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Published in Vadose Zone Journal 3:775-785 (2004)
© 2004 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA

SPECIAL SECTION: RESEARCH ADVANCES IN VADOSE ZONE HYDROLOGY THROUGH SIMULATIONS WITH THE TOUGH CODES

Multiphase Reactive Transport Modeling of Seasonal Infiltration Events and Stable Isotope Fractionation in Unsaturated Zone Pore Water and Vapor at the Hanford Site

Michael J. Singletona,*, Eric L. Sonnenthala, Mark E. Conrada, Donald J. DePaoloa and Glendon W. Geeb

a Earth Sciences Division, Lawrence Berkeley National Laboratory, Berkeley, CA 94720
b Hydrology Group, Environmental Technology Division, Pacific Northwest National Laboratory, Richland, WA

* Corresponding author (MJSingleton{at}lbl.gov)

Received 30 August 2003.

Numerical simulations of transport and isotope fractionation provide a method to quantitatively interpret vadose zone pore water stable isotope depth profiles based on soil properties, climatic conditions, and infiltration. We incorporate the temperature-dependent equilibration of stable isotopic species between water and water vapor, and their differing diffusive transport properties into the thermodynamic database of the reactive transport code TOUGHREACT. These simulations are used to illustrate the evolution of stable isotope profiles in semiarid regions where recharge during wet seasons disturbs the drying profile traditionally associated with vadose zone pore waters. Alternating wet and dry seasons lead to annual fluctuations in moisture content, capillary pressure, and stable isotope compositions in the vadose zone. Periodic infiltration models capture the effects of seasonal increases in precipitation and predict stable isotope profiles that are distinct from those observed under drying (zero infiltration) conditions. After infiltration, evaporation causes a shift to higher {delta}18O and {delta}D values, which are preserved in the deeper pore waters. The magnitude of the isotopic composition shift preserved in deep vadose zone pore waters varies inversely with the rate of infiltration.

Abbreviations: GMWL, global meteoric water line • LBNL, Lawrence Berkeley National Laboratory • LMWL, local meteoric water line • PNNL, Pacific Northwest National Laboratory • SMOW, standard mean ocean water




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J. N. Christensen, M. E. Conrad, D. J. DePaolo, and P. E. Dresel
Isotopic Studies of Contaminant Transport at the Hanford Site, Washington
Vadose Zone J., November 20, 2007; 6(4): 1018 - 1030.
[Abstract] [Full Text] [PDF]




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