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谢晓勇,侍克斌.干旱区平原水库渗流及下游土壤盐渍化分析水资源与水工程学报[J].,2014,25(2):180-183
干旱区平原水库渗流及下游土壤盐渍化分析
Analysis of plain reservoir seepage and downstream soil salinization in arid area
  
DOI:10.11705/j.issn.1672-643X.2014.02.038
中文关键词:  稳定渗流  地下水临界深度  土壤盐渍化  ABAQUS软件  平原水库
英文关键词:stable seepage  critical depth of groundwater  soil salinization  ABAQUS software  plain reservoir
基金项目:新疆科技支撑计划项目(201233132); 新疆水利水电工程重点学科基金资助项目(xjzdxk-2010-02-12)
作者单位
谢晓勇,侍克斌 (新疆农业大学 水利与土木工程学院 新疆 乌鲁木齐 830052) 
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中文摘要:
      为预测平原水库蓄水对下游生态环境的影响,在非饱和土力学理论的基础上,利用ABAQUS有限元软件模拟某大型平原水库蓄水后坝体坝基的稳定渗流形态,得到大坝下游的地下水埋藏深度,对比地下水临界深度,判断是否会出现土壤盐渍化现象。计算结果表明:①水库蓄水水位越高,渗流速度就越快,相应水库下游土壤盐渍化的范围也越广。②水库渗漏补充下游地下水,抬高地下水水位随着时间的推移最终会达到稳定状态,此时由水库蓄水引起的土壤盐渍化的程度和范围都达到极限。根据实际工程监测数据与本文计算结果中相对应部分的对比,证明所采用的方法基本可靠,可为平原水库周边土壤盐渍化的防治提供依据。
英文摘要:
      In order to predict the influence of water storage on plain reservoir, the paper used the finite element software ABAQUS to simulate the stabilize percolation structure of some plain reservoir so as to get the burial depth of groundwater and to determine whether there will be the phenomenon of soil salinization by comparing the depth on the basis of theory of unsaturated soil mechanics. The result indicates two sides: ① The higher the water level of reservoir, the faster the seepage velocity , meanwhile the wider the range of soil salinization in the downstream of related reservoir. ② The reservoir leakage recharges groundwater and heightens groundwater level, it finally reach a steady state with time, meanwhile, the degree and range of soil salinization resulting from water storage of reservoir can also reach a steady state. According to the comparison between the actual engineering monitoring data and the corresponding part of the results in this paper, it can be confirmed that the method is basically reliable and can provide the basis for the prevention of soil salinization around the plain reservoir.
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