We have conducted gas migration experiments in mixed wetting bead models saturated with water in which the beads were composed of oil-wetting and water-wetting beads.
In comparison with a fully saturated model, the model results revealed no acceptable model fit for young adults (chi-square/ df = 286/10, CFI =.987, TLI =.862, RMSEA =.140), middle-aged adults (chi-square/ df = 326/10, CFI =.991, TLI =.902, RMSEA =.131), or older adults (chi-square/ df = 95/10, CFI =.996, TLI =.959, RMSEA =.083).
The gas hydrate saturation estimated from electrical resistivity log and core data shows maximum 20%% pore spaces saturated with gas hydrate from anisotropic modeling, which is comparable to gas hydrate saturation along seismic profile estimated from inverted velocity constrained by logs.
Larger sparging influence zones (de-saturated zone due to air injection) were observed for the air sparging processes using the 2-D model initially saturated with high-viscosity solutions, than those without a thickener in the aqueous solution.
The model is saturated with experimental oil.
The model was saturated with crude oil at an injection rate of 0.2 mL/min.
Nield and Kuznetsov [8] investigated thermal instability in a porous medium saturated with nanofluid using the Brinkman model.
The procedure of experiment is described as follows: Open image in new window Fig. 2 Chart of experimental flow (1) The model is saturated with experimental oil.
The starting model is saturated with all fixed main effects, with all fixed interactions with time and with random intercepts and random slopes.
In this step, CO2 molecules within the pores were dissolved in water and consequently the model is fully saturated with water.
In this section we establish that increases in pCO2 perturb groundwater chemistry of domestic aquifers by comparing the geochemical signatures of the High Plains aquifer and a model aquifer column saturated with CO2(g) as a function of depth.
