We are thrilled to announce the publication of our recent paper titled “Probabilistic machine learning for predicting desiccation cracks in clayey soils.” In this groundbreaking research, we have developed a probabilistic machine learning (ML) framework to enhance the accuracy and reliability of deterministic models in predicting desiccation cracks in clayey soils, which have become increasingly prevalent due to climate change-induced heatwaves and drought-downpour cycles.
To achieve this, we utilized a comprehensive set of data-driven soil and environment parameters, including initial water content, crack water content, final water content, soil layer thickness, temperature, and relative humidity, as inputs to predict the crack surface ratio. We then employed various ML techniques, such as random forests, regression trees, gradient-boosted trees, support-vector machines, and artificial neural network-particle swarm optimization, to develop predictive models.
To account for uncertainties, we incorporated Monte Carlo simulation, which involved shuffling and randomizing samples, into our models. Additionally, we conducted sensitivity analyses, including input exclusion and partial dependence-individual conditional expectation plots, to assess the reliability of our predictions.
The results of our study revealed that the performance ranking of the developed ML models can be summarized as follows: support-vector machines > gradient-boosted trees > extreme gradient-boosted trees > artificial neural network-particle swarm optimization > random forests > regression trees. However, when considering the probabilistic modeling based on Monte Carlo simulation, gradient-boosted trees demonstrated the highest capability for predictions, exhibiting the lowest errors and uncertainties.
Furthermore, our sensitivity analyses highlighted the importance of various parameters, with the order of significance being final water content > crack water content > soil layer thickness > initial water content > temperature > relative humidity.