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It has a sand percentage of about 86%.
It has a very low sand percentage of about 10%.
This factor explains that the sand percentage in soil decreases with increase in silt content.
Four different fields were considered on the basis of soil texture variations; especially changes in sand percentage were made.
These subunits are about 532.42, 487.51 and 718.44 ft thick across the three wells with an average sand percentage of about 79%.
This can be explained by the larger W/C ratio and sand percentage, which does not fill the voids in the large granules.
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Open image in new window Fig. 8 Seismic facies and their corresponding sand percentages from interpretation.
The highest sand percentages detected by XS were attributed to local compositional sediment features.
Calculations of sand percent for the seismic facies permit prediction of reservoir potentials implying that seismic facies with higher sand percentages should conform to exploration targets (Fig. 8).
The calculated sand percentages from the log motifs together with lithofacies description of the log motifs were integrated to describe the paleoenvironment of the deposition.
Sand percentages were derived from the gamma-ray log motifs by subtracting one from the volume of shale, which is given as V sh = GRlog − GRmin/GRmax − GRmin, where V sh is the volume of shale, GRlog is the gamma-ray reading of the formation, GRmin is the minimum gamma-ray reading (sand baseline) and GRmax is the maximum gamma-ray reading (shale baseline).
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com