All other parameters needed for the fugacity model (octanolwater partition coefficient, soil sorption coefficient, bioconcentration factors, etc.) could be obtained, in theory, by means of property-to-property equations (e.g., from solubility). Nevertheless, the applicability of property-to-property equations has been shown to be relatively limited and to have great potential for error, particularly in the calculation of Kow, a key property in each type of evaluative model.
All other parameters needed for the fugacity model (octanolwater partition coefficient, soil sorption coefficient, bioconcentration factors, etc.) could be obtained, in theory, by means of property-to-property equations (e.g., from solubility). Nevertheless, the applicability of property-to-property equations has been shown to be relatively limited and to have great potential for error, particularly in the calculation of Kow, a key property in each type of evaluative model.
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