水位线性下降引起的软土一维固结解析解
nalytical solution for one-dimensional consolidation of soft soil induced by linear decline of water table
针对抽取地下水引起的地面沉降问题,推导了大面积抽水导致含水层水位线性下降情况下,相邻上部软土层的一维固结解析解,给出了相应的压缩量和平均固结度计算公式。通过一个算例研究,得到了如下结论:软土层在1m水头差作用下,能够产生相当于土层顶面施加5kPa均布荷载所引起的总压缩量;在含水层水位线性下降过程中,相邻上部软土层的固结速度逐渐加快,水位稳定以后,固结继续进行,但是速度逐渐变缓。
In this paper, the problem of land subsidence caused by groundwater withdrawal was studied. Analytical solution was derived for one-dimensional consolidation of soft soil when the water table of the lower soil layer is declining linearly due to large-scale groundwater withdrawal. Furthermore, formulas were given for calculating amount of compression and average degree of consolidation. Then, a case history was studied. The results show that the amount of compression of soft soil under 1m water head difference is equal to that induced by 5kPa uniformly distributed load on the top of the soil layer. The consolidation rate of soft soil accelerates when the water table of the lower soil layer is declining linearly. In contrast, the consolidation rate of soft soil slows down when the water table of the lower soil layer is steady.
黄大中、王玉林、陶立为、谢康和
水利工程基础科学
抽取地下水水位线性下降一维固结解析解压缩量平均固结度
groundwater withdrawalwater tabledeclining linearlyone-dimensional consolidationanalytical solutionamount of compressionaverage degree of consolidation
黄大中,王玉林,陶立为,谢康和.水位线性下降引起的软土一维固结解析解[EB/OL].(2010-12-30)[2025-08-16].http://www.paper.edu.cn/releasepaper/content/201012-1329.点此复制
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