Gravitational field rapid forward modeling method and inversion method based on Toplite kernel matrix
A technology of kernel matrix and gravity field, applied in the field of fast forward modeling method and inversion of gravity field
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Embodiment 1
[0119] This embodiment uses a lunar spherical shell forward model to verify the correctness and efficiency of the method proposed by the present invention, because only the spherical shell model has an analytical solution. The thickness of the spherical shell is 100km, the initial range is 1638 to 1738km (that is, the actual radius of the moon), and the spherical shell density is set to 1000kg / m 3 , the observation surface is a spherical surface at a height of 10km from the outer spherical shell, and the spherical shell is divided into 10 sections in the radial direction, with an interval of 10km. The interval between the longitude and latitude is 0.5° to 10°, and the relationship between the maximum relative error and the calculation time and the subdivision interval is calculated.
[0120] The relationship between the maximum relative error and the subdivision interval is as follows: image 3 As shown, the relationship between the relative calculation time and the subdivisi...
Embodiment 2
[0125] In order to further prove the validity and efficiency of the fast forward modeling method of the spherical coordinate system gravity field based on the Toplitze matrix frequency-domain FFT algorithm proposed in the application of the present invention, the following example provides an actual data inversion case, and the proposed The method is applied to the global-scale three-dimensional density imaging research of the moon, the details are as follows:
[0126] The global terrain of the moon is obtained by solving the latest lunar terrain spherical harmonic model LRO_LTM05_2050, such as Figure 5 Shown in (a).
[0127] The present invention uses the latest lunar gravity field model GL1500E to calculate free air gravity anomalies, such as Figure 5 As shown in (b), the terrain correction result is as follows Figure 5 Shown in (c). Boog Gravity Anomaly via Free Air Gravity Anomaly ( Figure 5 Middle (b)) minus the terrain correction ( Figure 5 In (c)) get, such as...
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