2018
DOI: 10.17159/2411-9717/2018/v118n7a2
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First-order exchange and spherical diffusion models of heap leaching in PhreeqC

Abstract: PhreeqC is an open-source software designed to perform geochemical calculations. It offers a feature for modelling heap leaching according to the most modern 'dual-porosity' visualization, as well as an extensive database of reactions and equilibria. It should represent an attractive option for modelling the chemical heap leaching of oxidized ores since it requires only the entering of the system characteristics and a minimal amount of coding to formulate kinetic expressions and output parameters.Both first-or… Show more

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Cited by 3 publications
(2 citation statements)
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“…In Van Staten and Petersen [ 117 ], a first-order exchange model (see Equation (29)) and spherical diffusion (see Equation (30)) [ 60 ] are compared with published short-term pulse test data, concluding that the former is simpler and more convenient to use, but the latter produced more realistic results over longer leaching periods. While in Hashemzadeh et al [ 118 , 119 ], chalcocite leaching kinetics using a variable order kinetic model are modeled, which were already successfully applied in the literature [ 56 , 120 ], and whose formulation are provided in Equation (79).…”
Section: Mineral Leaching Modelingmentioning
confidence: 99%
“…In Van Staten and Petersen [ 117 ], a first-order exchange model (see Equation (29)) and spherical diffusion (see Equation (30)) [ 60 ] are compared with published short-term pulse test data, concluding that the former is simpler and more convenient to use, but the latter produced more realistic results over longer leaching periods. While in Hashemzadeh et al [ 118 , 119 ], chalcocite leaching kinetics using a variable order kinetic model are modeled, which were already successfully applied in the literature [ 56 , 120 ], and whose formulation are provided in Equation (79).…”
Section: Mineral Leaching Modelingmentioning
confidence: 99%
“…It is to be considered as an artefact of discretisation, because the continuous exchange between the outer rim and the core of the grains is approximated by only two zones mixed with a first order exchange coefficient. An improved description of mass transfer kinetics, for example through a finite difference diffusional model [Parkhurst and Appelo, 1999;Van Staden and Petersen, 2018] or a multi-rate model that considers a higher number of exchanging zones [Haggerty and Gorelick, 1995], should improve these results.…”
Section: Mineral Reaction Log10(k)mentioning
confidence: 99%