风吹雪中雪粒破碎机制的离散元法研究
批准号:
12102364
项目类别:
青年科学基金项目(C类)
资助金额:
30.0 万元
负责人:
王正师
依托单位:
学科分类:
环境流体力学与颗粒流
结题年份:
2024
批准年份:
2021
项目状态:
已结题
项目参与者:
王正师
中文摘要
风吹雪作为重塑积雪时空分布的关键物理过程之一,深刻影响着全球的气候系统、生态演化、水文循环和其他自然过程。风吹雪中雪粒的破碎效应是其区别于一般两相流运动的重要特征之一,对于认识和刻画风吹雪的发展过程和输运特征至关重要,而现有模型几乎均未考虑这一机制。本项目拟对风吹雪中雪粒的破碎机制展开研究,由于雪粒的力学性质对温度和粒径的强烈依赖性,且雪粒的碰撞破坏模式与碰撞方位直接相关,本项目首先基于雪粒的力学特性构建雪粒的温度和粒径依赖本构关系,进而二次开发能够表征雪粒力学特性的离散单元接触模型;接着针对雪粒这种易碎材料设计一种非接触式冲击实验平台,开展雪粒的碰撞破碎实验并验证离散单元模型的有效性;最后,基于各种工况下雪粒碰撞过程的离散单元仿真,揭示雪粒碰撞破碎的微观机理和破碎特征,并进一步探索其对风吹雪运动的影响规律。本研究结果可为变参数材料的破坏模式和机理分析提供指导。
英文摘要
As one of the key physical process that reshapes the temporal and spatial distribution of snow cover, drifting snow profoundly affects the global climate system, ecosystem evolution, hydrology cycle and other natural processes. The fracture mechanism of snow particles is an important feature that distinguishes the drifting snow from common two-phase flow movement, which is also critical for the description of development sprocess and transportation features of drifting snow. However, current models mostly neglect this mechanism. This research will perform a study of the fracture mechanism in drifting snow. Due to the strongly dependences of the mechanical properties of ice on the temperature and particle size, and the failure mode of snow particles is directly related to the collision bearing. Firstly, we will construct the temperature and particle size dependent constitutive relation of snow particle based on its mechanical properties, and further secondary develops the discrete element contact model that can characterize the mechanical properties of snow particle exactly. Then, we will design a non-contact impacting experimental platform for snow particle considering its friable feature, with which we can perform the impact and fracture tests and compare the experimental data with the simulation results to validate the discrete element model. Finally, based on the discrete element simulations of the impact and fracture processes of snow particles under various conditions, we will further reveal the micro fracture mechanism and fracture features of snow particles, and further explores its effect on drifting snow movement. The results can provide guidance for the failure mode and mechanism analysis of variable parameter materials.
雪粒破碎机制是风吹雪区别于其它两相流运动的重要特征,对于精确刻画风雪运动的演化规律和输运特征至关重要,但现有模型几乎均未考虑这一机制,尤其是经过初次碰撞后接近球形的雪粒的破碎机制及其特征待进一步研究。基于此,针对风吹雪过程中运动雪粒极易破碎成碎片的现象,本项目采用离散元法直接模拟了雪粒碰撞破碎过程,讨论和分析了碰撞速度和角度对雪粒破碎过程的影响,并提出一套具有普遍适用性的碰撞破碎模型。取得如下重要进展:(1)构建了精确表征雪粒破坏特征的粘结模型,通过与实验结果的对比验证模型并进行接触模型参数校准;(2)定量分析了雪粒碰撞破碎特征,包括有效碎片的数量、质量与粒径等分布等,揭示出雪粒碰撞破碎过程主要受冲击速度的法向分量控制,其中碎片数目随法向速度先增大后减小,在8 m/s左右达到峰值,粘结键损伤程度则随法向加载率呈幂函数增长,最高增加了约60%;(3)揭示了雪粒碰撞破碎特征主要是由于拉伸强度控制,并且雪粒冲击破碎存在一个临界速度。不同角度雪粒冲击破碎后的碎片相对粒径分布均呈现对数正态分布,平均碎片粒径随着冲击角度的增加而减小;(4)构建了雪粒破碎的参数化模型,并进一步引入风吹雪模型中,探明了雪粒碰撞破碎效应可提高输雪通量30%,并且增加的质量通量主要是高处雪粒增多的结果。本研究构建的雪粒破碎模型可以为极地积雪分布的时空衍化以及定量预测提供模型支撑。
国内基金
海外基金