用于重力梯度仪标校的引力产生装置轨迹优化方法

本文主要讨论一种利用引力产生装置轨迹的移动进行引力梯度测试、标定和校准的方法。首先研究了引力产生装置对重力梯度测量系统的作用力影响,给出旋转式重力梯度仪的测量原理,推导了引力产生装置在重力梯度仪测量系统中的引力梯度信号输出表达式。文中设定了引力梯度测试参数,比较引力产生装置在空间中的不同位置移动区域产生的引力梯度信号的输出变化范围,确定引力产生装置的最佳轨迹。最后对重力梯度的测试标校方法作进一步分析。     

旋转式重力梯度仪自身梯度补偿研究

重力梯度仪安装在惯性稳定平台上,忽略载体姿态角改变等条件下的影响,在空间上保持方向不变,因此载体相对于重力梯度仪的旋转会改变其周围空间的质量分布,从而引起自身梯度的变化.这种自身梯度变化影响了重力梯度仪的测量精度,是动基座重力梯度测量误差的重要来源.由于周围环境物体到重力梯度仪的距离很近,采用基于中心引力梯度的方法计算自身梯度具有较大误差.推导了基于加速度计输出的重力梯度仪自身梯度补偿方法.仿真结果表明通过基于中心引力梯度的方法和基于加速度计输出的方法分别计算单位质量的质量点产生的自身梯度时,0.3m位置处自身梯度补偿的偏差超过5E,采用基于加速度计输出的方法进行自身梯度补偿更加精确.     

基于动基座重力梯度仪的导弹主动段飞行状态估计

弹道导弹主动段由于惯导系统工具误差和扰动引力的影响,使得导弹关机点状态参数偏离标准关机状态参数,大大影响了导弹的命中精度.为此,提出了基于动基座重力梯度仪的导弹主动段飞行状态估计方案,利用动基座重力梯度仪测得的导弹实际位置引力梯度信息,采用卡尔曼滤波方法,修正导弹当前的飞行状态.通过初步仿真,证明该方法理论上是可行的.     

基于旋转加速度计原理的重力梯度测量 技术研究与试验

旋转加速度计式重力梯度测量方法通过旋转调制的方式提取微弱的重力梯度信息。首先从测量原理出发,指出实现该方案的主要难点及对策,提炼出关键技术;其次,以多种方式开展引力梯度效应试验,验证了理论的正确性;最后,尝试了面向载体应用的动态适应性试验,达到地面低动态条件下的技术要求,为开展高动态条件下的重力梯度测量奠定基础。     

重力异常特征提取方法研究

将主元分析和独立分量分析相结合应用于重力异常信号的特征提取.采用主元分析对测量数据进行去相关和降维预处理,再利用独立分量分析算法提取重力信号的特征系数.结合重力异常变化与特征系数的关系,提出了应用特征量化参数表征重力异常信号变化程度的方法.基于实测的重力异常信号进行了仿真试验,试验结果表明,本文提出的特征量化参数能有效的反映重力异常的幅值变化程度.     

量子重力梯度仪研究进展

重力梯度是重力位的二阶微分,对地球密度扰动具有更高的分辨率,能够更加精细、全面地反映重力位在空间上的变化。高精度重力梯度测量在地质调查、地球重力场测绘、惯性导航以及基础科学研究等方面发挥着重要作用。量子重力梯度仪是近年来快速发展的一种基于激光操控原子技术的新型高精度重力梯度测量设备,具有测量精度高、长期稳定性好等特点,尤其是对振动噪声具有良好的抑制效果。目前,量子重力梯度仪的最佳灵敏度可达4E/√Hz,与最先进的旋转加速度计式重力梯度仪灵敏度3E/√Hz的水平相当。本文介绍了量子重力梯度仪的基本原理和应用,并分析了其国内外研究现状,最后讨论了目前限制量子重力梯度仪灵敏度的主要因素以及未来发展方向。     

超导重力仪器:机遇与挑战

超导重力仪器是利用超导电性构建的精密相对重力测量仪器，其工作于4.2K液氦温度，具有仪器固有噪声低、稳定性好的特点。阐述了超导重力仪和超导重力梯度仪两种仪器的工作原理与技术特征，简要介绍了作者所在课题组超导重力仪器研制的进展情况。分析了我国资源勘查用航空超导重力梯度仪研制所面临的机遇与挑战，提出了应对技术挑战的策略方法。     

