| Literature DB >> 31974439 |
Fumin Lu1, Huaien Zeng2.
Abstract
Nonlinear exponential trend model is linearized into the linear model, then linearized model parameters are regarded as the state vector containing the dynamic noise to erect Kalman filter model based on exponential trend model to predict the deformation of the rock landslide. Deformation observation values of the landslide are regarded as a time series to erect AR(1) model, then model parameters of AR(1) model are regarded as the state vector containing the dynamic noise to erect Kalman filter model based on AR(1) model to predict the deformation of the rock landslide. The deformation of the landslide is regarded as the function of the time, then Taylor series is used to determine the functional relationship between the deformation of the landslide and the time, and Taylor series is spread to erect Kalman filter model based on Taylor series to predict the deformation of the earthy landslide. The deformation of landslides relates to many factors, the rainfall and the temperature influence the deformation of landslides specially, thus Kalman filter model based on multiple factors is erect to predict the deformation of the earthy landslide on the basis of Taylor series. Numerical examples show that the fitting errors and the forecast errors of the four Kalman filter models are little.Entities:
Year: 2020 PMID: 31974439 PMCID: PMC6978391 DOI: 10.1038/s41598-020-57881-3
Source DB: PubMed Journal: Sci Rep ISSN: 2045-2322 Impact factor: 4.379
Horizontal displacement observation values and their filter values of the monitoring point FA.
| Observation time (year-month) | Observation value (mm) | Exponential trend model | Kalman filter model | ||
|---|---|---|---|---|---|
| Fitted value (mm) | Residual (mm) | Fitted value (mm) | Residual (mm) | ||
| 2007–12 | 10.32 | 20.45 | 10.13 | 13.45 | 3.13 |
| 2008–12 | 26.96 | 23.26 | −3.70 | 25.60 | −1.36 |
| 2009–12 | 34.07 | 26.45 | −7.62 | 34.43 | 0.36 |
| 2010–12 | 38.65 | 30.08 | −8.57 | 39.17 | 0.52 |
| 2011–12 | 42.98 | 34.21 | −8.77 | 43.32 | 0.34 |
| 2012–12 | 44.93 | 38.90 | −6.03 | 45.20 | 0.27 |
| 2013–12 | 47.16 | 44.24 | −2.92 | 47.33 | 0.17 |
| 2014–12 | 48.38 | 50.31 | 1.93 | 48.52 | 0.14 |
| 2015–12 | 49.95 | 57.22 | 7.27 | 50.04 | 0.09 |
| 2016–12 | 51.75 | 65.07 | 13.32 | 51.82 | 0.07 |
Vertical displacement observation values and their filter values of the monitoring point P10.
| Observation time (year-month) | Observation value (mm) | AR(1) model | Kalman filter model | ||
|---|---|---|---|---|---|
| Fitted value (mm) | Residual (mm) | Fitted value (mm) | Residual (mm) | ||
| 2016–01 | 36.4 | 35.21 | −1.19 | 36.29 | −0.11 |
| 2016–02 | 37.2 | 36.43 | −0.77 | 37.27 | 0.07 |
| 2016–03 | 37.6 | 37.32 | −0.28 | 37.60 | 0.00 |
| 2016–04 | 38.3 | 38.11 | −0.19 | 38.28 | −0.02 |
| 2016–05 | 38.5 | 38.61 | 0.11 | 38.50 | 0.00 |
| 2016–06 | 39.7 | 39.52 | −0.18 | 39.73 | 0.03 |
| 2016–07 | 40.2 | 40.33 | 0.13 | 40.21 | 0.01 |
| 2016–08 | 41.6 | 41.52 | −0.08 | 41.60 | 0.00 |
| 2016–09 | 42.0 | 42.17 | 0.17 | 42.02 | 0.02 |
| 2016–10 | 42.5 | 42.42 | −0.08 | 42.51 | 0.01 |
| 2016–11 | 42.9 | 43.18 | 0.28 | 42.92 | 0.02 |
| 2016–12 | 43.7 | 43.56 | −0.14 | 43.70 | 0.00 |
| 2017–01 | 43.9 | 43.99 | 0.09 | 43.89 | −0.01 |
| 2017–02 | 44.2 | 44.15 | −0.05 | 44.22 | 0.02 |
| 2017–03 | 44.6 | 44.69 | 0.09 | 44.57 | −0.03 |
| 2017–04 | 45.1 | 45.00 | −0.10 | 45.11 | 0.01 |
| 2017–05 | 45.9 | 45.28 | −0.62 | 45.91 | 0.01 |
| 2017–06 | 46.7 | 46.93 | 0.23 | 46.70 | 0.00 |
| 2017–07 | 48.0 | 47.11 | −0.89 | 48.03 | 0.03 |
| 2017–08 | 48.8 | 48.22 | −0.58 | 48.76 | −0.04 |
| 2017–09 | 49.2 | 49.33 | 0.13 | 49.21 | 0.01 |
| 2017–10 | 49.7 | 49.64 | −0.06 | 49.70 | 0.00 |
| 2017–11 | 50.3 | 50.77 | 0.47 | 50.28 | −0.02 |
Horizontal displacement observation values and their filter values of the monitoring point G8.
