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黄土潜水层深井降水三维有限元模拟研究
引用本文:康 婷,白应生,郭增玉.黄土潜水层深井降水三维有限元模拟研究[J].西北农林科技大学学报(社会科学版),2006,34(4):139-142.
作者姓名:康 婷  白应生  郭增玉
作者单位:1. 空军工程大学,工程学院,陕西,西安,710038
2. 西安理工大学,水利水建学院,陕西,西安,710048
摘    要:视抽水井为定流量边界,并假定流量沿井壁的分布是均匀的,在此条件下建立了黄土厚潜水层深井抽水时的三维渗流模型,并用C++语言编制了三维有限元程序,计算了单井抽水、双井抽水时水位随时间的变化规律,计算结果与观测结果误差较小。另计算了少陵塬隧洞第一期降水方案的降水效果,表明其不能满足施工进度的要求,并对此方案作了修改,在后期施工中取得了良好的降水效果。

关 键 词:黄土潜水层  三维有限元  深井降水
文章编号:1671-9387(2006)04-0139-04
收稿时间:2005-07-01
修稿时间:2005年7月1日

Three dimensional finite simulation of deep well dewatering in loess phreatic stratum
KANG Ting,BAI Ying-sheng,GUO Zeng-yu.Three dimensional finite simulation of deep well dewatering in loess phreatic stratum[J].Journal of Northwest Sci-Tech Univ of Agr and,2006,34(4):139-142.
Authors:KANG Ting  BAI Ying-sheng  GUO Zeng-yu
Institution:1 The Engineering Institute,Air Force Engineering University,Xi’an,Shannxi 710038,China;2 The Water Conservancy and Water Electricity Institute,Xi’an University of Technology,Xi’an,Shannxi 710048,China)
Abstract:Three dimensional seepage model of deep well dewatering in loess phreatic stratum was set up.Deep wells were regarded as invariable rate of flow boundary.It was supposed that the rate of flow was even on the wall of wells.Three dimensional program with computer language C~(++) was made in this paper.The rule in the change of groundwater table with time was analyzed on single well pumping and double wells pumping.The error between calculated results and tested results was small.The dewatering effect of No.1 plan in Shaolingyuan was also analyzed and the result showed that this plan could not meet the work speed.Therefore the plan was optimized based on calculation.From then on,dewatering effect was very good.
Keywords:phreatic stratum of loess  three-dimensional finite element  deep well dewatering
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