globalchange  > 气候变化事实与影响
CSCD记录号: CSCD:6302685
论文题名:
青藏高原真实环境冻融循环作用变化趋势---以五道梁地区为例
其他题名: Actual Field Freeze-thaw Cycles Variation Trend in Qinghai - Tibet Plateau Permafrost Regions: A Case Study of Wudaoliang Area
作者: 杨天军
刊名: 公路交通科技
ISSN: 1002-0268
出版年: 2018
卷: 35, 期:8, 页码:46-54
语种: 中文
中文关键词: 道路工程 ; 冻融循环 ; 青藏高原高寒地区 ; 气温 ; 统计
英文关键词: road engineering ; freeze-thaw cycle ; Qinghai - Tibet plateau permafrost region ; temperature ; statistics
WOS学科分类: TRANSPORTATION
WOS研究方向: Transportation
中文摘要: 青藏高原寒冷地区具有显著的高原气候特征,年平均气温低、日温差大、冻融循环频繁剧烈,导致公路在行车荷载与气候环境的综合作用下产生多种病害。路面结构性能快速衰减,使用寿命锐减,严重影响了道路的正常运营与服务水平。对青藏公路沿线五道梁地区近60 a的气温与降水气象数据进行了统计分析,提出了同时考虑冻结温度与融化温度的真实环境冻融作用强度划分准则,分析了五道梁地区累月冻融作用及其近60 a的变化趋势。利用M - K (Mann - Kendall)检验法、Morlet小波分析法和R/S分析法检验分析了五道梁地区真实环境冻融作用变化趋势。研究表明:五道梁地区冻融作用主要集中在3-6月与9-10月,年冻融作用在时间历程内呈波动变化,从20世纪90年代开始总体呈减小趋势;利用M - K检验方法验证了五道梁地区年冻融作用与月冻融作用变化趋势,不同强度下年冻融次数随时间序列都呈减小趋势,月冻融次数随外界影响较大变化复杂;根据小波分析得到五道梁地区冻融作用变化趋势明显的第1、第2、第3主周期,分别为25 ~ 27,13 ~ 15,5 ~ 7 a;经R/S分析可知,五道梁地区未来冻融变化趋势随机性较大。五道梁地区冻融作用次数随时间序列虽然相对减少,但冻融作用次数基数很大,冻融作用仍然是青藏高寒地区影响公路工程的主要因素。
英文摘要: Plateau climate characteristics are prominent in Qinghai - Tibet plateau permafrost region,such as low annual average temperature,larger daily temperature difference,frequent and critical freeze-thaw cycles. These traffic impacts and environmental factors resulted in highway pavement appearing various distresses, structure capacity rapid deterioration,lifecycle sharply shorten,pavement performance and serviceability attenuation. Nearly 60 years temperature and precipitation meteorological data in Wudaoliang area along the Qinghai - Tibet highway are statistical analysed,the freeze-thaw intensity classification criterion in real environment based on the freezing and thawing temperature is proposed. Nearly 60 years monthly freeze-thaw cycles and the variation trend are analyzed. Mann - Kendall test method,Morlet wavelet analysis method, and R /S analysis method are used to analyze the freeze-thaw variation trend of Wudaoliang area in real environment. The research result shows that (1) the freeze-thaw effect in Wudaoliang area is mainly concentrated in March to June and September to October,the annual variation of freeze-thaw is fluctuated, and the whole trend presents decline from the 1990s; (2) the variation trends of annual and monthly freezethaw changes are verified using M - K test method,the annual freeze-thaw cycles presents decline with time, while the monthly freeze-thaw cycles is complex due to the environment impact; (3) according to the wavelet analysis,the 1st,2nd and 3rd main periods of obvious freeze-thaw variation trends in Wudaoliang area are 25 - 27,13 - 15,5 - 7 years respectively; (4) by R /S analysis,the future freeze-thaw variation in Wudaoliang area shows random trend; (5) although the freeze-thaw cycles of Wudaoliang area shows decreasing with time,while the amount of freeze-thaw cycles is large,the freeze-thaw effect is still the main influencing factor of highway engineering in the Qinghai - Tibet plateau permafrost region.
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/157708
Appears in Collections:气候变化事实与影响

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作者单位: 交通运输部科学研究院, 北京 100029, 中国

Recommended Citation:
杨天军. 青藏高原真实环境冻融循环作用变化趋势---以五道梁地区为例[J]. 公路交通科技,2018-01-01,35(8):46-54
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