Abstract

Revealing the variation law of thermal diffusivity of sandy soil can provide a theoretical basis for the engineering design and construction in cold and arid regions. Based on experimental data of sandy soil samples, the distribution characteristics and influence of dry density and moisture content on thermal diffusivity are analyzed in this work. Then, the prediction model based on the empirical fitting formula and RBF neural network method for thermal diffusivity of frozen and unfrozen sandy soil is established, and the prediction accuracy of different prediction methods is compared. The results show that (1) thermal diffusivity of sandy soil is positively correlated with the particle size. With the increase of sand size, thermal diffusivity of sandy soil increases significantly. (2) Partial correlation among natural moisture content, dry density, and thermal diffusivity varies with different frozen and unfrozen conditions. (3) For unfrozen sandy soil, the binary RBF neural network prediction model is obviously better than that of the binary empirical fitting formula model. (4) The ternary prediction model has significantly higher prediction accuracy than that of the binary prediction model for frozen sandy soil, and the ternary RBF neural network model has the best prediction effect among the four methods.

Highlights

  • Academic Editor: Stefano PagnottaSandy soils are widely distributed in China, especially in the provinces of Inner Mongolia, Gansu, Xinjiang, Tibet, etc., which occupy more than 50% of China’s land surface [1].Compared to other soil types, the thermal diffusivity of sandy soil is relative large, which turns into a faster rate of heat transfer and a larger temperature variation [1,2]

  • The theoretical calculation is usually based on the assumption that the soil is a semi-unbounded medium with constant thermal diffusivity, and the calculation formula is obtained based on the one-dimensional heat conduction equation

  • Zhen et al [15] used the transient plane heat source method to study the influence of dry density and moisture content on the thermal conductivity of sandy soil, and the results showed that the thermal diffusivity of remolded sandy soil was positively correlated with moisture content

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Summary

Introduction

Sandy soils are widely distributed in China, especially in the provinces of Inner Mongolia, Gansu, Xinjiang, Tibet, etc., which occupy more than 50% of China’s land surface [1]. Li et al [8] calculated thermal diffusivity of Taklimakan desert soil at depths of 5 to 20 cm using four computation methods (harmonic method, phase method, amplitude method, and heat conduction convection method) based on the observation data from an atmospheric environment observatory. Zhen et al [15] used the transient plane heat source method to study the influence of dry density and moisture content on the thermal conductivity of sandy soil, and the results showed that the thermal diffusivity of remolded sandy soil was positively correlated with moisture content. Wang et al [16] used measured soil temperature data to calculate the heterogeneous soil thermal conductivity, and the results showed that the soil thermal conductivity had a significant tendency to increase with the increase in depth. The research results can help to provide data reference for the thermal design of engineering structures with sandy soil foundation

Source of Test Specimens
Calculation Method of Thermal Diffusivity
Binary Empirical Formula Fitting
Ternary Fitting of Frozen Soil Based on Thermal Diffusivity of Unfrozen Soil
Application Comparison of Thermal Diffusivity Prediction Model
Evaluation
Conclusions
Full Text
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