一种基于试验数据的发动机特性曲线拟合

准确的发动机特性曲线是其性能计算的基础。文章讨论了多种情况的特性曲线插值方法:在工作点位置区间内,对小数据情况引入了新的插值方法；多数据时,采用三次样条插值方法进行插值；在工作点位置区间外,数据较多时,基于最小二乘法进行不同工作点的拟合；当工作点位置数据较少,利用新的插值方法在区间内引入虚拟工作点增加数据点,后按照数据较多的情况处理。所得结果与实际数值比较,精度较高,具有一定的参考价值。     

一种新型的航空重力梯度测量数据调平方法

航空重力梯度测量的原始数据包含与测线方向呈强相关性的条带状噪声，该噪声会影响后续数据处理与解释的精度。首先，提出了一种针对重力梯度数据组合调平的方法，旨在去除条带状噪声的干扰。与低通滤波相比，组合调平可以保留更多的异常场细节。与传统的切割线调平相比，组合调平对切割线的依赖更小，可以适用于切割线稀疏的测量地区。最后，以加拿大Diavik地区的实测航空重力梯度数据为例，验证了组合调平方法的应用效果。     

捷联式航空重力测量系统的数据处理方法比较与分析

重力数据处理对获取高精度重力异常值有着重要作用，是重力测量的核心技术。重力仪在搭载运动载体进行重力测量时，载体的高频振动对重力测量数据和GPS数据均会产生不可避免的干扰，导致提取的重力异常粗值含有大量高频噪声。围绕重力数据的处理方法这一核心技术，介绍了FIR低通滤波、零相移滤波、标准Kalman滤波、正反Kalman滤波4种滤波方法的基本原理，运用这4种方法处理了SAG捷联式重力仪的某次实际飞行测量数据，比对了基于SINS/GPS组合导航和SINS/DGPS组合导航的重力测量数据处理结果。通过对本次试验重复测线内符合精度进行比对，验证了4种方法的可行性和优劣性，同时验证了SAG重力仪的测量精度。     

基于强跟踪UPF的重力梯度辅助定位方法

针对重力梯度辅助定位中,存在重力梯度的强非线性分布及系统模型偏差等问题,将STUPF引入匹配定位过程。该方法根据残差信息实时调节系统状态跟踪能力,有效应对模型偏差对定位的影响。基于真实INS数据的仿真实验结果表明,STUPF可达到较好的定位效果,且与标准PF、GPF算法相比,其在定位的精度、稳定性及运算量上具有一定优势。     

The Juno Gravity Science Instrument

The Juno mission’s primary science objectives include the investigation of Jupiter interior structure via the determination of its gravitational field. Juno will provide more accurate determination of Jupiter’s gravity harmonics that will provide new constraints on interior structure models. Juno will also measure the gravitational response from tides raised on Jupiter by Galilean satellites. This is accomplished by utilizing Gravity Science instrumentation to support measurements of the Doppler shift of the Juno radio signal by NASA’s Deep Space Network at two radio frequencies. The Doppler data measure the changes in the spacecraft velocity in the direction to Earth caused by the Jupiter gravity field. Doppler measurements at X-band (\(\sim 8\) GHz) are supported by the spacecraft telecommunications subsystem for command and telemetry and are used for spacecraft navigation as well as Gravity Science. The spacecraft also includes a Ka-band (\(\sim 32\) GHz) translator and amplifier specifically for the Gravity Science investigation contributed by the Italian Space Agency. The use of two radio frequencies allows for improved accuracy by removal of noise due to charged particles along the radio signal path.     

