affinity: Chemical Affinities of Formation Reactions

Description Usage Arguments Details Value References See Also Examples

View source: R/affinity.R

Description

Calculate the chemical affinities of formation reactions of species.

Usage

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  affinity(..., property=NULL, sout=NULL, exceed.Ttr=FALSE,
    return.buffer=FALSE, balance="PBB", iprotein=NULL, loga.protein=-3)

Arguments

...

numeric, zero or more named arguments, used to identify the variables of interest in the calculations

property

character, the property to be calculated. Default is A, for chemical affinity of formation reactions of species of interest

sout

list, output from subcrt

exceed.Ttr

logical, allow subcrt to compute properties for phases beyond their transition temperature?

return.buffer

logical. If TRUE, and a buffer has been associated with one or more basis species in the system, return the values of the activities of the basis species calculated using the buffer. Default is FALSE.

balance

character. This argument is used to identify a conserved basis species (or PBB) in a chemical activity buffer. Default is PBB.

iprotein

numeric, indices of proteins in thermo$protein for which to calculate properties

loga.protein

numeric, logarithms of activities of proteins identified in iprotein

Details

affinity calculates the chemical affinities of reactions to form the species of interest from the basis species. The equation used to calculate chemical affinity A is A=RT*ln(K/Q), where K denotes the equilibrium constant of the reaction and Q stands for the activity product of the species in the reaction. The calculation of chemical affinities relies on the current definitions of the basis species and species of interest. Calculations are possible at single values of temperature, pressure, ionic strength and chemical activities of the basis species, or as a function of one or more of these variables.

Zero, one, or more leading arguments to the function identify which of the chemical activities of basis species, temperature, pressure and/or ionic strength to vary. The names of each of these arguments may be the formula of any of the basis species of the system, or T, P, pe, pH, Eh, or IS (but names may not be repeated). The names of charged basis species such as K+ and SO4-2 should be quoted when used as arguments. The value of each argument is of the form c(min, max) or c(min, max, res) where min and max refer to the minimimum and maximum values of variable identified by the name of the argument, and res denotes the resolution, or number of points along which to do the calculations; red is assigned a default value of 128 if it is missing. For any arguments that refer to basis species, the numerical values are the logarithms of activity (or fugacity for gases) of that basis species.

If T, P, and/or IS are not among the vars, their constant values can be supplied in T, P, or IS (in mol kg^-1). The units of T and P are those set by T.units and P.units (on program start-up these are °C and bar, respectively). sout, if provided, replaces the call to subcrt, which can greatly speed up the calculations if this intermediate result is stored by other functions (e.g., transfer). exceed.Ttr is passed to subcrt so that the properties of mineral phases beyond their transition temperatures can optionally be calculated.

If one or more buffers are assigned to the definition of basis species, the logarithms of activities of these basis species are taken from the buffer (see buffer).

The iprotein and loga.protein arguments can be used to compute the chemical affinities of formation reactions of proteins that are not in the current species definition. iprotein contains the indices (rownumbers) of desired proteins in thermo$protein. This uses some optimizations to calculate the properties of many proteins in a fraction of the time it would take to calculate them individually.

When the length(s) of the variables is(are) greater than 3, the function enters the transect mode of operation. In this mode of operation, instead of performing the calculations on an n-dimensional grid, the affinities are calculated on a transect of changing T, P, and/or chemical activity of basis species.

The function can also be used to calculate other thermodynamic properties of formation reactions. Valid properties are A or NULL for chemical affinity, logK or logQ for logarithm of equilibrium constant and reaction activity product, or any of the properties available in subcrt except for rho. The properties returned are those of the formation reactions of the species of interest from the basis species. It is also possible to calculate the properties of the species of interest themselves (not their formation reactions) by setting the property to G.species, Cp.species, etc. Except for A, the properties of proteins or their reactions calculated in this manner are restricted to nonionized proteins.

Value

A list, elements of which are sout output from subcrt, property name of the calculated property (A for chemical affinity), basis and species definition of basis species and species of interest in effect at runtime, T and P temperature and pressure, in the system units of Kelvin and bar, set to numeric() (length=0) if either one is a variable, vars the names of the variables, vals the values of the variables (a list, one element for each variable), values the result of the calculation (a list, one element for each species, with names taken from the species index in thermo$obigt). The elements of the lists in vals and values are arrays of n dimensions, where n is the number of variables. The values of chemical affinity of formation reactions of the species are returned in dimensionless units (for use with decimal logarithms, i.e., A/2.303RT).

Names other than T or P in vars generally refer to basis species, and the corresponding vals are the logarithms of activity or fugacity. However, if one or more of pe, Eh or pH is among the variables of interest, vals holds the values of the those variables as indicated.

References

Helgeson, H. C., Richard, L, McKenzie, W. F., Norton, D. L. and Schmitt, A. (2009) A chemical and thermodynamic model of oil generation in hydrocarbon source rocks. Geochim. Cosmochim. Acta 73, 594–695. https://doi.org/10.1016/j.gca.2008.03.004

See Also

ionize.aa, activated if proteins are among the species of interest, H+ is in the basis, and thermo$opt$ionize is TRUE. equilibrate for using the results of affinity to calculate equilibrium activities of species, and diagram to plot the results.

Examples

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## set up a system and calculate
## chemical affinities of formation reactions
basis(c("SiO2", "MgO", "H2O", "O2"), c(-5, -5, 0, 999))
species(c("quartz","enstatite","forsterite"))
# chemical affinities (A/2.303RT) at 25 deg C and 1 bar
affinity()
# at higher temperature and pressure
affinity(T=500, P=2000)
# at 25 temperatures and pressures
affinity(T=c(500, 1000, 5), P=c(1000, 5000, 5))
# equilibrium constants of formation reactions
affinity(property="logK")
# standard molal Gibbs energies of species,
# user units (default: cal/mol)
affinity(property="G.species")
# standard molal Gibbs energies of reactions
affinity(property="G")
# a T,P-transect
# (fluid pressure from Helgeson et al., 2009 Fig. 7)
affinity(T=c(25, 110, 115, 215), P=c(11, 335, 500, 1450))

CHNOSZ documentation built on July 27, 2017, 3:01 a.m.