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- W2031618708 abstract "The authors have presented an interesting description of the occurrence and development of seepage steps in the semi-arid Great Plains. Subsurface flow at the contact between the more permeable surficial mantle material and the underlying more impermeable weathered bedrock is shown to be responsible for the formation of these features. It appears that an additional requisite for the development of seepage steps is a mantle material which is sufficiently cohesionless, or which becomes essentially cohesionless upon saturation by rainfall, and in which the grains are sufficiently small (fine sand or silt size) to be eroded at an exposed face by the seepage flow emerging at the contact of the permeable and more impermeable zones. The grain-size analyses show that the mantle material of the area studied meets these requirements, with approximately 75 pct of the soil constituents being of silt and fine sand size and from 20 to 2pct only of clay size (equivalent diameter less than 0.002 mm)." @default.
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- W2031618708 date "1956-01-01" @default.
- W2031618708 modified "2023-09-27" @default.
- W2031618708 title "Discussion of “Development and significance of seepage steps in slope erosion”rdquo;" @default.
- W2031618708 doi "https://doi.org/10.1029/tr037i005p00636" @default.
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