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Overall, our results showed that the extent of permanganate diffusion and reaction depended on rock properties, including porosity, mineralogy, and organic carbon.
In this study, a series of diffusion experiments were performed to measure the permanganate diffusion and reaction in four different types of sedimentary rocks (dark gray mudstone, light gray mudstone, red sandstone, and tan sandstone).
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Potassium permanganate was used to quantify the diffusion in the flow cell.
The diffusion coefficient of potassium permanganate was determined in stop flow measurements and the value, D = 4.0 × 10−5 cm2/s, agreed to previously reported values.
It was found that the error function, erf y/√(Dt)), where y was the position along the transverse line, D the diffusion coefficient of the solute and t was the time, gave reasonable approximation to the diffusion of potassium permanganate in the cell.
I remember permanganate of potash.
One is diffusion.
The United States uses gaseous diffusion.
The design screams diffusion line.
It's diffusion by defusion.
High temperature also hastens diffusion.
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