Entrapped air in soils beneath the water table is one of the key factors controlling the hydraulic behavior under conditions of ponded infiltration, in perched waters, and in unconfined aquifers. The term quasi‐saturated soils defines the soils with entrapped air, and the term quasi‐saturated hydraulic conductivity defines the relationship between the hydraulic conductivity and entrapped air content. This paper focuses on an investigation of how entrapped air, along with other factors, affects the three‐stage temporal behavior of the quasi‐saturated hydraulic conductivity of soils. During the first stage the quasi‐saturated hydraulic conductivity of soils decreases by as much as 5–8 times, presumably because mobile entrapped air blocks the largest pores. During the second stage, as the mobile entrapped air is discharged from the core, the quasi‐saturated hydraulic conductivity of the soils slowly increases. When the mobile air is removed, the remaining immobile entrapped air is discharged as a dissolved phase, and the quasi‐saturated hydraulic conductivity increases rapidly by about 1–2 orders of magnitude, essentially reaching the value of the saturated hydraulic conductivity. During the third stage the hydraulic conductivity is decreased to minimum values. The effects of sealing at the soil surface and microbiological activities are assumed to be major factors in the final decrease of the hydraulic conductivity. This three‐stage temporal behavior of percolation in loam soils is repeatable. A new power law and an exponential relationship are proposed to describe the quasi‐saturated hydraulic conductivity of loams as a function of the entrapped air content.
Boris Faybishenko (1995) studied this question.