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Slope stability of an unsaturated embankment with and without natural pore water salinity subjected to rainfall infiltration 被引量:1
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作者 SADEGHI Hamed KOLAHDOOZ Ali AHMADI Mohammad-Mehdi 《岩土力学》 EI CAS CSCD 北大核心 2022年第8期2136-2148,共13页
Natural soils contain a certain amount of salt in the form of dissolved ions or electrically charged atoms,originated from the long-term erosion by acidic rainwater.The dissolved salt poses an extra osmotic water pote... Natural soils contain a certain amount of salt in the form of dissolved ions or electrically charged atoms,originated from the long-term erosion by acidic rainwater.The dissolved salt poses an extra osmotic water potential being normally neglected in laboratory measurements and numerical analyses.However,ignorance of salinity may result in overestimation of stability,and the design may not be as conservative as thought.Therefore,this research aims to first experimentally examine the influence of pore water salinity on water retention curve and saturated permeability of natural dispersive loess under saline and desalinated conditions.Second,the measured parameters are used for stability analyses of a railway embankment in an area subjected to regional rainfall incident.Eventually,a numerical parametric study is carried out to explore the significance of different rainfall schemes,construction patterns,and anisotropic permeability on the factor of safety.Results reveal that desalinization suppresses the water retention capability,which in turn results in a tremendous declination of unsaturated hydraulic conductivity.Despite the natural saline embankment,rainfall can hardly infiltrate into the desalinated embankment due to the lower conductivity.Therefore,the factor of safety for natural saline conditions drops notably,while only marginal changes occur in the case of the desalinated embankment. 展开更多
关键词 slope stability water salinity osmotic potential dispersive loess rainfall patterns
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我国东部夏季三类雨型的诊断和预测方法研究 被引量:7
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作者 陈寅生 施能 刘海波 《应用气象学报》 CSCD 北大核心 1995年第3期327-332,共6页
采用三级逐步判别方法对我国东部地区夏季(6、7、8月)降水进行客观诊断和预测。结果表明,利用6个测站的夏季降水量即可定量诊断我国夏季雨型,利用冬季500hPa极涡面积和北半球遥相关型指数建立起来的三级判别函数只包含7... 采用三级逐步判别方法对我国东部地区夏季(6、7、8月)降水进行客观诊断和预测。结果表明,利用6个测站的夏季降水量即可定量诊断我国夏季雨型,利用冬季500hPa极涡面积和北半球遥相关型指数建立起来的三级判别函数只包含7个因子。历史拟合率为38/39,试报效果也较好,从而为我国东部地区夏季降水型的客观预报提供了有应用价值的预报模型。 展开更多
关键词 夏季 雨型 极涡面积 遥相关型 诊断 降水预报
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