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Quartz cement is considered the major porosity reducing element in quartz-dominated sandstones at depth greater than 2000 m (Ehrenberg 1990).
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Additionally, low porosity reduces the reactivity of the shale.
In the temperature range from 1300 to 1400 °C, the porosity reduces from 13 to 5%% (predominantly open porosity).
In a newly deposited ooze sediment, porosity ranges from 60%to80%0% but porosity reduces with burial.
However, following the ANN/GA optimization procedure, the porosity reduces to just 5.6%.
The pore size and porosity reduced as the content of GO was increased.
In inverse models using different initial values, the results had these similarities: (1) the effective porosity was always lower than the expected bulk porosity, (2) effective porosity in the center of the fresh water plume was always lower than surrounding values, and (3) small relative adjustments (a few percent) in effective porosity reduced the sum-of-squared errors by about 50%.
Compaction and cementation have exerted the major porosity loss in the Buchan Formation.
According to the reported data, although CF-Roll (which contains no coral microparticles) possesses high total porosity value, the major porosity percentage relates to the closed pores.
The other major benefit is reduced risk.
The analyses showed that cracks and porosity were reduced successfully.
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CEO of Professional Science Editing for Scientists @ prosciediting.com