| Observation time (year-month-day) | Observation value (mm) | Fitted value (mm) | Residual (mm) |
|---|---|---|---|
| 2017–01–12 | 468.6 | 468.3 | −0.3 |
| 2017–02–20 | 471.5 | 471.3 | −0.2 |
| 2017–03–18 | 487.1 | 486.0 | −1.1 |
| 2017–04–18 | 498.9 | 499.3 | 0.4 |
| 2017–05–18 | 525.3 | 524.6 | −0.7 |
| 2017–06–16 | 551.3 | 551.1 | −0.2 |
| 2017–07–16 | 577.1 | 577.8 | 0.7 |
| 2017–08–17 | 594.3 | 595.6 | 1.3 |
| 2017–09–19 | 623.0 | 622.3 | −0.7 |
| 2017–10–17 | 624.3 | 625.2 | 0.9 |
| 2017–11–11 | 639.0 | 638.1 | −0.9 |
Horizontal displacement observation values and their filter values of the monitoring point H4.
| Observation time (year-month-day) | Rainfall of month (mm) | Temperature (°C) | Observation value (mm) | Residual 1 (mm) | Residual 2 (mm) |
|---|---|---|---|---|---|
| 2016–04–19 | 49.5 | 18.2 | 118.3 | 33.30 | 0.56 |
| 2016–05–19 | 173.0 | 24.6 | 128.2 | 19.48 | 0.07 |
| 2016–06–18 | 124.6 | 26.3 | 172.7 | 15.49 | −0.92 |
| 2016–07–20 | 187.9 | 30.4 | 228.4 | −22.21 | 0.84 |
| 2016–08–18 | 114.9 | 27.4 | 253.9 | −23.93 | 0.95 |
| 2016–09–21 | 121.4 | 24.1 | 259.7 | −29.09 | −0.02 |
| 2016–10–18 | 46.0 | 18.9 | 290.3 | −36.90 | −0.78 |
| 2016–11–18 | 49.3 | 13.8 | 294.6 | −35.41 | −0.21 |
| 2016–12–14 | 8.6 | 8.5 | 298.3 | −12.99 | −0.36 |
| 2017–01–15 | 6.6 | 7.2 | 296.0 | 6.49 | 0.81 |
| 2017–02–25 | 20.8 | 9.8 | 299.3 | 16.16 | −0.57 |
| 2017–03–19 | 40.5 | 14.4 | 298.0 | 24.22 | 0.99 |
| 2017–04–18 | 76.0 | 17.8 | 304.9 | 24.50 | 0.21 |
| 2017–05–16 | 129.4 | 22.8 | 310.9 | 27.60 | 0.75 |
| 2017–06–15 | 86.9 | 25.6 | 338.7 | 38.51 | −0.11 |
| 2017–07–14 | 162.6 | 29.5 | 364.4 | 19.57 | 0.75 |
| 2017–08–16 | 198.7 | 28.2 | 380.9 | −3.41 | 0.98 |
| 2017–09–07 | 44.3 | 25.8 | 438.8 | −11.28 | 0.87 |
| 2017–10–13 | 102.0 | 19.2 | 449.9 | −50.38 | −0.51 |
*Residual 1 is the residual of quadratic polynomial regression model, Residual 2 is the residual of Kalman filter model.