Spatiotemporal Characteristics of the Mud Receiving Area Were Retrieved by InSAR and Interpolation
Abstract
:1. Introduction
2. Materials and Methods
2.1. Study Area
2.2. Analysis Method
2.2.1. Differential Radar Interferometry (D-InSAR) and TS-InSAR
2.2.2. Analysis of Variance for Randomized Block Design
2.2.3. Interpolation and Optimization
3. Results and Analyse
3.1. D-InSAR Spatial and Temporal Analysis of Sludge Area
3.2. Inversion of Seawall Road Settlement Using TS-InSAR
3.3. Integration Feasibility Assessment
3.4. Optimization and Interpolation
4. Discussion
5. Conclusions
- The dredging operation process of the channel should be reasonably standardized to avoid the occurrence of uneven accumulation, and the increase in sediment mobility will lead to the degradation of the surrounding land and the flooding of flooding.
- Areas close to water are favorable locations for urban development, and the risk of mud areas increases the possibility of flooding, thereby causing disasters to surrounding fields and villages [50], and waterproofing projects such as rivers can be built according to demand.
- Disaster assessment should be done in a timely manner for road sections with too fast road subsidence [51], such as coastal disaster vulnerability and social vulnerability index.
Author Contributions
Funding
Data Availability Statement
Acknowledgments
Conflicts of Interest
References
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Project | The Control Value of the Vertical Displacement | ||||
---|---|---|---|---|---|
Absolute Value (mm) | Rate of Change (mm/Month) | Cumulative Value/mm | |||
Earthen embankment | 10 10 | ±10 ±10 | ±10 ±10 | ||
HaiDi road | 10 | ±10 | ±10 | ||
Level | I | II | III | IV | V |
Sedimentation rate (mm/a) | 0–10 | 10–15 | 15–20 | 20–25 | >25 |
Degree grading | slight | average | severe | More severe | Extremely serious |
Level Measurement Time | Master Image | Slave Image | Imagery Parameters | Time Baseline /d | Spatial Baseline/m |
---|---|---|---|---|---|
20210810 | 20210806 | 20211017 | File type: SLC Polarization: VV Beam Mode: IW (TOPS mode) Direction: Ascending Subtype: SA Angle of incidence 21° | 72 | −19.580 |
20211017 | 20211017 | 20211204 | 48 | 41.365 | |
20211208 | 20211204 | 20211228 | 24 | 26.748 | |
20211226 | 20211228 | 20220121 | 24 | 12.218 | |
20220122 | 20220121 | 20220202 | 12 | 56.617 | |
20220204 | 20220202 | 20220226 | 24 | −139.093 | |
20220225 | 20220226 | 20220310 | 12 | 17.996 | |
20220309 | 20220310 | 20220403 | 24 | −55.028 | |
20220403 | 20220403 | 20220509 | 36 | 76.386 |
Dependent Variable: Settlement | |||||
---|---|---|---|---|---|
The Source | Class III Sum of Squares | Degrees of Freedom | The Mean Square | F | Significant |
Correction model | 28.722 | 6 | 4.787 | 4.972 | 0.021 |
intercept | 129.948 | 1 | 129.948 | 134.969 | 0.000 |
Point | 28.219 | 4 | 7.055 | 7.327 | 0.009 |
Method | 0.502 | 2 | 0.251 | 0.261 | 0.777 |
error | 7.702 | 8 | 0.963 | ||
total | 166.373 | 15 | |||
Total after correction | 36.424 | 14 |
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Hu, B.; Qiao, Z. Spatiotemporal Characteristics of the Mud Receiving Area Were Retrieved by InSAR and Interpolation. Remote Sens. 2023, 15, 351. https://doi.org/10.3390/rs15020351
Hu B, Qiao Z. Spatiotemporal Characteristics of the Mud Receiving Area Were Retrieved by InSAR and Interpolation. Remote Sensing. 2023; 15(2):351. https://doi.org/10.3390/rs15020351
Chicago/Turabian StyleHu, Bo, and Zhongya Qiao. 2023. "Spatiotemporal Characteristics of the Mud Receiving Area Were Retrieved by InSAR and Interpolation" Remote Sensing 15, no. 2: 351. https://doi.org/10.3390/rs15020351