show that the gravity gradient contains more high frequency information, and the gravity map contains more low frequency information in the same grid spacing. When the grid spacing is 50m, 100m and 200m, the variation of the standard deviation of gravity gradient is less than 1E, when the spacing is 400m, the variation of the standard deviation of gravity gradient is greater than 1E. If the accuracy of gravity gradiometer is less than 1E, the accuracy of navigation by gravity gradient under this terrain is less than 200m. When the grid spacing is 50m, 100m, 200m, 400m, the change of gravity standard deviation is less than 0.2mGal. If the accuracy of the gravimeter is less than 0.2mGal, the accuracy of navigation by gravity under this terrain is less than 400m.
基于地形异常的重力和重力梯度建模与分析
重力图或重力梯度图是基于重力场的辅助导航的三大要素之一。重力场图或重力梯度图的特征是实现重力场辅助导航的关键之一。本文在保证精度的条件下确定积分范围,利用地形异常体计算重力图和重力梯度图,分析了不同网格间距下重力图和重力梯度图的统计特征。仿真结果表明,在相同的网格间距下,重力梯度包含更多的高频信息,重力图包含更多的低频信息。当栅格间距为50m、100m、200m时,重力梯度标准差变化小于1E,当栅格间距为400m时,重力梯度标准差变化大于1E。若重力梯度仪精度小于1E,则该地形下重力梯度导航精度小于200m。网格间距为50m、100m、200m、400m时,重力标准差变化小于0.2mGal。如果重力仪的精度小于0.2mGal,则该地形下重力导航的精度小于400m。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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