Articles | Volume 23, issue 6
https://doi.org/10.5194/hess-23-2615-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-23-2615-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Mapping soil hydraulic properties using random-forest-based pedotransfer functions and geostatistics
Brigitta Szabó
Institute for Soil Sciences and Agricultural Chemistry, Centre for
Agricultural Research, Hungarian Academy of Sciences, Herman Ottó út
15, 1022 Budapest, Hungary
Georgikon Faculty, University of Pannonia, Deák Ferenc u. 16, 8360
Keszthely, Hungary
previously published under the name Tóth
Institute for Soil Sciences and Agricultural Chemistry, Centre for
Agricultural Research, Hungarian Academy of Sciences, Herman Ottó út
15, 1022 Budapest, Hungary
Katalin Takács
Institute for Soil Sciences and Agricultural Chemistry, Centre for
Agricultural Research, Hungarian Academy of Sciences, Herman Ottó út
15, 1022 Budapest, Hungary
Annamária Laborczi
Institute for Soil Sciences and Agricultural Chemistry, Centre for
Agricultural Research, Hungarian Academy of Sciences, Herman Ottó út
15, 1022 Budapest, Hungary
András Makó
Institute for Soil Sciences and Agricultural Chemistry, Centre for
Agricultural Research, Hungarian Academy of Sciences, Herman Ottó út
15, 1022 Budapest, Hungary
Georgikon Faculty, University of Pannonia, Deák Ferenc u. 16, 8360
Keszthely, Hungary
Kálmán Rajkai
Institute for Soil Sciences and Agricultural Chemistry, Centre for
Agricultural Research, Hungarian Academy of Sciences, Herman Ottó út
15, 1022 Budapest, Hungary
László Pásztor
Institute for Soil Sciences and Agricultural Chemistry, Centre for
Agricultural Research, Hungarian Academy of Sciences, Herman Ottó út
15, 1022 Budapest, Hungary
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68 citations as recorded by crossref.
- Global mapping of volumetric water retention at 100, 330 and 15 000 cm suction using the WoSIS database M. Turek et al. 10.1016/j.iswcr.2022.08.001
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- Digital mapping of soil physical and mechanical properties using machine learning at the watershed scale M. Ghavami et al. 10.1007/s11629-023-8056-z
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- A spatial machine learning model developed from noisy data requires multiscale performance evaluation: Predicting depth to bedrock in the Delaware river basin, USA P. Goodling et al. 10.1016/j.envsoft.2024.106124
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- Machine Learning for Predicting Field Soil Moisture Using Soil, Crop, and Nearby Weather Station Data in the Red River Valley of the North U. Acharya et al. 10.3390/soilsystems5040057
- Building inexpensive topsoil saturated hydraulic conductivity maps for land planning based on machine learning and geostatistics H. Aguilera et al. 10.1016/j.catena.2021.105788
- Modeling the Spatial Distribution of Soil Organic Carbon and Carbon Stocks in the Casanare Flooded Savannas of the Colombian Llanos J. Martín-López et al. 10.1007/s13157-023-01705-3
- Estimation of soil erodibility in Peninsular Malaysia: A case study using multiple linear regression and artificial neural networks M. Rehman et al. 10.1016/j.heliyon.2024.e28854
- Comparison of spectral and spatial-based approaches for mapping the local variation of soil moisture in a semi-arid mountainous area S. Fathololoumi et al. 10.1016/j.scitotenv.2020.138319
- In Situ Observation-Constrained Global Surface Soil Moisture Using Random Forest Model L. Zhang et al. 10.3390/rs13234893
- From EU-SoilHydroGrids to HU-SoilHydroGrids: A leap forward in soil hydraulic mapping B. Szabó et al. 10.1016/j.scitotenv.2024.171258
Latest update: 22 Nov 2024
Short summary
This paper analyzes differences in the performance of the indirect and direct mapping method to derive 3-D soil hydraulic maps. Maps of saturated water content, field capacity and wilting point are presented for a 5775 km2 catchment at 100 m resolution. Advantages and disadvantages of the two methods are discussed. The absolute difference in soil water retention values is less than 0.025 cm3 cm−3 between maps derived with indirect and direct methods for 65–86 % of the catchment.
This paper analyzes differences in the performance of the indirect and direct mapping method to...