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MULTICOMPONENT GEOCHEMICAL TRANSPORT MODELING USING HYDRUS‐1D AND HP1 1
Author(s) -
Š;imůnek Jirka,
Jacques Diederik,
Genuchten Martinus Th.,
Mallants Dirk
Publication year - 2006
Publication title -
jawra journal of the american water resources association
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.957
H-Index - 105
eISSN - 1752-1688
pISSN - 1093-474X
DOI - 10.1111/j.1752-1688.2006.tb06019.x
Subject(s) - biogeochemical cycle , leaching (pedology) , dissolution , environmental science , environmental chemistry , advection , soil water , chemistry , soil science , thermodynamics , physics
The transport of reactive contaminants in the subsurface is generally affected by a large number of nonlinear and often interactive physical, chemical, and biological processes. Simulating these processes requires a comprehensive reactive transport code that couples the physical processes of water flow and advective‐dispersive transport with a range of biogeochemical processes. Two recently developed coupled geochemical models that are both based on the HYDRUS‐1D software package for variably saturated flow and transport are summarized in this paper. One model resulted from coupling HYDRUS‐1D with the UNSATCHEM module. While restricted to major ion chemistry, this program enables quantitative predictions of such problems as analyzing the effects of salinity on plant growth and the amount of water and amendments required to reclaim salt‐affected soil profiles. The second model, HPI, resulted from coupling HYDRUS‐1D with the PHREEQC biogeochemical code. The latter program accounts for a wide range of instantaneous or kinetic chemical and biological reactions, including complexation, cation exchange, surface complexation, precipitation dissolution and/or redox reactions. The versatility of HP1 is illustrated in this paper by means of two examples: the leaching of toxic trace elements and the transport of the explosive TNT and its degradation products.