Xiao Enzhao, Li Shengquan, Matin Nazar Ali, Zhu Ronghua, Wang Yihe
Polar Research Institute of China, Shanghai 200136, China.
Ocean College, Zhejiang University, Zhoushan 316021, China.
Materials (Basel). 2024 Mar 25;17(7):1490. doi: 10.3390/ma17071490.
Snow failure is the process by which the stability of snow or snow-covered slopes is destroyed, resulting in the collapse or release of snow. Heavy snowfall, low temperatures, and volatile weather typically cause consequences in Antarctica, which can occur at different scales, from small, localized collapses to massive avalanches, and result in significant risk to human activities and infrastructures. Understanding snow damage is critical to assessing potential hazards associated with snow-covered terrain and implementing effective risk mitigation strategies. This review discusses the theoretical models and numerical simulation methods commonly used in Antarctic snow failure research. We focus on the various theoretical models proposed in the literature, including the fiber bundle model (FBM), discrete element model (DEM), cellular automata (CA) model, and continuous cavity-expansion penetration (CCEP) model. In addition, we overview some methods to acquire the three-dimensional solid models and the related advantages and disadvantages. Then, we discuss some critical numerical techniques used to simulate the snow failure process, such as the finite element method (FEM) and three-dimensional (3D) material point method (MPM), highlighting their features in capturing the complex behavior of snow failure. Eventually, different case studies and the experimental validation of these models and simulation methods in the context of Antarctic snow failure are presented, as well as the application of snow failure research to facility construction. This review provides a comprehensive analysis of snow properties, essential numerical simulation methods, and related applications to enhance our understanding of Antarctic snow failure, which offer valuable resources for designing and managing potential infrastructure in Antarctica.
雪灾是指雪或积雪覆盖的斜坡稳定性被破坏,导致雪体崩塌或滑落的过程。大雪、低温和多变的天气通常会在南极洲引发各种后果,这些后果可能在不同尺度上发生,从小范围的局部崩塌到大规模雪崩,对人类活动和基础设施构成重大风险。了解雪灾对于评估与积雪地形相关的潜在危害以及实施有效的风险缓解策略至关重要。本综述讨论了南极雪灾研究中常用的理论模型和数值模拟方法。我们重点关注文献中提出的各种理论模型,包括纤维束模型(FBM)、离散元模型(DEM)、细胞自动机(CA)模型和连续空穴扩展穿透(CCEP)模型。此外,我们概述了一些获取三维实体模型的方法及其相关优缺点。然后,我们讨论了用于模拟雪灾过程的一些关键数值技术,如有限元法(FEM)和三维(3D)物质点法(MPM),突出了它们在捕捉雪灾复杂行为方面所具有的特点。最后,介绍了不同的案例研究以及这些模型和模拟方法在南极雪灾背景下的实验验证,以及雪灾研究在设施建设中的应用。本综述对雪的特性、重要的数值模拟方法及相关应用进行了全面分析,以增进我们对南极雪灾的理解,为设计和管理南极潜在基础设施提供了宝贵资源。