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Study of SPT behavior of penetration resistance under influence of the groundwater level fluctuation, using geostatistical methodology

机译:利用地统计方法研究地下水位波动影响下的渗透阻力的SPT行为

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The kriging ordinary geostatistical methodology was used in mapping the ground-water level to verity the influence of its fluctuation on spatial behavior of the penetration resistance index of the standard penetration test (SPT). The geostatistical mapping was made by carefully separating the 241 boreholes into two big groups, using the criterion of data base analysis monthly and annual pluviometric of the studied area; and as an end result six maps were obtained: groundwater level fluctuation map, penetration resistance index variation maps at a depth of 1,5; 6,0; 8,5; 11,0 and 13,5 m. The greatest variations of penetration resistance index in increase as well as in reduction of the resistance, occurred at a depth of 6,0 and 8,5 m; and the remaining depths: 1,5; 11,0 and 13,5 m were the smallest variations to the penetration resistance index in both situations.
机译:使用克里金(Kriging)普通地统计学方法来绘制地下水位图,以验证其波动对标准渗透试验(SPT)的抗渗透指数空间行为的影响。地统计学图是通过将241个钻孔仔细分成两个大组来进行的,使用研究区域的月度和年度雨量法进行数据库分析。作为最终结果,获得了六个图:地下水位波动图,1.5深度处的渗透阻力指数变化图; 6,0; 8,5; 11,0和13,5 m。渗透阻力指数的最大变化在电阻的增加和减小中都发生在6,0和8.5 m的深度处;其余深度:1.5;在两种情况下,11,0 m和13,5 m是耐穿透性指数的最小变化。

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