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Both parameters indicate a significant reduction in recombination.
All parameters indicate that pure groundwater had been obtained.
Thermodynamic parameters indicate the nature of chromium sorption.
The location parameters indicate that the items were spread over the continuum of the scale.
Positive signs of values of both parameters indicate convex ellipsoidal surface.
These parameters indicate the formation of C S H phase with an increase in curing period.
BP, the alluvial architecture and grain-size parameters indicate a wandering river.
The validation parameters indicate that method was suitable for the intended purpose.
Thermodynamic parameters indicate the sorption process to be spontaneous and exothermic.
Kinetic parameters indicate that the formation of hydrocarbons can be suppressed in the presence of MnOx.
The lattice parameters indicate residual stress in the compact part of the deposit.
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