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Blockade of Trunk Highway in Southwest Mountains Areas
Tian Qiangchun , Zhu Hongzhou , Wang Qingzhen ,Gao Lingran
2014, 33(3):
41-44.
DOI: 10.3969/j.issn.1674-0696.2014.03.10
For geography , geology , climate , hydrology and hydrogeology characteristics of southwest mountainous areas , the
main features , blocking reasons and distribution law of trunk highway in southwest mountainous areas were analyzed by using
the statistics database of blockade of Chongqing trunk roads from 2007 to 2011. The results show that various causes , blocking
with a high concentration , great block accumulative influence and strongly concentrated of blocking regions are the main
features of the blockade of trunk highway in southwest mountainous areas. And sudden blocking is the main style; the incidence
of unexpected block is 79. 8 %. The main causes of blocking are geological disasters and adverse weather conditions ,
accounting to 57% and 19% respectively of the total blockade numbers. The second main blocked cause of geological disasters
blocking is landslides and mudslides , accounting to 33%and 32%of the total blockade numbers caused by various geological
disasters. The second blocked cause of inclement weather is rainfall and the blocking event rate is up to 68%. And
the peak of blocking occurs in winter and summer. Especially in January , June and July , the blocking occurs most frequently
and the blocking effects are rather larger. The total blocking times in these three months are over 50% of the total times
throughout the year. The blocking conditions of different state roads and provincial highways have great difference and the
accumulative blockade numbers of route G319 is the most.
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