It's not pH, but a mineral redox buffer is used to constrain this quantity for oxygen in a rock system, and in such an analysis the log of this quantity is plotted against temperature for each component of the rock. It's not heat, but in the McKay et al approach this quantity times its namesake capacity is equal to the concentration. In a high-pressure VLE, the equation for this quantity is modified with the Poynting correction factor. It doesn't appear in Raoult's law, but this quantity for a component is equal to its (*) mole fraction times its total by the Lewis-Randall rule. This quantity is equal to its standard form times the exponential of the difference of the current and standard chemical potential over RT. At a given chemical potential, this quantity is equal to the pressure for an ideal gas. For 10 points, name this quantity which gives the tendency of
It's not pH, but a mineral redox buffer is used to constrain this quantity for oxygen in a rock system, and in such an analysis the log of this quantity is plotted against temperature for each component of the rock. It's not heat, but in the McKay et al approach this quantity times its namesake capacity is equal to the concentration. In a high-pressure VLE, the equation for this quantity is modified with the Poynting correction factor. It doesn't appear in Raoult's law, but this quantity for a component is equal to its (*) mole fraction times its total by the Lewis-Randall rule. This quantity is equal to its standard form times the exponential of the difference of the current and standard chemical potential over RT. At a given chemical potential, this quantity is equal to the pressure for an ideal gas. For 10 points, name this quantity which gives the tendency of a molecule to escape a particular phase.
It's not pH, but a mineral redox buffer is used to constrain this quantity for oxygen in a rock system, and in such an analysis the log of this quantity is plotted against temperature for each component of the rock.
fugacity