干旱区研究 ›› 2023, Vol. 40 ›› Issue (11): 1729-1743.doi: 10.13866/j.azr.2023.11.03 cstr: 32277.14.j.azr.2023.11.03
张天意1,2(),刘杰1,2(),杨治纬2,王斌2,程秋连1,2
收稿日期:
2023-05-19
修回日期:
2023-07-11
出版日期:
2023-11-15
发布日期:
2023-12-01
作者简介:
张天意(1997-),男,硕士研究生,主要从事公路冰雪灾害防治. E-mail: 基金资助:
ZHANG Tianyi1,2(),LIU Jie1,2(),YANG Zhiwei2,WANG Bin2,CHENG Qiulian1,2
Received:
2023-05-19
Revised:
2023-07-11
Published:
2023-11-15
Online:
2023-12-01
摘要:
为精确识别雪崩流动特性及流态信息,全面分析其运动过程。本研究基于无人机倾斜摄影技术获取高分辨率航拍数据,以阿尔先沟雪崩易发区为例,通过现场调查、无人机遥感解译精细探测雪崩活动过程,确定RAMMS模型输入参数,在此基础上对不同类型雪崩事件进行模拟和重建,对比分析传统地面调查、无人机遥感解译结果与模拟结果的差异,探讨不同类型、不同雪层释放条件下雪崩活动过程。研究结果表明:(1) 以倾斜摄影技术为核心的雪崩调查分析体系,将传统的地面调查方法结合无人机遥感和数值模拟相互验证,提高了灾害发育状况评估的准确性。(2) 2月中旬阿尔先沟坡面积雪厚度趋近于临界厚度值,持续降雪使雪层失稳触发新雪雪崩。调查时仍处于灾害孕育阶段,雪层裂缝加剧变形,风力作用下雪檐自重逐步增大,有超过雪的抗断强度的趋势,整体稳定性较差。(3)以坡面上方积雪平台为潜在释放区的坡面型雪崩,释放量可达8.2669×104 m3,运动时长约为128 s,并在120 s内堆积区流动高度达到最大,约为3.55 m,最大流动速度为18.34 m·s-1,最大冲击力可达到32.67 kPa,形成面积3369.7 m2,体积1.8525×104 m3的堆积体。通过相互验证,坡面型雪崩并非积雪平台的释放,地面调查结果与数值模拟解译结果存在差异。(4) 沟槽—坡面复合型雪崩为沟槽坡面雪层断裂释放且断裂深度仅为临界厚度值的60%左右,雪崩持续时间接近于300 s,堆积区最大流动速度6.58 m·s-1,最大冲击力17.97 kPa,平均堆积深度为1.64 m,影响范围1178.5 m2,堆积量3107.76 m3,地面调查结果与数值模拟结果一致。研究结果一定程度上提高了雪崩事件信息获取的准确性,可为今后雪崩潜在危险预测、风险规避及灾害应急处置提供强有力的数据支撑及科学依据。
张天意, 刘杰, 杨治纬, 王斌, 程秋连. 基于空-地协同调查的西天山阿尔先沟雪崩过程数值模拟[J]. 干旱区研究, 2023, 40(11): 1729-1743.
ZHANG Tianyi, LIU Jie, YANG Zhiwei, WANG Bin, CHENG Qiulian. Numerical simulation of avalanche process in Aerxiangou, West Tianshan Mountains, based on air-ground cooperative investigation[J]. Arid Zone Research, 2023, 40(11): 1729-1743.
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