铁道学报
鐵道學報
철도학보
2015年
6期
112-117,118
,共7页
申林方%王志良%魏纲%谢建斌
申林方%王誌良%魏綱%謝建斌
신림방%왕지량%위강%사건빈
隧道%超孔隙水压力%保角变换%消散%盾构
隧道%超孔隙水壓力%保角變換%消散%盾構
수도%초공극수압력%보각변환%소산%순구
tunnel%excess pore water pressure%conformal mapping%dissipation%shield
基于Terzaghi‐Rendulic二维固结理论,将土体视为饱和弹性介质,采用保角变换的方法将含有圆环(隧道)的半无限空间区域映射为圆环域,建立衬砌在不透水的情况下隧道周围土体超孔隙水压力分布的控制方程。采用分离变量法对该控制方程进行求解,得到处于饱和弹性土体中隧道周围土体超孔隙水压力消散的解析解。结合算例分析不同隧道埋深的情况下隧道顶部及水平向超孔隙水压力随时间变化的情况,以及埋深一定时隧道上方土体超孔隙水压力的变化规律。研究结果表明:隧道埋深越深,周围土体中超孔隙水压力的消散速度越慢;在开始阶段超孔隙水压力消散速度较快,随着时间的推移消散速度逐渐减慢;隧道周围土体水平向超孔隙水压力的消散速度要比竖向的消散速度快;隧道上方土体距离隧道越近,超孔隙水压力的消散速度越快。
基于Terzaghi‐Rendulic二維固結理論,將土體視為飽和彈性介質,採用保角變換的方法將含有圓環(隧道)的半無限空間區域映射為圓環域,建立襯砌在不透水的情況下隧道週圍土體超孔隙水壓力分佈的控製方程。採用分離變量法對該控製方程進行求解,得到處于飽和彈性土體中隧道週圍土體超孔隙水壓力消散的解析解。結閤算例分析不同隧道埋深的情況下隧道頂部及水平嚮超孔隙水壓力隨時間變化的情況,以及埋深一定時隧道上方土體超孔隙水壓力的變化規律。研究結果錶明:隧道埋深越深,週圍土體中超孔隙水壓力的消散速度越慢;在開始階段超孔隙水壓力消散速度較快,隨著時間的推移消散速度逐漸減慢;隧道週圍土體水平嚮超孔隙水壓力的消散速度要比豎嚮的消散速度快;隧道上方土體距離隧道越近,超孔隙水壓力的消散速度越快。
기우Terzaghi‐Rendulic이유고결이론,장토체시위포화탄성개질,채용보각변환적방법장함유원배(수도)적반무한공간구역영사위원배역,건립츤체재불투수적정황하수도주위토체초공극수압력분포적공제방정。채용분리변량법대해공제방정진행구해,득도처우포화탄성토체중수도주위토체초공극수압력소산적해석해。결합산례분석불동수도매심적정황하수도정부급수평향초공극수압력수시간변화적정황,이급매심일정시수도상방토체초공극수압력적변화규률。연구결과표명:수도매심월심,주위토체중초공극수압력적소산속도월만;재개시계단초공극수압력소산속도교쾌,수착시간적추이소산속도축점감만;수도주위토체수평향초공극수압력적소산속도요비수향적소산속도쾌;수도상방토체거리수도월근,초공극수압력적소산속도월쾌。
Based on Terzaghi‐Rendulic two‐dimensional consolidation theory , soil is regarded as saturated elastic medium . With the semi infinite space area that contains circular ring (tunnel) being mapped to a circular ring region using conformal mapping method , the control equation for dissipation of excess pore water pressure in the soil around the tunnel was established in the case of impermeable lining . The method of separation of varia‐bles was applied to solve the control equation , to obtain the analytical solution for dissipation of excess pore water pressure in the soil around the tunnel that is situated in saturated elastic soil .Combined with the calcula‐tion ,an analysis was performed on the time‐varying excess pore water pressure at the top of tunnel and hori‐zontal level under different depth of tunnel ,as well as on the change law of excess pore water pressure in the soil above the tunnel . The results showed that the deeper the tunnel was , the slower the dissipating speed of excess pore water pressure in the surrounding soil . The dissipating speed of excess pore water pressure was faster at the beginning , while it became slower gradually with the passage of time . The dissipating speed of horizontal excess pore water pressure in the soil around the tunnel was faster than that of verticle excess pore water pressure .The closer the soil above the tunnel is to the tunnel ,the faster the dissipating speed of excess pore water pressure .