河道入渗试验过程中地下水水位演化规律研究
首发时间:2016-03-28
摘要:野外大型渗水试验可以有效避免水文地质参数应用中的尺度效应问题。通过监测滹沱河地下水库大型渗水试验中87口地下水位观测井的水位变化,分析渗水试验过程中地下水位滞后规律。6条监测断面上地下水位空间分布和随时间变化特征结果表明,受到地形、入渗场承渗位置等因素共同影响,地下水位的响应呈现明显的滞后现象,且滞后能力与观测孔和入渗场距离密切相关;87口观测井的地下水位响应要素与距离之间的相关关系可得,随着距离增加,地下水位开始响应时间和地下水位峰值出现时间呈现增大趋势,地下水位最大升幅和上升速度呈现减小的趋势;对比各曲线的拟合结果可以看出,入渗场北侧含水层的渗透性最好,其次是河心岛,最弱为入渗场南侧。
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Groundwater Level Variation during Infiltration Test
Abstract:Large-scale field infiltration test could avoid the scale effect of hydrogeological parameters application. Groundwater level lagging capacity has been analyzed based on the groundwater levels variation of 87 observation wells. The spatial and temporal variations of groundwater levels along the six cross sections show that, there is obvious lagging phenomenon, which affected by topography and infiltration locations; the analysis results of correlation between response parameters of groundwater level and distances show that, with the increasing of distance, the response time and the peaking time have a increasing trend, however, the arising ranges and arising speeds have a decrease trend; the contrast between the linear fitting results show that, the permeability order of aquifer is northern infiltration field (the best), central island and southern infiltration field ( the worst)
Keywords: Artificial recharge infiltration test groundwater level Shijiazhuang
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No.4681745152131458****
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