Abstract This paper presents a comprehensive review of published literature on soil piping phenomena. The first tools to design earth dams to resist piping were developed during 1910–1935. Filter criteria for dispersive soils was refined in the 1970’s. Piping phenomena are generally defined as: (1) heave, (2) internal erosion, (3) backwards erosion, although other modes are possible. Recent work on piping highlights the limitations of the occurrence of piping and the role that design and construction may play in a large percentage of piping failures. Standardized laboratory procedures are available to assess piping potential in cohesive materials, but no such methods exist for non-cohesive soils. However, methods are available for evalu-ati...
Filters represent a very important component of earth structures. Indeed a large percentage of emban...
Many field observations have led to speculation on the role of piping in embankment failures, landsl...
Internal instability of a widely graded cohesionless soil refers to a phenomenon in which its finer ...
Many embankment dams on soil and fractured rock foundations have failed due to the formation of pipe...
Backward erosion piping is a type of internal erosion. It occurs beneath water structures as a resul...
Backward Erosion Piping (BEP) is a form of internal erosion that is prevalent in sandy foundations o...
Background This research focuses on the Herbert Hoover Dike (HHD) and the soil it was built with. Th...
Piping is one of the most important causes of dam failure. Concentrated leak erosion, which occurs i...
Earth-fill dams are the most common types of dam and the most economical choice. However, they are m...
Seepage direction is crucial for understanding the critical state and development of piping erosion....
Backward erosion piping is one of the four main types of internal erosion threatening dams, dikes an...
Piping and hydraulic fracturing (heave) are phenomena which can threaten the stability of flood defe...
One of the most frequent causes of failure of earthen structures subjected to water seepage, such as...
This paper is an extension of previous work which characterises soil behaviours using the grading en...
This paper is an extension of previous work which characterises soil behaviours using the grading en...
Filters represent a very important component of earth structures. Indeed a large percentage of emban...
Many field observations have led to speculation on the role of piping in embankment failures, landsl...
Internal instability of a widely graded cohesionless soil refers to a phenomenon in which its finer ...
Many embankment dams on soil and fractured rock foundations have failed due to the formation of pipe...
Backward erosion piping is a type of internal erosion. It occurs beneath water structures as a resul...
Backward Erosion Piping (BEP) is a form of internal erosion that is prevalent in sandy foundations o...
Background This research focuses on the Herbert Hoover Dike (HHD) and the soil it was built with. Th...
Piping is one of the most important causes of dam failure. Concentrated leak erosion, which occurs i...
Earth-fill dams are the most common types of dam and the most economical choice. However, they are m...
Seepage direction is crucial for understanding the critical state and development of piping erosion....
Backward erosion piping is one of the four main types of internal erosion threatening dams, dikes an...
Piping and hydraulic fracturing (heave) are phenomena which can threaten the stability of flood defe...
One of the most frequent causes of failure of earthen structures subjected to water seepage, such as...
This paper is an extension of previous work which characterises soil behaviours using the grading en...
This paper is an extension of previous work which characterises soil behaviours using the grading en...
Filters represent a very important component of earth structures. Indeed a large percentage of emban...
Many field observations have led to speculation on the role of piping in embankment failures, landsl...
Internal instability of a widely graded cohesionless soil refers to a phenomenon in which its finer ...