路基工程
路基工程
로기공정
SUBGRADE ENGINEERING
2012年
4期
196-201
,共6页
肖楼%董德惠%李金平%章金钊
肖樓%董德惠%李金平%章金釗
초루%동덕혜%리금평%장금쇠
岛状多年冻土%冻土路基%变形特征%沉降变形
島狀多年凍土%凍土路基%變形特徵%沉降變形
도상다년동토%동토로기%변형특정%침강변형
patchy permafrost%subgrade in permafrost regions%deformation characteristics%settlementand deformation
通过漠北公路沿线各试验段不同冻土条件和工程措施下各层土体沉降变形状况,分析东北高纬度岛状多年冻土区路基沉降变形主要发生土层部位及其破坏原因。分析结果表明:路基施工完成后早期路基变形较大,主要由工后不均匀沉降变形引起,变形主要由原天然地面下季节活动层的沉降压缩变形等引起,由于运营时间较短,由多年冻土融化引起的沉降变形很小。路基沉降变形主要发生在暖季,在冷季(11月~次年6月)路基基本保持稳定,变形很小。路基整体变形状况与冻土含冰量、冻土地温有一定的关系。高温多年冻土区比低温多年冻土区变形大。
通過漠北公路沿線各試驗段不同凍土條件和工程措施下各層土體沉降變形狀況,分析東北高緯度島狀多年凍土區路基沉降變形主要髮生土層部位及其破壞原因。分析結果錶明:路基施工完成後早期路基變形較大,主要由工後不均勻沉降變形引起,變形主要由原天然地麵下季節活動層的沉降壓縮變形等引起,由于運營時間較短,由多年凍土融化引起的沉降變形很小。路基沉降變形主要髮生在暖季,在冷季(11月~次年6月)路基基本保持穩定,變形很小。路基整體變形狀況與凍土含冰量、凍土地溫有一定的關繫。高溫多年凍土區比低溫多年凍土區變形大。
통과막북공로연선각시험단불동동토조건화공정조시하각층토체침강변형상황,분석동북고위도도상다년동토구로기침강변형주요발생토층부위급기파배원인。분석결과표명:로기시공완성후조기로기변형교대,주요유공후불균균침강변형인기,변형주요유원천연지면하계절활동층적침강압축변형등인기,유우운영시간교단,유다년동토융화인기적침강변형흔소。로기침강변형주요발생재난계,재랭계(11월~차년6월)로기기본보지은정,변형흔소。로기정체변형상황여동토함빙량、동토지온유일정적관계。고온다년동토구비저온다년동토구변형대。
In connection with the settlement and deformation of soil mass at every layer under different frozen soil conditions and engineering measures in the experimental sections along MOBEI Highway, the subgrade in high-latitude patchy permafrost regions in the Northeast is analyzed against the location where settlement and deformation will mainly occur in the soil layers as well as the failure causes. The analysis result shows that the subgrade is deformed to a greater extent in early period after the construction, mainly caused by uneven post- construction settlement and deformation, wherein the deformation is mostly resulted from the subsidence and compression deformation of seasonal active layers under original natural ground surface and that from thawed permafrost is small due to short operating time. The subgrade will be settled and deformed mainly in warm season, while it stays stable with small deformation in cold season (i.e. from November to June of the following year). The overall deformation has certain relationship with ice content and ground temperature of frozen soil. The deformation in high-temperature permafrost regions is larger than that in low-temperature permafrost regions.