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Detection of the freezing state and non-closure distances of loess with different water contents under bidirectional freezing by ultrasonic testing 超声检测双向冻结条件下不同含水率黄土的冻结状态和不闭合距离
IF 3.8 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2026-01-10 DOI: 10.1016/j.coldregions.2026.104827
Jiwei Zhang , Jiahao Zhang , Qingzhi Wang , Song Zhang , Shujie Liu , Yao Liu , Yuhao Wang , Ligang Zhang , Xiongbo Zhang
Accurately determining the freezing state and non-closure distances of artificial frozen walls is crucial for evaluating their development effectiveness. However, under complex field conditions, traditional thermometer hole monitoring methods have limitations such as a limited number and fixed positions, leading to difficulties in detection or inaccurate results. This study conducted laboratory bidirectional freezing tests, integrating temperature and water content monitoring with NM-4A non-metallic ultrasonic testing technology to systematically analyze the evolutionary patterns of ultrasonic time-frequency parameters during the freezing process of loess with different water contents. The results show that phased sharp increases in P-wave velocity (Vp) and head wave amplitude (Ah), the transition of the frequency spectrum from multi-peak to single-peak, and abrupt changes in centroid frequency (fc) and kurtosis of the frequency spectrum (KFS) can serve as key criteria for judging frozen wall closure. Dynamic changes in the reflection coefficient (rI), transmission coefficients (tP, tI), and acoustic impedance field are the main mechanisms affecting ultrasonic propagation characteristics. Based on ray acoustics theory, a prediction equation for non-closure distances was established. Validation demonstrated high accuracy, with error ranges of 0.001–6.293 mm for laboratory tests and the accuracy range is 76.82% ∼ 91.56% for field measurements. Incorporating the four parameters (Vp, Ah, fc, KFS) into radar charts enables qualitative evaluation of the frozen wall closure state. The ultrasonic testing method formed by combining this qualitative evaluation with the prediction equation provides an efficient and reliable technical means for judging the closure and quantifying the non-closure distance of bidirectionally frozen loess walls.
准确确定人工冻结墙的冻结状态和不闭合距离是评价人工冻结墙开发效果的关键。然而,在复杂的现场条件下,传统的温度计孔监测方法存在数量有限、位置固定等局限性,导致检测困难或结果不准确。本研究通过室内双向冻结试验,将温度、含水量监测与NM-4A非金属超声检测技术相结合,系统分析了不同含水量黄土在冻结过程中超声时频参数的演化规律。结果表明:p波速度(Vp)和头波幅度(Ah)的阶段性急剧增加,频谱由多峰向单峰转变,频谱质心频率(fc)和峰度(KFS)的突变可以作为判断冻结壁闭合的关键标准。反射系数(rI)、透射系数(tP、tI)和声阻抗场的动态变化是影响超声传播特性的主要机制。基于射线声学理论,建立了非闭合距离的预测方程。验证证明了高准确度,实验室测试的误差范围为0.001-6.293 mm,现场测量的准确度范围为76.82% ~ 91.56%。将Vp、Ah、fc、KFS这四个参数纳入雷达图,可以对冻结壁闭合状态进行定性评价。将该定性评价与预测方程相结合形成的超声检测方法,为双向冻结黄土墙体闭合性判断和不闭合距离量化提供了一种高效可靠的技术手段。
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引用次数: 0
Annual heat budget and seasonal variations in a northern river with ice processes 含冰过程的北部河流年热收支和季节变化
IF 3.8 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2026-01-10 DOI: 10.1016/j.coldregions.2026.104829
Can Ding , Shicheng Li , Joshua Johnson , Hailay Zeray Tedla , Eliisa Lotsari
Understanding the heat budget dynamics of high-latitude rivers is crucial for predicting thermal regimes, assessing the impacts of climate change on aquatic ecosystems, and informing effective water resource management. Despite their importance, detailed studies on the seasonal and transitional heat exchange processes in cold region environments remain limited. This study investigates the annual heat budget and seasonal variations of the Vantaanjoki River in southern Finland, with a particular focus on the influence of ice cover processes. Using meteorological, remote sensing, and in-situ measurements data collected from November 2022 to October 2023, a water/ice-air heat exchange analysis was performed to analyze four primary heat components: shortwave radiation, longwave radiation, sensible heat, and latent heat. The results show pronounced seasonal variations, with summer months dominated by shortwave radiation as the main heat gain source, while winter periods are characterized by significant heat losses due to longwave radiation. The annual net heat flux averaged −11.6 W/m2, indicating a near-balanced energy exchange over the year. Ice dynamics were monitored via image-based estimation of ice cover fraction, allowing classification into three surface conditions: open channel, partially ice-covered, and fully ice-covered. During freezing periods, longwave radiation accounted for over 60% of total heat loss, while shortwave radiation contributed marginally. In contrast, during melting periods, shortwave radiation became a more prominent heat gain component. The results provide critical insights into river heat budgets in high-latitude environments and contribute to improved understanding of river-atmosphere interactions under changing climatic conditions.
