| Literature DB >> 35808540 |
Jing Li1, Lichen Su2, Fang Wang1, Kailong Li3, Lili Zhang1,4.
Abstract
In the field of high accuracy dual-axis rotational inertial navigation system (RINS), the calibration accuracy of the gyroscopes and accelerometers is of great importance. Although rotation modulation can suppress the navigation error caused by scale factor error and bias error in a static condition, it cannot suppress the scale factor errors thoroughly during the maneuvering process of the vehicle due to the two degrees of rotation freedom. The self-calibration method has been studied by many researchers. However, traditional calibration methods need several hours to converge, which is unable to meet the demand for quick response to positioning and orientation. To solve the above problems, we do the following work in this study: (1) we propose a 39-dimensional online calibration Kalman filtering (KF) model to estimate all calibration parameters; (2) Error relationship between calibration parameters error and navigation error are derived; (3) A backtracking filtering scheme is proposed to shorten the calibration process. Experimental results indicate that the proposed method can shorten the calibration process and improve the calibration accuracy simultaneously.Entities:
Keywords: Kalman filter; gradient descent; inertial measurement unit (IMU) calibration; strapdown inertial navigation system (SINS)
Year: 2022 PMID: 35808540 PMCID: PMC9269788 DOI: 10.3390/s22135036
Source DB: PubMed Journal: Sensors (Basel) ISSN: 1424-8220 Impact factor: 3.847
Figure 1The conversion relationship between the non-orthogonal coordinate frame of the gyro and the orthogonal coordinate frame of the IMU.
Error propagation form of self-calibration parameters under transposition excitation.
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Rotation path of self-calibration process.
| Time | Rotation Axis (Inner (I) ( | Rotation Angle along I/O Axis | Attitude after Rotation (XYZ) (East-North-Upward) |
|---|---|---|---|
| 0 s | - | - | ENU |
| 180 s | O | +90 | EUS |
| 270 s | O | +180 | EDN |
| 360 s | O | +180 | EUS |
| 450 s | I | +90 | UWS |
| 540 s | I | +180 | DES |
| 630 s | I | +180 | UWS |
| 720 s | O | +90 | SWD |
| 810 s | O | +180 | NWU |
| 900 s | O | +180 | SWD |
| 990 s | O | +90 | DWN |
| 1080 s | O | +90 | NWU |
| 1170 s | O | +90 | UWS |
| 1260 s | I | +90 | WDS |
| 1350 s | I | +90 | DES |
| 1440 s | I | +90 | EUS |
| 1530 s | O | +90 | ESD |
| 1620 s | O | +90 | EDN |
| 1710 s | O | +90 | ENU |
The observability degree of each state.
| State Variable | Singular Value | State Variable | Singular Value |
|---|---|---|---|
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| 232.6811 |
| 197.5225 |
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| 51.2133 |
| 43.6781 |
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| 30.7752 |
| 22.1765 |
Figure 2Diagram of self-calibration process based on backtracking scheme.
Figure 3Dual-axis RINS.
Figure 4Structure of the Dual-axis RINS.
Figure 5IMU raw data.
Figure 6Estimation curves of gyroscope and accelerometer bias errors.
Figure 7Estimation curves of gyroscope and accelerometer scale factor errros.
Figure 8Estimation curves of gyroscope and accelerometer installation angle errors.
Figure 9Estimation curves of inner lever arm and accelerometer quadratic coefficient errors.
Estimation results of different methods.
| Estimated Parameters | Proposed Method | Traditional Method | Reference Values |
|---|---|---|---|
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| −0.01345 | −0.03953 | −0.01955 |
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| 0.012587 | 0.04478 | 0.01685 |
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| 0.04521 | 0.1023 | 0.04002 |
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| 412.23 | 415.22 | 412.75 |
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| −812.36 | −813.56 | −813.74 |
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| 694.25 | 691.57 | 695.12 |
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| 206,263.25 | 206,269.44 | 206,263.25 |
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| 206,269.34 | 206,260.98 | 206,268.87 |
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| 206,267.22 | 206,268.74 | 206,267.84 |
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| 98,021.66 m/ | 98,020.97 m/ | 98,021.39 m/ |
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| 98,015.23 m/ | 98,019.37 m/ | 98,015.54 m/ |
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| 98,036.94 m/ | 98,031.52 m/ | 98,036.56 m/ |
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| 3.547′ | 4.125′ | 3.368′ |
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| −2.365′ | −3.122′ | −2.674′ |
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| 11.245′ | 11.544′ | 10.941′ |
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| 9.124′ | 9.426′ | 9.221′ |
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| 7.586′ | 7.138′ | 7.225′ |
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| 1.747′ | 1.529′ | 1.596′ |
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| −5.618′ | −5.221′ | −5.625′ |
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| 3.027′ | 3.291′ | 3.171′ |
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| 6.107′ | 5.822′ | 6.128′ |
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| −5.754 ppm | −7.225 ppm | −5.551 ppm |
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| 23.485 ppm | 29.569 ppm | 21.993 ppm |
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| 30.241 ppm | 27.226 ppm | 30.453 ppm |