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The ideal value for the potassium-rich alkali feldspars is 2.56, which is less than the lowest value for the plagioclases (namely, 2.62 for albite).
The ideal value is 1.
The actual coefficient is 1.5 2.2 times the ideal value.
The values for Ag are close to the ideal value.
The formulas are easy to use and statistically identical to the ideal value of tortuosity factor.
The ideal value is less than 750 µS/cm (Richards 1954).
In the following experiment, the DRR was fixed and corresponds to the ideal value.
The ideal value of adjustment is 1.00, but values between 0.50 and 1.50 are acceptable.
The ideal value of regression coefficient is equal to 1. Relative percentage of error (RPE).
The average hydraulic permeability of the filter was 0.025 Darcy, which is about 5-fold lower than the ideal value.
The critical resolved shear stress of a Fe 31.2 Pd (at.%) single crystal is close to the ideal value.
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