了解高纬度河流的热收支动态对于预测热状态、评估气候变化对水生生态系统的影响以及为有效的水资源管理提供信息至关重要。尽管它们很重要,但对寒区环境中季节性和过渡性热交换过程的详细研究仍然有限。本研究探讨了芬兰南部Vantaanjoki河的年热收支和季节变化,特别关注冰盖过程的影响。利用2022年11月至2023年10月的气象、遥感和现场测量数据,进行了水/冰-空气热交换分析,分析了短波辐射、长波辐射、感热和潜热4种主要热量成分。结果表明,夏季以短波辐射为主,而冬季以长波辐射为主。年净热通量平均为- 11.6 W/m2,表明全年能量交换接近平衡。通过基于图像的冰覆盖率估计来监测冰的动态,将表面状况分为三种:明渠、部分冰覆盖和完全冰覆盖。在冻结期,长波辐射占总热损失的60%以上,短波辐射贡献较小。相反,在融化期间,短波辐射成为更突出的热增益成分。这些结果为高纬度环境下的河流热收支提供了重要的见解,并有助于提高对气候条件变化下河流-大气相互作用的理解。
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引用次数: 0
Durable icephobicity: A lubricant-infused nickel scaffold approach 持久的疏冰性:一种注入润滑剂的镍支架方法
IF 3.8 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2026-01-08 DOI: 10.1016/j.coldregions.2026.104823
Mengjuan Wu , Jie Wang , Sanliang Ling , Richard Whealthy , Yizhou Shen , Xianghui Hou
The wind turbine blades are prone to icing phenomena under harsh and extreme environmental conditions, which significantly jeopardize the operational safety. In response to the critical challenges posed by the high energy consumption and low efficiency of current ice protection technology, the study aims to propose an optimized design for icephobic structure, leveraging the synergistic effect of phase change and the solid-ice interfacial mechanical behaviours. The proposed structure incorporates metallic scaffolds within polydimethylsiloxane (PDMS) matrix infused with ice-depressing liquid. In this study, glycol and glycerol were selected as the ice-depressing liquids for this investigation. By leveraging the infused ice-depressing liquid, the concentration of existing hydroxyl groups on the layer surface increased, which effectively lowered the freezing point of supercooled droplets at the liquid-solid interfaces. Furthermore, the embedded metallic scaffolds play a dual role in enhancing both the mechanical durability and de-icing performance of the composite structure. The remarkable reduction in ice adhesion was effectively achieved through the enhanced micro-crack propagation behaviour and diminished fracture toughness at the solid-ice interfaces, primarily stemming from the enhanced elastic-plastic disparities between the various phases, which facilitate both crack initiation and propagation at the interface. Consequently, this process undermines interfacial bonding, thereby promoting a more effortless removal of ice. The newly developed icephobic structure exhibited impressive icephobicity and durability: the ice nucleation delay duration of supercooled water droplets at −20 °C on Ni scaffolds-PDMS infused with glycerol (NP-glycerol) has been prolonged to 179.7 ± 4.5 s, whereas the icing time of pure Al plate of equivalent thickness exhibited an icing time of only 9.0 ± 1.2 s. Furthermore, the ice adhesion strength of NP-glycerol remained remarkably stable at approximately 0.7 ± 0.1 kPa even after 50 icing/de-icing cycles, highlighting the exceptional durability of the fabricated structure. These findings suggest that the proposed icephobic structure, incorporating metallic scaffolds and ice-depressing liquid within PDMS matrix, offers a promising avenue for developing durable and effective anti-icing surfaces for diverse applications. Future research will focus on optimizing the scaffold geometry and investigating the influence of ice-depressing liquids to further enhance the icephobic performance.
