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Next, we simulated water saturation in a porous medium (sand) with a bank, by using both the ASG method and a modified Picard (MP) method.
Total four stratigraphic units: unit A (gravel) – with a lens of medium sand (unit A′) is the oldest; overlain by units B – medium to coarse sand; unit C – with fine to medium sand; and unit D – fine to medium sand with scattered gravel were observed in trench.
The deepest core along the Gyra fan structure (LEF 1) shows well sorted fine to medium sand with a unimodal grain size distribution at its base.
The grain size is medium sand with a slight tendency to finer sand in the easterly outcrops, and sorting is moderate to well (Fig. 4d).
According to grain size distribution, soil type can be classified as a sandy soil with 96%% of grains between 0.063 and 1 mm (matching a medium sand with high amount of fine sand).
And also, it shows fine sand with clay from a depth of less than 3 m, followed by fine to medium sand with clay, quartzite pieces with clay and kankar, gravel with sand and clay, and clay with fine sand from depths of 3 to 10, 10 to 34, 34 to 64 and 64 to 174 m from surface, respectively, at Motumala.
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The seafloor sediments consist largely of fine to medium sands with low mud content (<5%).
The sand fraction is also much coarser than at the other two sites, being dominated by medium sand and with relatively little fine sand.
Oil was infiltrated and allowed to redistribute across the horizontal length of a two-dimensional tank filled with medium sand.
Experiments were performed to investigate the pressure drops for both single and immiscible two component liquid-liquid aqueous-organic flows through the same rectangular serpentine channel with medium sand packing.
The slide involved the sequence of coarse to medium friable sand units overlying fine to medium sand body inter-bedded with thin, impermeable claystone layers.
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