Open AccessModeling Coupled Hydrologic and Chemical Processes: Long‐Term Uranium Transport following Phosphorus Fertilization
Author(s) -
Jacques D.,
Šimůnek J.,
Mallants D.,
Genuchten M.Th.
Publication year - 2008
Publication title -
vadose zone journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.036
H-Index - 81
ISSN - 1539-1663
DOI - 10.2136/vzj2007.0084
Subject(s) - biogeochemical cycle , vadose zone , fertilizer , chemistry , sorption , phosphorus , partition coefficient , soil water , adsorption , environmental chemistry , soil science , hydrology (agriculture) , environmental science , geology , geotechnical engineering , organic chemistry , chromatography
Coupling physical and geochemical processes within one integrated numerical simulator provides a process‐based tool for investigating the mobility of contaminants as affected by changing hydrologic regimes and geochemical conditions. We review interactions between physical and biogeochemical processes in the vadose zone, and then present a case study demonstrating these complex interactions. A hypothetical application is presented of the HP1 multicomponent transport simulator to predict the transport of two major elements (Ca and P) and one trace element (U) applied annually for 200 yr to a field soil in the form of an inorganic P fertilizer. Interactions of Ca, P, and U with the solid phase are described using cation exchange and surface complexation reactions. Simulations assuming steady‐state or transient flow conditions were analyzed in terms of temporal variations of the linear distribution coefficient, K d , which depends strongly on pH and the composition of the aqueous phase. If the composition of the aqueous phase is constant, adsorption of Ca and U increases with increasing pH. Due to the annual addition of Ca, P, and U, and competition between P and U for sorption sites, the K d of these elements decreased with time near the soil surface. Deeper in the soil, the K d of U followed the pH increase because of a lack of competition from P. Because of the combined effects of changing hydrologic and geochemical conditions, the Ca and U distribution coefficients and solute fluxes during the transient simulation exhibited large short‐time variations of up to three orders of magnitude.