Global Gravity Field Recovery Using Solely GPS Tracking and Accelerometer Data from Champ

A new long-wavelength global gravity field model, called EIGEN-1, has been derived in a joint German-French effort from orbit perturbations of the CHAMP satellite, exploiting CHAMP-GPS satellite-to-satellite tracking and on-board accelerometer data over a three months time span. For the first time it becomes possible to recover the gravity field from one satellite only. Thanks to CHAMP'S tailored orbit characteristics and dedicated instrumentation, providing continuous tracking and on-orbit measurements of non-gravitational satellite accelerations, the three months CHAMP-only solution provides the geoid and gravity with an accuracy of 20 cm and 1 mgal, respectively, at a half wavelength resolution of 550 km, which is already an improvement by a factor of two compared to any pre-CHAMP satellite-only gravity field model. This revised version was published online in August 2006 with corrections to the Cover Date.     

Possible Future Use of Laser Gravity Gradiometers

With the GRACE mission under way and the GOCE mission well along in the design process, detailed questions concerning the type of future mission that may follow them have arisen. It is generally agreed that determining the time variations in the Earth's gravity field with as high spatial and temporal resolution as is feasible will be the main driver for such a mission. The possible use of laser heterodyne measurements between separate satellites in such a mission has been discussed by a number of people. The first suggestion of emphasizing time variation measurements in a laser mission was the TIDES concept presented in 1992 by Colombo and Chao. Then, in 2000, a GRACE Follow-On mission using laser measurements between two drag-free satellites was discussed by Watkins el al. (2000). More recently, the possibility of utilizing laser measurements between more than two satellites in order to determine two or more components of the gravity gradient tensor simultaneously has been proposed by Balmino. This approach may be desirable in order to reduce the aliasing of time variations between geopotential terms of different degree and order, as well as to improve the resolution in longitude, despite the cost of the additional satellites. In this paper, we discuss specific possible mission geometries for measuring the two diagonal in-plane components of the gravity gradient tensor simultaneously. This could be done, for example, by laser heterodyne measurements between two pairs of satellites in coplanar and nearly polar orbits. This revised version was published online in August 2006 with corrections to the Cover Date.     

三轴惯性平台式航空重力仪机载重力测量试验研究

介绍了自主研制的GIPS-1A三轴惯性平台式航空重力仪的组成、工作流程及技术指标,并给出了机载重力测量试验系统的集成方法和数据处理方法.经实际机载航空重力重复线精度测试和试生产测试,重复线内符合精度优于0.6mGal@0.01Hz;与国际上性能优异的GT-2A重力仪相比,重复线符合度好,试生产交叉点总精度相当,且异常形...     

弹道导弹制导计算中扰动引力的快速赋值

主动段扰动引力是引起弹道导弹制导方法误差的主要因素。因此,要提高导弹的制导精度,就必须能够在弹上实时计算扰动引力。但现有方法在计算快速性和存储量之间无法得到有效协调。为此,把广义延拓逼近思想引入有限元逼近方法中,将插值单元周围节点的信息也包含到单元内一点扰动引力的计算当中,建立了一种新的数学模型。对所选发射空域,在发射坐标系中进行了直角坐标划分。计算结果表明,这种方法能够更加精确地逼近弹道导弹主动段的扰动引力,在600 km×250 km×6 km的主动段飞行区域内,只需要保存60个节点数据,就能使由逼近误差导致的落点偏差小于10 m,是一般有限元逼近方法精度的4倍以上。     

Gravity modeling in aerospace applications

The science of inertial navigation has evolved to the point that the traditional gravity model is a principal error source in advanced, precise systems. Specifically, the unmodeled vertical deflections of the earth's gravitational field are a major contributor to CEP (circular error probable) divergence in precise terrestrial inertial navigation systems (INS). Over the years, several studies have been undertaken to the development of advanced techniques for accurate, real-time compensation of gravity disturbance vectors. More complex on-board gravity models which compute vertical deflection components will reduce the CEP divergence rate, but imperfect modeling due to on-board processing limitations will still cause residual vertical deflection errors. In order to eliminate or reduce gravity-induced errors in the INS requires measurement of gravity disturbance values and in-flight compensation to the inertial navigator. It is assumed in this paper that gravity disturbance values have been measured prior to the airborne mission and various techniques for compensation are to be considered. As part of a screening process in this study, several gravity compensation techniques (both deterministic and stochastic models) were investigated. The screening process involved identification of gravity models and algorithms, and developments of selection criteria for subsequent screening of the candidates.