在恶劣和极端的环境条件下,风力发电机组叶片容易发生结冰现象,严重危及运行安全。针对当前防冰技术高能耗、低效率的严峻挑战,本研究旨在利用相变和固冰界面力学行为的协同效应,提出一种防冰结构的优化设计。所提出的结构将金属支架纳入注入抑冰液体的聚二甲基硅氧烷(PDMS)基质中。本研究选择乙二醇和甘油作为抑冰液。通过注入抑冰液,增加了层表面现有羟基的浓度,有效降低了液固界面处过冷液滴的凝固点。此外,嵌入金属支架在提高复合材料结构的力学耐久性和除冰性能方面具有双重作用。冰附着的显著降低是通过增强的微裂纹扩展行为和降低的固冰界面断裂韧性来实现的,这主要是由于不同相之间的弹塑性差异的增强,这有利于裂缝在界面处的萌生和扩展。因此,这一过程破坏了界面结合,从而促进了更轻松的除冰。新开发的疏冰结构具有良好的疏冰性和耐久性:在- 20 °C下,注入甘油的Ni支架- pdms (NP-glycerol)上的过冷水滴冰核延迟时间延长至179.7 ± 4.5 s,而同等厚度的纯Al板的结冰时间仅为9.0 ± 1.2 s。此外,即使在50次结冰/除冰循环后,np -甘油的冰粘附强度仍保持在约0.7 ± 0.1 kPa的稳定水平,突出了制造结构的卓越耐久性。这些发现表明,在PDMS基质中加入金属支架和抑冰液体的疏冰结构为开发耐用和有效的防冰表面提供了一条有前途的途径,可用于各种应用。未来的研究将集中在优化支架的几何形状和研究抑冰液体的影响,以进一步提高其憎冰性能。
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引用次数: 0
Residual stress evolution during ice accretion from a single water droplet 单水滴结冰过程中的残余应力演化
IF 3.8 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2026-01-08 DOI: 10.1016/j.coldregions.2026.104824
Motoki Sakaguchi , Kanta Ishida , Koichiro Tanaka , Moeka Tsukamoto , Chao Kang , Yu Kurokawa
Ice accretion on solid surfaces at low temperatures causes serious problems in numerous engineering applications, such as aircraft, wind turbines, and power lines. To develop effective anti-icing and de-icing technologies, understanding the mechanism of residual stress evolution within the ice film during the accretion process is essential. In this study, experiments were conducted to clarify the residual stress evolution during the solidification of a single water droplet dropped onto a low-temperature stainless steel substrate. In-situ observations of the droplet impact, spreading, and solidification were performed, varying the substrate temperature as a key parameter. Simultaneously, strain was measured on the substrate's backside using a strain gauge, showing that tensile strain develops on the substrate as the droplet solidifies. Furthermore, the residual strain increased with the decreasing substrate temperature. Cracking occurred immediately at lower substrate temperatures, whereas higher temperatures required additional cooling for cracking. Numerical analysis reproduced these experimental observations, quantifying the stress evolution within the ice film. Temperature-dependent material properties were incorporated in the analysis, as well as a creep constitutive equation based on stress relaxation tests, thereby capturing the time-dependent residual strain on the substrate and elucidating the distribution and evolution of tensile residual stress within the ice film. Ultimately, tensile stress developed during solidification and increased with cooling, reaching approximately 7–8 MPa at the time of cracking. These findings provide a fundamental understanding of the thermo-mechanical processes during ice accretion, crucial for developing robust anti-icing and de-icing strategies.
