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Digital mapping of soil physical and mechanical properties using machine learning at the watershed scale.
- Source :
- Journal of Mountain Science; Oct2023, Vol. 20 Issue 10, p2975-2992, 18p
- Publication Year :
- 2023
-
Abstract
- Knowledge about the spatial distribution of the soil physical and mechanical properties is crucial for soil management, water yield, and sustainability at the watershed scale; however, the lack of soil data hinders the application of this tool, thus urging the need to estimate soil properties and consequently, to perform the spatial distribution. This research attempted to examine the proficiency of three machine learning methods (RF: Random Forest; Cubist: Regression Tree; and SVM: Support Vector Machine) to predict soil physical and mechanical properties, saturated hydraulic conductivity (K<subscript>s</subscript>), Cohesion measured by fall-cone at the saturated (P<subscript>sat</subscript>) and dry (P<subscript>dry</subscript>) states, hardness index (HI) and dry shear strength (SS) by integrating environmental variables and soil features in the Zayandeh-Rood dam watershed, central Iran. To determine the best combination of input variables, three scenarios were examined as follows: scenario I, terrain attributes derivative from a digital elevation model (DEM) + remotely sensed data; scenario II, covariates of scenario I + selected climatic data and some thematic maps; scenario III, covariates in scenario II + intrinsic soil properties (Clay, Silt, Sand, bulk density (BD), soil organic matter (SOM), calcium carbonate equivalent (CCE), mean weight diameter (MWD) and geometric weight diameter (GWD)). The results showed that for K<subscript>s</subscript>, P<subscript>sat</subscript>P<subscript>dry</subscript> and SS, the best performance was found by the RF model in the third scenario, with R<superscript>2</superscript>= 0.53, 0.32, 0.31 and 0.41, respectively, while for soil hardness index (HI), Cubist model in the third scenario with R<superscript>2</superscript>= 0.25 showed the highest performance. For predicting K<subscript>s</subscript> and P<subscript>sat</subscript>, soil characteristics (i.e. clay and soil SOM and BD), and land use were the most important variables. For predicting P<subscript>dry</subscript>, HI, and SS, some topographical characteristics (Valley depth, catchment area, mlti-resolution of ridge top flatness index), and some soil characteristics (i.e. clay, SOM and MWD) were the most important input variables. The results of this research present moderate accuracy, however, the methodology employed provides quick and cost-effective information serving as the scientific basis for decision-making goals. [ABSTRACT FROM AUTHOR]
Details
- Language :
- English
- ISSN :
- 16726316
- Volume :
- 20
- Issue :
- 10
- Database :
- Complementary Index
- Journal :
- Journal of Mountain Science
- Publication Type :
- Academic Journal
- Accession number :
- 173515981
- Full Text :
- https://doi.org/10.1007/s11629-023-8056-z