首页|基于近场动力学的土冻结过程热传导模拟

基于近场动力学的土冻结过程热传导模拟

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寒区冻土工程在极端气候下面临挑战,土壤温度变化威胁工程结构稳定和安全,准确预测温度变化对工程安全至关重要。由于土壤冻结涉及材料相变,模拟预测中会出现非连续问题,基于连续性假设的热传导模型和局部偏微分方程的传统数值方法在求解该类问题时常产生奇异性。为此,本文引入近场动力学微分算子(PDDO),将经典连续介质力学中的偏微分方程转化为非局部积分形式,并基于热焓法建立相变热传导模型。选取不同近场范围模拟二维热传导过程并与解析解进行对比,确定在近场范围δ=3Δx时具有较高精度。选取不同相变材料模拟二维相变材料热传导过程,准确地模拟出相变材料在热传导过程中的温度变化以及材料相变过程。最后模拟了不同冻结温度下二维土体的冻结过程,准确捕捉到了相变温度并明显展现出相变温度平台。证实了本文提出的基于近场动力学的土冻结过程热传导模拟方法可以在给定条件下准确预测冻土温度变化。
Simulation of heat transfer during soil freezing based on peridynamics
Frozen soil is a critical type of porous medium that is widespread in high-latitude and high-altitude re-gions around the world.This soil type is characterized by the freezing of pore water in cold environments,which leads to significant changes in the soil's particle structure and pore configuration.These alterations can compro-mise the structural integrity of the soil,potentially resulting in severe damage or even complete failure of soil-based engineering systems.As such,understanding the mechanical properties and deformation behaviors of fro-zen soil is crucial for the stability and safety of infrastructure in cold climates.The accurate modeling of tempera-ture fields within frozen soils is essential,as these fields directly affect the soil's deformation and mechanical properties.Heat conduction in frozen soil is complicated by phase transitions,particularly the conversion of liq-uid pore water to solid ice at temperatures below the freezing point.This phase transition introduces substantial nonlinearity and discontinuity into the heat conduction problem,which poses significant challenges for tradition-al modeling approaches.Conventional heat transfer models,which rely on continuity assumptions and local par-tial differential equations(PDEs),frequently encounter computational singularities,leading to inaccuracies or instability in predictions.To address these challenges,this paper introduces an innovative numerical approach known as the Differential Operator of Near-Field Dynamics(PDDO).PDDO is a sophisticated non-local opera-tor derived from partial differential(PD)non-local theory and the orthogonality of PD functions.Unlike tradi-tional local PDE methods,PDDO defines the local derivative of any order for a material point as a non-local inte-gral expression within the local space or time domain.This transformation of partial differential equations into non-local integral forms effectively resolves the singularity issues associated with phase transitions,enhancing the accuracy and stability of numerical simulations.The research applies the PDDO method to develop a phase transition heat transfer model based on the enthalpy approach.This model is used to conduct detailed numerical simulations of heat conduction processes in one-dimensional and two-dimensional frozen soil scenarios.Various near-field ranges are systematically tested to identify the optimal range for achieving high precision in simula-tions.The results indicate that PDDO significantly outperforms traditional methods,providing more accurate and stable solutions to the nonlinearity and discontinuity challenges inherent in phase transition problems.Addi-tionally,the study extends the application of PDDO to simulate heat conduction in two-dimensional phase change materials,successfully capturing temperature variations and phase transition behaviors.The accuracy of these simulations validates PDDO's effectiveness in predicting temperature changes during phase transitions,demonstrating its robustness and applicability in handling complex material behaviors.Moreover,the paper in-vestigates the freezing process in two-dimensional soil under various freezing temperatures.The simulations ac-curately capture the phase transition temperature and highlight the distinctive plateau characteristics of the phase transition temperature,which is critical for understanding soil behavior under freezing conditions.This aspect of the research underscores the reliability and practical applicability of the PDDO-based simulation method in pre-dicting frozen soil behavior across a range of temperature conditions.In conclusion,the frozen soil heat conduc-tion simulation method based on PDDO presented in this paper represents a significant advancement in the analy-sis and modeling of frozen soil and phase transition phenomena.This method offers both theoretical and practi-cal improvements,providing a robust tool for accurately predicting the behavior of frozen soils in cold environ-ments.By overcoming the limitations of conventional approaches,PDDO enhances the precision and stability of simulations,thereby improving the design,safety,and stability of engineering projects in challenging frozen soil conditions.The findings and advancements from this research are expected to make a substantial contribu-tion to the development of more reliable and effective engineering solutions for managing and utilizing frozen soils,ultimately benefiting a range of applications from infrastructure development to environmental manage-ment in cold regions.

permafrostPDDOphase transition heat transfersoil freezing

鲁洋、穆彦虎、王建、郑军威、杨子越、朱戎熙

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河海大学水利水电学院,江苏南京 210098

中国科学院西北生态环境资源研究院冰冻圈科学与冻土工程重点实验室,甘肃兰州 730000

中国科学院大学,北京 100049

河海大学卓越工程师学院,江苏南京 210098

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冻土 近场动力学微分算子 相变热传导 土体冻结

2024

冰川冻土
中国地理学会 中国科学院寒区旱区环境与工程研究所

冰川冻土

CSTPCD
影响因子:2.546
ISSN:1000-0240
年,卷(期):2024.46(6)