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Geosphere; June 2006; v. 2; no. 4; p. 210-219; DOI: 10.1130/GES00021.1
© 2006 Geological Society of America
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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


Figure 01
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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).

 

Figure 02
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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).

 

Figure 03
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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.

 

Figure 04
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Figure 4. Measured concentrations (symbols) of exchanged Na reported and computed results (lines) for the Aquia aquifer.

 

Figure 05
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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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