铁道工程学报
鐵道工程學報
철도공정학보
JOURNAL OF THE RAILWAY ENGINEERING SOCIETY
2013年
11期
7-12
,共6页
孙文%吴亚平%蔺鹏臻%胡莉莉
孫文%吳亞平%藺鵬臻%鬍莉莉
손문%오아평%린붕진%호리리
青藏铁路%次生不良冻土%数值分析%防治措施
青藏鐵路%次生不良凍土%數值分析%防治措施
청장철로%차생불량동토%수치분석%방치조시
Qinghai -Tibet railway%secondary harmful frozen soil%numerical analysis%control measures
研究目的:多年冻土区修筑路基工程会形成次生不良冻土现象,次生不良冻土对铁路、公路路基等建筑物会产生各种危害。研究多年冻土区不良冻土现象的形成机理和发育对防治次生不良冻土的发生和发展,保证工程的稳定和安全有着非常重要的意义。本文通过对次生不良冻土现象中的热融滑坍进行数值分析并提出次生灾害的防治及工程的保护措施。研究结论:本文对多年冻土区次生不良灾害的形成机理及变化过程进行研究,得出如下结论:(1)路基的阴坡和阳坡之间存在热差异,在吸收热量时路基阳坡融化深度比阴坡融化深度要大,阴阳坡效应对路基融化深度的影响是不容忽视的;(2)考虑热融沟渗流作用的影响时路基横向的不均匀变形会加剧,从而会形成路基纵向裂缝的病害,严重影响路基的稳定性;(3)本文为在多年冻土地区的工程建设提供了一定的理论依据,对防治次生不良冻土灾害具有参考意义。
研究目的:多年凍土區脩築路基工程會形成次生不良凍土現象,次生不良凍土對鐵路、公路路基等建築物會產生各種危害。研究多年凍土區不良凍土現象的形成機理和髮育對防治次生不良凍土的髮生和髮展,保證工程的穩定和安全有著非常重要的意義。本文通過對次生不良凍土現象中的熱融滑坍進行數值分析併提齣次生災害的防治及工程的保護措施。研究結論:本文對多年凍土區次生不良災害的形成機理及變化過程進行研究,得齣如下結論:(1)路基的陰坡和暘坡之間存在熱差異,在吸收熱量時路基暘坡融化深度比陰坡融化深度要大,陰暘坡效應對路基融化深度的影響是不容忽視的;(2)攷慮熱融溝滲流作用的影響時路基橫嚮的不均勻變形會加劇,從而會形成路基縱嚮裂縫的病害,嚴重影響路基的穩定性;(3)本文為在多年凍土地區的工程建設提供瞭一定的理論依據,對防治次生不良凍土災害具有參攷意義。
연구목적:다년동토구수축로기공정회형성차생불량동토현상,차생불량동토대철로、공로로기등건축물회산생각충위해。연구다년동토구불량동토현상적형성궤리화발육대방치차생불량동토적발생화발전,보증공정적은정화안전유착비상중요적의의。본문통과대차생불량동토현상중적열융활담진행수치분석병제출차생재해적방치급공정적보호조시。연구결론:본문대다년동토구차생불량재해적형성궤리급변화과정진행연구,득출여하결론:(1)로기적음파화양파지간존재열차이,재흡수열량시로기양파융화심도비음파융화심도요대,음양파효응대로기융화심도적영향시불용홀시적;(2)고필열융구삼류작용적영향시로기횡향적불균균변형회가극,종이회형성로기종향렬봉적병해,엄중영향로기적은정성;(3)본문위재다년동토지구적공정건설제공료일정적이론의거,대방치차생불량동토재해구유삼고의의。
Research purposes:In permafrost regions,secondary harmful frozen soil phenomena can be formed by constructing subgrade engineering,and the secondary harmful frozen soil has many harmful impacts on buildings such as railway,highway roadbed.Studying the formation mechanism and development of the adverse phenomenon about frozen soil in permafrost regions has very important significance for controlling the happening and development of the secondary harmful frozen soil,and at the same time for guaranteeing the stability and safety of the engineering.In this article,we put forward the prevention of secondary disasters and engineering protection measures by analysising the thaw -frozenlandslide in secondary harmful frozen soil phenomena. Research conclusions:In this paper,we studied the formation mechanism and changing process of secondary harmful frozen soil in permafrost regions and got the following conclusions:(1 )Thermal differences exist between shady slope and sunny slope of roadbed,melting depth in sunny slope is bigger than shady slope when absorbing heat,and the effect of shady and sunny slope on the depth of roadbed melting cannot be ignored;(2)Considering the seepage effect,roadbed transverse inhomogeneous deformation will increase,which will form the disease of roadbed longitudinal cracks and have serious influence on the stability of the roadbed;(3)In this paper,we provide some theoretical foundations about the engineering construction in permafrost regions,which have reference meaning for controlling the secondary harmful frozen soil.