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基于圆盘裂隙物理模型的岩体单一裂隙渗流规律试验研究 被引量:3
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作者 王明玉 刘庆哲 +1 位作者 曲辞晓 李金柱 《岩土力学》 EI CAS CSCD 北大核心 2020年第11期3523-3530,共8页
岩体中裂隙平行板渗流模型被广泛地应用于实际岩体裂隙渗流过程与特征的定量描述与刻画,但实际岩体裂隙渗流的空间域与平行板假设可能相差甚远。因此,裂隙平行板渗流模型应用于实际裂隙渗流条件下的模型有效性及适宜的修正表达方法成为... 岩体中裂隙平行板渗流模型被广泛地应用于实际岩体裂隙渗流过程与特征的定量描述与刻画,但实际岩体裂隙渗流的空间域与平行板假设可能相差甚远。因此,裂隙平行板渗流模型应用于实际裂隙渗流条件下的模型有效性及适宜的修正表达方法成为关注点。选取更接近实际裂隙空间分布的圆盘形状,在室内构建单圆盘裂隙物理模型。通过改变圆盘裂隙的隙宽和裂隙相交产生的水流进出口交线长度,进行不同压力梯度下的渗流试验,探讨不同岩体隙宽和交线长度下的裂隙水渗流规律。试验结果表明,针对不同雷诺数下的非达西流态,达西定律模型在一定程度仍能较好地刻画岩体裂隙渗流量和压力梯度的统计关系,但Forchheimer模型精准度更高。值得注意的是,Forchheimer模型中参数A与B的计算式需要修正。提出了修正方法,并依据试验数据获得了具有一定应用范围的A与B相应修正计算式。研究成果可望为岩体中单一裂隙及复杂裂隙网络渗流研究与工程应用提供一定理论基础与方法借鉴。 展开更多
关键词 岩体裂隙渗流 圆盘裂隙模型 渗流试验 渗流规律 模型修正
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Analysis on temporal and spatial variations of groundwater hydrochemical characteristics in the past decade in southern plain of Beijing, China 被引量:1
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作者 JIANG Ti-sheng qu ci-xiao +3 位作者 WANG Ming-yu SUN Yan-wei HU Bo CHU Jun-yao 《Journal of Groundwater Science and Engineering》 2017年第3期235-248,共14页
Groundwater utilization and protection are crucial for sustainable urban development. This is especially true for Beijing, where groundwater is an important source for urban water supply. In this study, statistical me... Groundwater utilization and protection are crucial for sustainable urban development. This is especially true for Beijing, where groundwater is an important source for urban water supply. In this study, statistical methods, including descriptive statistics, correlation analysis, principal component analysis, and Piper-Tri-linear diagram, were used in analyzing the temporal and spatial variations of the hydrochemical characteristics of groundwater based on monitored data from the southern plain of Beijing, China. Results indicated consistent changes of groundwater's hydrochemical characteristics in different aquifers in the study area. The percentage of HCO_3^-in total anion increased significantly in the groundwater, and hydrochemical water type evolved gradually from Ca-Mg-Cl-SO_4 based to Ca-Mg-HCO_3 based from period 2005-2007 to period 2013-2015. In shallow groundwater, the concentration of Na^+, Ca^(2+), SO_4^(2-), HCO_3^-, and total dissolved solids(TDS) increased from period 2005-2007 to period 2013-2015, and the greatest change came from HCO_3^-, rising from 428.93 to 528.96 mgL^(-1). The changes of main ionic concentrations in the deep groundwater were consistent with those in the shallow groundwater for both periods. However, the variations in deep groundwater were less than those in shallow groundwater. The temporal and spatial variations of hydrochemical characteristics reflect the groundwater quality in the study area. This study could facilitate decision-making process on the protection of groundwater resources to ensure its sustainable utilization. 展开更多
关键词 BEIJING GROUNDWATER Hydrochemical characteristics Temporal and spatial variation Water quality
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