低温下固体表面上的冰积聚在许多工程应用中引起了严重的问题,如飞机、风力涡轮机和电力线。为了开发有效的防冰和除冰技术,了解冰膜内残余应力的演化机制至关重要。在本研究中,通过实验来阐明单个水滴在低温不锈钢基体上凝固过程中的残余应力演变。在改变基体温度作为关键参数的情况下,进行了液滴撞击、扩散和凝固的现场观察。同时,用应变计测量了基底背面的应变,结果表明,随着液滴凝固,基底上产生了拉伸应变。残余应变随基体温度的降低而增大。在较低的基材温度下,裂缝立即发生,而较高的温度下,裂缝需要额外的冷却。数值分析再现了这些实验观察,量化了冰膜内的应力演化。分析中纳入了与温度相关的材料特性,以及基于应力松弛试验的蠕变本构方程,从而捕获了基材上与时间相关的残余应变,并阐明了冰膜内拉伸残余应力的分布和演变。最终,拉伸应力在凝固过程中产生,并随着冷却而增大,在开裂时达到约7-8 MPa。这些发现提供了对冰增生过程热力过程的基本理解,对于制定强有力的防冰和除冰策略至关重要。
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引用次数: 0
Thawing permafrost under Qinghai-Xizang Highway and its impacts on road performance based on multi-source observed data 青藏公路冻土融化及其对道路性能的影响——基于多源观测数据
IF 3.8 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2026-01-08 DOI: 10.1016/j.coldregions.2026.104828
Guoyu Li , Mingtang Chai , Wei Ma , Fujun Niu , Dun Chen , Qingsong Du , Yu Zhou , Shunshun Qi , Yapeng Cao , Jianbing Chen , Liyun Tang , Yan Zhang
The Qinghai-Xizang Highway (QXH) exhibits widespread pavement damages because of underlying permafrost thawing. To comprehensively reflect the pavement damages and their controlling factors, images were processed and compared from ground penetrating radar (GPR) and unmanned aerial vehicle (UAV) in 7 typical sections along the QXH in the permafrost regions. The field monitoring data of ground temperature, embankment deformation were also collected to jointly investigate distribution, formation process and development mechanisms of roadway distress based on multi-source data. Indices such as distress ratio, pavement roughness and lateral deformation of the QXH were calculated by image segmentation and spatial analysis based on the UAV images. Results showed that (1) the temporal-spatial distribution of standard deviation of pavement altitude from the UAV image can quantitatively reflect the pavement roughness caused by embankment settlement and and vehicle loading during the roadway operation. The standard deviation has the maximum of difference of with 20–30 cm/a. (2) The average lateral deformation of the QXH can be extracted from the UAV image in thick embankment sections, which was 0.09 m/a in 4 of the 7 selected sections (K3059, K3119, K3177 and K3188). (3) Field monitoring data revealed the climate warming and permafrost thawing along the QXH. The GPR results and the UAV image can mutually verified for the explanation for the formation and development of the pavement damages. The findings can provide a comprehensive analysis method for the pavement damage and embankment distress based on multi-sourced data, and scientific guide for distress prediction and roadway maintenance.
青藏公路(QXH)由于下垫层冻土融化而出现广泛的路面破坏。为全面反映冻土区QXH沿线7个典型路段的路面损伤及其控制因素,对探地雷达(GPR)和无人机(UAV)图像进行了处理和对比。收集地温、路堤变形等现场监测数据,结合多源数据,共同探讨巷道破坏的分布、形成过程及发展机制。基于无人机图像,通过图像分割和空间分析,计算出QXH的破损率、路面平整度和侧向变形等指标。结果表明:(1)无人机图像路面高度标准差的时空分布可以定量反映道路运行过程中路堤沉降和车辆荷载引起的路面粗糙度。标准偏差最大差值为20 ~ 30cm /a。(2)在较厚路堤断面中,无人机图像可提取QXH的平均侧向变形,选取的7个断面中有4个(K3059、K3119、K3177和K3188)的平均侧向变形量为0.09 m/a。(3)野外监测数据揭示了青藏高原气候变暖和多年冻土融化。GPR结果与无人机图像可以相互验证,用于解释路面损伤的形成和发展。研究结果可为路面损伤和路堤损伤提供基于多源数据的综合分析方法,为路面损伤预测和道路养护提供科学指导。
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引用次数: 0
The impact of soluble salt on the reconstruction of saline gap-graded soil particle composition during freeze-thaw cycles 冻融循环中可溶性盐对盐隙级配土壤颗粒组成重建的影响
IF 3.8 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2026-01-07 DOI: 10.1016/j.coldregions.2025.104813
Weitong Xia , Yujie Wang , Shicong Sun , Fengyuan Wu , Jing Liu , Qingbo Yu
