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Hydrology And Drainage Of A Thin Colluvium Hillside In Delhi Township, Ohio. Public Deposited
The hydrology of a thin colluvium hillside at the Delhi Pike landslide complex, approximately 15 km west of downtown Cincinnati, is controlled by infiltration and evapotranspiration. Pore water pressures approach $-$10 m H$\sb2$O during summer and autumn, but rise to $-$1 m H$\sb2$O or higher after several days of steady winter rains. This state of near saturation is maintained until large trees leaf out and pore pressures fall dramatically in late spring.
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Permanent link to this page: https://scholar.uc.edu/show/bn9996777