The value of Z depends on the chemical and can be calculated using the equilibrium partitioning
coefficients of the chemicals, Henry’s law constant and other related physical-chemical properties.
The value of f is same for a system that is at equilibrium for each media. Fugacity capacity depends
upon the nature of chemical, nature of media, and temperature
c. Modelling applications
The model can help in identification of the relative importance of chemical specific
partitioning and transformation.
It can help in determination of bioaccumulation in organisms in different trophic levels of
the food web and in checking the consistency of monitoring data
It can be used for the prediction of chemical distribution, the result of which can be useful
in understanding the fate and transport of the chemical in a multimedia environment.
It can act as a decision supporting tool documenting the sources and nature of contamination
and feasible remedial strategies.
It can be used to understand a chemical’s behavior in the natural environment, which can
then be put to use in designing a chemical with desired environmental characteristics,
managing environmental emissions of said chemical, ranking chemicals, and environmental
policy making.
Modelling methods
For building the model, the initial step is to set up a mass balance equation for each phase in
question that includes fugacities, concentrations, fluxes and amounts. The values for different
characteristics of the media like it’s volumes (Vi), fugacity capacities (Zi), advective flows through
compartments (Gi), inflow concentrations (CB,i), and the first order reaction rates (ki) are also
required. The Z values for air (1), water (2), soil (3), and sediment (4) compartments can be
calculated from the physical-chemical properties of the chemical as follows:
𝑍1= 1
𝑅𝑇 𝑍2= 1
𝐻
𝑍3= 𝐾𝑠−𝑤𝑍2= 0.41𝑌
𝑠𝑜𝑖𝑙𝐾𝑂−𝑊𝜌𝑠𝑜𝑖𝑙
𝑍4= 𝐾𝑠−𝑤𝑍2= 0.41𝑌
𝑠𝑒𝑑𝐾𝑂−𝑊𝜌𝑠𝑒𝑑