Carbonate saline soil affected by soluble salts show a bimodal grain-size distribution and is highly erodible and prone to engineering hazards such as seepage erosion and slope instability. However, detailed studies on the influence mechanism of soluble salts on gap-graded characteristics remain limited, especially concerning the more complex particle reorganisation under freeze-thaw (F-T) cycles. Therefore, this study investigated non-saline soil (NS), low-salinity saline soil (LS), and high-salinity saline soil (HS) to examine their differences in particle size distribution, the uniformity coefficient, the degree of soil particle variation, and microstructural characteristics under different F-T cycles. The particle size distribution of NS was unimodal, while LS and HS exhibited a distinct bimodal particle size distribution. A critical boundary particle size of approximately 30 μm was identified, effectively demarcating the dominant processes: coarse particles larger than 30 μm predominantly underwent fragmentation, while those smaller than 30 μm tended to agglomerate. Soluble salts influenced the gap-graded characteristics through the dispersing effect of dissolved salts on fine particles and the cementing effect of crystalline salts on coarse particles. Therefore, compared with NS, both LS and HS exhibited larger dominant particle sizes and a higher uniformity coefficient before F-T cycles. After F-T cycles, driven by the diffuse double layer shell effect and cryogenic suction, unfrozen water in fine inter-particle pores migrated continuously into coarse inter-particle pores and underwent ice formation. This process simultaneously induced recrystallisation and agglomeration of fine particles, whereas the degree of fragmentation of coarse particles increased significantly. Furthermore, soil salinity had a two-phase impact on the agglomeration of fine particles. Specifically, compression of the diffuse double layer induced by high sodium ion concentrations during the freezing process counteracted the tendency of the diffuse double layer to thicken under low sodium ionic valence, further promoting the agglomeration of fine particles. The findings from this study can provide a theoretical foundation for mitigating salinisation and erosion hazards in saline soils of regions that undergo seasonal freezing.
碳酸盐盐渍土受可溶性盐的影响,粒度分布呈双峰型,易受侵蚀,易发生渗漏侵蚀和边坡失稳等工程灾害。然而,关于可溶性盐对间隙梯度特性的影响机制的详细研究仍然有限,特别是关于冻融循环下更复杂的颗粒重组。因此,本研究以非盐渍土(NS)、低盐盐渍土(LS)和高盐盐渍土(HS)为研究对象,研究不同F-T循环条件下土壤粒度分布、均匀系数、颗粒变异程度和微观结构特征的差异。NS的粒径分布呈单峰分布,LS和HS的粒径分布呈明显的双峰分布。临界边界粒径约为30 μm,有效地划分了优势过程:大于30 μm的粗颗粒以破碎为主,而小于30 μm的粗颗粒则倾向于团聚。可溶性盐通过溶解盐对细颗粒的分散作用和结晶盐对粗颗粒的胶结作用影响间隙梯度特性。因此,与NS相比,LS和HS在F-T循环前均表现出更大的优势粒径和更高的均匀系数。经过F-T循环后,在弥漫性双层壳效应和低温吸力的驱动下,细小颗粒间孔隙中的未冻水不断向粗颗粒间孔隙迁移并形成冰。这一过程同时诱导了细颗粒的再结晶和团聚,而粗颗粒的破碎程度显著增加。此外,土壤盐度对细颗粒团聚有两相影响。具体来说,在冻结过程中,高钠离子浓度引起的弥散双层压缩抵消了低钠离子价下弥散双层增厚的趋势,进一步促进了细颗粒的团聚。本研究结果可为减轻季节性冻结地区盐渍土的盐渍化和侵蚀危害提供理论基础。
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引用次数: 0
Uniaxial compressive behavior of frozen silty clay at extreme low temperature with varying initial water content 冻结粉质粘土在极低温下随初始含水量变化的单轴压缩特性
IF 3.8 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2026-01-06 DOI: 10.1016/j.coldregions.2026.104825
Jiaming Xian , Wansheng Pei , Yuanming Lai , Mingyi Zhang , Fan Yu , Yanyan Chen
Current researches on frozen soil mechanics mainly focus on temperature above −30 °C. However, increasing extreme low temperature conditions (e.g., extreme cold weather in cold regions, artificial ground freezing construction, and liquefied natural gas storage) demands a clear understanding of frozen soil mechanics below −30 °C. In this study, uniaxial compression tests were conducted on silty clay samples at varied initial mass water contents (12%, 14%, 16%, 18%, and 20%) and temperatures ranging from −10 °C to −130 °C. The influence of extreme low temperature and initial water content on the mechanical behavior and failure mode were analyzed by combining the