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首页> 外文期刊>Journal of Geography and Geology >A Framework for Assessing Spatial Distribution of Soil Properties in Levee Systems Based on Underlying Geology and River Morphology
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A Framework for Assessing Spatial Distribution of Soil Properties in Levee Systems Based on Underlying Geology and River Morphology

机译:基于基础地质学和河流形态学的堤防系统土壤性质空间分布评估框架

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摘要

Flood protection systems are complex, interconnected engineered systems, where failure at one location means the failure of the entire system. Earthen levees, the systems’ major component, are at risk from many causes of failure including seepage, overtopping, erosion and instability due to seismic loading. Levees stretch for long distances and are formed through various geologic processes and human activities over time, however information regarding soil properties is collected only at limited point locations and varies significantly both laterally and with depth. Prediction of levee performance in locations where no soil data is available becomes a limitation for system risk assessment studies. This study attempts to test the hypotheses that spatial variability of soil properties is correlated to regional variables such as distance from nearest river segment, river meandering sinuosity index and surface geology. A geostatistical ordinary kriging approach was used for developing these correlations. The specific areas used for data collection and analysis and model development in this study were sub-sections of the larger Sacramento River Flood Control Project (SRFCP) in northern California. Soil strength parameters of identified levee stratigraphy layers were statistically analyzed using a geostatistical ordinary kriging approach and correlated to preselected regional variables. Global observations that applied across the study area included the increasing trend of undrained shear strength for cohesive soils, Su, with increasing distance from the river, and decreasing trend of Su with increasing river Sinuosity Index levels. Only local trends were observed in the relation of friction angle of cohesionless soils, ?, with Sinuosity Index, as well as in the relation of Su and ? with geological formations.
机译:防洪系统是复杂的,相互连接的工程系统,其中一个位置的故障意味着整个系统的故障。土堤是系统的主要组成部分,它受到许多破坏原因的威胁,包括渗水,翻倒,侵蚀和地震荷载引起的不稳定。堤坝伸展很长一段距离,并通过各种地质过程和人类活动随时间而形成,但是有关土壤性质的信息仅在有限的点位置收集,并且在横向和深度上都有很大变化。在没有土壤数据可用的地方,堤防性能的预测成为系统风险评估研究的局限。这项研究试图检验以下假设:土壤性质的空间变异性与区域变量有关,例如距最近河段的距离,河曲曲率指数和地表地质。地统计学的普通克里金法被用于发展这些相关性。本研究中用于数据收集,分析和模型开发的特定区域是加利福尼亚北部萨克拉曼多河防洪项目(SRFCP)的小节。使用地统计普通克里金法对确定的堤坝地层的土壤强度参数进行统计分析,并将其与预选的区域变量相关联。在整个研究区域内应用的全球观测结果包括:粘性土壤Su的不排水抗剪强度随距河的距离增加而增加,而Su随河水细度指数水平增加而减少的趋势。在无粘性土的摩擦角与sinosusity指数之间的关系,以及与Su和α的关系中,仅观察到局部趋势。与地质构造。

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