AIR ENTRAPMENT EFFECTS ON INFILTRATION-RATE AND FLOW INSTABILITY

Experiments were conducted to quantify the effects of entrapped air on water infiltration into a loamy sand. Transparent three-dimensional ( 3-D) and 2-D columns were used for experiments carried out for two inf iltration conditions: (1) when air was free to move ahead of the wetti ng front and leave the bottom of the column (air draining) and (2) whe n air was confined ahead of the wetting front and hence could escape o nly through the soil surface (air confining). The measurement setup wa s composed of a tension-pressure infiltrometer, an air flowmeter, wate r manometers, and video-picture cameras. We applied both positive and negative water pressures at the soil surface and measured the simultan eous changes in the rates of water inflow and air outflow, the air pre ssure ahead of the wetting front, and the dynamic behavior and advance of the wetting front. The air pressure ahead of the wetting front for the air-confining condition was generally found to increase with time rather than reaching a constant level, as observed in other studies b y other researchers. The air pressure fluctuated locally because of ai r escaping from the soil surface. On the basis of an analysis of the r esults we present two empirical equations to predict the maximum air p ressure at which air begins to erupt from the soil surface and to pred ict the minimum air pressure at which air eruption stops. We found tha t the infiltration rate was always equal to, and controlled by, the ra te of air outflow. The infiltration rate varied inversely with the air pressure ahead of the wetting front and with the pending depth at the soil surface. The infiltration rate fluctuated with time rather than undergoing changes in a three-stage process, as is often characterized in the literature. The volume of residual entrapped air in the air-co nfining condition increased 7% on average, and the infiltration rate d ecreased threefold to tenfold as compared to the air-draining conditio n. Finally, it was shown that the air-confining infiltration flow is f ingered and unstable, consistent with the predictions of an existing t heory.