macro test and material compositions. The results show that the uniaxial compressive strength (UCS) and elastic modulus increase as temperature decreases for soil with lower initial water content (12% to 16%). In contrast, at higher initial water content (18% to 20%), the UCS rises to a peak at −110 °C and then declines with further cooling. Meanwhile, the shapes of stress-strain curves have three types, including strain softening, strain hardening, and brittleness. All samples exhibit pronounced brittle transition at approximately −110 °C. Two brittleness evaluation methods were employed to quantitatively assess the brittleness level of the soil samples. Moreover, the failure mode also changes with temperature and initial water content, including the localized failure with shear band, the bulge failure, the splitting failure, and the crushing failure. The strength variation at extreme low temperature is attributed to the combined effect of the strength variation of the pore ice and the mineral compositions in soil particles, and the bond effect between ice and soil particles. These findings elucidate the mechanical behavior and the evolution of brittleness in frozen silty clay under extreme low temperature conditions. They can provide a scientific basis for safer geotechnical design and infrastructure resilience in cold environments.
目前的冻土力学研究主要集中在−30℃以上的温度。然而,越来越多的极端低温条件(例如,寒冷地区的极端寒冷天气,人工地面冻结施工和液化天然气储存)需要清楚地了解- 30°C以下的冻土力学。在这项研究中,粉质粘土样品在不同的初始质量含水量(12%、14%、16%、18%和20%)和温度范围(- 10°C至- 130°C)下进行单轴压缩试验。结合宏观试验和材料成分分析了极低温和初始含水量对材料力学行为和破坏模式的影响。结果表明:初始含水量较低(12% ~ 16%)时,土体单轴抗压强度和弹性模量随温度降低而增大;相比之下,在较高的初始含水量(18%至20%)下,UCS在- 110°C时达到峰值,然后随着进一步冷却而下降。同时,应力-应变曲线的形状有应变软化、应变硬化和脆性三种类型。所有样品在约- 110°C时表现出明显的脆性转变。采用两种脆性评价方法定量评价土样的脆性水平。破坏模式也随温度和初始含水量的变化而变化,包括局部剪切带破坏、鼓包破坏、劈裂破坏和破碎破坏。极低温条件下的强度变化主要是孔隙冰强度变化与土壤颗粒矿物组成的综合作用,以及冰与土壤颗粒之间的粘结作用。这些发现阐明了极低温条件下冻结粉质粘土的力学行为和脆性演化。它们可以为更安全的岩土工程设计和寒冷环境下基础设施的恢复能力提供科学依据。
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引用次数: 0
Data-driven natural gas pipeline reliability evaluation focusing on the mitigation effectiveness for frost heave in cold regions 基于数据驱动的寒区天然气管道冻胀缓解效果可靠性评估
IF 3.8 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2026-01-06 DOI: 10.1016/j.coldregions.2026.104826
Tian Xu , Peng Zhang , Pan Guo , Wei Liu
Natural gas pipelines are widely distributed across cold regions, where they are threatened by frost heave. Parameter uncertainty and the complex mechanism of frost heave limit the reliability assessment of pipelines in cold regions. This study presents a novel framework to overcome these limitations in implementing reliability analysis. In the framework, the Monte Carlo Simulation (MCS) method is incorporated to quantify uncertainty by generating a larger number of samples. A data-driven Back Propagation Neural Network (BPNN) model is developed to avoid the complex Limit State Function (LSF) for calculating pipeline damage. A closed-form Elastic Foundation Beam Model (EFBM) is developed to evaluate frost-heave-induced pipeline damage and to generate the database for training the BPNN model. The results indicate that the developed BPNN model can accurately predict frost-heave-induced bending stress, with a maximum error of 13.6 MPa. From the perspective of hazard mitigation, the finding reveals that targeting the frost-heave height is the most effective measure for improving reliability, which reduces additional failure probability by 18% and 42% compared with other measures. As mitigation levels increase, the uncertainty-induced pipeline failure probability discrepancy reaches 10.7%. The analysis results can guide targeted management strategies to improve the structural resilience of pipelines in cold regions.
