Machine learning-based pseudo-continuous pedotransfer function for predicting soil freezing characteristic curve

• Pedotransfer function for soil freezing characteristic curve (SFCC) is proposed. • Quantitatively understanding the variation of unfrozen water with temperature. • Influential mechanisms of dominant factors characterizing SFCCs are determined. Unfrozen water plays a crucial role in thermophysical processes occurring in frozen ground. Measurement difficulties require approximate approaches to describe the relationship between unfrozen water content ( θ ) and soil temperature, known as soil freezing characteristic curve (SFCC). Despite significant progress, model characteristics, freezing-thawing hysteresis, and phase equilibrium remain challenging. This study developed an alternative approach to estimate θ using a pedotransfer function (PTF) implemented with extreme gradient boosting (XGB). The XGB-PTF model was trained using SFCC data available in the literature, and cooperative game theory was utilized to assess potential impacts on θ predictions. The performance of the XGB-PTF was rigorously evaluated and compared with two high-performance empirical models. Significant reductions in root mean square error and mean absolute error of 42% and 55%, respectively, demonstrated the superiority of the XGB-PTF. The XGB-PTF’s usability was also verified by experimental validation. A notable advantage of the proposed model is its capacity to provide a credible range containing the actual θ with a 95% confidence level. Coupling the XGB-PTF with game theory indicated that the primary factors influencing the SFCC were in order of porosity ( n ), initial saturation degree ( S r ), and clay fraction ( F clay ) for fine-grained soils, while for coarse-grained soils, the order is F clay , n , and S r . Furthermore, insights derived from game theory aligned with previous experimental studies concerning the phase transition of pore water across various temperature ranges. The proposed XGB-PTF, with its straightforward predictors, efficiency, and transparency, is expected to serve as a versatile tool for advancing SFCC studies.

Authors

Institutions

Publication Details

Journal
Geoderma
Published
2024-12-20
DOI
https://doi.org/10.1016/j.geoderma.2024.117145
Citations
7
Primary Topic
Climate change and permafrost
Type
article
Field-Weighted Citation Impact
2.63
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Machine learning-based pseudo-continuous pedotransfer function for predicting soil freezing characteristic curve

Hangseok Choi, Khanh Pham, Yoonsik Choe, Sangyeong Park
7 citations
Geoderma
Climate change and permafrost
2.63
article

Machine learning-based pseudo-continuous pedotransfer function for predicting soil freezing characteristic curve

Hangseok Choi, Khanh Pham, Yoonsik Choe, Sangyeong Park
article en
7 citations

Abstract

• Pedotransfer function for soil freezing characteristic curve (SFCC) is proposed. • Quantitatively understanding the variation of unfrozen water with temperature. • Influential mechanisms of dominant factors characterizing SFCCs are determined. Unfrozen water plays a crucial role in thermophysical processes occurring in frozen ground. Measurement difficulties require approximate approaches to describe the relationship between unfrozen water content ( θ ) and soil temperature, known as soil freezing characteristic curve (SFCC). Despite significant progress, model characteristics, freezing-thawing hysteresis, and phase equilibrium remain challenging. This study developed an alternative approach to estimate θ using a pedotransfer function (PTF) implemented with extreme gradient boosting (XGB). The XGB-PTF model was trained using SFCC data available in the literature, and cooperative game theory was utilized to assess potential impacts on θ predictions. The performance of the XGB-PTF was rigorously evaluated and compared with two high-performance empirical models. Significant reductions in root mean square error and mean absolute error of 42% and 55%, respectively, demonstrated the superiority of the XGB-PTF. The XGB-PTF’s usability was also verified by experimental validation. A notable advantage of the proposed model is its capacity to provide a credible range containing the actual θ with a 95% confidence level. Coupling the XGB-PTF with game theory indicated that the primary factors influencing the SFCC were in order of porosity ( n ), initial saturation degree ( S r ), and clay fraction ( F clay ) for fine-grained soils, while for coarse-grained soils, the order is F clay , n , and S r . Furthermore, insights derived from game theory aligned with previous experimental studies concerning the phase transition of pore water across various temperature ranges. The proposed XGB-PTF, with its straightforward predictors, efficiency, and transparency, is expected to serve as a versatile tool for advancing SFCC studies.

GeodermaVol. 453
Vietnam National University Ho Chi Minh City (VN), Georgia Institute of Technology (US), Korea University (KR), Ho Chi Minh City International University (VN), Texas A&M University (US)
Zero hunger
Openalex Percentile: Top 10%
Climate change and permafrost
2.63
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.