Geosphere; June 2006; v. 2; no. 4;
p. 210-219; DOI: 10.1130/GES00021.1
© 2006 Geological Society of America
Identifying geochemical processes by inverse modeling of multicomponent reactive transport in the Aquia aquifer
Zhenxue Dai*1,
Javier Samper*2 and
Robert Ritzi, Jr*3
1 Earth and Environmental Sciences Division, Los Alamos National Laboratory, Los Alamos, New Mexico 87545, USA
2 Escuela Técnica Superior de Ingenieros de Caminos, Canales y Puertos, Universidad de La Coruña, La Coruña 15192, Spain
3 Department of Geological Sciences, Wright State University, Dayton, Ohio 45435, USA

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Figure 1. Outline of the Aquia aquifer in Maryland showing the estimated prepumping head distribution and flow path (adapted from Chapelle and Knobel, 1983; Appelo, 1994).
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Figure 2. Schematic cross section of the Aquia aquifer. Recharge occurs at the outcrop, while discharge takes place evenly in the downstream part of the aquifer (adapted from Appelo, 1994).
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Figure 3. Measured (symbols) and computed concentrations (lines) of Na+, K+, Ca2+, Mg2+, HCO3–, and pH of the Aquia aquifer obtained in step 7 of the inverse problem of Aquia.
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Figure 4. Measured concentrations (symbols) of exchanged Na reported and computed results (lines) for the Aquia aquifer.
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Figure 5. Cumulative calcite dissolution (negative values) or precipitation (positive values) in the Aquia aquifer at different times.
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Copyright © 2009 by Geological Society of America