天然气管道广泛分布在寒冷地区,在那里它们受到冻胀的威胁。冻胀参数的不确定性和机理的复杂性限制了寒区管道可靠性评估。本研究提出了一个新的框架来克服实施可靠性分析的这些限制。在该框架中,采用蒙特卡罗模拟(MCS)方法,通过生成大量样本来量化不确定性。为了避免复杂的极限状态函数(LSF)计算管道损伤,提出了一种数据驱动的反向传播神经网络(BPNN)模型。建立了一种封闭形式的弹性基础梁模型(EFBM),用于评估管道冻胀损伤,并生成了用于训练BPNN模型的数据库。结果表明,所建立的BPNN模型能较准确地预测冻胀引起的弯曲应力,最大误差为13.6 MPa。从减少危害的角度来看,研究结果表明,针对冻胀高度是提高可靠性的最有效措施,与其他措施相比,可将额外失效概率降低18%和42%。随着缓解水平的增加,不确定性引起的管道失效概率差异达到10.7%。分析结果可以指导有针对性的管理策略,以提高寒区管道的结构弹性。
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引用次数: 0
Stress-rate-controlled compression behavior of compacted snow 压实雪的应力-速率控制压缩特性
IF 3.8 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2026-01-06 DOI: 10.1016/j.coldregions.2026.104821
Yuanpeng Zheng , Tao Chen , Chao Jiang , Qinghua Huang , Xiang-Lin Gu
While many previous compression tests on compacted snow have employed displacement-controlled loading, studies under stress-rate control remain limited, even though compression under external pressure may better reflect engineering reality. To advance understanding of the compressive behavior of compacted snow under stress-controlled loading, this study prepared two types of specimens with average densities of 566 and 662 kg/m3 and conducted uniaxial compression tests across a wide range of stress rates, from 1.11 to 555.56 kPa/s, to capture transitions in failure behavior. Analysis of stress-strain curves, loading rate time histories, and visual records identified two ductile and three brittle failure modes that emerged with increasing stress rate, including modes not documented in displacement-controlled investigations. It was found that while the relationship between compressive strength and loading rate aligns with existing conclusions, the trend between modulus of deformation and stress rate depends on the types of specimens, which differed markedly in overall integrity during compression failure. Comparisons between stress-rate- and displacement-controlled compression further revealed their inherent complexity, indicating distinct physical mechanisms governing instability and failure under different loading controls, and demonstrating the inadequacy of mechanical testing conducted solely under the displacement-controlled regime. This study emphasizes the need to distinguish between local and overall failure when characterizing the mechanical properties of compacted snow, reaffirms the importance of snow densification, and identifies boundary stress rates between failure modes, offering useful context for future experimental and engineering studies involving compacted snow.
虽然以前许多压实雪的压缩试验都采用了位移控制加载,但在应力率控制下的研究仍然有限,尽管外部压力下的压缩可能更能反映工程实际。为了进一步了解压实雪在应力控制载荷下的压缩行为,本研究准备了两种平均密度分别为566和662 kg/m3的试件,并在1.11至555.56 kPa/s的大应力速率范围内进行了单轴压缩试验,以捕捉破坏行为的转变。应力-应变曲线分析、加载速率时间历史和视觉记录确定了随着应力速率增加而出现的两种延性和三种脆性破坏模式,包括位移控制研究中未记录的模式。研究发现,虽然抗压强度与加载速率的关系与已有结论一致,但变形模量与应力速率之间的趋势取决于试件的类型,试件在压缩破坏过程中的整体完整性存在显著差异。应力速率控制和位移控制压缩的对比进一步揭示了它们内在的复杂性,表明了不同加载控制下控制失稳和破坏的不同物理机制,并表明了仅在位移控制下进行力学试验的不足。该研究强调了在描述压实雪的力学特性时需要区分局部和整体破坏,重申了雪致密化的重要性,并确定了破坏模式之间的边界应力率,为未来涉及压实雪的实验和工程研究提供了有用的背景。
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引用次数: 0
Climate snow-avalanche linkage revealed by geomorphological, historical and tree-ring records in the central Spanish Pyrenees 西班牙比利牛斯山脉中部地貌、历史和树木年轮记录揭示的气候雪崩联系
IF 3.8 2区 工程技术 Q1 ENGINEERING, CIVIL Pub Date : 2026-01-05 DOI: 10.1016/j.coldregions.2026.104819
