Wind Energy Environments and Its Impacts on Railway Sand Hazards along Gerlha Section of the Qinghai-Tibet Railway

Cai Diwen; Zhang Kecun; An Zhishan; Guo Zichen

doi:10.7522/j.issn.1000-694X.2015.00272

Journal of Desert Research >

2017 , Vol. 37 >Issue 1: 40 - 47

DOI: https://doi.org/10.7522/j.issn.1000-694X.2015.00272

Wind Energy Environments and Its Impacts on Railway Sand Hazards along Gerlha Section of the Qinghai-Tibet Railway

Cai Diwen ,
Zhang Kecun ,
An Zhishan ,
Guo Zichen

Expand

1. Dunhuang Gobi and Desert Ecology and Environment Research Station/Key Laboratory of Desert and Desertification, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China;
2. University of Chinese Academy of Sciences, Beijing 100049, China

Received date: 2015-01-06

Revised date: 2015-11-30

Online published: 2017-01-20

Fold

Abstract

Based on the meteorological station statistical data from 1955 to 2014 and field observation data along Gerlha section of the Qinghai-Tibet Railway, this paper studied the characteristics of wind energy environments in terms of wind direction, gale days and sand-dust storm days, sand drift potential and decadal variations of annual mean wind speed, and demonstrated their impacts to railway sand hazards. Mono wind direction, relatively high wind energy environments and the sand hazards going worse were our conclusion. This research has important meaning in monitoring the sand hazards developing trends and improving sand control system along Qinghai-Tibet Railway. It also can be a good reference for the design of other highway and railway sand control system which pass sandy regions as well.

Key words： Qinghai-Tibet Railway; sand hazards; wind energy environments

Cite this article

Cai Diwen , Zhang Kecun , An Zhishan , Guo Zichen . Wind Energy Environments and Its Impacts on Railway Sand Hazards along Gerlha Section of the Qinghai-Tibet Railway[J]. Journal of Desert Research, 2017 , 37(1) : 40 -47 . DOI: 10.7522/j.issn.1000-694X.2015.00272

References

[1] 谢胜波,屈建军,刘冰,等.青藏铁路沙害及其防治研究进展[J].中国沙漠,2014,34(1):42-48.
[2] Zhang K C,Qu J J,Han Q J,et al.Wind energy environments and aeolian sand characteristics along the Qinghai-Tibet Railway,China[J].Sedimentary Geology,2012,273/274:91-96.
[3] 张克存,屈建军,姚正毅,等.青藏铁路格拉段风沙危害及其防治[J].干旱区地理,2014(1):74-80.
[4] 安志山,张克存,屈建军,等.青藏铁路沿线风沙灾害特点及成因分析[J].水土保持研究,2014(2):285-289.
[5] 白虎志,李栋梁,董安祥,等.青藏铁路沿线的大风特征及风压研究[J].冰川冻土,2005,27(1):111-116.
[6] Wang Z H.Geological environment and disasters along railway line in the Qinghai-Tibet Plateau[J].Earth Science Frontiers,2007,14(6):31-37.
[7] 潘保田,李吉均.青藏高原:全球气候变化的驱动机与放大器(Ⅲ):青藏高原隆起对气候变化的影响[J].兰州大学学报:自然科学版,1996,32(1):108-115.
[8] 刘桂芳,卢鹤立.1961～2005年来青藏高原主要气候因子的基本特征[J].地理研究,2010(12):2281-2288.
[9] 宋辞,裴韬,周成虎.1960年以来青藏高原气温变化研究进展[J].地理科学进展,2012(11):1503-1509.
[10] Du SH H,Wang Q,Guo L.Spatially varying relationships between land-cover change and driving factors at multiple sampling scales[J].Journal of Environmental Management,2014,137:101-110.
[11] 胡光印,董治宝,逯军锋,等.黄河源区1975-2005年沙漠化时空演变及其成因分析[J].中国沙漠,2011,31(5):1079-1086.
[12] 张克存,屈建军,董治宝,等.风沙流中风速脉动对输沙量的影响[J].中国沙漠,2006,26(3):336-340.
[13] 张正偲,董治宝,赵爱国,等.输沙量与输沙势的关系[J].中国沙漠,2011,31(4):824-827.
[14] AL-Awadhi J M,AL-Helal A,AL-Enezi A.Sand drift potential in the desert of Kuwait[J].Journal of Arid Environments,2005,63:425-438.
[15] Fryberger S G.Dune forms and wind regime[M]//Mckee E D.A Study of Global Sand Seas.US Geological Survey Professional Paper,1979:137-169.
[16] Yang Y H,Qu ZH Q,Shi P J,et al.Wind regime and sand transport in the corridor between the Badain Jaran and Tengge rdeserts,central Alxa Plateau,China[J].Aeolian Research,2014,12:143-156.
[17] Zhang K C,Qu J J,Niu Q H,et al.Characteristics of wind-blown sand in the region of Crescent Moon Spring of Dunhuang,China[J].Environment Earth Science,2013,70:3173-3113.
[18] 房彦杰,赵景峰,郭永平,等.FRYBERGER输沙势计算方法及其估算值偏差分析——以塔克拉玛干沙漠为例[J].干旱区地理,2015(1):95-102.
[19] 李红军,杨青,何清.艾比湖地区的输沙势分析[J].干旱区研究,2003(4):322-325.
[20] 王永胜,杨文斌,李永华,等.库姆塔格沙漠东缘荒漠绿洲过渡带风况及输沙势[J].干旱区资源与环境,2015(1):140-144.
[21] 张正偲,董治宝,钱广强,等.腾格里沙漠西部和西南部风能环境与风沙地貌[J].中国沙漠,2012,32(6):1528-1533.
[22] 周成龙,杨兴华,刘厚勇,等.塔克拉玛干沙漠腹地塔中地区的风动力环境[J].水土保持通报,2014(3):218-222.
[23] 俎瑞平,张克存,屈建军.塔克拉玛干沙漠风沙活动强度特征[J].地理研究,2005(5):699-707.
[24] 凌裕泉.最大可能输沙量的工程计算[J].中国沙漠,1997,17(4):362-368.
[25] 朱震达,赵兴梁,凌裕泉,等.治沙工程学[M].北京:中国环境科学出版社,1998.
[26] 白虎志,董安祥,李栋梁,等.青藏高原及青藏铁路沿线大风沙尘日数时空特征[J].高原气象,2005,24(3):311-315.
[27] 张克存,牛清河,屈建军,等.青藏铁路沱沱河路段风沙危害特征及其动力环境分析[J].中国沙漠,2010,30(5):1006-1011.
[28] Bagnold R A.风沙与荒漠沙丘物理学[M].钱宁,等译.北京:科学出版社,1959.
[29] Kidron G J,Zohar M.Wind speed determines the transition from biocrust-stabilized to active dunes[J].Aeolian Research,2014,15:261-267.
[30] 黄以职,郭东信,赵秀峰.青藏高原冻土区沙漠化及其对环境的影响[J].冰川冻土,1993,15(1):52-57.
[31] Yang M X,Wang S L,Yao T D,et al.Desertification and its relationship with permafrost degradation in Qinghai-Xizang (Tibet) pleatu[J].Cold Regions Science and Technology,2004,39:47-53.
[32] 董玉祥.藏北高原土地沙漠化现状及其驱动机制[J].山地学报,2001(5):385-391.
[33] 胡光印,董治宝,魏振海,等.江河源区沙漠化研究进展与展望[J].干旱区资源与环境,2008(7):41-45.

Options

Outlines

模态框（Modal）标题

Abstract

Cite this article

References