Random Forest Modeling of Soil Properties in Saline Semi-Arid Areas
Моделирование свойств почв методом случайного леса в солонцовых полусухих районах
2023-04-28
SCID: 54.1/ktduqncd
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Random ForestTrans-Ural semi-arid (steppe) zoneremote sensing data (RSD)soil organic carbon (SOC)soil salinity (dry residue)
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Abstract (AI)
The problem of salinization/spreading of saline soils is becoming more urgent in many regions of the world, especially in context of climate change. The monitoring of salt-affected soils’ properties is a necessary procedure in land management and irrigation planning and is aimed to obtain high crop harvest and reduce degradation processes. In this work, a machine learning method was applied for modeling of the spatial distribution of topsoil (0–20 cm) properties—in particular: soil organic carbon (SOC), pH, and salt content (dry residue). A random forest (RF) machine learning approach was used in combination with environmental variables to predict soil properties in a semi-arid area (Trans-Ural steppe zone). Soil, salinity, and texture maps; topography attributes; and remote sensing data (RSD) were used as predictors. The coefficient of determination (R2) and the root mean square error (RMSE) were used to estimate the performance of the RF model. The cross-validation result showed that the RF model achieved an R2 of 0.59 and an RMSE of 0.68 for SOM; 0.36 and 0.65, respectively, for soil pH; and 0.78 and 1.21, respectively for dry residue prediction. The SOC content ranged from 0.8 to 2.8%, with an average value of 1.9%; soil pH ranged from 5.9 to 8.4, with an average of 7.2; dry residue varied greatly from 0.04 to 16.8%, with an average value of 1.3%. A variable importance analysis indicated that remote sensing variables (salinity indices and NDVI) were dominant in the spatial prediction of soil parameters. The importance of RSD for evaluating saline soils and their properties is explained by their absorption characteristics/reflectivity in the visible and near-infrared spectra. Solonchak soils are distinguished by a salt crust on the land surface and, as a result, reduced SOC contents and vegetation biomass. However, the change in saline and non-saline soils over a short distance with mosaic structure of soil cover requires high-resolution RSD or aerial images obtained from unmanned aerial vehicle/drones for successful digital mapping of soil parameters. The presented results provide an effective method to estimate soil properties in saline landscapes for further land management/reclamation planning of degraded soils in arid and semi-arid regions.
Key Findings
1
Cross-validation performance: RF achieved R2=0.36 and RMSE=0.65 for soil pH.
2
Cross-validation performance: RF achieved R2=0.59 and RMSE=0.68 for soil organic matter (SOC).
3
Cross-validation performance: RF achieved R2=0.78 and RMSE=1.21 for dry residue (salt content) prediction.
4
High-resolution remote sensing or UAV/aerial imagery is required to map mosaic saline/non-saline soil patterns accurately for digital soil mapping and reclamation planning.
5
Measured ranges and averages: SOC 0.8–2.8% (avg 1.9%), pH 5.9–8.4 (avg 7.2), dry residue 0.04–16.8% (avg 1.3%).
6
Random Forest (RF) models using environmental predictors can spatially predict topsoil (0–20 cm) properties (SOC, pH, dry residue) in a semi-arid Trans-Ural steppe zone.
7
Remote sensing data are effective for evaluating saline soils due to their visible and near-infrared reflectivity/absorption characteristics.
8
Solonchak (salt-crusted) soils have reduced SOC and vegetation biomass compared with non-saline soils.
9
Variable importance analysis showed remote sensing variables (salinity indices and NDVI) were dominant predictors for soil parameter spatial prediction.
Research Object
Topsoil (0–20 cm) in saline semi-arid areas (Trans-Ural steppe zone) including solonchak soils
Research Subject
Spatial distribution and prediction of topsoil properties—soil organic carbon (SOC), pH, and salt content (dry residue)—modeled using Random Forest with environmental and remote sensing predictors
Publication Details
Publication Date
2023-04-28
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