Osvaldo Franco-Ramos , Jaime Boyano-Galiano , Alberto Muñoz-Torrero Manchado , Juan Ignacio López-Moreno , Juan Antonio Ballesteros-Cánovas
Snow avalanches are significant natural hazards in mountainous regions, and their frequency and magnitude are increasingly influenced by changing climatic conditions. This study presents a multi-proxy reconstruction of snow avalanche activity over the past century (1910–2014 CE) in the Canfranc Valley, Central Spanish Pyrenees. The reconstruction integrates geomorphic mapping, dendrochronology, historical archives, and climatic data. A total of 345 trees were sampled and analysed, yielding 1322 growth disturbances (GD), which enabled the reconstruction of 30 and 27 avalanche events in the Estiviellas (ES) and Rinconada (RI) paths, respectively. The analysis was complemented by geomorphological assessments based on high-resolution LiDAR-derived terrain models, along with historical records and fieldwork validation. Also, avalanche size was estimated using a bivariate statistical model based on runout distance and width, both inferred from the most distal affected trees. These size proxies, combined with return period analyses, indicate that the largest avalanches (e.g., 1962, 1986, 1993) occurred more frequently in the second half of the 20th century, while recent decades have been characterized by smaller but more frequent events, typically confined to upper slopes. Structural Equation Modelling (SEM) was applied to examine the relationships between reconstructed avalanche activity, snowpack, climate variables, and atmospheric circulation anomalies. Results show that negative phases of the North Atlantic Oscillation (NAO) enhance precipitation and lower temperatures, thereby increasing snowpack depth and avalanche probability. Snowpack emerged as the principal mediator between meteorological variables and avalanche activity. Although long-term trends indicate increasing temperatures and precipitation, their direct influence on avalanche size was limited. These findings underscore the non-linear and threshold-dependent nature of avalanche dynamics and highlight the critical role of snowpack and regional climate variability. The observed decline in avalanche size and the shift toward smaller, more frequent events may reflect broader cryospheric transformations under warming conditions. This study provides valuable insights for risk assessment and the development of adaptive hazard management strategies in mountain environments affected by climate change.
雪灾是山区重大的自然灾害,其发生频率和强度越来越受气候条件变化的影响。本研究对过去一个世纪(1910-2014 CE)在西班牙比利牛斯山脉中部Canfranc山谷的雪崩活动进行了多代理重建。重建整合了地貌制图、树木年代学、历史档案和气候资料。共对345棵树进行了采样和分析,产生了1322个生长干扰(GD),分别在Estiviellas (ES)和Rinconada (RI)路径上重建了30和27个雪崩事件。该分析还辅以基于高分辨率激光雷达地形模型的地貌评估,以及历史记录和实地工作验证。此外,使用基于跳动距离和宽度的二元统计模型估计雪崩大小,这两个模型都是从最远的受影响树木推断出来的。这些规模指标与回归期分析相结合表明,最大的雪崩(如1962年、1986年和1993年)在20世纪下半叶发生得更为频繁,而最近几十年的特征是较小但更频繁的事件,通常局限于较高的斜坡。利用结构方程模型(SEM)分析了重建的雪崩活动、积雪量、气候变量和大气环流异常之间的关系。结果表明,北大西洋涛动(NAO)负相增加了降水,降低了气温,从而增加了积雪深度和雪崩概率。积雪是气象变量与雪崩活动之间的主要中介。虽然长期趋势表明气温和降水增加,但它们对雪崩规模的直接影响有限。这些发现强调了雪崩动力学的非线性和阈值依赖性,并强调了积雪和区域气候变率的关键作用。观测到的雪崩规模的减少和向更小、更频繁事件的转变可能反映了在变暖条件下更广泛的冰冻圈转变。该研究为气候变化影响下山地环境的风险评估和适应性灾害管理策略的制定提供了有价值的见解。
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引用次数: 0
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Cold Regions Science and Technology
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