It is seen that the fugacity
of non-associating components in the mixture depends on the association constant (K) of the associating component.
The high reactivity is shown by the potential difference between the upper edge of the field where metallic Nb is stable and the line where the fugacity
of hydrogen is [10.
coefficient of pure species A; Equation (25)
4] C/mol) [MATHEMATICAL EXPRESSION NOT REPRODUCIBLE IN ASCII] fugacity
Iron partitioning between basaltic melts and clinopyroxene as a function of oxygen fugacity
21) The Petrarchan lover's four perturbations of the mind are further exacerbated by his deep awareness of time's fugacity
, which he sees at work in his body, as he watches his hair turn white, as well as in his soul, as he commiserates with himself because time robs him of his own cupidity's aspirations, while weighing him down with increased fear and sadness.
Buddington and Lindsley (1964) have shown that hematite will not reduce to magnetite at 500[degrees] C unless the oxygen fugacity
is less than [10.
Nature unfolds without reference to human concepts of energy, entropy, or fugacity
We will explore the influences of pressure, temperature, oxygen fugacity
and key bulk compositional variables such as Na2O/CO2 on very deep subduction of carbonate and on the volumes and compositions, and fates of carbonated partial melts.
The interaction of long-chain polymers with an impenetrable surface can be modelled by restricting SAWs to a half-space, and associating another fugacity
y with vertices (or edges) in the boundary of the half-space which are visited by a walk.
2009) developed a fugacity
model for an office to estimate emission rates of PBDEs from specific office products.
Diffusional transport of atomic hydrogen depends on the hydrogen fugacity
(function of gas pressure) at the crack tip, the kinetics of the dissociation reaction, and the concentration (activity) and stress field in the steel near the crack tip.
After definition of the EoS (PC-SAFT or SL) and assuming that polymers are monodisperse with a molecular weight of 100,000 g/mol, conventional relationships can be applied to the fugacity
calculations in the liquid-fluid equilibria (LFE):
The compositions of coexisting magnetite and ilmenite can be used to estimate liquidus temperatures and oxygen fugacity
(Andersen and Lindsley, 1988) of magmas, although subsolidus exsolution produces intergrowths that complicate application of the geothermometer/oxygen barometer in slowly cooled, coarse-grained rocks.
Detailed mineral compositions (EMPA) are employed to evaluate P, T, and fugacity
conditions for magmatic-hydrothermal activity related to the granodiorite, based on various geothermobarometric calibrations.