scholarly journals Scale Factor Calibration for a Rotating Accelerometer Gravity Gradiometer

Sensors ◽  
2018 ◽  
Vol 18 (12) ◽  
pp. 4386
Author(s):  
Zhongguang Deng ◽  
Chenyuan Hu ◽  
Xiangqing Huang ◽  
Wenjie Wu ◽  
Fangjing Hu ◽  
...  

Rotating Accelerometer Gravity Gradiometers (RAGGs) play a significant role in applications such as resource exploration and gravity aided navigation. Scale factor calibration is an essential procedure for RAGG instruments before being used. In this paper, we propose a calibration system for a gravity gradiometer to obtain the scale factor effectively, even when there are mass disturbance surroundings. In this system, four metal spring-based accelerometers with a good consistency are orthogonally assembled onto a rotary table to measure the spatial variation of the gravity gradient. By changing the approaching pattern of the reference gravity gradient excitation object, the calibration results are generated. Experimental results show that the proposed method can efficiently and repetitively detect a gravity gradient excitation mass weighing 260 kg within a range of 1.6 m and the scale factor of RAGG can be obtained as (5.4 ± 0.2) E/μV, which is consistent with the theoretical simulation. Error analyses reveal that the performance of the proposed calibration scheme is mainly limited by positioning error of the excitation and can be improved by applying higher accuracy position rails. Furthermore, the RAGG is expected to perform more efficiently and reliably in field tests in the future.

1985 ◽  
Vol GE-23 (4) ◽  
pp. 527-530 ◽  
Author(s):  
Werner Kahn ◽  
Friedrich Von Bun

Geophysics ◽  
1993 ◽  
Vol 58 (4) ◽  
pp. 508-514 ◽  
Author(s):  
Christopher Jekeli

The Gravity Gradiometer Survey System (GGSS) was designed to measure the local and regional gravity field from a ground or airborne moving platform. With the first and only airborne field test, the GGSS was able to recover five‐arcminute by five‐arcminute mean gravity anomalies to an accuracy of a few mGal. These results were obtained by flying the system, with an operational precision of about 10 Eötvös (ten‐second average), on a grid of orthogonal tracks spaced 5 km apart at an altitude of about 700 m above the terrain. Despite perpetual navigation problems with the Global Positioning System and several periods of excessive system noise, the results of a performance analysis on 19 out of 128 tracks demonstrated the potential accuracy and efficiency of the GGSS as an airborne gravity mapping system. The ground tests (both road and railway), suffering from undue vehicle vibrations and from a lack of ground truth data, were correspondingly less successful, but they also showed no surprises in the system corrupted by these adverse conditions. Unfortunately, the GGSS program has terminated; and it is appropriate to reflect on its accomplishments. Without going into technical details, this somewhat historical review summarizes the field tests, the data reduction algorithms, and the test results, which together portray the breadth of expertise the program engendered in the area of gravity gradiometry.


2018 ◽  
Vol 2018 ◽  
pp. 1-8
Author(s):  
Junhui Zhang ◽  
Yongsheng Yao ◽  
Jianlong Zheng ◽  
Xiangqun Huang ◽  
Tian Lan

To determine the degree of compaction of subgrades filled with fine-grained soil, the compaction test and light dynamic penetrometer (LDP) test were carried out for low liquid-limit clay samples with different water contents in laboratory. Then, a prediction equation of the penetration ratio (PR) defined as the depth per drop of the hammer of LDP, degree of compaction (K), and water content (ω) was built. After that, the existing fine-grained soil subgrades on LDP-based field tests were excavated. The on-site PR values, water contents, and degrees of compaction of slopes were obtained. The estimated degrees of compaction using the prediction equation were compared with measured values of the degree of compaction in field. The results show that there is good consistency between them, and an error within 3.5% was obtained. In addition, the water content should be determined firstly while using the prediction equation which is proposed in this study. Therefore, a numerical method of the water content of a subgrade was developed, and the predicted and measured water contents were compared, which shows a relatively high relativity. Then, the degree of compaction of fine-grained soil subgrades can be calculated according to the predicting equation, which involves the penetration ratio (PR) and the numerically calculated water content as input instead of the measured value in the field.


Geophysics ◽  
2016 ◽  
Vol 81 (4) ◽  
pp. G67-G79 ◽  
Author(s):  
Cericia Martinez ◽  
Yaoguo Li

The inherent relationship among different components of gravity gradiometer data requires applied processing to be consistent among the components. This restricts the applicability of some traditional potential-field processing techniques, but it highlights opportunities for methods uniquely suited for such data sets. The equivalent source technique is one such method. We have applied fast equivalent source construction to two aspects of gravity gradient data processing. First, we denoised multicomponent data and obtained estimates of the incoherent errors for the observations. Second, we have proposed a method that can be used to estimate errors associated with the denoised data. Through synthetic and field examples, we have evaluated the effectiveness of equivalent source processing for denoising and noise estimation.


Sensors ◽  
2018 ◽  
Vol 18 (4) ◽  
pp. 1247 ◽  
Author(s):  
Xiangqing Huang ◽  
Zhongguang Deng ◽  
Yafei Xie ◽  
Ji Fan ◽  
Chenyuan Hu ◽  
...  

Geophysics ◽  
2016 ◽  
Vol 81 (3) ◽  
pp. G49-G57 ◽  
Author(s):  
Carlos Cevallos

Rotating the gravity gradient tensor about a vertical axis by an appropriate angle allows one to express its components as functions of the curvatures of the equipotential surface. The description permits the identification of the gravity gradient tensor as the Newtonian tidal tensor and part of the tidal potential. The identification improves the understanding and interpretation of gravity gradient data. With the use of the plunge of the eigenvector associated with the largest eigenvalue or plunge of the main tidal force, it is possible to estimate the location and depth of buried gravity sources; this is developed in model data and applied to FALCON airborne gravity gradiometer data from the Canning Basin, Australia.


Geophysics ◽  
2013 ◽  
Vol 78 (4) ◽  
pp. G81-G88 ◽  
Author(s):  
Carlos Cevallos ◽  
Peter Kovac ◽  
Sharon J. Lowe

We apply equipotential surface curvatures to airborne gravity gradient data. The mean and differential curvature of the equipotential surface, the curvature of the gravity field line, the zero contour of the Gaussian curvature, and the shape index improve the understanding and geologic interpretation of gravity gradient data. Their use is illustrated in model data and applied to FALCON airborne gravity gradiometer data from the Canning Basin, Australia.


2009 ◽  
Vol 419-420 ◽  
pp. 221-224
Author(s):  
Lin Zhao ◽  
Feng Ming Liu ◽  
Hai Jing Yuan ◽  
Hong Bin Zhao

The design and manufacture for GGI are different and only several countries have the ability to produce it. Devising the feasible scheme for gravity gradiometer is the primary question.In this paper, a new type of GGI is designed using twelve accelerometers. First, the mathematical relationship between the accelerometer and GGI is derived and the method to separate the angular velocity and gravity gradient is disscussed. Second, the model of twelve-accelerometer gravity gradiometer is provided. Third, the estimation of angular velocity is analyzed when the GGI is installed in the form of strapdown or stabilized state. Finally, it is concluded that a new type of inertial navigation system using gravity gradiometers will be configured when it becomes possible to precisely measure gravity gradient.


1998 ◽  
Vol 81 (5) ◽  
pp. 971-974 ◽  
Author(s):  
M. Snadden ◽  
J. McGuirk ◽  
P. Bouyer ◽  
K. Haritos ◽  
M. Kasevich

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